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Atlas 2m thermal infrared image, Atlanta, GA. Units: kW/m 2 /day Source: R. L. Sass, Rice Univ., Houston, TX http://www.ruf.rice.edu/~sass/UHI.html. Atmospheric Moisture. Environmental Significance of Water. Important component of global energy fluxes (latent heat)
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Units: kW/m2/day Source: R. L. Sass, Rice Univ., Houston, TX http://www.ruf.rice.edu/~sass/UHI.html
Environmental Significance of Water • Important component of global energy fluxes (latent heat) • Powerful agent of erosion • Universal solvent – transports nutrients and contaminants • Required for biological processes – availability determines species distributions
Outline • Hydrologic cycle (water balance) • Atmospheric moisture (precipitation) • Clouds and implications for climate change
Water Balance Describes the relationship among fluxes of water Land surface Oceans Precipitation Input Input Evaporation Transpiration Output -- Output Runoff Output Input Land: Precipitation = Runoff + Evapotranspiration Oceans: Precipitation + Runoff = Evaporation
Water Balance Describes the relationship among fluxes of water Land surface Precipitation Input Evaporation Transpiration Output Runoff Output Land: Precipitation - Evapotranspiration = Runoff
Atmospheric Moisture Amount of moisture held in air depends upon air temperature 26 g/kg 15 g/kg 2 g/kg
Dew point temperature Atmospheric Moisture http://www.weather.com Dew point temperature: Temperature of an air mass at which it is saturated with moisture
Atmospheric Moisture http://www.weather.com Relative humidity: Amount of water vapor currently in air relative to what air could hold at that temperature if saturated If air on 70o F day held 5 g/kg water, RH = 5/15 = 33%
Atmospheric Moisture Who cares?
Atmospheric Moisture As air rises, it cools. Cooler air holds less mositure Adiabatic Cooling
Atmospheric Lifting Mechanisms Convection – local heating
Atmospheric Lifting Mechanisms Orographic Lifting – topographic barriers
Atmospheric Lifting Mechanisms Frontal Lifting – cold / warm air masses
Atmospheric Lifting Mechanisms Convergence – high / low pressure gradients
Clouds Cloud form • Stratiform - horizontal • Cumuliform - vertical • Cirroform – wispy, ice crystals
Role of Clouds in Global Climate System http://www.giss.nasa.gov/research/briefs/delgenio_03/
High clouds – Less reflective, absorb longwave radiation Role of Clouds in Global Climate System Low clouds – reflect shortwave radiation
Global albedo with clouds Role of Clouds in Global Climate System Global albedo without clouds Source: E. F. Harrisson et al., http://eumetcal.meteo.fr/euromet/english/satmet/s8220/s8220210.htm
Diurnal (day-night) variations in longwave radiation Role of Clouds in Global Climate System Global longwave radiation Source: Eugene S. Takle, 2006 http://www.meteor.iastate.edu/gccourse/influ/influ_lecture_new.html
Implications of clouds for climate change • Surface warming may induce more cloud formation • Clouds reduce incoming shortwave (albedo) • Clouds increase counterradiated longwave (greenhouse gas) • Clouds introduce considerable uncertainty to climate change scenarios
Summary • Hydrologic cycle describes processes controlling fluxes of water • Water balance used to describe relationship between precipitation, runoff and evaporation/transpiration • Moisture content of air is temperature dependent (warmer air holds more moisture) • Air must be cooled for precipitation to occur (atmospheric lifting mechanisms)
Summary (cont.) • Atmospheric lifting creates clouds. • Clouds have varying effects on net radiation • Effects of climate change on cloud formation introduces considerable uncertainty into predictions