青藏高原多年冻土区不同海拔土壤含水量对气候变化的响应
Response of soil water content at different altitudes to climate change in the permafrost region of the Qinghai-Tibet Plateau： an ELM model analysis
青藏高原多年冻土区不同海拔土壤含水量对气候变化的响应 |
| 张方园, 常娟, 刘健, 孙文军 |
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Response of soil water content at different altitudes to climate change in the permafrost region of the Qinghai-Tibet Plateau： an ELM model analysis |
| Fangyuan ZHANG, Juan CHANG, Jian LIU, Wenjun SUN |
| 图8 土壤含水量对气温升高的响应 |
| Fig. 8 Response of soil water content to temperature increase ［（a）， （c） and （e） represent the response process of soil water content to temperature at depths of 20 cm， 40 cm， and 65 cm on the upper slope， respectively； （b）， （d） and （f） represent the response process of soil water content to temperature at depths of 20 cm， 40 cm， and 65 cm on the downhill slope， respectively］ |
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