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The importance of clouds
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http://www.dkrz.de/dkrz/broschuere-eng/research/climatesystem.html The Global Climate System http://www.lwr.kth.se/Grundutbildning/1B1292/Compendium_online/ch05s01s02.html
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Radiation in the climate system Kiehl and Trenberth, BAMS, 1997
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Net cloud radiative effect from ERBE -90 -70 -50 -40 -30 -20 -10 0 10 20 30 40
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Combined satellite rainfall measurements Reflects locations of major precipitating cloud systems spatiotemporal variability Latent Heating
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http://www.dkrz.de/dkrz/broschuere-eng/research/water.html The Global Hydrological Cycle
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From global to local – range of scales 1000 km 100 km 10 km 1 km
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Impact of cloud type upon radiation
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Distribution of cloud types Tropical East Pacific Anvils Mid-level High Low Deep convection Stratocumulus
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Radiative effect of cloud types Mid-level High Low
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Factors influencing cloud types
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ERBE net cloud forcing SST anomaly from zonal mean
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ISCCP inferred St/Sc amount
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Tropical- subtropical general circulation from Randall et al., J. Atmos. Sci., 37, 125-130, 1980 cold SST warm SST
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Seasonal cycle of precipitation Jan 2004 Jul 2004
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Interannual variability of precipitation Jan 1998 Jan 1999 El Niño La Niña
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Global frequency and distribution of lightning as observed from space Christian et al., J. Geophys. Res., 2003.
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Tight couplings between SST, winds, and clouds
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Clouds and precipitation associated with midlatitude cyclones warm conveyor
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Orographic precipitation enhancement
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Clouds and climate change
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Clouds in climate models - change in low cloud amount for 2 CO 2 from Stephens (2005) GFDL CCM model number
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IPCC, 2007
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Pacific Northwest Projected River Flow
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Cloud effects on atmospheric chemistry Acidity of rain Gas-particle conversion Biogeochemical feedbacks to tropical cloud pattern
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Hobbs 2000
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Modeling clouds and precipitation Forecasting of precipitation Climate impacts
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From the sublime…. 10x10x5 m resolution 20x20x3 km domain Stevens et al. (2002)
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….to the ridiculous, but necessary 3x3 o resolution global domain climateprediction.net
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Hobbs 2000 O 3 photolyzed OH
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