HR: 17:00h
AN: H34D-05    [Abstracts]
TI: Pan Evaporation Measurements to Estimate Actual Evaporation
AU: * Szilagyi, J
EM: jszilagyi1@unl.edu
AF: Budapest University of Technology and Economics, Muegyetem Rkp. 3, Budapest, H-1111, Hungary
AU: * Szilagyi, J
EM: jszilagyi1@unl.edu
AF: University of Nebraska-Lincoln, 625 Hardin Hall, Lincoln, NE 68583, United States
AB: Pan evaporation as a form of apparent potential evaporation (PEA) can be employed to infer actual evaporation (E). With PEA measurements the Complementary Relationship of evaporation becomes asymmetric, the degree of which can be estimated as a simple function of the air temperature. An extended and modified version of the Advection-Aridity (AA) model is formulated to estimate E either from PEA or true potential evaporation measures. New findings explain important features of the Morton model and show that the modified AA model improves upon Morton's evaporation estimates.
DE: 1218 Mass balance (0762, 1223, 1631, 1836, 1843, 3010, 3322, 4532)
DE: 1818 Evapotranspiration
DE: 1840 Hydrometeorology
SC: Hydrology [H]
MN: 2007 Fall Meeting