Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1029/2020GL091923 |
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
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ISSN | 0094-8276 |
EISSN | 1944-8007 |
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 |
推荐引用方式 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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