数据资源: 中文期刊论文

中国天山玛纳斯河流域积雪垂直分布及其与温度的关系(英文)



编号 zgly0001583998

文献类型 期刊论文

文献题名 中国天山玛纳斯河流域积雪垂直分布及其与温度的关系(英文)

作者 郑文龙  都金康  周小兵  宋明明  卞国栋  谢顺平  冯学智 

作者单位 DepartmentofGeographicInformationScience  NanjingUniversity  JiangsuCenterforCollaborativeInnovationinGeographicalInformationResourceDevelopmentandApplication  DepartmentofGeophysicalEngineering  MontanaTechoftheUniversityofMontan 

母体文献 Journal of Geographical Sciences 

年卷期 2017年04期

年份 2017 

分类号 P426.635 

关键词 snowcover  verticaldistribution  temperatureinversion  ManasiRiver  correlationanalysis 

文摘内容 How snow cover changes in response to climate change at different elevations within a mountainous basin is a less investigated question. In this study we focused on the vertical distribution of snow cover and its relation to elevation and temperature within different elevation zones of distinct climatology, taking the mountainous Manasi River Basin of Xinjiang, Northwest China as a case study. Data sources include MODIS 8-day snow product, MODIS land surface temperature(LST) data from 2001 to 2014, and in situ temperature data observed at three hydrological stations from 2001 to 2012. The results show that:(1) the vertical distribution of snow areal extent(SAE) is sensitive to elevation in low(<2100 m) and high altitude(>3200 m) regions and shows four different seasonal patterns, each pattern is well correspondent to the variation of temperature.(2) The correlation between vertical changes of the SAE and temperature is significant in all seasons except for winter.(3) The correlation between annual changes of the SAE and temperature decreases with increasing elevation, the negative correlation is significant in area below 4000 m.(4) The snow cover days(SCDs) and its long-term change show visible differences in different altitude range.(5) The long-term increasing trend of SCDs and decreasing trend of winter temperature have a strong vertical relation with elevation below 3600 m. The decreasing trend of SCDs is attributed to the increasing trend of summer temperature in the area above 3600 m.

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