Research output: Contribution to journal › Article › peer-review
Estimation is made of the summer moisture content in the 1 m soil layer and the annual runoff under the global warming to 1° and 2°C. Calculations are based on a comprehensive method of determination of evaporation from the land surface and on analyzing paleoclimatic data for two past warm periods: 1) the Holocene optimum with the mean global air temperature higher by 1°C than the present one; and 2) the Mikulinsky interglacial epoch when the mean global air temperature was higher by 2°C. -English summary
Original language | Russian |
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Pages (from-to) | 5-10 |
Number of pages | 6 |
Journal | Meteorologiya i Gidrologiya |
Volume | 3 |
State | Published - 1 Jan 1990 |
ID: 52206864