我国典型海洋型冰川区高海拔区输出水量变化对气候变暖的响应

李宗省; 何元庆; 温煜华; 庞洪喜; 贾文雄; 和献中; 蒲焘

doi:10.3799/dqkx.2010.005

Volume 35 Issue 1

Jan. 2010

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LI Zongxing, HE Yuanqing, WEN Yuhua, PANG Hongxi, JIA Wenxiong, HE Xianzhong, PU Tao, 2010. Response of Runoff in High Altitude Area over the Typical Chinese Monsoonal Temperate Glacial Region to Climate Warming. Earth Science, 35(1): 43-50. doi: 10.3799/dqkx.2010.005

Citation:

LI Zongxing, HE Yuanqing, WEN Yuhua, PANG Hongxi, JIA Wenxiong, HE Xianzhong, PU Tao, 2010. Response of Runoff in High Altitude Area over the Typical Chinese Monsoonal Temperate Glacial Region to Climate Warming. Earth Science, 35(1): 43-50. doi: 10.3799/dqkx.2010.005

Citation:

LI Zongxing, HE Yuanqing, WEN Yuhua, PANG Hongxi, JIA Wenxiong, HE Xianzhong, PU Tao, 2010. Response of Runoff in High Altitude Area over the Typical Chinese Monsoonal Temperate Glacial Region to Climate Warming. Earth Science, 35(1): 43-50. doi: 10.3799/dqkx.2010.005

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Response of Runoff in High Altitude Area over the Typical Chinese Monsoonal Temperate Glacial Region to Climate Warming

doi: 10.3799/dqkx.2010.005

1.
State Key Laboratory of Cryosphere Science, Yulong Snow Mountain Glaciers and Environmental Observation Station, Cold and Arid Region Environment and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
2.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
3.
College of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000, China

Received Date: 2009-05-20
Publish Date: 2010-01-01

Abstract

Abstract

Based on the the hydrological and meteorological data in Lijiang basin, the precipitation, groundwater and runoff in this typical monsoonal temperate glacier area increase significantly, which suggests that water cycle over the region more rapidly under the climate warming. The increase amplitude of runoff in the downstream region of the glaciated area is much stronger than that of precipitation, resulting from the prominent increase of melt water from Mt. Yulong. It indicates that the contribution made by melt water to runoff increase is great under the climate warming, especially in autumn, winter and spring. It is also obvious in Hailuogou basin according to the preliminary analysis of the observational hydrological and meteorological data. The results in this paper are significant to study the glacier variation, water balance and glacier disaster in Chinese monsoonal temperate glacier regions.
- climate warming,
- monsoonal temperate glacier region,
- Mt. Yulong,
- Mt.Gongga,
- runoff

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References(31)

References

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Response of Runoff in High Altitude Area over the Typical Chinese Monsoonal Temperate Glacial Region to Climate Warming

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