Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.jhydrol.2020.124744 |
Spatiotemporal dynamics of soil moisture in the karst areas of China based on reanalysis and observations data | |
Deng, Yuanhong1,2,3; Wang, Shijie1,4; Bai, Xiaoyong1,5,6; Luo, Guangjie6; Wu, Luhua1,3; Chen, Fei1,7; Wang, Jinfeng1,7; Li, Qin1,3; Li, Chaojun1,8; Yang, Yujie1,8; Hu, Zeyin1,3; Tian, Shiqi1,8 | |
通讯作者 | Bai, Xiaoyong |
来源期刊 | JOURNAL OF HYDROLOGY |
ISSN | 0022-1694 |
EISSN | 1879-2707 |
出版年 | 2020 |
卷号 | 585 |
英文摘要 | Soil moisture is one of the restricting factors in a fragile karst ecological environment. However, its spatio-temporal evolution characteristics in the karst areas of China remain poorly understood. Thus, based on soil moisture from reanalysis (ERA-Interim product) and ground stations, this study used the Mann-Kendall test, the Theil-Sen slope estimator, sensitivity analysis and stepwise regression and obtained the following results: 1) ERA-Interim soil moisture well reflected the interannual change of observational soil moisture at 0-7, 7-28 and 28-100 cm. 2) The reanalysis and station data showed that soil at various depths in the karst areas was dominated by a drying trend in 1982-2015. 3) Soil moisture in karst areas of southern China was high but decreased fastest. In the karst areas of northern China, soil moisture was low and declined quickly. Nevertheless, soil wetting was observed in the central karst areas of Qinghai-Tibet Plateau. 4) Changes of soil moisture throughout the karst region of China and its subareas were mainly affected by precipitation, followed by temperature. 5) In Qinghai-Tibet Plateau and southern China, soil moisture in karst areas is overall higher than that in non-karst areas when under low vegetation coverage levels (NDVI <= 0.3) of some climate zones, possibly caused by the centralized allocation of precipitation in karst areas due to exposed rocks. In conclusion, climate, vegetation, and geological background make the spatiotemporal distributions of soil moisture differ within the karst region, while the soil drying trend in recent decades and global climate change are not conducive to the ecological restoration of vulnerable karst areas. |
英文关键词 | Karst Soil moisture China Climate NDVI Sensitivity analysis |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
收录类别 | SCI-E |
WOS记录号 | WOS:000544230000016 |
WOS关键词 | ROCKY DESERTIFICATION ; TIBETAN PLATEAU ; LOESS PLATEAU ; WATER ; VEGETATION ; TRENDS ; RESTORATION ; VARIABILITY ; PATTERNS ; INCREASE |
WOS类目 | Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources |
WOS研究方向 | Engineering ; Geology ; Water Resources |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/319660 |
作者单位 | 1.Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, 99 Lincheng West Rd, Guiyang 550081, Peoples R China; 2.Chinese Acad Sci, Ctr Lunar & Planetary Sci, Inst Geochem, Guiyang 550081, Peoples R China; 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China; 4.Chinese Acad Sci, Puding Karst Ecosyst Observat & Res Stn, Puding 562100, Peoples R China; 5.CAS Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Shaanxi, Peoples R China; 6.Guizhou Educ Univ, Guizhou Prov Key Lab Geog State Monitoring Waters, Guiyang 550018, Peoples R China; 7.Guizhou Univ, Coll Resources & Environm Engn, Guiyang 550025, Peoples R China; 8.Guizhou Normal Univ, Sch Geog & Environm Sci, Guiyang 550001, Guizhou, Peoples R China |
推荐引用方式 GB/T 7714 | Deng, Yuanhong,Wang, Shijie,Bai, Xiaoyong,et al. Spatiotemporal dynamics of soil moisture in the karst areas of China based on reanalysis and observations data[J],2020,585. |
APA | Deng, Yuanhong.,Wang, Shijie.,Bai, Xiaoyong.,Luo, Guangjie.,Wu, Luhua.,...&Tian, Shiqi.(2020).Spatiotemporal dynamics of soil moisture in the karst areas of China based on reanalysis and observations data.JOURNAL OF HYDROLOGY,585. |
MLA | Deng, Yuanhong,et al."Spatiotemporal dynamics of soil moisture in the karst areas of China based on reanalysis and observations data".JOURNAL OF HYDROLOGY 585(2020). |
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