| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6537991 | Agricultural and Forest Meteorology | 2012 | 9 Pages |
Abstract
⺠Water exchange in a black spruce forest on permafrost was examined over seven years. ⺠Evapotranspiration (E) was supported by soil thawing and snowmelt water. ⺠The presence of ice-rich permafrost helps the accumulation of water in the soil. ⺠Cumulative E did not show noticeable interannual variability. ⺠Whether ice-rich permafrost exists is an important factor for determining the magnitude of the variation in E in boreal forests.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
Hiroki Iwata, Yoshinobu Harazono, Masahito Ueyama,