Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1029/2018JD028436 |
Is There a Change From a Warm-Dry to a Warm-Wet Climate in the Inland River Area of China? Interpretation and Analysis Through Surface Water Balance | |
Long, Biao1; Zhang, Baoqing1; He, Chansheng1,2; Shao, Rui1; Tian, Wei1 | |
2018-07-27 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2018 |
卷号 | 123期号:14页码:7114-7131 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China; USA |
英文摘要 | The Inland River Area of China (IRAC), being the most water-stressed region in the world, faced with increasingly severe ecological degradation risk and water shortage issue under global climate warming. Previous studies indicated that the climate of IRAC have changed from warm-dry to warm-wet, because both precipitation (P) and air temperature have increased. However, the analysis in this study, considering the effects of climate change on hydrologic cycle rather than simply on climate conditions, indicates that there has been no substantial change from a warm-dry to a warm-wet climate in the IRAC during 1948-2010. The Standardized Moisture Anomaly Index (SZI), which is a comprehensive multiscalar drought indicator, was used to identify the patterns of dry and wet weather. The Global Land Data Assimilation System 2 (GLDAS2) Noah model, based on advanced land surface modeling and data assimilation techniques, were used to provide input surface water-energy variables for calculating SZI. The results show that both the forcing data and the output of the GLDAS2 Noah model are in good agreement with different types of observations. The variabilities in SZI are more consistent with evidence of multiple droughts (including residual water/energy ratio, evapotranspiration deficit, and historical drought records) than the Standardized Precipitation Index (SPI) and the Standardized Precipitation Evapotranspiration Index (SPEI). Based on SZI, it is known that increases in the water supply (P) are balanced by the increased water demand caused by significant climate warming; that is, terrestrial water storage has generally remained balanced over the past four decades. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000441965400005 |
WOS关键词 | STANDARDIZED PRECIPITATION INDEX ; DROUGHT SEVERITY INDEX ; MESOSCALE ETA-MODEL ; REMOTE-SENSING DATA ; NORTHWEST CHINA ; SOIL-MOISTURE ; EVAPOTRANSPIRATION PRODUCTS ; METEOROLOGICAL DROUGHT ; LAND EVAPORATION ; SOUTH-AMERICA |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/33988 |
专题 | 气候变化 |
作者单位 | 1.Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Minist Educ, Lanzhou, Gansu, Peoples R China; 2.Western Michigan Univ, Dept Geog, Kalamazoo, MI 49008 USA |
推荐引用方式 GB/T 7714 | Long, Biao,Zhang, Baoqing,He, Chansheng,et al. Is There a Change From a Warm-Dry to a Warm-Wet Climate in the Inland River Area of China? Interpretation and Analysis Through Surface Water Balance[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2018,123(14):7114-7131. |
APA | Long, Biao,Zhang, Baoqing,He, Chansheng,Shao, Rui,&Tian, Wei.(2018).Is There a Change From a Warm-Dry to a Warm-Wet Climate in the Inland River Area of China? Interpretation and Analysis Through Surface Water Balance.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,123(14),7114-7131. |
MLA | Long, Biao,et al."Is There a Change From a Warm-Dry to a Warm-Wet Climate in the Inland River Area of China? Interpretation and Analysis Through Surface Water Balance".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 123.14(2018):7114-7131. |
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