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Published byCameron Barton Modified over 9 years ago
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Water Cycle 1.Formulation of the hydrological cycle 2.Equations of Hydrology 3.Observations
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Formulation of the hydrological cycle
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Global water content 13.1x10 15 kg (~2.5cm) Annual mean precipitation ~1m Overturning ~40 times/year (9 days)
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Equations of Hydrology S=P-E-R 0 -R u S- rate of storage of water P- precipitation rate (liquid and solid phase) E- evaporation rate R 0 - surface runoff R u -subterranean runoff -time-averaging,-space-averaging For large areasis small, thus accurately measured semiempiric estimates
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Runoff
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Balance Equations for Water Wapor -amount of precipitable water [g/m 2 ] -areal runoff, -equation for the atmospheric branch of the hydrological cycle couples land and atmospheric branches, thus Globally E=P -transport trough one parallel -vertical transport
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Water Wapor in the Atmosphere (Horizontal patterns)
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Water Wapor in the Atmosphere (Vertical patterns) More than 50 percent of the water vapor is below 850mb (90 percent below 500mb)
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NH: Summer-Winter 1.2cm water SH: Summer-Winter 0.7cm water Global mean water content 2.5cm
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Transport of Water Vapor
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Aerial Runoff
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