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World Weather Extremes - MAY 2012

#1 User is online   Ian Williams 

  • Group: Warnings Team
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Posted 04 May 2012 - 19:10

Instead of doing this has a daily post i am going to copy Morganes Extremes in France thread and post each day in here, I will always be a day or so behind because the rainfall and minimum temperature for the previous day on the Australian Beaureau of Metoerology gives its figures for the day before, i.e for the 1st May it gives the figures for the 30th April. Only the maximums are correct for the day in question.

http://www.bom.gov.a...012&mon=5&day=2

1st May 2012

Owase in Japan



Climate
Owase has a humid subtropical climate, with comfortable spring and autumn seasons, and warm winters with practically no snow. The warm Kuroshio Current makes its closest contact with the Japanese coast at Owase, and combined with the high mountains falling almost to the sea, this gives Owase an extremely heavy annual rainfall of 3,850 millimetres (150 in), which is the highest in the world in subtropical and warm temperate latitudes.[1] Only certain parts of southern Chile, coastal British Columbia and the Adriatic Sea coast have as much rain at low elevations outside the tropics.

Despite the excessive wetness of the climate, summers are no more uncomfortable or humid than in the rest of southern Japan: indeed humidity is marginally lower than on cities close to the Seto Inland Sea or on the southern Sea of Japan.

[hide]Climate data for Owase, Japan (1981~2010)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 21.2
(70.2)
27.1
(80.8)
26.1
(79.0)
30.3
(86.5)
32.6
(90.7)
37.3
(99.1)
38.0
(100.4)
38.4
(101.1)
36.6
(97.9)
31.2
(88.2)
29.8
(85.6)
24.3
(75.7)
38.4
(101.1)
Average high °C (°F) 11.3
(52.3)
12.0
(53.6)
14.9
(58.8)
19.4
(66.9)
22.8
(73.0)
25.5
(77.9)
29.2
(84.6)
30.4
(86.7)
27.7
(81.9)
23.0
(73.4)
18.5
(65.3)
13.9
(57.0)
20.72
(69.29)
Average low °C (°F) 1.6
(34.9)
2.1
(35.8)
4.9
(40.8)
9.8
(49.6)
14.1
(57.4)
18.4
(65.1)
22.4
(72.3)
23.1
(73.6)
20.3
(68.5)
14.3
(57.7)
8.8
(47.8)
3.8
(38.8)
11.97
(53.54)
Record low °C (°F) −6.9
(19.6)
−6.2
(20.8)
−5
(23)
−1.9
(28.6)
2.8
(37.0)
8.6
(47.5)
13.8
(56.8)
12.6
(54.7)
9.4
(48.9)
3.7
(38.7)
−1.3
(29.7)
−4.6
(23.7)
−6.9
(19.6)
Rainfall mm (inches) 100.7
(3.965)
118.8
(4.677)
253.1
(9.965)
289.4
(11.394)
371.8
(14.638)
405.7
(15.972)
397.2
(15.638)
468.2
(18.433)
691.9
(27.24)
395.7
(15.579)
249.8
(9.835)
106.5
(4.193)
3,848.8
(151.528)
% humidity 60 60 64 68 74 81 82 80 79 75 70 64 71.4
Avg. rainy days (≥ 0.5 mm) 6.7 7.3 11.8 10.9 12.8 15.1 14.5 13.3 14.9 12.1 8.4 5.8 133.6
Mean monthly sunshine hours 179.4 168.3 184.0 183.9 173.7 129.5 155.7 175.3 130.5 142.4 151.9 177.9 1,952.5
Source no. 1: Japan Meteorological Agency[2]
Source no. 2: Japan Meteorological Agency (records)[3]

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#2 User is online   Ian Williams 

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Posted 04 May 2012 - 20:17

2nd May 2012



Geography
Posted Image Posted Image Grand mosque N'djamena Posted Image Posted Image Astronaut View of NDjamena Posted Image Posted Image The cathedral in N'Djamena, Chad, as it was before it was severely damaged during the civil war. N'Djamena is located at 12°6'47" N, 15°2'57" E, on the confluence of the Chari and Logone rivers.[1]

While primarily an administrative center, the city includes the Nassara Strip commercial centre and residential areas such as Mbololo, Chagoua, Paris Congo and Moursal. The main commercial avenue of the city is the Avenue Charles de Gaulle.


Climate
N'Djamena features a semi-arid climate with a short wet season and a lengthy dry season. Despite the fact that the city receives on average approximately 750 mm of rain annually, due to the area’s very high evapotranspiration, N'Djamena still falls under the semi-arid climate category. The wet season covers from June to September, with the heaviest precipitation occurring in August. The dry season essentially covers the remaining eight months. Based on annual temperatures, N'Djamena is one of the hottest major cities on the planet. Only one month of the year (August) do average monthly high temperatures fail to cross the 32°C (90°F) mark. The city's highest temperatures are usually seen between March and June, just before the onset of the heavier rains. However outside of the warmest months of the year, nights in N'Djamena are generally tolerable.

[hide]Climate data for N'Djamena (1961-1990)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) 32.4
(90.3)
35.2
(95.4)
38.7
(101.7)
41.0
(105.8)
39.9
(103.8)
37.2
(99.0)
33.5
(92.3)
31.6
(88.9)
33.7
(92.7)
36.9
(98.4)
35.8
(96.4)
33.5
(92.3)
35.78
(96.41)
Average low °C (°F) 14.3
(57.7)
16.6
(61.9)
21.0
(69.8)
24.8
(76.6)
25.8
(78.4)
24.7
(76.5)
23.1
(73.6)
22.4
(72.3)
22.7
(72.9)
21.8
(71.2)
17.8
(64.0)
14.8
(58.6)
20.82
(69.47)
Precipitation mm (inches) 0.0
(0)
0.0
(0)
0.3
(0.012)
10.3
(0.406)
25.8
(1.016)
51.0
(2.008)
143.8
(5.661)
174.4
(6.866)
84.3
(3.319)
20.3
(0.799)
0.1
(0.004)
0.0
(0)
510.3
(20.091)
% humidity 29 23 21 28 39 52 68 76 72 49 33 31 43.4
Avg. precipitation days (≥ 0.1 mm) 0 0 1 3 6 9 13 15 9 3 1 0 60
Mean monthly sunshine hours 297.6 277.2 282.1 273.0 285.2 258.0 213.9 201.5 228.0 285.2 300.0 303.8 3,205.5
Source no. 1: WMO
Source no. 2: CMA

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This post has been edited by Ian Williams: 04 May 2012 - 20:19

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#3 User is offline   Chris Alder 

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Posted 04 May 2012 - 22:28

Nice, average annual max temp of 97f :)
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#4 User is online   Ian Williams 

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Posted 05 May 2012 - 18:38

3rd May 2012


Utsunomiya, Tochigi

Utsunomiya (宇都宮市 Utsunomiya-shi?) is the capital and most populous city of Tochigi Prefecture, Japan. In October 2010 the city had an estimated population of 510,416 and a population density of 1,224.49 people per square kilometer. The total area is 416.84 km². Greater Utsunomiya (宇都宮都市圏 Utsunomiya Toshi-ken?) had a population of 888,005 in the 2000 Census. The nearby city of Oyama, Tochigi is included in Greater Tokyo, but Greater Utsunomiya is not, despite the two areas amalgamating somewhat.

Utsunomiya is approximately 100 km north of Tokyo. It is accessible by car via the Tohoku Expressway and by train via Utsunomiya Station on the Tohoku Shinkansen line. Narita International Airport is about three hours away by car or bus. The historic town of Nikkō is approximately 25 km northwest of Utsunomiya.


History
The Battle of Utsunomiya Castle took place between May 10–14, 1868, during the Boshin War (a park now exists on the castle grounds). The city itself was founded on April 1, 1896. In 1954–55, Utsunomiya city incorporated with Suzumenomiya town and Hiraishi, Yokokawa, Mizuhono, Kunimoto, Shiroyama, Tomiya, Toyosato, and Sugatagawa villages and the part of Shinoi village from Kawachi District and Kiyohara village from Haga District. The city added the towns of Kamikawachi and Kawachi, both from Kawachi District, on March 31, 2007, pushing the population of Utsunomiya city over 500,000.


Climate
[hide]Climate data for Utsunomiya (1981~2010)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 21.0
(69.8)
24.6
(76.3)
25.9
(78.6)
30.4
(86.7)
33.2
(91.8)
37.5
(99.5)
38.7
(101.7)
37.5
(99.5)
36.5
(97.7)
32.5
(90.5)
25.1
(77.2)
24.7
(76.5)
38.7
(101.7)
Average high °C (°F) 8.3
(46.9)
9.1
(48.4)
12.6
(54.7)
18.5
(65.3)
22.5
(72.5)
25.2
(77.4)
28.7
(83.7)
30.5
(86.9)
26.4
(79.5)
20.9
(69.6)
15.5
(59.9)
10.7
(51.3)
19.1
(66.4)
Average low °C (°F) −2.7
(27.1)
−1.9
(28.6)
1.5
(34.7)
7.0
(44.6)
12.5
(54.5)
16.9
(62.4)
20.8
(69.4)
22.2
(72.0)
18.4
(65.1)
11.8
(53.2)
5.0
(41.0)
−0.7
(30.7)
9.3
(48.7)
Record low °C (°F) −14.8
(5.4)
−13.3
(8.1)
−12.4
(9.7)
−6.4
(20.5)
−0.8
(30.6)
4.7
(40.5)
10.3
(50.5)
11.4
(52.5)
5.5
(41.9)
−2.7
(27.1)
−6.7
(19.9)
−10.9
(12.4)
−14.8
(5.4)
Precipitation mm (inches) 33.9
(1.335)
42.9
(1.689)
88.4
(3.48)
120.5
(4.744)
146.6
(5.772)
174.7
(6.878)
205.8
(8.102)
209.8
(8.26)
220.4
(8.677)
146.5
(5.768)
68.1
(2.681)
35.5
(1.398)
1,493.1
(58.783)
Snowfall cm (inches) 10
(3.9)
10
(3.9)
5
(2)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
3
(1.2)
28
(11)
% humidity 62 60 61 64 70 77 80 78 79 74 71 66 70.2
Avg. precipitation days (≥ 0.5 mm) 4.4 5.9 9.9 11.1 12.5 14.8 16.2 12.7 14.2 11.1 7.1 4.0 123.9
Avg. snowy days 3.6 3.8 1.9 0.2 0.0 0.0 0.0 0.0 0.0 0.0 0.0 1.1 10.6
Mean monthly sunshine hours 204.8 186.2 187.9 179.5 166.9 112.1 114.1 138.9 112.2 145.0 164.5 199.1 1,911.2
Source no. 1: Japan Meteorological Agency[1]


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uploads/monthly_05_2012/post-30656-0-70185700-1336243095_thumb.gifSource no. 2: Japan Meteorological Agency (records)[2]

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This post has been edited by Ian Williams: 05 May 2012 - 18:39

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#5 User is online   Ian Williams 

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Posted 06 May 2012 - 20:24

4th May 2012

Young - New South Wales Australia


Young is a town in the South West Slopes region of New South Wales, Australia and is the centre of Young Shire. At the 2006 census, Young had a population of 7,141.[1]

Young is marketed as the Cherry Capital Of Australia and every year hosts the National Cherry Festival. Young is situated on the Olympic Highway and is approximately 2 hours drive from the Canberra area. Young is situated in a valley, with surrounding hills. The town is named after Sir John Young, the Governor of NSW during 1861-7.[2]





History
Posted Image Posted Image Brass breast plate presented to the Aboriginal leader Coborn Jackey of the Burrowmunditory tribe by the squatter James White. The artifact is held in the museum at Young. The indigenous people of the district were members of the Burrowmunditory tribe, part of the Wiradjuri people.[3]

James White was the first European settler in the district and established Burrangong Station in 1826 with a squatting claim of 100 square miles (260 km2).[3] Gold was found in the district in 1860. Until that time the area was called Lambing Flat, a reference to the grazing of sheep that was the main industry until mining. The town was gazetted in 1861. The goldfields produced 470,000 ounces of gold sent by escort from the fields. Up to 20,000 miners worked the fields including about 2,000 Chinese miners.[3]

Lambing Flat Post Office opened on 1 March 1861 and was renamed Young in 1863.[4]

From November 1860 through to June 1861 anti-Chinese miners attacked Chinese gold miners in the area, now known as the infamous Lambing Flat riots. As gold became scarce, European miners began to resent what they saw as the greater success of the more industrious Chinese, and hence many Chinese miners were attacked, robbed and killed. The anti-Chinese rebels rallied in numbers of up to 3,000. Eventually the rioters were controlled, Chinese miners had their claims restored to them, but the New South Wales Parliament passed the Chinese Immigration Bill which restricted the number of Chinese that could be brought in to New South Wales on any ship and imposed a tax per head on entry.

In 1889 Young was one of the first towns in Australia other than the capital cities to install electricity into the streets and homes of the township. Young is acknowledged as the first Local Government Area to institute a rural school bus system in New South Wales[3]

In 1928, Young's rugby league club's Jack Kingston was selected to play for the Australian national team.


Climate
[hide]Climate data for Young Airport
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 42.5
(108.5)
42.0
(107.6)
38.6
(101.5)
32.1
(89.8)
25.4
(77.7)
21.9
(71.4)
19.9
(67.8)
23.6
(74.5)
26.9
(80.4)
34.2
(93.6)
41.1
(106.0)
41.1
(106.0)
42.5
(108.5)
Average high °C (°F) 31.6
(88.9)
30.3
(86.5)
27.2
(81.0)
22.7
(72.9)
17.9
(64.2)
13.9
(57.0)
12.9
(55.2)
14.5
(58.1)
17.7
(63.9)
21.5
(70.7)
25.7
(78.3)
29.0
(84.2)
22.1
(71.8)
Average low °C (°F) 14.6
(58.3)
14.7
(58.5)
11.0
(51.8)
6.4
(43.5)
3.5
(38.3)
2.3
(36.1)
1.1
(34.0)
1.4
(34.5)
3.3
(37.9)
5.5
(41.9)
9.4
(48.9)
11.8
(53.2)
7.1
(44.8)
Record low °C (°F) 1.4
(34.5)
2.3
(36.1)
0.8
(33.4)
−4.1
(24.6)
−5.8
(21.6)
−6.1
(21.0)
−6.4
(20.5)
−6.5
(20.3)
−4.7
(23.5)
−3.8
(25.2)
−1.9
(28.6)
−0.2
(31.6)
−6.5
(20.3)
Precipitation mm (inches) 41.3
(1.626)
48.9
(1.925)
36.3
(1.429)
30.1
(1.185)
36.8
(1.449)
61.2
(2.409)
59.4
(2.339)
51.2
(2.016)
53.0
(2.087)
50.7
(1.996)
65.2
(2.567)
61.9
(2.437)
596.8
(23.496)
Avg. precipitation days 6.6 7.0 6.4 5.5 9.4 14.1 17.6 15.1 11.7 9.4 9.0 7.1 118.9
Source: [5]
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#6 User is online   Ian Williams 

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Posted 07 May 2012 - 20:54

5th May 2012















Port Blair (Hindi: पोर्ट ब्लेयर Posted Image pronunciation , Tamil: போர்ட் ப்ளேர், Bengali: পোর্ট ব্লেয়ার, ) is the largest town and a municipal council in Andaman district in the Andaman Islands and the capital of the Andaman and Nicobar Islands, a union territory of India. It lies on the east coast of South Andaman Island and is the main entry point to the islands.

Port Blair is the headquarters for the Indian district of South Andaman, and the local administrative sub-division (tehsil), which is also called Port Blair. It is home to several museums and a major base for the Indian Navy and the Indian Coast Guard. It is also the headquarters of the Tri Services Command.



History
Posted Image Posted Image The Ross Island Prison Headquarters, 1872 In 1789 the government of Bengal established a penal colony on Chatham Island in the southeast bay of Great Andaman, named Port Blair to honor Lieutenant Archibald Blair of the British East India Company. After two years, the colony moved to the northeast part of Great Andaman and was named Port Cornwallis after Admiral William Cornwallis. However, there was much disease and death in the penal colony, and the government ceased operating it in May 1796.

In 1824 Port Cornwallis was the rendezvous of the fleet carrying the army to the First Anglo-Burmese War. In the 1830s and 1840s, shipwrecked crews who landed on the Andamans were often attacked and killed by the natives, alarming the British government. In 1855, the government proposed another settlement on the islands, including a convict establishment, but the Indian Rebellion of 1857 forced a delay in its construction.

However, since the rebellion provided the British with a lot of new prisoners, it made the new Andaman settlement and prison an urgent necessity. Construction began in November 1857 at the renovated Port Blair, avoiding the vicinity of a salt swamp which seemed to have been the source of many of the old colony's problems. The penal colony was originally on Viper Island, named after Lieutenant Blair's vessel, The Viper. The convicts, mostly political prisoners, suffered life imprisonment at hard labor under cruel and degrading conditions. Many were hanged, while others died of disease and starvation. Between 1864 and 1867 a penal establishment was also built with convict labor on the northern side of Ross Island.[1] These structures are now in ruins.[2]

As the Indian freedom movement continued to grow in the late 19th Century, an enormous Cellular Jail was constructed between 1896 and 1906 to house Indian convicts, mostly political prisoners, in solitary confinement. The Cellular Jail is also known as Kala Pani (translated as "Black Waters"), a name given to it due to the torture and general ill-treatment towards its Indian convicts.

From 1943-1944 during World War II, Port Blair was the headquarters of the Azad Hind government under Subhash Chandra Bose.

Although affected by the Tsunami and 2004 Indian Ocean earthquake, Port Blair survived sufficiently to act as a base for relief efforts in the islands.


Geography and climate
Port Blair has a tropical monsoon climate, with little variation in average temperature and large amounts of precipitation throughout the year. All months except January, February and March receive substantial rainfall.

[hide]Climate data for Port Blair
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) 29.4
(84.9)
30.2
(86.4)
31.5
(88.7)
32.5
(90.5)
31.1
(88.0)
29.6
(85.3)
29.2
(84.6)
29.1
(84.4)
29.1
(84.4)
29.6
(85.3)
29.7
(85.5)
29.4
(84.9)
30.03
(86.06)
Average low °C (°F) 23.1
(73.6)
22.5
(72.5)
23.2
(73.8)
24.7
(76.5)
24.7
(76.5)
24.4
(75.9)
24.3
(75.7)
24.2
(75.6)
23.7
(74.7)
23.7
(74.7)
23.9
(75.0)
23.6
(74.5)
23.83
(74.90)
Precipitation mm (inches) 46.4
(1.827)
26.5
(1.043)
29.3
(1.154)
69.0
(2.717)
360.4
(14.189)
501.1
(19.728)
423.7
(16.681)
425.1
(16.736)
463.0
(18.228)
300.7
(11.839)
235.0
(9.252)
154.6
(6.087)
3,034.8
(119.48)
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#7 User is online   Ian Williams 

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Posted 08 May 2012 - 19:39

6th May 2012

Heyuan, China 122.0 mm



Heyuan
From Wikipedia, the free encyclopedia Jump to: navigation, search
Heyuan
河源
Prefecture-level city
河源市
Posted Image
Posted Image Location of Heyuan City within Guangdong
Posted Image Posted Image Heyuan Location in China
Coordinates: Posted Image23°45′N 114°42′ECoordinates: Posted Image23°45′N 114°42′E
Country People's Republic of China
Province Guangdong
City seat Yuancheng District
Area
• Total 15,478 km2 (5,976 sq mi)
Population
• Total 3,320,000
• Density 210/km2 (560/sq mi)
Time zone China Standard (UTC+8)
Area code(s) 762
License Plate 粤P
Heyuan (Chinese: 河源; Mandarin Pinyin: Héyuán; Jyutping: Ho⁴jyun⁴) , historically known as Hoyün, is a prefecture-level city of Guangdong province in the People's Republic of China. Heyuan has a population of about 207,600. The majority of the people are Hakka. The city includes many rainforests and the largest lake in Guangdong: Xinfengjiang Reservoir. The literal meaning of the city's name is "origin of the river".


Contents

Geography
Heyuan is located in the north-east region of Guangdong, upper reach of Dong River at its confluence with the Xingeng River. It is 114°13'- 115°35' longitude east, and 23°10'-24°50' latitude north. It borders on Huizhou to the south, Ganzhou (Jiangxi province) to the north, Meizhou to the east and Shaoguan to the west. Heyuan is a regional hub that connects the coastal areas of Guangdong and the interior countryside.

Heyuan is rich in natural resources and fertile land. There are 1,000 square kilometres (390 sq mi) of cultivated land, 13,600 square kilometres (5,300 sq mi) of hilly land, and 640 square kilometres (250 sq mi) of water area. Many mineral deposits such as iron ore, tungsten, tin, fluorite are found in Heyuan.


Climate
Heyuan has a monsoon-influenced humid subtropical climate (Köppen Cfa), with short, mild to warm winters, and long, hot, humid summers. Typhoons can strike from August to October, but monthly rainfall usually has already tapered off by then. Monthly daily means range from 12.7 °C (54.9 °F) in January to 28.4 °C (83.1 °F) in July, with an annual mean temperature of 21.5 °C (70.7 °F).

[hide]Climate data for Heyuan (1971-2000)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) 18.1
(64.6)
18.4
(65.1)
21.7
(71.1)
25.8
(78.4)
29.2
(84.6)
31.4
(88.5)
33.2
(91.8)
33.1
(91.6)
31.7
(89.1)
28.9
(84.0)
24.2
(75.6)
20.1
(68.2)
26.3
(79.3)
Average low °C (°F) 9.1
(48.4)
10.7
(51.3)
14.2
(57.6)
18.7
(65.7)
22.1
(71.8)
24.3
(75.7)
25.1
(77.2)
24.9
(76.8)
23.5
(74.3)
20.0
(68.0)
14.9
(58.8)
10.4
(50.7)
18.2
(64.8)
Rainfall mm (inches) 53.4
(2.102)
94.3
(3.713)
153.3
(6.035)
259.5
(10.217)
338.1
(13.311)
345.5
(13.602)
218.2
(8.591)
246.1
(9.689)
157.5
(6.201)
61.0
(2.402)
39.3
(1.547)
39.8
(1.567)
2,006
(78.98)
% humidity 70 75 79 81 82 83 80 81 77 70 66 66 75.8
Avg. rainy days (≥ 0.1 mm) 8.0 12.5 16.4 17.8 20.1 19.5 16.7 17.8 12.6 6.1 5.3 5.8 158.6
Mean monthly sunshine hours 135.8 91.7 85.3 92.8 122.5 155.3 219.0 200.9 189.7 197.1 180.5 172.0 1,842.6
Source: China Meteorological Administration

Language
In the great majority of Heyuan areas, Hakka Chinese is in general use.

In the greater part of areas in the city, Dongyuan County, Lianping County, Heping County, Longchuan County etc., it belongs to the Yuezhong dialect group, while in Zijin County and part of Longchuan County, it belongs to the Yuetai dialect group.

Also, in some areas on the banks of the Dongjiang, Dongjiang Bendihua is in general use. Its classification is disputed between the Yuezhong division of Hakka and the Huihe division of Yue.

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#8 User is online   Ian Williams 

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Posted 09 May 2012 - 18:38

7th May 2012

Jakarta, Indonesia 62.0 mm



Geography and climate

Geography
Jakarta is located on the northwest coast of Java, at the mouth of the Ciliwung River on Jakarta Bay, which is an inlet of the Java Sea. Officially, the area of the Jakarta Special District is 662 km2 of land area and 6,977 km2 of sea area.[39] Jakarta lies in a low, flat basin, averaging 7 metres (23 ft) above sea level;[citation needed] 40% of Jakarta, particularly the northern areas, is below sea level,[40] while the southern parts are comparatively hilly. Rivers flow from the Puncak highlands to the south of the city, across the city northwards towards the Java Sea; the most important[clarification needed] is the Ciliwung River, which divides the city into the western and eastern principalities. Other rivers include the Pesanggrahan, and Sunter.

These rivers, combined with Jakarta's low topography make it prone to flooding from swollen rivers in the wet season and high sea tides. Other contributing factors include clogged sewage pipes and waterways that service an increasing population, in addition to deforestation near rapidly urbanizing Bogor and Depok in Jakarta's hinterland. Furthermore, Jakarta is an urban area with complex socio-economic problems that indirectly contribute to triggering a flood event.[41] Major floods occurred in 1996[42][43] when 5,000 hectares of land were flooded[44] and 2007.[45] Losses from infrastructure damage and state revenue were at least 5.2 trillion rupiah (572 million US dollars) and at least 85 people were killed[46] and about 350,000 people forced from their homes.[47] Approximately 70% of Jakarta's total area was flooded with water up to four meters deep in parts of the city.[48][49]

In May 2011, the Jakarta Environmental Management Agency categorized all rivers in Jakarta as polluted; 71% of them were heavily polluted, 20% were partly polluted and 9% were lightly polluted.[50]

East Flood Canal (BKT) in eastern Jakarta was a national project which began in 2003 and late 2009 reached the Java sea and will be accomplished in 2011. It was 23.5 kilometers length which linking five rivers: Cipinang, Sunter, Buaran, Jati Kramat and Cakung. It will reduce flood and hope as a 2 kilometers rowing sport venue too.[51] To ease from flood, Jakarta Emergency Dredging Innitiave (JEDI) phase-2 will make underground canal (siphon) from Ciliwung river to Cipinang river and then go through to East Flood Canal. It will lowering flood at Cawang, Kampung Melayu, Bukit Duri and Kebun Baru. The length will be one kilometer and will be finished at 2016.[52]

Besides flood from the rivers, Jakarta is also sinking about 5 to 10 centimeters each year and up to 20 centimeters in northern Jakarta mainland. To solve it, the Netherlands will give $4 million for a feasibility study to build a dike on Jakarta Bay. The ring dike will be provided with pumping system and retention area, would regulate and control seawater and use also as additional toll road. The project will be built by 2025.[53]

The Thousand Islands, which are administratively a part of Jakarta, are located in Jakarta Bay north of the city.

Posted Image Posted Image The view of Central Jakarta from the viewing tower at the National Monument
Climate
Jakarta has a hot and humid tropical monsoon climate (Aw) according to the Köppen climate classification system. Despite being located relatively close to the equator, the city has distinct wet and dry seasons. Wet seasons in Jakarta cover the majority of the year, running from November through June. The remaining four months forms the city’s dry season. Located in the western-part of Indonesia, Jakarta's wet season rainfall peak is January with average monthly rainfall of 389 millimetres (15.3 in), and its dry season low point is September with a monthly average of 30 millimetres (1.2 in).

[hide]Climate data for Jakarta
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) 31.5
(88.7)
32.3
(90.1)
32.5
(90.5)
33.5
(92.3)
33.5
(92.3)
34.3
(93.7)
33.3
(91.9)
33.0
(91.4)
32.0
(89.6)
31.7
(89.1)
31.3
(88.3)
32.0
(89.6)
31.8
(89.2)
Average low °C (°F) 24.2
(75.6)
24.3
(75.7)
25.2
(77.4)
25.1
(77.2)
25.4
(77.7)
24.9
(76.8)
25.1
(77.2)
24.9
(76.8)
25.5
(77.9)
25.5
(77.9)
24.9
(76.8)
24.9
(76.8)
24.8
(76.6)
Precipitation mm (inches) 389.7
(15.343)
309.8
(12.197)
100.3
(3.949)
257.8
(10.15)
139.4
(5.488)
83.1
(3.272)
30.8
(1.213)
34.2
(1.346)
30.0
(1.181)
33.1
(1.303)
175.0
(6.89)
123.0
(4.843)
1,706.2
(67.173)
Avg. rainy days 26 20 15 18 13 17 5 5 6 9 22 12 168

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Source: World Meteorological Organisation[54]

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This post has been edited by Ian Williams: 10 May 2012 - 17:51

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#9 User is online   Ian Williams 

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Posted 10 May 2012 - 17:58

Firstly i have had to do a re-issue on the 7th, the table for north and south america had the 8th`s data on it instead of the 7th

The 8th saw the hottest temperature so far this year at Kaolack in Senegal with 47.8C, beating Birdsville in Australia`s 47.5C set in early January.

If anyone has any climate figures for Kaolack please post them, would be much appreciated. :)

Kaolack, Senegal 47.8C


Kaolack (Kawlax in Wolof) is a town of 172,305 people (2002 census) on the north bank of the Saloum River and the N1 road in Senegal. It is the capital of the Kaolack Region, which borders The Gambia to the south. Kaolack is an important regional market town and is Senegal's main peanut trading and processing center. As the center of Ibrahimiyya branch of the Tijaniyyah Sufi order founded by Ibrayima Ñas, it is also a major center of Islamic education. The Medina Baay mosque (right) in Kaolack is one of the largest and best known in Senegal.

Posted Image Posted Image Central Kaolack Kaolack is situated on the Saloum River about 100 kilometers from its mouth. It is the successor city to Kahone, historic capital of the kingdom of Saloum. Kahone, originally a place marked by a sacred tree on the right bank of the Saloum River facing the island of Kouyong, became capital of the mostly Sereer kingdom of Saloum in the early 16th century. In the 17th and 18th centuries it consisted of a number of distinct neighborhoods separated by open fields, each of which was under the jurisdiction of a different dignitary or official. One of these wards, Kaolack (eight km down river), was founded by two Sereer princesses from Baol. Another, Maka Kahone, was inhabited by Muslims and administered by clerics. Otherwise, the population of the town practiced traditional religion and court ceremonies centered on the river bank, Kouyong Island, and various monumental baobab trees.

French interests in the Saloum River increased in the early 19th century as legitimate articles of trade were sought to replace trade in slaves. By mid-century peanut production had been introduced to the kingdom of Saloum and, with the permission of its king, a fortified factory was established by the French on the riverfront at Kaolack.

Posted Image Posted Image Kaolack Market Kaolack was more favorably placed for shipping than Kahone. The French laid out a first grid of lots in 1860, in what would become the city center, or "Escale" neighborhood. The construction of a rail spur from the port to the Dakar-Niger line in 1911 caused the town to boom as a peanut processing and export center. Its population grew rapidly, rising from 5,600 in 1925 to 44,000 in 1934.

It is at this time that Kaolack became an important center for the Tijaniyyah Sufi order, with a first major zâwiyah, or “lodge”, opening in Leona neighborhood in 1910 and a second one opening in Madina Baye in the early 1930s. The Tijaniyyah of Madina Baye is an international institution with disciples in many cities, including Kano, Nigeria, and Chicago, Illinois.

There is a peanut oil processing plant with its own port facilities in the downstream suburb of Lyndiane, while Salt pans across the Saloum river constitute the city’s only other major industrial activity

Among Kaolack's many neighborhoods are:

Posted Image Posted Image Children in 2007 Posted Image Posted Image Road
  • Lewna (Léona in French), which includes much of the city center. It includes Lewna Ñaseen (Léona Niassène in French), the headquarters of the branch of the Tijānī Islamic order founded in 1910 by Allaaji Abdulaay Ñas after his exile in Gambia.
  • Jaleñ (Dialègne in French), between Lewna Ñaseen and Medina Mbàbba.
  • Medina Mbàbba (Médina Mbaba in French), also called "Medina I", named after Baabakar Njaay, nicknamed "Mbàbba Njaay," who was the Serer chief of the village when it was incorporated into Kaolack.
  • Medina Baay (Médina Baye in French), also called "Medina II", on the northeast edge of the city. It is the center of the Ibrāhīmiiya branch of the Tijānī order founded in 1930 by Allaaji Abdulaay Ñas's son, Ibrayima Ñas, known to his followers as "Baay" ("Father" in Wolof). The name in Arabic means "The City of Baay."
  • Saam (Sam in French), west of Medina Baay in the north of Kaolack, also founded by Ibrayima Ñas. Saam was originally designated as the fields and orchards of Ibrayima Ñas's disciples, but since the 1970s the trees have been replaced by houses.
  • Ndoorong (Ndorong in French), west of Saam, founded by Bashiru Mbàkke and his Murid disciples.
  • Coofog (Thiofoke in French), north of Saam, which existed before Kaolack as a Serer village ruled by the Gelwaar dynasty.
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#10 User is online   Ian Williams 

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Posted 11 May 2012 - 11:08

9th May 2012

Abu Dhabi, U.A.E 45.3C


Abu Dhabi (Arabic: أبو ظبي‎ Abu Dhabi, Father of Deer)[3] is the capital and the second largest city of the United Arab Emirates in terms of population and the largest of the seven member emirates of the United Arab Emirates. Abu Dhabi lies on a T-shaped island jutting into the Persian Gulf from the central western coast. The city proper had an estimated population of 896,800 in 2009.[4]

Abu Dhabi houses important offices of the federal government, and is the seat for the United Arab Emirates Government and the home for the Abu Dhabi Emiri Family and the President of the UAE from this family. Abu Dhabi has grown to be a cosmopolitan metropolis. Its rapid development and urbanisation, coupled with the relatively high average income of its population, has transformed Abu Dhabi to a larger and advanced metropolis. Today the city is the country's center of political, industrial activities, and a major cultural, and commercial centre due to its position as the capital. Abu Dhabi alone generated 56.7% of the GDP of the United Arab Emirates in 2008.[5][6]

Abu Dhabi is home to important financial institutions such as the Abu Dhabi Securities Exchange, the Central Bank of the United Arab Emirates and the corporate headquarters of many companies and numerous multinational corporations. One of the world's largest producers of oil, Abu Dhabi has actively attempted to diversify its economy in recent years through investments in financial services and tourism.

Abu Dhabi is the second most expensive city for expatriate employees in the region, and 67th most expensive city in the world.[7] Fortune magazine & CNN stated that Abu Dhabi is the richest city in the world.[8]


Geography and climate
Main article: Geography of the United Arab Emirates Posted Image Posted Image Abu Dhabi seen from SPOT satellite The city of Abu Dhabi is located on the northeastern part of the Persian Gulf in the Arabian Peninsula. It is on an island less than 250 metres from the mainland and is joined to the mainland by the Maqta and Mussafah Bridges. A third, Sheikh Zayed Bridge, designed by Zaha Hadid, opened in late 2010. Abu Dhabi Island is also connected to Saadiyat Island by a five-lane motorway bridge. Al-Mafraq bridge connects the city to Reem Island and was completed in early 2011. This is a multilayer interchange bridge and it has 27 lanes which allow roughly 25,000 automobiles to move per hour. There are three major bridges of the project, the largest has eight lanes, four leaving Abu Dhabi city and four coming in.[14]

Most of Abu Dhabi city is located on the island itself, but it has many suburbs on the mainland, for example: Khalifa City A, B, and C; Al Raha Beach; Al Bahia City A, B, and C; Al Shahama; Al Rahba; Between Two Bridges; Baniyas; and Mussafah Residential.

The Emirate of Abu Dhabi’s land surface measures 67,340 square kilometres, which is equivalent to about 80% of the UAE’s total land area. Only 30% of the emirate is inhabited, with the remaining vast expanses covered mainly by desert and arid land — constituting about 93% of the total land area.

Land cultivation and irrigation for agriculture and forestation over the past decade has increased the size of “green” areas in the emirate to about 5% of the total land area, including parks and roadside plantations. About 1.2% of the total land area is used for agriculture. A small part of the land area is covered by mountains, containing several caves. The coastal area contains pockets of wetland and mangrove colonies. Abu Dhabi also has dozens of islands, mostly small and uninhabited, some of which have been designated as sanctuaries for wildlife.

Abu Dhabi has a hot arid climate. Sunny blue skies can be expected throughout the year. The months of June through September are generally hot and humid with maximum temperatures averaging above 35 °C (95 °F). During this time, sandstorms occur intermittently, in some cases reducing visibility to a few meters.

The weather is cooler from November to March. This period also sees dense fog on some days. The oasis city of Al Ain, about 150 km (93 mi) away, bordering Oman, regularly records the highest summer temperatures in the country; however, the dry desert air and cooler evenings make it a traditional retreat from the intense summer heat and year-round humidity of the capital city.[15]

[hide]Climate data for Abu Dhabi
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 33
(91)
35
(95)
41
(106)
44
(111)
46
(115)
46
(115)
45
(113)
40
(104)
36
(97)
34
(93)
32
(90)
35
(95)
46
(115)
Average high °C (°F) 23
(73)
31
(88)
35
(95)
40
(104)
44
(111)
45
(113)
42
(108)
39
(102)
34
(93)
32
(90)
25
(77)
23
(73)
35
(95)
Average low °C (°F) 12
(54)
14
(57)
26
(79)
30
(86)
30
(86)
30
(86)
28
(82)
23
(73)
20
(68)
17
(63)
15
(59)
14
(57)
20
(68)
Record low °C (°F) 6
(43)
10
(50)
15
(59)
20
(68)
25
(77)
23
(73)
20
(68)
21
(70)
23
(73)
15
(59)
10
(50)
7
(45)
6
(43)
Precipitation mm (inches) 2
(0.08)
6
(0.24)
5
(0.2)
0
(0)
0
(0)
6
(0.24)
16
(0.63)
30
(1.18)
30
(1.18)
10
(0.39)
4
(0.16)
4
(0.16)
109
(4.29)
Mean monthly sunshine hours 244.9 232.4 251.1 282.0 341.0 336.0 313.1 306.9 303.0 303.8 288.0 257.3 3,459.5
Source no. 1: [16]
Source no. 2: Hong Kong Observatory[17]
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#11 User is online   Ian Williams 

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Posted 12 May 2012 - 19:27

10th May 2012

Merida, Mexico 39.3C


Mérida (pronounced: [ˈmeɾiða]) (T'hó' /d̥ʼχøʼ/ or Ichkanzihóo /isʃkan'siχœ/) (the original name in Modern Maya) is the capital and largest city of the Mexican state of Yucatán and the Yucatán Peninsula. It is located in the northwest part of the state, about 35 km (22 mi) from the Gulf of Mexico coast. The city is also the municipal seat of the Municipality of Mérida, which includes the city and the areas around it.

According to the 2010 census, the population of Mérida was 970,377, ranking 12th among the most populous Mexican metropolitan areas. The municipality's area is 858.41 km2 (331.43 sq mi). The metropolitan area includes the municipalities of Mérida, Umán and Kanasín and had a population of 1,035,238 in the same 2010 census. It is the largest of the four cities of the world that share the name Mérida, the other three being in Spain, Venezuela and The Philippines. The city like much of the state has heavy French, British and to a lesser extent Dutch influences. Merida has the highest percentage of indigenous persons of any large city in Mexico.

Mérida is serviced by Manuel Crescencio Rejón International Airport (IATA airport code: MID)





Geography
Posted Image Posted Image The city as seen from the 16th floor of Hyatt Posted Image Posted Image Monument to the Yucatan caste war Mérida is located in the Northwest part of the state of Yucatán, which occupies the northern portion of the Yucatán Peninsula. To the east is the state of Quintana Roo, to the west is the state of Campeche, to the north is the Gulf of Mexico, and far to the south is the state of Chiapas. The city is also located in the Chicxulub Crater. It has a very flat topography and is only 30 feet (9 m) above sea level. The land outside of Mérida is covered with smaller scrub trees and former henequen fields. Almost no surface water exists, but several cenotes (underground springs and rivers) are found across the state. Mérida has a centro historico typical of colonial Spanish cities. The street grid is based on odd-numbered streets running east/west and even-numbered streets running north/south, with Calles 60 and 61 bounding the "Plaza Grande" in the heart of the city. The more affluent neighborhoods are located to the north and the most densely populated areas are to the south. The Centro Historico area is becoming increasingly popular with American and other expats who are rescuing and restoring the classic colonial structures. The Los Angeles Times recently noted this surge of interest in rescuing Mérida's historic downtown.[5]


Weather
Merida features a tropical wet and dry climate.[6] The city lies in the trade wind belt close to the Tropic of Cancer, with the prevailing wind from the east. Mérida's climate is hot and humidity is moderate to high, depending on the time of year. The average annual high temperature is 33 °C (91 °F), ranging from 28 °C (82 °F) in January to 36 °C (97 °F) in May, but temperatures often rise above 38 °C (100 °F) in the afternoon in this time. Low temperatures range between 18 °C (64 °F) in January to 23 °C (73 °F) in May and June. It is most often a few degrees hotter in Mérida than coastal areas due to its inland location and low elevation. The rainy season runs from June through October, associated with the Mexican monsoon which draws warm, moist air landward. Easterly waves and tropical storms also affect the area during this season.

[hide]Climate data for Mérida
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) 31.3
(88.3)
31.8
(89.2)
34.1
(93.4)
35.3
(95.5)
36.1
(97.0)
35.0
(95.0)
34.8
(94.6)
34.7
(94.5)
34.1
(93.4)
32.9
(91.2)
31.9
(89.4)
30.9
(87.6)
33.6
(92.5)
Average low °C (°F) 17.0
(62.6)
17.1
(62.8)
18.2
(64.8)
19.6
(67.3)
21.3
(70.3)
21.0
(69.8)
20.8
(69.4)
20.8
(69.4)
21.1
(70.0)
20.5
(68.9)
19.3
(66.7)
17.3
(63.1)
19.5
(67.1)
Rainfall mm (inches) 38.2
(1.504)
31.8
(1.252)
25.0
(0.984)
25.4
(1)
71.9
(2.831)
143.1
(5.634)
171.1
(6.736)
138.7
(5.461)
173.7
(6.839)
122.8
(4.835)
61.2
(2.409)
47.5
(1.87)
1,050.4
(41.354)
Avg. rainy days (≥ 0.1 mm) 3.8 3.0 2.6 1.7 4.5 10.4 12.9 12.6 13.5 9.7 5.8 4.6 85.1
Mean monthly sunshine hours 207.7 209.1 241.8 255.0 272.8 231.0 244.9 248.0 207.0 217.0 213.0 201.5 2,748.8
Source: Weatherbase [7]

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This post has been edited by Ian Williams: 12 May 2012 - 19:30

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#12 User is online   Ian Williams 

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Posted 13 May 2012 - 19:40

Kochi or Cochin in India 110.0 mm

11th May 2012


Kochi (Malayalam: കൊച്ചി, Kocci ? [koˈtʃːi] (Posted Image listen)), formerly Cochin, is a major port city on the west coast of India by the Arabian Sea. Kochi is part of the district of Ernakulam in the state of Kerala.

Kochi is often called by the name Ernakulam, which refers to the eastern part of the mainland Kochi. The civic body that governs the city is the Corporation of Cochin, which was constituted in the year 1967, and the statutory bodies that oversee its development are the Greater Cochin Development Authority and the Goshree Islands Development Authority.

The city of Kochi (pop. 601,574) is Kerala's second largest city and is part of an extended metropolitan region (pop. 2.1 million), which is the largest urban agglomeration in Kerala. It is the most densely populated city in the state. Kochi city is also a part of Greater Cochin region[5][6] and is classified as a B-1 grade city[7] by the Government of India, making it the highest graded city in the state. Kochi ranks first in the total number of international and domestic tourists in Kerala.[8][9] Kochi has been ranked the sixth best tourist destination in India according to a survey conducted by the Nielsen Company on behalf of the Outlook Traveller magazine.[10]

The city lies about 220 kilometres (137 mi) north of the state capital, Thiruvananthapuram, and about 180 kilometres (112 mi) south of Kozhikode, the third largest city in Kerala. In 1102 AD, Kochi became the seat of the Kingdom of Cochin, which traced its lineage to the Kulasekhara Empire. Heralded as the Queen of Arabian Sea, Kochi was an important spice trading centre on the Arabian Sea coast from the 14th century. Occupied by the Portuguese Empire in 1503, Kochi was the first of the European colonies in India. It remained the main seat of Portuguese India until 1530, when Goa was chosen instead. The city was later occupied by the Dutch and the British, with the Kingdom of Cochin becoming a princely state.

Kochi is home for the Southern Naval Command, of the Indian Navy, state headquarters (DHQ4)[11][12] and Air Squadron 747[13] of the Indian Coast Guard, maritime-related facilities including the Port of Kochi, an International Container Transshipment Terminal, the Cochin Shipyard, offshore SPM of the Kochi Refineries,[14][15] and the Kochi Marina. Kochi is also home for the Cochin Stock Exchange, International Pepper Exchange, major chemical industries like the FACT, TCC, IREL, HOCL[16] and Kochi Refineries, industrial parks like the Cochin Special Economic Zone and Infopark. Kochi is home for the High Court of Kerala & Lakshadweep, and the Cochin University of Science and Technology.





Geography and climate

Geography
Main article: Geography of Kochi Posted Image Posted Image A view of the Kochi harbour mouth from Willingdon Island Kochi is located on the southwest coast of India at 9°58′N 76°13′E, spanning an area of 94.88 square kilometres (36.63 sq mi). The city straddles the backwaters, encompassing the northern end of a peninsula, several islands and a portion of the mainland. To the west lies the Arabian Sea, and to the east is the urbanized region in the rest of the mainland area. Much of Kochi lies at sea level, with a coastline of 48 km.[18]

The current metropolitan limits of Kochi include the mainland Ernakulam, Fort Kochi, the suburbs of Edapally, Kalamassery and Kakkanad to the northeast; Tripunithura to the southeast; and a group of islands closely scattered in the Vembanad Lake. Most of these islands are very small, varying in extent from six square kilometre to less than a square kilometre (1,500 to less than 250 acres).[citation needed]

Soil consists of sediments such as alluvium, teri's, brown sands, etc. Hydromorphic saline soils are also found in the areas surrounding the backwaters.[18]

Predominant rock types found here are Archaean-basic dykes, Charnockites and Gneisses. An ecologically sensitive area, the Mangalavanam Bird Sanctuary is located in the central part of the city. It has a wide range of mangrove species and is nesting ground for a vast variety of migratory birds.


Climate
Under the Köppen climate classification, Kochi features a tropical monsoon climate. Kochi's proximity to the equator along with its coastal location results in little seasonal temperature variation, with moderate to high levels of humidity. Annual temperatures range between 23 and 31 °C (73–88 °F) with the record high being 38 °C (100 °F), and record low 17 °C (63 °F).[31] From June to September, the south-west monsoon brings in heavy rains as Kochi lies on the windward side of the Western Ghats. From October to December, Kochi receives lighter (yet significant) rain from the northeast monsoon, as it lies on the leeward side. Average annual rainfall is 3,228.3 mm (127.10 in),[32] with an annual average of 132 rainy days.

[hide]Climate data for Kochi
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 35
(95)
37
(99)
37
(99)
34
(93)
35
(95)
33
(91)
35
(95)
35
(95)
38
(100)
35
(95)
34
(93)
33
(91)
38
(100)
Average high °C (°F) 30
(86)
31
(88)
31
(88)
31
(88)
31
(88)
28
(82)
28
(82)
28
(82)
28
(82)
29
(84)
30
(86)
30
(86)
30
(86)
Average low °C (°F) 23
(73)
25
(77)
26
(79)
26
(79)
26
(79)
25
(77)
24
(75)
24
(75)
25
(77)
25
(77)
25
(77)
23
(73)
25
(77)
Record low °C (°F) 17
(63)
18
(64)
20
(68)
21
(70)
22
(72)
21
(70)
21
(70)
20
(68)
22
(72)
20
(68)
20
(68)
19
(66)
17
(63)
Precipitation mm (inches) 21.9
(0.862)
22.9
(0.902)
35.3
(1.39)
124.0
(4.882)
395.7
(15.579)
720.7
(28.374)
697.2
(27.449)
367.8
(14.48)
289.4
(11.394)
302.3
(11.902)
175.1
(6.894)
48.3
(1.902)
3,228.3
(127.098)
Source no. 1: [33]
Attached Image: ScreenShot015.gifSource no. 2: [34]

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#13 User is online   Ian Williams 

  • Group: Warnings Team
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Posted 14 May 2012 - 17:06

12th May 2012

Nanchang, China 155.0 mm


Nanchang (Chinese: 南昌; pinyin: Nánchāng) is the capital of Jiangxi Province in southeastern China. It is located in the north-central portion of the province. As it is bounded on the west by the Jiuling Mountains, and on the east by Poyang Lake, it is famous for its scenery, rich history and cultural sites. Owing to its central location relative to the Yangtze and Pearl River Delta regions, it is a major railroad hub in Southern China.


Contents

History
The modern Jiangxi area – including Nanchang – was first incorporated into Chinese territory during the Qin dynasty, when it was conquered from the Baiyue peoples and organized as Jiujiang Commandery (Chinese: 九江郡).[1] In 201 BC, during the Han dynasty, the city was given the Chinese name Nanchang and became the administrative seat of Yuzhang Commandery (Chinese: 豫章郡), and was governed by Guan Ying (Chinese: 灌嬰), one of Emperor Gaozu of Han's generals.[1] The name Nanchang means "southern flourishing", and is from a motto of developing what is now southern China that is traditionally attributed to Emperor Gaozu himself.[1]

In AD 589, during the Sui dynasty, this commandery was changed into a prefecture named Hongzhou (Chinese: 洪州), and after 763 it became the provincial center of Jiangxi, which was then beginning the rapid growth that by the 12th century made it the most populous province in China.

In 653, the Tengwang Pavilion was constructed. In 675, Wang Bo wrote the classic "Tengwang Ge Xu". The building as well as the city became celebrated for Wang's introduction article and the author is known to all Chinese-speaking population by this masterpiece. The Pavilion has been destroyed and rebuilt several times throughout China's history. In its present form, Tengwang Pavilion was reconstructed in the 1980s after being destroyed in 1929 during the Chinese Civil War.

In 959, under the Southern Tang regime, it became Nanchang superior prefecture and also the southern capital. After the conquest by the Song regime in 981 it reverted to the name Hongzhou. In 1164 it was renamed Longxing prefecture, which name it retained until 1368. At the end of the Yuan (Mongol) period (1279–1368), it became a battleground between Zhu Yuanzhang, the founder of the Ming dynasty (1368–1644), and the rival local warlord, Chen Youliang. At the beginning of the 16th century it was the power base from which Zhu Chenhao, the prince of Ning, launched a rebellion against the Ming regime.

During the reign of the Wanli Emperor of the Ming dynasty, it housed relatives of the emperor who had been exiled because they were potential claimants of the imperial throne, members of the imperial family constituting about one quarter of the city's population; as a result of this, Matteo Ricci came here when trying to gain entry to Beijing.[2]

In the 1850s it suffered considerably as a result of the Taiping Rebellion (1850–64), and its importance as a commercial center declined as the overland routes to Canton were replaced by coastal steamship services in the latter half of the 19th century. Nanchang has, however, remained the undisputed regional metropolis of Jiangxi.

On August 1, 1927, Nanchang was the site of one of a series of insurrections organized by the Chinese Communist Party. The Nanchang Uprising, led by pro-communist Kuomintang officers under Russian direction, succeeded in holding the city for only a few days, and provided a core of troops and a method of organization from which the People's Liberation Army (PLA) later developed.

In 1939, the Battle of Nanchang, a ferocious battle between the Chinese National Revolutionary Army and the Japanese Imperial Japanese Army in the Second Sino-Japanese War took place.

In 1949 Nanchang was still essentially an old-style administrative and commercial city, with little industry apart from food processing; it had a population of about 275,000. Nanchang first acquired a rail connection in 1915, when the line to Jiujiang, a port on the Yangtze River, was opened. Several other rail links have since been opened. After World War II a line was completed to Linchuan and Gongqi in the Ru River Valley to the south-southeast.

Since 1949 Nanchang has been extensively industrialized. It is now a large-scale producer of cotton textiles and cotton yarn. Papermaking is also a large industry, as is food processing (especially rice milling). Heavy industry began to be important in the mid-1950s. A large thermal-power plant was installed and uses coal brought by rail from Fengcheng, to the south. A machinery industry also grew up, at first mainly concentrating on the production of agricultural equipment and diesel engines. Nanchang then became a center of the automotive industry, producing trucks and tractors and also such equipment as tires. An iron-smelting plant helping to supply local industry was installed in the later 1950s. There is also a large chemical industry, producing agricultural chemicals and insecticides as well as pharmaceuticals.


Geography and climate
Nanchang is located 130 km south of the Yangtze River and is situated on the right bank of the Gan River just below its confluence with the Jin River[disambiguation needed Posted Image] and some 40 km southwest of its discharge into Poyang Lake.

Nanchang has a monsoon-influenced humid subtropical climate (Koppen Cfa) with four distinct seasons. Winters are short and cool with occasional frosts; snow is not unheard of but heavy falls are otherwise rare. Summer is long and humid, with amongst the highest temperatures in China. Rain is greatest from March to June, and least in fall and early winter. Monthly averages in the city range from 5.3 °C (41.5 °F) in January to 29.2 °C (84.6 °F) in July, with an annual mean of 17.6 °C (63.7 °F).

[hide]Climate data for Nanchang (1971-2000)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) 8.7
(47.7)
10.4
(50.7)
14.6
(58.3)
21.2
(70.2)
26.3
(79.3)
29.4
(84.9)
33.4
(92.1)
33.0
(91.4)
28.7
(83.7)
23.7
(74.7)
17.6
(63.7)
12.1
(53.8)
21.6
(70.9)
Average low °C (°F) 2.7
(36.9)
4.4
(39.9)
8.2
(46.8)
14.3
(57.7)
19.2
(66.6)
22.8
(73.0)
25.8
(78.4)
25.6
(78.1)
21.6
(70.9)
16.3
(61.3)
10.1
(50.2)
4.6
(40.3)
14.6
(58.3)
Precipitation mm (inches) 74.0
(2.913)
100.7
(3.965)
175.6
(6.913)
223.8
(8.811)
243.8
(9.598)
306.7
(12.075)
144.0
(5.669)
128.9
(5.075)
68.7
(2.705)
59.7
(2.35)
56.8
(2.236)
41.5
(1.634)
1,624.4
(63.953)
% humidity 77 78 81 81 80 83 77 77 77 73 72 70 77.2
Avg. precipitation days (≥ 0.1 mm) 13.0 13.2 18.0 17.7 16.6 15.5 10.8 10.3 7.7 8.8 7.9 7.8 147.3
Mean monthly sunshine hours 91.9 83.7 85.2 114.4 151.1 160.2 248.7 243.2 185.8 167.0 147.5 141.7 1,820.4

Source: 中国气象局 国家气象信息中心
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#14 User is online   Ian Williams 

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Posted 15 May 2012 - 14:18

13th May 2012


Mardie, Western Australia 37.4oC



Mardie Station
From Wikipedia, the free encyclopediaCoordinates: Posted Image21°11′46″S 118°00′56″EMardie Station is a pastoral lease and sheep then cattle station that was established in 1866 in the Pilbara Region of Western Australia near the mouth of the Fortescue River. The original pastoral lease was taken by Simpson and MacIntoch who worked for the Denison Plains Pastoral Company. The company equipped the barque Warrier in Melbourne and had intended to sail to Roebuck Bay to settle in another area but following a succession of calms the ship had to land at Cossack when the stock started to die of dehydration. Upon landing the group decided to trek south west and eventually squatted at Mardie Springs. The station was established and by 1883 three paddocks were fenced, several wells had been dug and the flock was about 18,000 head of sheep.[1]

The station was owned at one time by members of the Withnell family who also established many other stations in the North West including Sherlock, Mount Welcome, Mallina, Karratha, Chirritta and Edjudina.[2]

The station covers an area of about 225,000 hectares (560,000 acres)[3] and has over 8,000 head of specially bred cattle.[4]

The station was hard hit by flooding in 1894 when the Fortescue River, usually about 10 miles (16 km) away from the homestead, rose to within metres of the front door. The stockyards were destroyed and hundreds of sheep were washed away.[5]

The station was sold by J.A. Withnell to B.H. Sharpe (who owned Wooleen Station) along with 30,000 head of sheep and 100 cattle in 1923 for £50,000.[1]

It switched from sheep to cattle in 1998.[6] It is owned by CITIC-Pacific, a Hong Kong-based company, who bought the station in 2007.[7]

Home to the largest infestation of Mesquite in the state, following the introduction of two trees as shade trees around the homestead and shearing shed in the 1930s, it is estimated that around 150,000 hectares (370,000 acres) of the station now contain the plant.[3][8] About 30,000 hectares (74,000 acres) of the infestation is described as dense.[6] Stock must be quarantined in paddocks free of Mesquite so the seeds can pass through their guts before they can be moved on to prevent the pest from spreading further.[8]

The station has an arid climate with very hot summers and mild to warm winters. Rainfall is generally low but highly variable and unpredictable; 300 millimetres (12 in) has fallen in one day and the station experienced a 15-month stretch with no rainfall in 1924.[6] It received Western Australia's highest temperature of 50.5 °C (122.9 °F) on 19 February 1998.[9] On 19 February 1975, during Cyclone Trixie, it recorded a wind gust of 259 kilometres per hour (161 mph), the highest wind gust in Australia at that time.[10]



[hide]Climate data for Mardie
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °C (°F)49.0
(120.2)
50.5
(122.9)
47.2
(117.0)
43.7
(110.7)
40.5
(104.9)
35.4
(95.7)
34.3
(93.7)
38.1
(100.6)
41.0
(105.8)
46.0
(114.8)
47.0
(116.6)
48.8
(119.8)
50.5
(122.9)
Average high °C (°F)38.0
(100.4)
37.5
(99.5)
37.6
(99.7)
35.8
(96.4)
31.5
(88.7)
28.1
(82.6)
27.7
(81.9)
29.5
(85.1)
32.2
(90.0)
34.9
(94.8)
36.4
(97.5)
37.6
(99.7)
33.9
(93.0)
Average low °C (°F)25.0
(77.0)
25.3
(77.5)
24.1
(75.4)
21.0
(69.8)
16.9
(62.4)
13.8
(56.8)
11.8
(53.2)
12.4
(54.3)
14.3
(57.7)
17.3
(63.1)
20.0
(68.0)
22.9
(73.2)
18.7
(65.7)
Record low °C (°F)16.1
(61.0)
17.3
(63.1)
13.3
(55.9)
10.0
(50.0)
7.8
(46.0)
3.9
(39.0)
2.9
(37.2)
4.4
(39.9)
6.0
(42.8)
7.6
(45.7)
12.8
(55.0)
14.8
(58.6)
2.9
(37.2)
Rainfall mm (inches)37.9
(1.492)
60.4
(2.378)
50.4
(1.984)
19.9
(0.783)
36.9
(1.453)
37.2
(1.465)
13.4
(0.528)
7.4
(0.291)
1.4
(0.055)
0.9
(0.035)
1.5
(0.059)
8.4
(0.331)
275.5
(10.846)
Source: [11]
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#15 User is online   Ian Williams 

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Posted 15 May 2012 - 21:51

13th May 2012 News
http://www.weatheron...xt&DAY=20120513


World Weather40 die in Chinese hailstormBeijing, May 13, 2012 (AFP) - Forty people were killed when a brief but violent hailstorm and torrential rain swept through a mountainous region of northwest China, the local government said on Sunday. Eighteen others remained missing in Min county, a disaster-prone area of Gansu province, while 87 had been sent to hospital, the county government said in a statement on its website. Officials said 29,300 people had been evacuated after rain and hail battered the county for just 60 minutes late Thursday afternoon. It had "wreaked havoc" on all of the county's 18 townships and had affected more than two-thirds of its 450,000 residents, the state-controlled Xinhua news agency reported. "Roads were blocked, houses collapsed, farmland was destroyed, and the power supply and telecommunications services were disrupted by the extreme weather," the agency said, quoting Xu Guangyao, a senior county official. Min county is 150 kilometres (94 miles) from Zhouqu county, where a rain-triggered mudslide killed about 1,500 people in August 2010.



This post has been edited by Ian Williams: 15 May 2012 - 21:51

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#16 User is online   Ian Williams 

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Posted 16 May 2012 - 14:18

14th May 2012


Sancti Spiritus, Cuba 71.4 mm


Sancti Spíritus is a municipality and capital city of the province of Sancti Spíritus in central Cuba. Sancti Spíritus, Latin for "Holy Spirit," is one of the best preserved cities in the Caribbean from the time of the sugar trade.

Posted ImagePosted ImageA cultural festival in the boulevard of the city organized by Facultad de Ciencias Medicas Sancti SpiritusPosted ImagePosted ImageA cultural Exhibition in the boulevard of the city organized by Facultad de Ciencias Medicas Sancti Spiritus

Contents
[show]

[edit]History
The city was founded by Diego Velázquez de Cuéllar in 1514.[1] Francisco Iznaga, a rich Basque landowner in the western portion of Cuba during the first thirty years of the colonization of Cuba, was elected mayor of Bayamo in 1540. Iznaga was the originator of a powerful lineage that finally settled in Sancti Spiritus and Trinidad where Torre Iznaga is. Iznaga's descendants fought for the Independence of Cuba and the Annexation to the US from 1820 to 1900.

The Parroquial Mayor is located two blocks south of the town's main square; it is a venerable green-towered church whose early 16th-century origins make it the country's oldest. Nearby is the Museo de Arte Colonial (Colonial Art Museum), one of Sancti Spíritus's most splendid colonial homes and a standout attraction. The opulent former palatial mansion of the Valle Iznaga clan, one of Cuba's most elite families who fled Cuba after Fidel's Revolution, it became the property of the state in 1961. Ninety percent of what you see inside, from furniture to paintings, is original. Though the family obviously kept an impressive collection of Limoges porcelain, French gilded mirrors, Italian marble tables, and Baccarat crystal chandeliers here, it wasn't their primary residence; the house was used mostly to host family members in transit, so the furnishings were rather eclectic. The three bedrooms are decorated in grand style, though, with handmade lace, embroidered sheets, and hand-painted glass. There is a gorgeous and very Cuban leather sillón fumador (smoking chair) and, in the music room, the mid-18th-century American piano, one of only two of its type in Cuba. In the tearoom is the family seal, which says a lot about the arrogance of the rich and powerful: "El que más vale no vale tanto como Valle vale" ("He who has the greatest worth isn't worth as much as a Valle is worth" -- playing off the Spanish word for "worth" with the family surname).

Another interesting landmark is one of Cuba's older bridges over the Yayabo river. Built in 1815 with clay bricks it forms five arcs, the center being 9 meters tall. The entire bridge is only 85 meters long and was designed for pedestrians and carriages during colonial-era Cuba but has thus far resisted heavier modern traffic.

Sancti Spíritus has a worldwide famous Medical University located at the Main road in Olivos III. It has students from all over the world representing 34 nationalities. It is also the home of the Sancti Spíritus Gallos baseball team.




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#17 User is online   Ian Williams 

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Posted 17 May 2012 - 16:21

15th May 2012


San Antonio, Texas U.S.A 102.0 mm


San Antonio (Posted Image /ˌsænænˈtni./) is the seventh-largest city in the United States of America and the second-largest within the state of Texas, with a population of 1.3 million.[2] Located in the American Southwest and the south–central part of Texas, the city serves as the seat of Bexar County. San Antonio has characteristics of other western urban centers in which there are sparsely populated areas and a low density rate outside of the city. It was the fourth-fastest growing large city in the U.S. from 2000 to 2006[3] and the fifth-fastest-growing from 2007 to 2008.[4] The San Antonio-New Braunfels metropolitan area, commonly referred to as Greater San Antonio, has a population of 2.2 million based on the 2011 U.S. Census estimate, making it the 24th-largest metropolitan area in the United States and third-largest in the state of Texas.

The city was named for San Antonio de Padua, whose feast day is on June 13, when a Spanish expedition stopped in the area in 1691. Famous for Spanish missions, the Alamo, the River Walk, the Tower of the Americas, the Alamo Bowl, Marriage Island and host to SeaWorld and Six Flags Fiesta Texas theme parks, the city is visited by approximately 26 million tourists per year according to the San Antonio Convention and Visitors Bureau. The city is home to the four-time NBA champion San Antonio Spurs and the annual San Antonio Stock Show & Rodeo, one of the largest in the country.

San Antonio has a strong military presence—it is home to Fort Sam Houston, Lackland Air Force Base, Randolph Air Force Base, and Brooks City-Base, withCamp Bullis and Camp Stanley outside the city. Kelly Air Force Base operated out of San Antonio until 2001, when the airfield was transferred over to Lackland AFB and the remaining portions of the base became Port San Antonio, an industrial/business park. San Antonio is home to five Fortune 500 companies and the South Texas Medical Center, the only medical research and care provider in the South Texas region.





Geography
San Antonio
Climate chart (explanation)
JFMAMJJASOND
1.7 6239 1.8 6742 1.9 7450 2.6 8057 4.7 8666 4.3 9172 2 9574 2.6 9574 3 9069 3.9 8259 2.6 7149 2 6441
Average max. and min. temperatures in °F
Precipitation totals in inches
Source: NOAA
San Antonio is located near 29.5°N 98.5°W. It is about 80 miles to the southwest of its neighboring city, Austin. According to the United States Census Bureau, in 2000 the city had a total area of 412.07 square miles (1,067.3 km2)—407.56 square miles (1,055.6 km2) (98.9%) of land and 4.51 square miles (11.7 km2) (1.1%) of water. The city sits on the Balcones Escarpment.The altitude of San Antonio is 772 feet (235 m) above sea level.

The primary source of drinking water for the city is the Edwards Aquifer. Impounded in 1962 and 1969, respectively, Victor Braunig Lake and Calaveras Lakewere among the first reservoirs in the country built to use recycled treated wastewater for power plant cooling, reducing the amount of groundwater needed forelectrical generation.


[edit]Neighborhoods
Further information: Neighborhoods of San AntonioFurther information: Downtown San Antonio
[edit]Climate
San Antonio lies near the western edge of the humid subtropical climate zone. Its weather is alternately dry or humid depending on prevailing winds, turning hot in the summer, warm to cool winters subject to descending northern cold fronts in the winter with cool to cold nights, and comfortably warm and rainy in the spring and fall.

San Antonio receives about a dozen subfreezing nights each year, occasionally (about once every few winters) seeing some sort of wintry precipitation (i.e. sleet/freezing rain), but accumulation and snow itself are not very common. Many winters may pass without any freezing precipitation at all. According to the National Weather Service, there have been 31 instances of snowfall (a trace or more) in the city in the past 122 years, for an average of about once every four years. However a decade or more may pass between snowfalls.[15] In 1985, the city received a record snowfall of 16 inches (41 cm).[16]

San Antonio is one of the most flood-prone regions in North America.[17] The October 1998 Central Texas floods were one of the costliest floods in United States history, resulting in $750 million in damage and 32 deaths. In 2002, from June 30 to July 7, 35 inches of rain fell in the San Antonio area, resulting in widespread flooding and 12 fatalities.[18]

Instances of tornadoes within the city limits have been reported as recently as October 2011, although they seldom occur.[19] An F2 tornado will land within 50 miles of the city on average once every five years. San Antonio has experienced two F4 tornados, one in 1953 and another in 1973. The 1953 tornado resulted in two deaths and 15 injuries.[20]

In San Antonio, July and August tie for the average warmest months, with an average high of 95°F (35°C). The highest temperature ever to be recorded was 111 °F(44 °C) on September 5, 2000.[15] The average coolest month is January. The lowest recorded temperature ever was 0 °F (−18 °C) on January 31, 1949.[15] May, June, and October have quite a bit of precipitation. For the last 135 years, the average annual precipitation has been 29.05 inches (738 mm), with a maximum of 52.28 inches (1,328 mm) and a minimum of 10.11 inches (256.8 mm) in one year.[21]


[hide]Climate data for San Antonio (San Antonio Int'l), 1981-2010 normals
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °F (°C)89
(32)
100
(38)
100
(38)
101
(38)
103
(39)
107
(42)
106
(41)
108
(42)
111
(44)
99
(37)
94
(34)
90
(32)
111
(44)
Average high °F (°C)63.0
(17.2)
67.0
(19.4)
73.6
(23.1)
80.7
(27.1)
87.1
(30.6)
92.4
(33.6)
94.7
(34.8)
96.1
(35.6)
90.4
(32.4)
82.3
(27.9)
72.3
(22.4)
64.1
(17.8)
80.31
(26.84)
Average low °F (°C)40.7
(4.8)
44.2
(6.8)
50.9
(10.5)
58.2
(14.6)
66.9
(19.4)
72.6
(22.6)
74.7
(23.7)
74.8
(23.8)
69.1
(20.6)
60.2
(15.7)
50.1
(10.1)
41.7
(5.4)
58.68
(14.82)
Record low °F (°C)0
(−18)
4
(−16)
19
(−7)
31
(−1)
43
(6)
48
(9)
60
(16)
57
(14)
46
(8)
27
(−3)
21
(−6)
6
(−14)
0
(−18)
Precipitation inches (mm)1.76
(44.7)
1.79
(45.5)
2.31
(58.7)
2.10
(53.3)
4.01
(101.9)
4.14
(105.2)
2.74
(69.6)
2.08
(52.8)
3.03
(77)
4.10
(104.1)
2.28
(57.9)
1.91
(48.5)
32.25
(819.2)
Snowfall inches (cm).7
(1.8)
.1
(0.3)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
0
(0)
.7
(1.8)
Avg. precipitation days (≥ 0.01 in)7.07.28.86.48.57.55.24.76.66.96.77.583
Avg. snowy days0.20.300000000000.5
Mean monthly sunshine hours158.1172.3217.0210.0223.2276.0310.0294.5234.0217.0171.0148.82,631.9
Source: NOAA [22], The Weather Channel (records) [23], HKO (sun, 1961-1990) [24]



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#18 User is online   Ian Williams 

  • Group: Warnings Team
  • Posts: 14987
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Posted 18 May 2012 - 17:18

16th May 2012


Espiritu Santo (Vanuatu) 182.0 mm


Espiritu Santo[1] is the largest island in the nation of Vanuatu, with an area of 3,955.5 km2 (1,527.2 sq mi). It belongs to the archipelago of the New Hebrides in the Pacific region of Melanesia. It is in the Sanma Province of Vanuatu.

The town of Luganville, on Espiritu Santo's southeast coast, is Vanuatu's second-largest settlement and the provincial capital. Roads run north and west from Luganville but most of the island is far from the limited road network.

Vanuatu's highest peak is the 1879 metre (6165 foot) Mount Tabwemasana in west-central Espiritu Santo.

In 1998, Santo hosted the Melanesia Cup.


Contents
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[edit]History
Posted ImagePosted ImageChampagne Beach, North SantoPosted ImagePosted ImageLocal childrenThe Portuguese explorer Pedro Fernandes de Queirós, working for Spain, established a settlement in 1606 at Big Bay on the north side of the island. Espiritu Santo takes its name from Queirós, who named the entire island group La Austrialia [sic][2] del Espíritu Santo in acknowledgment of the Spanish king's descent from the royal House of Austria, and believing he had arrived in the Great Southern Continent, Terra Australis. During the time of the British–French Condominium, Hog Harbour, on the northeast coast, was the site of the British district administration, while Segond, near Luganville was the French district administration.[3]

Posted ImagePosted ImageID check at the entrance to the base during WWIIDuring World War II, particularly after the Japanese attack on Pearl Harbor, the island was used by Allied forces as a military supply and support base, naval harbor, and airfield. In highly fictionalized form, it is the locale of James Michener'sTales of the South Pacific and the subsequent Rogers and Hammerstein musical, South Pacific. The presence of the Allies later contributed to the island's diving tourism, as the United States dumped most of their equipment and refuse at what is now known as 'Million Dollar Point'.[4] Another wreck off Espiritu Santo, the SS President Coolidge, is also a popular diving spot. The SS President Coolidge was a converted luxury liner that hit a mine during the war.

Between May and August 1980 the island was the site of a rebellion during the transfer of power over the colonial New Hebrides from the condominium to independent Vanuatu. Jimmy Stevens' Nagriamel movement, in alliance with private French interests and backed by the Phoenix Foundation and American libertarians hoping to establish a tax-free haven, declared the island of Espiritu Santo independent of the new government. A Republic of Vemerana was proclaimed on May 28. France recognized the independence on June 3. On June 5 the tribal chiefs of Santo named the French Ambassador Philippe Allonneau "King of Vemerana", Jimmy Stevens became Prime Minister. Luganville is renamed Allonneaupolis. But negotiations with Port-Vila failed and from July 27 to August 18, British Royal Marines and a unit of the French Garde Mobile were deployed to the Vanuatu's capital island but did not invade Espiritu Santo as the soon-to-be government had hoped. The troops were recalled shortly before independence. Following independence, Vanuatu, now governed by Father Walter Lini, requested assistance fromPapua New Guinea, whose forces invaded and conquered Espiritu Santo.


[edit]Culture
Posted ImagePosted ImageBest Point, South SantoPosted ImagePosted ImageRoadside market, east SantoSanto, with many wrecks and reefs to be explored, is a very popular tourist destination for divers. Champagne Beach draws tourists with its pink sand and clear waters. The "Western Side" of the island contains many caves which may be explored, and cruise ships often stop in at Luganville.

The local people make their living by supporting the tourist trade, by cash-crop farming, mostly copra but some cacao and kava as well as peanuts, or by subsistence farming and fishing.

Most Santo people are Christians. The largest church groups on the island are the Presbyterian Church of Vanuatu, the Roman Catholic Church and the Church of Melanesia (Anglican). Also active are the Apostolic Church, the Church of Christ, the Seventh-day Adventist Church, and others. However, in many villages, particularly in Big Bay and South Santo, the people are "heathen", a term that in Vanuatu has no pejorative connotation — it simply denotes someone who has not embraced Christianity. Customary beliefs of a more modern sort are found among followers of the Nagriamel movement based in Fanafo.

For almost all Santo's people custom plays a large part in their lives, regardless of their religion. The chief system continues strongly in most areas.

The people of Santo face some health problems, especially malaria, and tuberculosis . Although there is a hospital, most locals consult either their own witch doctoror medical clinics set up by western missionaries. Kava is the popular drug of the island, although alcohol is becoming more prevalent. With the rising number of adults using alcohol, there is a rising crime rate, especially involving violence toward women, and tribal warfare.


[edit]Economy and Infrastructure
These villages are mostly self-sufficient with their own vegetable gardens, chickens and pigs. The airport is about five km from town. From Luganville, three ‘main’ roads emerged. One road runs along the south coast for about 40 km to end at the village of Tasiriki. Luganville is the only town on the island, the rest of the island is dotted with small villages.

Santo is home to a number of cattle farms (including the famous Belmol Cattle Project, originally established by French settlers) and exports much of its beef to Japan, Australia and other Pacific Island countries.

Besides beef, tin fish and rice, bought in town, Santo has many foods that locals take for granted and that tourists enjoy as delicacies. Among these are sweet pineapples, mangoes, island cabbage, flying fox and coconut crab, as well as local nuts such as natapoa and the sweet fleshy-fruit nouse. There is a market in Luganville where local food such as manioc, taro, yam, cabbage and other freshly grown island staples are being sold. For groceries and many packaged goods,several small supermarkets(such as LCM, Unity Shell and Au bon Marche) exists where one can do his/her shopping.

Many local people still rely on subsistence farming for their food. Most villages have a garden that is tended by men and women alike. Taro and yam are commonly grown in these gardens, and are mainstays of the local diet.


[edit]Biodiversity
The island of Espiritu Santo is home to all of Vanuatu's endemic birds, including the Santo Mountain Starling, a species restricted entirely to Santo. Two protected areas have been established to safeguard the island's biodiversity; the Loru Conservation Area on the east coast and the Vatthe Conservation area in the north.

Vathe conservation area: Situated in Big Bay, on the North side of the island, you will walk through the rain forest as your guide tells you about the local plants, trees and birds. A great tour for bird watchers and nature lovers. It is an easy but long walk. There are many mosquitoes, you will need good walking shoes and mosquito repellent.

The Loru Rainforest Protected Area: It is situated in the lowland rainforests of Santo. Established in 1993 by Chief Caleb Ser, the 220 hectare reserve supports a rich variety of Vanuatu's bird, bat and plant life as well as a diverse range of marine species in the two-kilometre stretch of fringing reef.[5]


Climate
Posted ImagePosted ImageEratap Beach, VanuatuThe climate is sub-tropical with approximately nine months of warm to hot rainy weather and the possibility of cyclones and three to four months of cooler drier weather characterized by winds from the southeast.[13] The water temperature ranges from 72 °F (22 °C) in winter to 82 °F (28 °C) in the summer.[13] Cool between April and September, the days become hotter and more humid starting in October.[13] The daily temperature ranges from 68 °F (20 °C) to 90 °F (32 °C).[13] South easterly trade winds occur from May to October.[13]

Vanuatu has a long rainy season, with significant rainfall usually occurring almost every month.[13] The wettest and hottest months are December through to April, which also constitute the cyclone season.[13] The driest months are June through November.[13] Rainfall averages about 2,360 millimetres (93 in) per year but can be as high as 4,000 millimetres (160 in) in the northern islands.[16]















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#19 User is online   Ian Williams 

  • Group: Warnings Team
  • Posts: 14987
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Posted 20 May 2012 - 15:37

17th May 2012


Allahabad, India 46.3C


Allahabad ([ɪlɑhɑbɑd̪]; Hindi: इलाहाबाद; Urdu: الہ آباد), or Settled by God in Persian, is a major city of India and is one of the main holy cities of Hinduism. It was renamed by the Mughal emperor Akbar from the original (still unofficially used) native name of Prayaga, and is by some accounts the second-oldest city in India. It is located in the north Indian state of Uttar Pradesh, lying some 205 kilometres (127 mi) south of the state capital, Lucknow. It is the administrative headquarters of the Allahabad District. Allahabad has been ranked the world's 130th fastest growing city (growth rate: 2.09 per cent (2011)).[citation needed] The ancient name of the city is Prayaga (Sanskrit for "place of sacrifice"), as it is believed to be the spot where Brahma offered his first sacrifice after creating the world. It is one of four sites of the mass Hindu pilgrimage Kumbh Mela, the others being Haridwar, Ujjain and Nashik. It has a position of importance in Hindu scriptures for it is situated at Triveni Sangam, the confluence of the holy rivers Ganges and Yamuna, and the ancient Sarasvati River.[2]

Many government offices of both central and state government are present in the city, which is also home to India's 4th oldest university, AU and UP's singleNational Institutes of Technology

Allahabad is a home to seven out of fourteen Prime Ministers of India. Jawaharlal Nehru, Lal Bahadur Shastri, Indira Gandhi, Rajiv Gandhi, Gulzarilal Nanda,Vishwanath Pratap Singh and Chandra Shekhar were all either born in Allahabad, were alumni of Allahabad University or got elected from a constituency in Allahabad.[citation needed]

The Government of India has selected Allahabad as one of the mission cities for the Jawaharlal Nehru National Urban Renewal Mission, with the goals of improving urban infrastructure, efficient governance and basic services to urban citizens.[3]

Other cities that are fairly close include Kanpur, Varanasi, Lucknow and Rewa.





Geography
Posted ImagePosted ImageSurroundings of Allahabad.Allahabad is at 25.45°N 81.84°E in the southern part of Uttar Pradesh at an elevation of 98 metres (322 ft) and stands at the confluence of two rivers, the Ganges and Yamuna. The region was known in antiquity as the Vats country. To its south and southeast is the Bagelkhand region, to its east is the mid Ganges valley of North India, or Purvanchal, to its southwest is the Bundelkhand region, to its north and northeast is the Awadh region and to its west along with Kaushambi it forms the Lower Doab region.

Allahabad stands at a strategic point both geographically and culturally. An important part of the Ganges-Yamuna Doab region, it is the last point of the Yamuna River and is the last frontier of the Indian west.

The land of the Allahabad district that falls between the Ganges and Yamuna is just like the rest of Doab, fertile but not too moist, and is especially suitable for the cultivation of wheat. The non-Doabi (southern and eastern) part of the district, are somewhat similar to those of adjoining Bundelkhand and Bagelkhand regions: dry and rocky.

Allahabad is 343 km (213 mi) north of Jabalpur on the same longitude. Indian Standard Time is calculated from 82.5° E longitude, just west of the town of Mirzapur, near Allahabad.





Climate
Allahabad
Climate chart (explanation)
JFMAMJJASOND
19 249 16 2711 9 3417 6 3923 10 4227 85 4029 300 3426 308 3326 190 3325 40 3321 12 3014 3 259
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: IMD
Allahabad has the humid subtropical climate common to cities in the plains of North India. Allahabad experiences three seasons: hot dry summer, cool dry winter and warm humid monsoon. Summer lasts from April to June with maximum temperatures ranging from 40 °C (104 °F) to 45 °C (113 °F). Monsoon begins in early July and lasts till September. Winter lasts from December to February. Temperatures rarely drop to the freezing point. Maximum temperatures are around 22 °C (72 °F) and minimum around 10 °C (50 °F). Allahabad also witnesses severe fog in January resulting in massive traffic and travel delays. It does not snow in Allahabad.

Lowest temperature recorded, −2 °C (28 °F); highest 48 °C (118 °F).[6]




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The new Yamuna Bridge at Allahabad




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