Aerosols, Monsoon Rainfall Variability, and Climate Change

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Enhanced surface warming <strong>and</strong> accelerated melting of snowpack in the Himalayas <strong>and</strong> Tibetan Plateau induced by absorbing aerosols William K. M. Lau, Laboratory for Atmospheres NASA/Goddard Space Flight Center Coauthors: K.M. Kim, R. Gautam, C. Hsu, T. Yasunari, M.K. Kim, W. S. Lee
National Geographic
Page 1 and 2: Aerosol, Asian Monsoon and Climate
Page 4 and 5: Global Warming ≠ Climate Change C
Page 6 and 7: Energy demands by types in China co
Page 8 and 9: “……human influences are signi
Page 10 and 11: Definition of aerosol An aerosol is
Page 12 and 13: Microphysics (indirect) effects of
Page 14 and 15: Aerosols have done a lot more than
Page 16 and 17: NASA’s Satellites Taking the Puls
Page 18 and 19: Aerosol-induced anomalies of surfac
Page 20 and 21: Characteristic EHP large scale patt
Page 22 and 23: Climate Change is “a clear and pr
Page 24 and 25: Accelerated melting of Himalaya-Tib
Page 26 and 27: EHP induced heating and moistening
Page 28 and 29: “Snow Darkening Effect”: Black
Page 30 and 31: Estimated “lower limit” of BC d
Page 32 and 33: Building up the case for importance
Page 34 and 35: Back Up
Page 36 and 37: Absorbing aerosols (dust and BC) re
Page 38 and 39: Interannual Variation of Snow Water
Page 40 and 41: Relative percentage change of surfa
Page 44 and 45: AOT of total GOCART aerosols May Ar
Page 46 and 47: The Elevated Heat Pump Hypothesis (
Page 48 and 49: Seasonal mean of snow cover fractio
Page 50 and 51: Generalized glacier Equilibrium Lin
Page 52 and 53: Possible major causes of accelerate
Page 54 and 55: State of Gujar at Western India Wha
Page 56 and 57: MODIS Terra true-color composite Th
Page 58 and 59: EHP associated teleconnection (1987
Page 60 and 61: May/June Difference between 2004 an

Aerosols, Monsoon Rainfall Variability, and Climate Change

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