Dave, you by now know what a pedantic old bastard I am! I want to see some actual papers on this, please! We can all of us post stuff on blogs, but without references it is of little value!
Cheers - John
![]() |
![]() |
![]() |
![]() |
| Observations: | Precip, Obs, Synopsis, Obs & Stats, Lightning (Sferics), Satellite, Soundings, SST's, UKww AWS, UK AWS Live Weather UK | Orgs: | RMS, TORRO, COL ESTOFEX |
| Forecasts: | UK Forecast, Wetterzentrale, Westwind, NOAA Plots, PSU Plots, Lightning Wizard, NAO | Tools: | Plotter, Translation, Glossary |
| Sponsors: | Csouk's - Commercial sponsors of UKww | UKww: | UKweatherworld Terms and Conditions, Meet the team |
Posted --
Dave, you by now know what a pedantic old bastard I am! I want to see some actual papers on this, please! We can all of us post stuff on blogs, but without references it is of little value!
Cheers - John
Posted --
Posted --
A recent one to add. Only the abstract, unfortunately. The full text would be worth getting hold of. There's a week or two's reading mounting up!!
Paleo-perspectives on ocean acidification (Pelejero et al 2010)
Discussion that cites the above:
http://www.skepticalscience.com/ocean-acidification-global-warming-intermediate.htm
Cheers - John
Posted --
Posted --
Posted --
Not true, Dave - I believe it is important to read right round a subject before coming to conclusions: therefore the past is also vitally important as a key to the present and the future. The same or similar processes have occurred throughout the Phanerozoic: the exceptions being the one you listed - stratospheric O3 removal - and the one you omitted - taking the world's sequestered carbon and burning a lot of it in - geologically speaking - the blink of an eye! The Veron paper in particular I found an excellent review of the causes of mass extinction.
Cheers - John
Posted --
Posted --
Quote
Just quickly addressing a couple of points as I have things that need doing! Firstly, I don't see any stable end-point as the problem: rather, the problem is the rate of transition to that state.
Quote
This is incorrect. At the K-T boundary, solar radiance was at 99% of current levels. It has increased at approx 10%/109 years.
I've plotted it from the start of the Cambrian, using the figure in part 2 of Royer, 2006:
Reference: Royer, D.L. (2006): CO2-forced climate thresholds during the Phanerozoic. Geochimica et Cosmochimica Acta 70, 5665–5675.
Cheers - John
Posted --
Posted --
Quote
Hey Dave,
From the papers I have read, it's not a minority opinion!
Reference 17 cited above addresses the Archaean soils mineralogy problem wrt to the composition of the atmosphere at that time and proposes a very low albedo value as a forcing agent as opposed to insanely high GHG levels in order to satisfy the faint young sun paradox - I only read the same reference a couple of days back. It's certainly one of the areas where one can readily say that the science ain't settled! However, it has nothing to do with your claim (above) of solar luminance being 5% less than the present day 65 million years ago at the KT Boundary - it is that claim that is clearly a minority view!
Cheers - John
Posted --
Posted --
Posted --
Ah - I think we've been at crossed purposes here - you were talking radiance, in terms of energy hitting Earth's surface? I was talking luminance - the "strength" of the sun itself!
Cheers - John
Posted --
Posted --
No - it was your "even with the sun at 5% stronger now then 65 mya" comment that had me thinking you meant luminosity!
Anyway, there's a stack of reading from the links you provided so I'll have to get stuck into that the next few days [y]
Cheers - John
Posted --
Posted --
Just looking through the literature linked to above, Dave. I'll paste three of the "meaty bits" from the abstracts:
Watson et al 2009 - observations indicating substantial variability in the CO2 uptake by the North Atlantic on time scales of a few years
Schuster & Watson MS - Additionally, there has been an inter-decadal decline, evident throughout the study region 11
but especially significant in the northeast of the area covered, with the sink reducing 12
>50% from the mid-nineties to the period 2002-2005....Declining rates of 16
winter-time mixing and ventilation between surface and subsurface waters due to 17
increasing stratification, linked to variation in the North Atlantic Oscillation, are 18
suggested as the main cause of the change. These are exacerbated by a contribution from 19
the changing buffer capacity of the ocean water, as the carbon content of surface waters 20
increases.
Perez et al2008 - The North Atlantic Oscillation shift
from a positive to a negative phase in 1996 led to a reduction of the air-sea heat loss in
the Labrador Sea. The consequent convection weakening accompanied by an increase 10
in stratification lowered the effciency of the northern North Atlantic CO2 sink.
All studies are focussed on the North Atlantic, and they find variations in CO2 uptake, driven over periods of a few years by NAO variations and affected by buffering as seawater chemistry changes.
Firstly, this ought to be expected as solubility of atmospheric CO2 will vary according to influences such as sea temps - which in turn are influenced by climatic patterns such as the NAO/AO and the new kid on the block, the Arctic Dipole pattern.
Secondly, the studies cited concentrate on one area of ocean, that has quite a temperature range at surface via a number of influences. I would want to see data from the Caribbean, the Tropical Pacific & Indian Oceans, the variabilities caused by ENSO, what goes on in the Southern Ocean and so on.
Therefore, I think it is a major "leap of faith" to go from that to your conclusion: "So the idea of ocean acidification by CO2 is clearly in question. If we add to that the issue of total CO2 in the ocean it should also be dropping hence participating in a possible reduction in phytoplankton bloom which does seem to be validated by the final study."
This table is quick & dirty and comes from the Wikipedia Ocean Acidification page - so of course the usual caution is required and I too need to check it is properly referenced. Anyway:
| Time | pH | pH change | Source | H+ concentration change relative to pre-industrial |
|---|---|---|---|---|
| Pre-industrial (18th century) | 8.179 | 0.000 | analysed field[3] | 0% |
| Recent past (1990s) | 8.104 | -0.075 | field[3] | + 18.9% |
| Present levels | ~8.069 | -0.11 | field[4][5][7][12] | + 28.8% |
| 2050 (2×CO2 = 560 ppm) | 7.949 | -0.230 | model[2] | + 69.8% |
| 2100 (IS92a)[13] | 7.824 | -0.355 | model[2] | + 126.5% |
Maybe it's the hydrogen ions we should be worried about!!
Geologically rapid seawater chemistry changes, including the pH reduction discussed here, that move faster than evolution can keep up with, are a severe risk in terms of mass-extinctions of marine life.
Parts of the conclusion of Veron (2008) - link above - are perhaps worth repeating:
If acidi?cation was in fact a major cause of mass
extinctions and reef gaps as the above discussion sug-
gests, prospects for the future are frightening, not because
of any immediate impact on corals, but because of
commitment. Commitment embodies the concept of
unstoppable inevitability, according to which the nature
and health of future environments will be determined, not
by our actions at some future date but by what is hap-
pening now. The oceans, including the ocean depths,
respond slowly to atmospheric conditions, whether a
temperature increase or a CO2 build-up, which means that
the full effects of acidi?cation will take decades to cen-
turies to develop. Nevertheless, this is only a delay: the
factors causing acidi?cation will have irretrievably com-
mitted the Earth to the process long before its effects
become anywhere near as obvious as those of mass
bleaching today......
.....The levels of CO2 and pH predicted by the end of this
century may not have occurred since the Middle Eocene,
but the all-important rate of change we are currently
experiencing has no known precedent. There can be no
evolutionary solution for such a rate of change.
Ultimately—and here we are looking at centuries rather
than millennia—the ocean pH will drop to a point at which
a host of other chemical changes, including anoxia, would
be expected. If this happens, the state of the oceans at the
end of K/T, or something like it, will become a reality and
the Earth will enter the sixth mass extinction. Another 1–3
decades like our last will see the Earth committed to a
trajectory from which there will be no escape.
Such words may attract the "alarmist" tag, but the more I read, the more I think we have every reason to be alarmed. I say again that it is not the endpoint that matters - at some time geologically soon (few million years), in the absence of fossil fuel burning, we would likely head back to a stable hothouse lasting tens of millions of years in which, given a slow natural transition, evolution would handle things as it has done in the past. Instead, it is the speed at which we are setting the transition in motion. That is what appears to be unprecedented.
Cheers - John
Posted --
Posted --