Bulletin of the American Meteorological Society, Volumen80American Meteorological Society., 1999 Vols. for 1990- contain supplemental membership directory. |
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Página 2232
... optical thickness from a 12 - yr time series of aerosol optical thickness obtained using a Meteosat one - channel algorithm . Reflection Function ( 0.61 μm ) Reflection Function ( 0.61 μm ) 0.4 0.3 8 = 60 ° = 0 ° w = 0.96 0.4 0.2 0.1 ...
... optical thickness from a 12 - yr time series of aerosol optical thickness obtained using a Meteosat one - channel algorithm . Reflection Function ( 0.61 μm ) Reflection Function ( 0.61 μm ) 0.4 0.3 8 = 60 ° = 0 ° w = 0.96 0.4 0.2 0.1 ...
Página 2249
American Meteorological Society. FIG . 8. ( a ) Aerosol optical thickness ( 0.63 μm ) from AVHRR data and ( b ) TOMS data ( 0.38 μm ) in Apr 1997 . FIG . 9. First false - color images ( 10. scribed in Eq . ( 9 ) . Figure 8b a shows the ...
American Meteorological Society. FIG . 8. ( a ) Aerosol optical thickness ( 0.63 μm ) from AVHRR data and ( b ) TOMS data ( 0.38 μm ) in Apr 1997 . FIG . 9. First false - color images ( 10. scribed in Eq . ( 9 ) . Figure 8b a shows the ...
Página 2277
... optical thicknesses in this one . The optical thickness maximum is more pro- ounced in a zonal monthly mean . The midlatitude torm tracks do not produce very distinctive cloud roperty extremes in the annual mean . Table 5 summa- izes ...
... optical thicknesses in this one . The optical thickness maximum is more pro- ounced in a zonal monthly mean . The midlatitude torm tracks do not produce very distinctive cloud roperty extremes in the annual mean . Table 5 summa- izes ...
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