twisting_edge said:
The drought claim has always puzzled me greatly, and as far as I know, runs contrary to most climate models. Water certainly evaporates more as you add more heat. But it is a closed system. Where is the evaporated water supposed to go? It comes back as rain. More heat means more rain. Since some 75% of the Earth's surface was covered by water the lst time I looked, increased evaporation from the land masses shoudl be more than offset by increased evaporation (and subsequent rainfall) from the oceans.
More heat doesn't necessarily mean more rain (although part of the problem is getting the rain on a regular basis, rather than having a dry spell followed by torrential rains). The southern and eastern parts of Africa are having significant drought problems, such that the food production has decreased. Australia is having their worst drought (in the third year) ever recorded. Most of the biggest wheat producing areas around the world are seeing dramatic reductions in production - due to reduced rainfall or drought!
Drought means - it's not raining or it's not raining sufficiently.
Drought intensifies over eastern and southern Australia as spring rains fail
http://www.bom.gov.au/climate/drought/drought.shtml
Droughts & Flooding Rain
http://www.abc.net.au/science/scribblygum/august2006/
Droughts & Flooding Rain
http://www.guardian.co.uk/australia/story/0,,1941942,00.html
http://en.wikipedia.org/wiki/2006_Horn_of_Africa_food_crisis
http://www.dfid.gov.uk/News/files/horn-drought-2006.asp
Africa: Weather hazards assessment 19 - 25 Oct 2006
http://www.reliefweb.int/rw/rwb.nsf/db900SID/LZEG-6UPQ9W?OpenDocument
http://earthobservatory.nasa.gov/NaturalHazards/shownh.php3?img_id=13329
In the US -
http://www.drought.unl.edu/dm/monitor.html
But - some areas are getting too much rain
Floods in East Africa
http://earthobservatory.nasa.gov/NaturalHazards/shownh.php3?img_id=13958
Floods ravage Horn of Africa
http://www.abc.net.au/news/newsitems/200611/s1791983.htm
Guinea: Floods
http://www.reliefweb.int/rw/RWB.NSF/db900SID/JOPA-6U7BJ7?OpenDocument
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Some references from
http://www.ocean.washington.edu/courses/oc588/
IPCC (2001) Climate Change 2001: the scientific basis, Contribution of Working Group I in the Third Assessment Report of the Intergovernmental Panel on Climate Change (Houghton et al., eds.), Cambridge University Press, Cambridge, U.K. and New York, NY, USA, 881 pp.
Toggweiller, R. and J. Sarmiento (1985) Glacial to interglacial changes in atmospheric carbon dioxide: The critical role of ocean surface water at high latitudes, in: The Carbon Cycle and Atmospheric CO2: Natural variations Archean to Present, (Sundquist, E. and Broecker, W. S., eds) A.G.U. Geophysical Monograph 32, Wash. D. C.
Sabine, C.L., et al., The oceanic sink for anthropogenic CO2, Science, 305, 367-371, 2004.
Takahashi, T., The fate of industrial carbon dioxide, Science, 305, 352-353, 2004.
Quay, P., et al., Carbon isotopic composition of atmospheric CH4: Fossil and biomass burning source strengths, Global Biogeochemical Cycles, 5, 25-47, 1991.
Long, S.P., E.A. Ainsworth, A. Rogers, and D.R. Ort, Rising atmospheric carbon dioxide: Plants FACE the Future, Annu. Rev. Plant Biol., 55, 591-628, 2004.
C. Korner, Through enhanced tree dynamics carbon dioxide enrichment may cause tropical forests to lose carbon, Phil. Trans. R. Soc. Lond. B, 359, 493-498, 2004.