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Estimation of Regional Evapotranspiration Using Remotely Sensed Land Surface Temperature. Part 2: Application of Equilibrium Evaporation Model to Estimate Evapotranspiration by Remote Sensing Technique. [Japan
| Content Provider | Semantic Scholar |
|---|---|
| Author | Kotoda, Kazuo Nakagawa, Shinsuke Yoshino, Masatoshi M. Takeda, Kaoru Seki, Kazuhisa |
| Copyright Year | 1985 |
| Abstract | In order to study the distribution of evapotranspiration in the humid region through the remote sensing technology, first, in the Part I of this paper, the parameter (o0 in the Priestley-Taylor model was determined. The daily means of the parameter ot= 1.14 can be available from summer to autumn and u= 1.5-2.0 in winter. Secondly, in Part II of the present paper, the results of the satellite and the airborne sensing done on 21st and 22nd January, 1983, were described. Using the vegetation distribution in the Tsukuba Academic New town, the radiation temperature obtained by the remote sensing and the radiation data observed at the ground surface, the evapotranspiration was calculated for each vegetation type by the Priestley-Taylor method. The daily mean evapotranspiration on 22nd January, 1983, was approximately 0.4 mm/day. The differences of evapotranspiration between the vegetation types were not detectable, because the magnitude of evapotranspiration is very little in winter. PARTI Measurementof Evapotranspirationat the Environmental ResearchCenter, Universityof Tsukuba |
| File Format | PDF HTM / HTML |
| Alternate Webpage(s) | https://ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/19850014922.pdf |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |
