Arid
DOI10.1109/JSTARS.2018.2857827
Spatiotemporal Distributions of Cloud Parameters and the Temperature Response Over the Mongolian Plateau During 2006-2015 Based on MODIS Data
Bao, Shanhu1; Letu, Husi2; Zhao, Chuanfeng3,4; Tana, Gegen3,4; Shang, Huazhe2; Wang, Tianxing2; Lige, Bi5; Bao, Yuhai1; Purevjav, Gomboluudev6; He, Jie2; Zhao, Jun7
通讯作者Tana, Gegen ; Zhao, Jun
来源期刊IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING
ISSN1939-1404
EISSN2151-1535
出版年2019
卷号12期号:2页码:549-558
英文摘要The Mongolian Plateau (MP) has important influences on regional and global climate change. The spatiotemporal variations in the cloud cover and cloud optical thickness of total, high, middle, and low clouds over the MP during the daytime from 2006 to 2015 are analyzed using MODIS level 2 atmospheric data. Results show that the annual average total cloud cover over the MP decreases from the forest area in the northeast to the desert area in the southwest. The total cloud cover over the MP is obviously higher in summer than in other seasons, in which high clouds have a largest proportion, with the substantial total cloud cover changes. The spatial distributions of the high, middle, and low cloud covers over the MP are highly variable. The cooling effect of the cloud net radiative forcing is greater during the daytime in summer than in other seasons, which is likely associated with thick cloud optical thickness or large cloud cover in summer. Combined with the analyses of relationships among cloud cover, cloud optical thickness, cloud radiative forcing, and air temperature, the results show that significantly negative correlations exist between cloud optical thickness and cloud radiative forcing, and between total cloud cover and air temperature in the MP. The decrease in air temperature in summer over the MP during daytime confirm that the increase in the daytime total cloud cover strengthen the cooling effects of clouds and decrease the air temperature, especially in the high-value area with cloud cover distribution over the northeast MP.
英文关键词Air temperature cloud classification cloud cover cloud radiative forcing Mongolian Plateau (MP)
类型Article
语种英语
国家Peoples R China ; Mongolia
收录类别SCI-E
WOS记录号WOS:000460663600014
WOS关键词TIBETAN PLATEAU ; TEMPORAL INTERPOLATION ; CLIMATE ; PERSPECTIVE ; RETRIEVAL ; MISSION ; SYSTEM ; TRENDS ; IMPACT ; TERRA
WOS类目Engineering, Electrical & Electronic ; Geography, Physical ; Remote Sensing ; Imaging Science & Photographic Technology
WOS研究方向Engineering ; Physical Geography ; Remote Sensing ; Imaging Science & Photographic Technology
来源机构北京师范大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/216247
作者单位1.Inner Mongolia Normal Univ, Coll Geog Sci, Hohhot 010022, Peoples R China;
2.Chinese Acad Sci, Inst Remote Sensing & Digital Earth RADI, Beijing 100094, Peoples R China;
3.Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China;
4.Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China;
5.Meteorol Sci Inst Inner Mongolia, Hohhot 010051, Peoples R China;
6.Inst Meteorol Hydrol & Environm, Res Div Climate Change & Resource, Ulaanbaatar 15160, Mongolia;
7.Northwest Normal Univ, Coll Geog & Environm Sci, Lanzhou 730070, Gansu, Peoples R China
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GB/T 7714
Bao, Shanhu,Letu, Husi,Zhao, Chuanfeng,et al. Spatiotemporal Distributions of Cloud Parameters and the Temperature Response Over the Mongolian Plateau During 2006-2015 Based on MODIS Data[J]. 北京师范大学,2019,12(2):549-558.
APA Bao, Shanhu.,Letu, Husi.,Zhao, Chuanfeng.,Tana, Gegen.,Shang, Huazhe.,...&Zhao, Jun.(2019).Spatiotemporal Distributions of Cloud Parameters and the Temperature Response Over the Mongolian Plateau During 2006-2015 Based on MODIS Data.IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING,12(2),549-558.
MLA Bao, Shanhu,et al."Spatiotemporal Distributions of Cloud Parameters and the Temperature Response Over the Mongolian Plateau During 2006-2015 Based on MODIS Data".IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING 12.2(2019):549-558.
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