Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1007/s00704-018-2655-6 |
Decadal decline of summer precipitation fraction observed in the field and from TRMM satellite data across the Mongolian Plateau | |
Qin, Fuying1,2; Jia, Gensuo3; Yang, Jie1; Na, Yintai4; Bao, Yuhai2 | |
通讯作者 | Jia, Gensuo |
来源期刊 | THEORETICAL AND APPLIED CLIMATOLOGY |
ISSN | 0177-798X |
EISSN | 1434-4483 |
出版年 | 2019 |
卷号 | 137期号:1-2页码:1105-1115 |
英文摘要 | Shifts in precipitation regimes have been given increased attention along with climate trends in the arid and semiarid Mongolian Plateau (MP), because precipitation is the dominant factor that controls vegetation growth and land-use practices in the region. However, the temporal variability and spatial heterogeneity of decadal trends in summer precipitation fraction have not been well understood. In this study, the temporal variability and spatial heterogeneity of annual and summer precipitation change were investigated with the major focus on the summer precipitation fraction across the entire MP, using monthly precipitation data from 141 meteorological stations and the Tropical Rainfall Measuring Mission (TRMM) precipitation data. The Mann-Kendall trend test, Sen's regression, and Spatial Analyst methods were used for time series analysis. Results show that the regional summer precipitation fraction declined significantly at a rate of -1.0%/decade (p<0.05) during 1961-2010, which was supported by TRMM satellite data with a rate of -2.86%/decade over 1998-2016. Interestingly, rates of decrease in the summer precipitation fraction varied by ecoregion. Spatially, trend in summer precipitation fraction was very heterogeneous, with significant decreasing trends in the eastern typical steppe and southeastern agro-pastoral ecotone, but increasing trends in the southwestern desert and Gobi desert region. In conclusion, the summer precipitation fraction declined because of the asymmetric decreasing or increasing rates in summer and non-summer precipitation during both 1961-2010 and 1998-2010. This implies a major shift of precipitation regime in the region. This is likely driven by decadal changes of the East Asia monsoon system. |
英文关键词 | Precipitation Climate change Mongolian Plateau Satellite Seasonal fraction Monsoon |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China ; Japan |
收录类别 | SCI-E |
WOS记录号 | WOS:000475737500075 |
WOS关键词 | INNER-MONGOLIA ; CLIMATE-CHANGE ; SOIL-MOISTURE ; TRENDS ; VARIABILITY ; MONSOON ; CHINA ; TEMPERATURE ; DROUGHT ; ASIA |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源机构 | 中国科学院大气物理研究所 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/219096 |
作者单位 | 1.Inner Mongolia Univ, Sch Ecol & Environm, Hohhot 010021, Peoples R China; 2.Inner Mongolia Normal Univ, Coll Geog Sci, Hohhot 010022, Peoples R China; 3.Chinese Acad Sci, Inst Atmospher Phys, Key Lab Reg Climate Environm Temperate East Asia, Beijing 100029, Peoples R China; 4.Rakuno Gakuen Univ, Grad Sch Dairy Sci, Ebetsu, Hokkaido 0698501, Japan |
推荐引用方式 GB/T 7714 | Qin, Fuying,Jia, Gensuo,Yang, Jie,et al. Decadal decline of summer precipitation fraction observed in the field and from TRMM satellite data across the Mongolian Plateau[J]. 中国科学院大气物理研究所,2019,137(1-2):1105-1115. |
APA | Qin, Fuying,Jia, Gensuo,Yang, Jie,Na, Yintai,&Bao, Yuhai.(2019).Decadal decline of summer precipitation fraction observed in the field and from TRMM satellite data across the Mongolian Plateau.THEORETICAL AND APPLIED CLIMATOLOGY,137(1-2),1105-1115. |
MLA | Qin, Fuying,et al."Decadal decline of summer precipitation fraction observed in the field and from TRMM satellite data across the Mongolian Plateau".THEORETICAL AND APPLIED CLIMATOLOGY 137.1-2(2019):1105-1115. |
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