Actual evapotranspirtion estimation in the upper reaches of the Jinghe River basin with the Advection-Aridity model

DOI

10.2991/ifeesm-15.2015.195How to use a DOI?

Keywords

Evapotranspiration; Complementary Relationship; AA model; the Jinghe River

Abstract

Evapotranspiration is the largest component of water loss from storage and has a major influence on all hydrological processes. Based on meteological and hydrological in the upper reaches of the Jinghe River basin, Advection-Aridity model was applied to estimate the actual evapotranspiration from 1966 to 2012. The results showed that the average annual actual evapotranspiration is 529.4 mm in the study area, and the variation of actual evapotranspiration was described as four phases. Model calculation results can reflect the regional evapotranspiration loss and provide the basis for the regional soil moisture and green water analysis.

Copyright

© 2015, the Authors. Published by Atlantis Press.

Open Access

This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

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TY  - CONF
AU  - S.z. Dang
AU  - G.t. Dong
AU  - F.r. Zhang
AU  - K. Du
PY  - 2015/09
DA  - 2015/09
TI  - Actual evapotranspirtion estimation in the upper reaches of the Jinghe River basin with the Advection-Aridity model
BT  - Proceedings of the 2015 International Forum on Energy, Environment Science and Materials
PB  - Atlantis Press
SP  - 1055
EP  - 1060
SN  - 2352-5401
UR  - https://doi.org/10.2991/ifeesm-15.2015.195
DO  - 10.2991/ifeesm-15.2015.195
ID  - Dang2015/09
ER  -