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9 升温情况下土壤含水量不同时期变化 |
| Fig. 9 Changes of soil water content in different periods under temperature rising ［（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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