Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1002/joc.6728 |
Dominant factor of dry-wet change in China since 1960s | |
Xu, Jinqin; Wang, Dandan; Qiu, Xinfa; Zeng, Yan; Zhu, Xiaochen; Li, Mengxi; He, Yongjian; Shi, Guoping | |
通讯作者 | Qiu, XF |
来源期刊 | INTERNATIONAL JOURNAL OF CLIMATOLOGY
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ISSN | 0899-8418 |
EISSN | 1097-0088 |
英文摘要 | The dry-wet climate conditions of an area are mainly determined by the water input (e.g., precipitation, P) and output (e.g., potential evapotranspiration, PET). Based on three dry-wet indices and the differential equation, this study designed a new attribution method to quantify the contributions of P and PET to the dry-wet change, so as to determine the dominant factors of the dry-wet change over whole China (CHINA) and various hydroclimate regions (i.e., arid region, AR; semi-arid region, SAR; semi-humid region, SHR; and humid region, HR) during 1960-2018 and six interdecadal periods. Results showed that the overall weak drying in CHINA was dominated by an increase in PET, while climate humidification in AR and HR was dominated by an increase in P, climate drying in SHR was dominated by the reduced P, and the weak drying in SAR was co-dominated by P and PET during 1960-2018. The dominant factors of dry-wet change over CHINA and each hydroclimate region varied in different decades. Briefly, climate humidification in CHINA and various hydroclimate regions was basically dominated by P in different decades, and the drying was mainly dominated by P in the 1960s-1980s, but the contribution of PET to climate drying began to become prominent after the 1980s. Besides, we found that P contributed more to dry-wet change than PET on the station and regional scales, but the contribution of P to climate drying on a national scale was underestimated to some extent due to the regional offset effect of the increase/decrease in P during 1960-2018, as well as in the 1990s. These findings implied that the importance of research on the regional or local scale, and equal attention should be paid to the effects of P and PET changes in the future drought or dry-wet change research. |
英文关键词 | dominant factor dry-wet change potential evapotranspiration precipitation |
类型 | Article ; Early Access |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000548415800001 |
WOS关键词 | SEA-SURFACE TEMPERATURES ; CLIMATE-CHANGE ; RIVER-BASIN ; REFERENCE EVAPOTRANSPIRATION ; TEMPORAL VARIABILITY ; DROUGHT SEVERITY ; POTENTIAL EVAPOTRANSPIRATION ; ANNUAL PRECIPITATION ; TRENDS ; ATTRIBUTION |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源机构 | 南京信息工程大学 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/328095 |
作者单位 | [Xu, Jinqin; Qiu, Xinfa; Zhu, Xiaochen; Li, Mengxi] Nanjing Univ Informat Sci & Technol, Sch Appl Meteorol, Nanjing 210044, Peoples R China; [Wang, Dandan] Huzhou Meteorol Bur, Huzhou, Peoples R China; [Zeng, Yan] Jiangsu Meteorol Bur, Jiangsu Res Inst Meteorol Sci, Nanjing, Peoples R China; [Zhu, Xiaochen] Univ Kentucky, Dept Plant & Soil Sci, Lexington, KY USA; [He, Yongjian; Shi, Guoping] Nanjing Univ Informat Sci & Technol, Sch Geog Sci, Nanjing, Peoples R China |
推荐引用方式 GB/T 7714 | Xu, Jinqin,Wang, Dandan,Qiu, Xinfa,et al. Dominant factor of dry-wet change in China since 1960s[J]. 南京信息工程大学. |
APA | Xu, Jinqin.,Wang, Dandan.,Qiu, Xinfa.,Zeng, Yan.,Zhu, Xiaochen.,...&Shi, Guoping. |
MLA | Xu, Jinqin,et al."Dominant factor of dry-wet change in China since 1960s".INTERNATIONAL JOURNAL OF CLIMATOLOGY |
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