Abstract
The estimation of evapotranspiration (E) in forested areas is required for various practical purposes (e.g. evaluation of drought risks) in Japan. This study developed a model that estimates monthly forest E in Japan with the input of monthly temperature (T). The model is based on the assumptions that E equals the equilibrium evaporation rate (Eeq) and that Eeq is approximated by a function of T. The model formulates E as E (mm month-1) = 3.48 T (°C) + 32.3. The accuracy of the model was examined using monthly E data derived using short-term water balance (WB) and micrometeorological (M) methods for 15 forest sites in Japan. The model estimated monthly E more accurately than did the Thornthwaite and Hamon equations according to regression analysis of the estimated E and E derived using the WB and M methods. Although the model tended to overestimate monthly E, the overestimation could be reduced by considering the effect of precipitation on E. As T data are commonly available all over Japan, the model would be a useful tool to estimate forest E in Japan.
Original language | English |
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Pages (from-to) | 1896-1911 |
Number of pages | 16 |
Journal | Hydrological Processes |
Volume | 24 |
Issue number | 13 |
DOIs | |
Publication status | Published - Jun 1 2010 |
All Science Journal Classification (ASJC) codes
- Water Science and Technology