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DOI | 10.1007/s00382-020-05422-z |
Ground observed climatology and trend in snow cover phenology across China with consideration of snow-free breaks | |
Ma, Ning; Yu, Kunlun; Zhang, Yinsheng; Zhai, Jianqing; Zhang, Yongqiang; Zhang, Hongbo | |
通讯作者 | Ma, N (通讯作者) |
发表日期 | 2020 |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
起始页码 | 2867 |
结束页码 | 2887 |
卷号 | 55期号:9-10 |
英文摘要 | Accurate understanding of snow cover phenology and its changes is important to hydrological processes and climate system. Having recognized the potential uncertainties in remote sensing snow cover products, we used daily snow depth observations from 514 meteorological stations across China to investigate the spatiotemporal variations in snow cover phenology during 1970-2014. Climatologically, the snow cover onset date (D-o) and end date (D-e) as well as the number of snow cover days (D-s) depended on latitude at most stations outside of the Tibetan Plateau (TP). For the high-elevation stations, which were mainly in the TP, multiple snow-free breaks (SFBs) during the cold season made D-s insensitive to D-o and D-e. Furthermore, the number of SFBs (D-b) increased significantly with the rise in elevation, explaining why higher altitudes in TP did not necessarily have greater D-s values despite the earlier D-o and later D-e values. From 1970 to 2014, most stations in China exhibited delayed D-o and advanced D-e due mainly to the increased temperature, but such trends were significant at only 10.5% and 15.4% of the stations, respectively. During the same period, shortened D-s primarily occurred south of similar to 40 degrees N, whereas the opposite ones dominated north of similar to 40 degrees N. Most stations (except those in Hexi Corridor) with significant growth in D-s were characterized by delayed D-o and advanced D-e. Such a phenomenon of increased snow cover days during shortened cold season was due to the significant shrinkage in D-b values. The spatial pattern of the trends in annual total snow depth overall follows that of D-s, suggesting that the D-s, when takes SFBs into consideration, could be an indicator of variations of snow water resources in China. The trends in D-o, D-e and D-s were not elevation dependent in TP. |
关键词 | TIBETAN PLATEAUSPATIOTEMPORAL VARIABILITYALTITUDINAL DEPENDENCEWATER AVAILABILITYIN-SITUWESTERNPRODUCTSDEPTHCOMBINATIONEQUIVALENT |
英文关键词 | Snow cover phenology; Snow-free breaks; The number of snow cover days; Snow depth; Station measurements; Altitudinal dependence |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000563843100003 |
来源期刊 | CLIMATE DYNAMICS |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259863 |
推荐引用方式 GB/T 7714 | Ma, Ning,Yu, Kunlun,Zhang, Yinsheng,et al. Ground observed climatology and trend in snow cover phenology across China with consideration of snow-free breaks[J]. 中国科学院青藏高原研究所,2020,55(9-10). |
APA | Ma, Ning,Yu, Kunlun,Zhang, Yinsheng,Zhai, Jianqing,Zhang, Yongqiang,&Zhang, Hongbo.(2020).Ground observed climatology and trend in snow cover phenology across China with consideration of snow-free breaks.CLIMATE DYNAMICS,55(9-10). |
MLA | Ma, Ning,et al."Ground observed climatology and trend in snow cover phenology across China with consideration of snow-free breaks".CLIMATE DYNAMICS 55.9-10(2020). |
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