Actual evapotranspirtion estimation in the upper reaches of the Jinghe River basin with the Advection-Aridity model
S.z. Dang, G.t. Dong, F.r. Zhang, K. Du
Available Online September 2015.
- https://doi.org/10.2991/ifeesm-15.2015.195How to use a DOI?
- Evapotranspiration; Complementary Relationship; AA model; the Jinghe River
- 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.
- Open Access
- This is an open access article distributed under the CC BY-NC license.
Cite this article
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 - https://doi.org/10.2991/ifeesm-15.2015.195 ID - Dang2015/09 ER -