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10 降水增加情况下不同时期土壤含水量平均值变化 |
| Fig. 10 Changes of average soil water content in different periods under precipitation increasing ［（a）， （c） and （e） represent the response results of soil water content to precipitation at depths of 20 cm， 40 cm， and 65 cm on the upper slope， respectively； （b）， （d） and （f） represent the response results of soil water content to precipitation at depths of 20 cm， 40 cm， and 65 cm on the downhill slope， respectively］ |
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