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Seasonal variability of the complementary relationship in the Asian monsoon region
complementary relationship seasonal variability wet environment evaporation Priestley–Taylor equation fl ux measurement
2013/7/25
The complementary relationship (CR) between potential evaporation (LEp) and actual evaporation (LE) is widely used to explainthe evaporation paradox and to estimate LE, in which wet environment evapor...
Variability of complementary relationship and its mechanism on different time scales
complementary relationship temporal scales wet environment evapotranspiration Priestley-Taylor equation state space
2013/7/25
In the complementary relationship (CR) between actual and potential evapotranspiration, wet environment evapotranspiration (Ew) is usually calculatedusing the Priestley-Taylor (P-T) equation. Based on...
Interpreting the complementary relationship in non-humid environments based on the Budyko and Penman hypotheses
the complementary relationship non-humid environments
2013/7/25
The Budyko, Bouchet, and Penman hypothesestogether describe, using different formulae, the tightconnections and feedbacks between water – energy
balances and the landscape. The discrepancy between th...