CLIMATE: response to climate change
Ummm, here is another example of selective quotation.Almost nothing is known about the great heat engine of the upper atmosphere which sheds heat into space and which is affected by incoming cosmic radiation. All the discussion concentrates on the heat-blanketing effect of the lower atmosphere. Also, while the discussion is centred on the melting of Arctic sea-ice (and some Greenland glaciers), and also the melting sea-ice of the western Antarctic peninsula, the increasing amount of snow and ice of the eastern Antarctic is hardly ever mentioned. Equally ignored is the recent world-wide ocean survey by the US National Oceanic and Atmospheric Administration’s Pacific Marine Environmental Laboratory which shows that ocean remperatures have been cooling steeply in the last few years. The oceans contain far more heat than the atmosphere and it can only be a matter of time before the atmosphere starts cooling, too, if the ocean temperatures decline continues as they do now.
True, there have been reports of cooling in Antarctica in journals. But this is logical.
Simply speaking, climate systems (a coupled atmosphere-ocean) are arranged in wide cells geographically over the world ('cells' for lack of a better word for laymen). Picture a globe and draw arbitrary cells from Arctic to Antarctic. These cells are irregular, and generally have similar climate. A cell would be an example of the Thar desert in India/Pakistan. Taklamakan in China. Deccan rain forest in India etc...
Whatever happens in one cell pushes out to another cell. So if you get something hotter in Arctic, the global climate system 'tries' to get something else cooler, so the cooling in certain cells. Why not the cooling in immediate cells right now? Adjacent cells will be affected, give it time. My guess is that cells which comprise mostly of countryside (where we grow our crops) will be affected. Why? Less daily temperature variation in rural areas. Also, temperature is not precise, because it is measured in a grid. A sample taken in a 5 km by 5 km grid is interpolated to cover all of it. When we know that a reading of 30C in a city block will change to 33C in a different city block, hardly 100 meters away. If you really want to confirm, ask farmers what changes they have had. Ask two farmers in different 'farmland' cell separated by a city cell. Seasons are changing slightly, either advancing or retarding by a few days/weeks. Best example is of our Monsoon.
Ok, why the cooling so far away in Antarctica? Why in southern hemisphere? Because the southern hemisphere is mostly water. My guess is any 'resultant natural cooling' will be compensated via water, because water can store heat better. Remember the rich get richer, the poor poorer? Western Siberia will accelerate melting, maybe Eastern Siberia will compensate. Adjacent eastern countries (to Vladivostok) like Korea, Japan may get colder. NZ, Tasmania, Southern Australia may get either hotter or cooler because of their proximity to Antarctica...
If compensatory cooling does not occur, we would be in a positive feedback loop, and completely go crazy. I hope this argument is put to rest for you guys.
Regarding NOAA PMEL's ocean cooling paper, actually by Lyman et al (2006)
It is only upper ocean cooling, less than 1000 m depth. The average depth of world's oceans is 3500-3800 m. The major volume is not upper ocean, but deep ocean. Sure the cooling occurs at 400 m and is strong at 750 m. But the deep water takes a while to cool.
There are problems of inadequate sampling intervals and sample grid size. I think that the average upper ocean would probably cool over the globe, because of the additional input of melt water. Snow which doesn't float but is sitting on a continental plate adds additional water, picture a hot cup of tea, add more water, what happens?
But if you read the paper 'Recent Cooling of the Upper Ocean' by Lyman et al. (2006) the globally averaged sea level is still rising. Logically speaking, you will have these regional anomalies.

