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滇西北山地末次冰期冰川发育及其基本特征 被引量:13
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作者 张威 刘蓓蓓 《冰川冻土》 CSCD 北大核心 2014年第1期30-37,共8页
对滇西北海拔4000~4500m山地的第四纪冰川发育和平衡线高度进行了研究.结果表明:古冰川发育主要依托海拔4000~4300m的夷平面,早中期发育小型的冰帽以及流入四周谷地的山谷冰川,晚期主要发育规模较小的冰斗冰川.冰川主要发育期为... 对滇西北海拔4000~4500m山地的第四纪冰川发育和平衡线高度进行了研究.结果表明:古冰川发育主要依托海拔4000~4300m的夷平面,早中期发育小型的冰帽以及流入四周谷地的山谷冰川,晚期主要发育规模较小的冰斗冰川.冰川主要发育期为末次冰期,古冰川平衡线、山体最高峰以及夷平面的高度显示,冰川发育所依托的夷平面在末次冰期时超过古平衡线,二者差值为50~400m,为冰川发生提供了良好的地形与地势条件.冰川规模演化表明,滇西北地区多处山地MIS3中期的冰川规模大于末次冰盛期(LGM),可能与MIS3中期较强南亚季风带来较丰富的降水有关.古气候研究资料以及研究区的冰期系列表明,滇西北海拔4000—4500m山地末次冰期的冰川作用是构造和气候相耦合的结果. 展开更多
关键词 末次冰期 构造运动 冰川规模 平衡线 滇西北
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Glacier extent changes and possible causes in the Hala Lake Basin of Qinghai-Tibet Plateau 被引量:5
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作者 LI Dong-Sheng CUI Bu-Li +2 位作者 WANG Ying XIAO Bei JIANG Bao-Fu 《Journal of Mountain Science》 SCIE CSCD 2019年第7期1571-1583,共13页
Glacier is a common sensitivity indicator of environmental and global climate change.Examining the relationship between glacier area and climate change will help reveal glacier change mechanisms and future trends.Glac... Glacier is a common sensitivity indicator of environmental and global climate change.Examining the relationship between glacier area and climate change will help reveal glacier change mechanisms and future trends.Glacier changes are also of great significance to the regulation of regional water resources.This study selected the Hala Lake Basin in the northeastern Qinhai-Tibet Plateau as a study area,and examined the relationships between the temporal and spatial change of glaciers in the northeastern Qinghai-Tibet Plateau and climate change based on remote sensing imagery,climatological data,and topographic data during the past 30 years.Results showed that glacier area in the Hala Lake basin fluctuated and decreased from106.24 km2 in 1986 to 78.84 km2 in 2015,with a decreasing rate of 0.94 km2·yr-1.The number of glacier patches,mean patch area,and largest patch index all decreased from 1986 to 2015,while the splitting index increased from 1986 to 2015,indicating that the landscape fragmentation of glacier in the Hala Lake Basin was increasing significantly during the study period.Glacier area change was mainly concentrated in the slopes>25°with an altitude of 4500-5000 m,and the retreating rate of glacier of sunny slope was obviously higher than that of shady slope.Geometric center of glacier in the basin moved from southwest to northeast towards high altitude.Results of the response of glacier extent to climate change showed that temperature was the dominant factor affecting glacier area dynamic change in the Hala Lake Basin.It is predicted that in future several years,the glacier area will decrease and fragment continually as a result of global warming on the Tibetan Plateau. 展开更多
关键词 glacier extent Climate change Hala LAKE Basin Qinghai-Tibet PLATEAU
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