摘要: Increased global warming can lead to greater evaporation of water into the atmosphere, and vapor is itself an excellent greenhouse gas. For this reason, a proper understanding behavior in atmosphere crucial formulating accurate climate models. In his Perspective, Rind discusses recent efforts unravel very important complex feedback mechanism.
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Steven R. Schroeder, James P. McGuirk, Widespread tropical atmospheric drying from 1979 to 1995 Geophysical Research Letters. ,vol. 25, pp. 1301- 1304 ,(1998) , 10.1029/98GL01029
Simon J. Evans, Ralf Toumi, John E. Harries, Martyn R. Chipperfield, James M. Russell, Trends in stratospheric humidity and the sensitivity of ozone to these trends Journal of Geophysical Research. ,vol. 103, pp. 8715- 8725 ,(1998) , 10.1029/98JD00265
S. J. Oltmans, D. J. Hofmann, Increase in lower-stratospheric water vapour at a mid-latitude Northern Hemisphere site from 1981 to 1994 Nature. ,vol. 374, pp. 146- 149 ,(1995) , 10.1038/374146A0
Richard S. Lindzen, Some Coolness Concerning Global Warming Bulletin of the American Meteorological Society. ,vol. 71, pp. 288- 299 ,(1990) , 10.1175/1520-0477(1990)071<0288:SCCGW>2.0.CO;2
B.A. Callander, L.G. Meira Filho, John Theodore Houghton, K. Maskell, N. Harris, J.A. Lakeman, A. Katternberg, Climate change 1995 The science of climate change. ,vol. 572, ,(1996)