| contributor author | Marsh, Philip | |
| contributor author | Rouse, Wayne R. | |
| contributor author | Woo, Ming-ko | |
| date accessioned | 2017-06-09T13:58:13Z | |
| date available | 2017-06-09T13:58:13Z | |
| date copyright | 1981/06/01 | |
| date issued | 1981 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-10082.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4145160 | |
| description abstract | Recent studies have demonstrated empirical relationships between surface soil moisture and the α? parameter in Priestley and Taylor's version of the combination model. An evaporation study conducted at a high arctic site shows that for gravel and loamy surfaces underlain by permafrost, α? can be expressed as the following function of soil moisture (Sm): α? = 1.26/[exp (5.24 ? 21.56 Sm) + 1] . Comparison with α? and soil moisture relationships obtained in more temperate latitudes suggests that under drying conditions the evaporation rate will be a response to the particular site characteristics, so that there is no unique relationship between surface soil moisture and evaporation rates. | |
| publisher | American Meteorological Society | |
| title | Evaporation at a High Arctic Site | |
| type | Journal Paper | |
| journal volume | 20 | |
| journal issue | 6 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1981)020<0713:EAAHAS>2.0.CO;2 | |
| journal fristpage | 713 | |
| journal lastpage | 716 | |
| tree | Journal of Applied Meteorology:;1981:;volume( 020 ):;issue: 006 | |
| contenttype | Fulltext | |