Arid
DOI10.1029/2020GL091923
Near-Surface Warming Reduces Dew Frequency in China
Dou, Youjun; Quan, Jiannong; Jia, Xingcan; Wang, Qianqian; Liu, Yangang
通讯作者Quan, JN (corresponding author), Chinese Meteorol Adm, Inst Urban Meteorol, Beijing, Peoples R China. ; Quan, JN ; Liu, YG (corresponding author), Brookhaven Natl Lab, Environm & Climate Sci Dept, Upton, NY 11973 USA.
来源期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2021
卷号48期号:7
英文摘要Long-term (1961-2010) observations of dew data collected at 597 stations over China show that dew frequency decreased by 5.2 days per decade due primarily to near-surface warming and associated decreases in relative humidity (RH). Moreover, the percentage decreasing rate of dew frequency in arid regions (precipitation PR <400 mm yr(-1)) are larger than that in humid regions (PR >= 800 mm yr(-1)). Compared with the 1960s, the mean dew frequency in the 2000s decreased by 28%, 40%, 50% in humid, semihumid (400 <= PR < 800 mm yr(-1)), and arid regions, respectively. Surface warming is larger in arid regions in northwestern China than its humid and semihumid regions during recent global warming, which leads to larger decreases in surface RH and makes dew events less likely. Since dew contributes significantly to surface water balance in arid regions, the large decreases in dew frequency may contribute to the drier getting drier response to global warming over arid regions. Plain Language Summary Here we show, by analyzing 50 years (1961-2010) of data collected at 597 stations in China, that dew occurrence in China exhibits a clear decreasing trend, and the decreasing rate of dew frequency in arid regions is higher than that in semihumid and humid regions. Compared with the 1960s, the mean dew frequency in the 2000s decreased by 28%, 40%, 50% in the humid, semihumid, and arid regions of China, respectively. Further analysis reveals that the decreased dew frequency is caused primarily by near- surface warming and drying. Large decreases in surface relative humidity in arid regions associated with large warming makes dew events less likely. This could make the region drier as dew is a significant water source in arid regions.
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000641974600019
WOS关键词DESERT AMPLIFICATION ; DROUGHT ; DRYLANDS ; CLIMATE ; TRENDS
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/350423
作者单位[Dou, Youjun; Quan, Jiannong; Jia, Xingcan; Wang, Qianqian] Chinese Meteorol Adm, Inst Urban Meteorol, Beijing, Peoples R China; [Quan, Jiannong; Liu, Yangang] Brookhaven Natl Lab, Environm & Climate Sci Dept, Upton, NY 11973 USA
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GB/T 7714
Dou, Youjun,Quan, Jiannong,Jia, Xingcan,et al. Near-Surface Warming Reduces Dew Frequency in China[J],2021,48(7).
APA Dou, Youjun,Quan, Jiannong,Jia, Xingcan,Wang, Qianqian,&Liu, Yangang.(2021).Near-Surface Warming Reduces Dew Frequency in China.GEOPHYSICAL RESEARCH LETTERS,48(7).
MLA Dou, Youjun,et al."Near-Surface Warming Reduces Dew Frequency in China".GEOPHYSICAL RESEARCH LETTERS 48.7(2021).
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