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uk.sci.weather (UK Weather) (uk.sci.weather) For the discussion of daily weather events, chiefly affecting the UK and adjacent parts of Europe, both past and predicted. The discussion is open to all, but contributions on a practical scientific level are encouraged. |
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#1
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http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm
I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. Please note I am asking the question rather than trying to prove a point ! Cheers -- James Brown |
#2
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On Fri, 14 Aug 2009 21:16:52 +0100, James Brown wrote in
http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. That piece featured on the BBC news yesterday. I cannot believe GW is not a large contributory factor. Please note I am asking the question rather than trying to prove a point! :-) -- Mike Tullett - Coleraine 55.13°N 6.69°W posted 8/14/2009 8:41:05 PM GMT |
#3
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James Brown wrote:
http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. I think the Antarctic SST's are stable - or even have been lower than normal - because the excess melting of of the land ice has provided a larger supply of cold, fresh water than normal. -- Graham P Davis, Bracknell, Berks., UK. E-mail: newsman not newsboy "I wear the cheese. It does not wear me." |
#4
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![]() "Graham P Davis" wrote in message ... James Brown wrote: http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. I think the Antarctic SST's are stable - or even have been lower than normal - because the excess melting of of the land ice has provided a larger supply of cold, fresh water than normal. Graham, am I correct to say that the ocean flow round Antartica is largely decoupled from the rest of the planet? Will -- |
#5
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Will Hand wrote:
"Graham P Davis" wrote in message ... James Brown wrote: http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. I think the Antarctic SST's are stable - or even have been lower than normal - because the excess melting of of the land ice has provided a larger supply of cold, fresh water than normal. Graham, am I correct to say that the ocean flow round Antartica is largely decoupled from the rest of the planet? Not something I know too much about but, after some googling, I'd say no. For instance, see http://oceanworld.tamu.edu/resources...apter13_04.htm -- Graham P Davis, Bracknell, Berks., UK. E-mail: newsman not newsboy "I wear the cheese. It does not wear me." |
#6
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![]() "Graham P Davis" wrote in message ... Will Hand wrote: "Graham P Davis" wrote in message ... James Brown wrote: http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. I think the Antarctic SST's are stable - or even have been lower than normal - because the excess melting of of the land ice has provided a larger supply of cold, fresh water than normal. Graham, am I correct to say that the ocean flow round Antartica is largely decoupled from the rest of the planet? Not something I know too much about but, after some googling, I'd say no. For instance, see http://oceanworld.tamu.edu/resources...apter13_04.htm Thanks Graham, quoteThe Antarctic Circumpolar Current is an important feature of the ocean's deep circulation because it transports deep and intermediate water between the Atlantic, Indian, and Pacific Ocean, and because it contributes to the deep circulation in all basins. /quote So, what goes on in the Antarctic *is* important for the planet. Paul, Is this the explanation you were hoping Lawarence would have provided? OK we can argue about it but I am not an expert on complicated interactions between ocean and atmosphere, which is why I have kept quiet. Also, I would certainly never go as far to say that - just because the Antartic is stable or getting colder it means GW is going away, it is far more complex than that. Cheers, Will -- |
#7
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On Aug 15, 9:34*am, "Will Hand" wrote:
"Graham P Davis" wrote in ... Will Hand wrote: "Graham P Davis" wrote in message ... James Brown wrote: http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. I think the Antarctic SST's are stable - or even have been lower than normal - because the excess melting of of the land ice has provided a larger supply of cold, fresh water than normal. Graham, am I correct to say that the ocean flow round Antartica is largely decoupled from the rest of the planet? Not something I know too much about but, after some googling, I'd say no. For instance, see http://oceanworld.tamu.edu/resources...ter13/chapter1... Thanks Graham, *quoteThe Antarctic Circumpolar Current is an important feature of the ocean's deep circulation because it transports deep and intermediate water between the Atlantic, Indian, and Pacific Ocean, and because it contributes to the deep circulation in all basins. /quote So, what goes on in the Antarctic *is* important for the planet. Paul, Is this the explanation you were hoping Lawarence would have provided? OK we can argue about it but I am not an expert on complicated interactions between ocean and atmosphere, which is why I have kept quiet. Also, I would certainly never go as far to say that - just because the Antartic is stable or getting colder it means GW is going away, it is far more complex than that. Cheers, Will --- Hide quoted text - - Show quoted text - I think Alistair is on the right lines and your own summary captures the difficulties of interpretation. Graham may well be right too! Personally, I think that problem here is the lack of data in terms of observations, both on land and over sea and in terms of ice changes over time. The GW difficulty is that warmer temperatures, especially in the oceans, should produce more melting around the fringes of the continent. On the other hand warmer temperatures in the atmosphere may produce more precipitation, thus adding to the glacier inputs. Maybe the research by Prof Wingham, showing thinning of the Pine Island glacier indicates something, but why is that glacier losing mass? Is if from less snowfall, or more ablation? In addition, is the Pine Island glacier typical of all Antarctic glaciers, or even typical of that area? Are increasing ocean temps responsible for melting at the Antarctic fringes? ocean An Australian study in 2008 came to the conclusion that sea level rises around Antarctica were due to warming oceans, not ice melting (both could be due to GW, of course): http://www.abc.net.au/science/articl...18/2165549.htm This adds to the difficulties as well; a study by the BAS showed that increasing Antarctic sea ice could be due to the influence of the Antarctic ozone hole: http://www.antarctica.ac.uk/press/pr...ase.php?id=838 Zhang's paper from 2007, concludes that increasing Antarctic sea ice in a warming climate could be due to a reduction in upward heat transfer, but also recognises that there could be other mechanisms. http://psc.apl.washington.edu/zhang/...20-11-2515.pdf The overall need is for more research. The answer to your question, of course, is that I have no idea what Lawrence would have said, but how anyone can assert that increasing Antarctic sea ice could be used as a support to an argument about GW having finished, just doesn't understand the complexity of drawing conclusions from either the present ice amount, or the trend over time. So few researchers, so few measurements combined with a regional approach = a great lack of surety as to exactly how Antarctic sea ice will react to GW. |
#8
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![]() "Graham P Davis" wrote in message ... James Brown wrote: http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. I think the Antarctic SST's are stable - or even have been lower than normal - because the excess melting of of the land ice has provided a larger supply of cold, fresh water than normal. -- Graham P Davis, Bracknell, Berks., UK. E-mail: newsman not newsboy "I wear the cheese. It does not wear me." Oh here we go again when its colder its AGW and when its warmer it AGW |
#9
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James Brown wrote:
http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. Please note I am asking the question rather than trying to prove a point ! Cheers "according to research seen by the BBC" - I closed the window after that sentence. -- Brian Wakem |
#10
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![]() "Brian Wakem" wrote in message ... James Brown wrote: http://news.bbc.co.uk/1/hi/sci/tech/8200680.stm I'm wondering if this is purely a byproduct of GW or why it should be accelerating - given Antarctic SST's fairly stable etc. Please note I am asking the question rather than trying to prove a point ! Cheers "according to research seen by the BBC" - I closed the window after that sentence. -- Brian Wakem The BBC jump on this stuff with such eager glee that facts and eventual retractions get left by the wayside of western guilt and angst. |
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