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Published byHenry Joseph Modified over 9 years ago
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Surface Water Balance (1)
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Review of last lecture: Surface energy balance dT/dt SWdn =Scos SWup =SWdn LWdn = Tair 4 LWup = Ts 4 LH= C d LV(q surface - q air ) SH= C d C p V(T surface - T air ) Fc = - dT/dz Incoming shortwave + Incoming longwave = Reflected shortwave + Emitted longwave + Latent heat flux + Sensible heat flux + Subsurface conduction What is sensible heat flux? What is latent heat flux? Bowen ratio B= SH/LH = C p (T surface - T air ) / L(q surface - q air ) provides a simple way for estimating SH and LH when the net radiative flux Fr is available LH=Fr/(B+1), SH=Fr B/(B+1) Factors affecting soil thermal conductivity Other heat sources: precipitation, biochemical, anthropogenic
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The global water cycle
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Components of global water cycle Ocean water Land soil moisture, rivers, snow cover, ice sheet and glaciers Sea ice Atmosphere water vapor, clouds, precipitation Water in biosphere (including human beings)
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Component I: Ocean Covers 70% of the Earth’s surface
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Observed Changes in Global Sea Level
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Observed Changes in Sea Level Largest in the western part of ocean basin
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Observed Changes in Ocean Heat Content
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Component II: Land Soil moisture
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Component II: Land >1000 major rivers flow on the seven continents Amazon river (#1)Yangtze river (#4)Mississippi river (#6)
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Component II: Land Snow cover
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Observed Changes in Snow Cover: Significant melting
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Component II: Land Ice sheet
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Retreat of Greenland Ice Sheet – a huge contributor to sea level rise today Greenland is responsible for about 10% of the observed global sea level rise and accelerating. Greenland holds 7 m of sea level equivalent.
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Component II: Land Glaciers
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Retreat of Mountain Glaciers: a major contributor to sea level rise IPCC (2001) Glacier retreat is a world-wide phenomena. Will affect water supply for millions: Kenya/Tanzania Northern India Andes Mountains
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Melting in Glacier National Park
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Component III: Sea ice
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Observed Changes in Arctic Sea Ice: Significant melting
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Reduced Arctic sea ice: A result of warming that leads to more warming
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Component IV: Atmosphere Water vapor flows in the atmosphere
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Observed Changes in Water Vapor Significant increase
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Component IV: Atmosphere Clouds drifts with the winds
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Component IV: Atmosphere Precipitation drives many atmospheric circulations which in turn transport water around the world Hadley Circulation Monsoons Walker Circulation
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Observed Changes in Precipitation: Significant change in many places
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A significant fraction of the human body is water (~75%) The remaining: fat, protein, carbonhydrate, other solids
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So the water in our bodies may come from … A stream in the Niagara Fall … A white cloud over the tropical Pacific … A raindrop in the Amazon rainforest … Therefore we need to protect the environment because any pollution we put into the environment may someday come back into our bodies An ice sheet in the Arctic Ocean…
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Summary: Components of global water cycle Ocean water Land soil moisture, rivers, snow cover, ice sheet and glaciers Sea ice Atmosphere water vapor, clouds, precipitation Water in biosphere (including human beings)
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