Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1029/2018JD029798 |
An Examination of Temperature Trends at High Elevations Across the Tibetan Plateau: The Use of MODIS LST to Understand Patterns of Elevation-Dependent Warming | |
Pepin, Nick1,2; Deng, Haijun3,4; Zhang, Hongbo2; Zhang, Fan2,5; Kang, Shichang5,6,7; Yao, Tandong2,5 | |
2019-06-16 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
![]() |
ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2019 |
卷号 | 124期号:11页码:5738-5756 |
文章类型 | Article |
语种 | 英语 |
国家 | England; Peoples R China |
英文摘要 | Research has revealed systematic changes in warming rates with elevation (EDW) in mountain regions. However, weather stations on the Tibetan plateau are mostly located at lower elevations (3,000-4,000 m) and are nonexistent above 5,000 m, leaving critical temperature changes unknown. Satellite LST (Land Surface Temperature) can fill this gap but needs calibrating against in situ air temperatures (T-air). We develop a novel statistical model to convert LST to T-air, developed at 87 high-elevation Chinese Meteorological Administration stations. T-air (daily maximum/minimum temperatures) is compared with Moderate Resolution Imaging Spectroradiometer (MODIS) Aqua LST (1330 and 0130 local time) for 8-day composites during 2002-2017. Typically, 80-95% of the difference between LST and T-air (Delta T) is explained using predictors including LST diurnal range, morning heating/nighttime cooling rates, the number of cloud free days/nights, and season (solar angle). LST is corrected to more closely represent T-air by subtracting modeled Delta T. We validate the model using an AWS on Zhadang Glacier (5800 m). Trend analysis at the 87 stations (2002-2017) shows corrected LST trends to be similar to original T-air trends. To examine regional contrasts in EDW patterns, elevation profiles of corrected LST trends are derived for three ranges (Qilian Mountains, NyenchenTanglha, and Himalaya). There is limited EDW in the Qilian mountains. Maximum warming is observed around 4,500-5,500 m in NyenchenTanglha, consistent with snowline retreat. In common with other studies, there is stabilization of warming at very high elevations in the Himalaya, including absolute cooling above 6,000 m, but data there are compromised by frequent cloud. |
英文关键词 | land surface temperature elevation-dependent-warming mountain climate temperature trends Tibetan Plateau |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000477718400003 |
WOS关键词 | LAND-SURFACE TEMPERATURE ; AIR-TEMPERATURE ; VARIABILITY ; SNOW ; MOUNTAINS ; WINTER ; SKIN |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/184122 |
专题 | 气候变化 |
作者单位 | 1.Univ Portsmouth, Dept Geog, Portsmouth, Hants, England; 2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China; 3.Fujian Normal Univ, Sch Geog Sci, Fujian Prov Engn Res Ctr Monitoring & Assessing T, Fuzhou, Fujian, Peoples R China; 4.Fujian Normal Univ, Sch Geog Sci, Fuzhou, Fujian, Peoples R China; 5.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China; 6.Chinese Acad Sci, State Key Lab Cryospher Sci, Northwest Inst Ecoenvironm & Resources, Lanzhou, Gansu, Peoples R China; 7.Univ Chinese Acad Sci, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Pepin, Nick,Deng, Haijun,Zhang, Hongbo,et al. An Examination of Temperature Trends at High Elevations Across the Tibetan Plateau: The Use of MODIS LST to Understand Patterns of Elevation-Dependent Warming[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2019,124(11):5738-5756. |
APA | Pepin, Nick,Deng, Haijun,Zhang, Hongbo,Zhang, Fan,Kang, Shichang,&Yao, Tandong.(2019).An Examination of Temperature Trends at High Elevations Across the Tibetan Plateau: The Use of MODIS LST to Understand Patterns of Elevation-Dependent Warming.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,124(11),5738-5756. |
MLA | Pepin, Nick,et al."An Examination of Temperature Trends at High Elevations Across the Tibetan Plateau: The Use of MODIS LST to Understand Patterns of Elevation-Dependent Warming".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 124.11(2019):5738-5756. |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论