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7 二输入变量ELM模型模拟后14天模拟土壤含水量动态变化 |
| Fig. 7 Dynamic change process of soil water content after 14 days simulated by ELM model with two input variables ［（a）， （c） and （e） represent the changes in soil water content at depths of 20 cm， 40 cm， and 65 cm on the upper slope， respectively；（b）， （d） and （f） represent the changes in soil water content at depths of 20 cm， 40 cm， and 65 cm on the downhill slope， respectively］ |
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