Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.atmosres.2015.09.001 |
Changes in extreme temperature and precipitation events in the Loess Plateau (China) during 1960-2013 under global warming | |
Sun, Wenyi1; Mu, Xingmin1; Song, Xiaoyan2; Wu, Dan3; Cheng, Aifang4; Qiu, Bing5 | |
通讯作者 | Song, Xiaoyan |
来源期刊 | ATMOSPHERIC RESEARCH |
ISSN | 0169-8095 |
EISSN | 1873-2895 |
出版年 | 2016 |
卷号 | 168页码:33-48 |
英文摘要 | In recent decades, extreme climatic events have been a major issue worldwide. Regional assessments on various climates and geographic regions are needed for understanding uncertainties in extreme events’ responses to global warming. The objective of this study was to assess the annual and decadal trends in 12 extreme temperature and 10 extreme precipitation indices in terms of intensity, frequency, and duration over the Loess Plateau during 1960-2013. The results indicated that the regionally averaged trends in temperature extremes were consistent with global warming. The occurrence of warm extremes, including summer days (SU), tropical nights (TR), warm days (TX90), and nights (TN90) and a warm spell duration indicator (WSDI), increased by 2.76 (P < 0.01), 1.24 (P < 0.01), 2.60 (P = 0.0003), 3.41 (P < 0.01), and 0.68 (P = 0.0041) days/decade during the period of 1960-2013, particularly, sharp increases in these indices occurred in 1985-2000. Over the same period, the occurrence of cold extremes, including frost days (FD), ice days (ID), cold days (DUO) and nights (TN10), and a cold spell duration indicator (CSDI) exhibited decreases of 3.22 (P < 0.01), 2.21 (P = 0.0028), 2.71 (P = 0.0028), 431 (P < 0.01), and 0.69 (P = 0.0951) days/decade, respectively. Moreover, extreme warm events in most regions tended to increase while cold indices tended to decrease in the Loess Plateau, but the trend magnitudes of cold extremes were greater than those of warm extremes. The growing season (GSL) in the Loess Plateau was lengthened at a rate of 3.16 days/decade (P < 0.01). Diurnal temperature range (DTR) declined at a rate of -0.06 degrees C/decade (P = 0.0931). Regarding the precipitation indices, the annual total precipitation (PRCPTOT) showed no obvious trends (P = 0.7828). The regionally averaged daily rainfall intensity (SDII) exhibited significant decreases (-0.14 mm/day/decade, P = 0.0158), whereas consecutive dry days (CDD) significantly increased (1.96 days/decade, P = 0.0001) during 1960-2013. Most of stations with significant changes in SDII and CDD occurred in central and southeastern Loess Plateau. However, the changes in days of erosive rainfall, heavy rain, rainstorm, maximum 5-day precipitation, and very-wet-day and extremely wet-day precipitation were not significant. Large-scale atmospheric circulation indices, such as the Western Pacific Subtropical High Intensity Index (WPSHII) and Arctic Oscillation (AO), strongly influences warm/cold extremes and contributes significantly to climate changes in the Loess Plateau. The enhanced geopotential height over the Eurasian continent and increase in water vapor divergence in the rainy season have contributed to the changes of the rapid warming and consecutive drying in the Loess Plateau. (C) 2015 Elsevier B.V. All rights reserved. |
英文关键词 | Extreme climatic events Temperature Precipitation The Loess Plateau in China Large-scale atmospheric circulation |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
收录类别 | SCI-E |
WOS记录号 | WOS:000364892100004 |
WOS关键词 | YANGTZE-RIVER BASIN ; VEGETATION COVER ; SOIL-EROSION ; ARID REGION ; LAND-USE ; TRENDS ; CLIMATE ; VARIABILITY ; IMPACTS ; RAINFALL |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源机构 | 西北农林科技大学 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/191635 |
作者单位 | 1.Northwest A&F Univ, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China; 2.Northwest A&F Univ, Coll Water Resources & Architectural Engn, 23 Weihui Rd, Yangling 712100, Shaanxi, Peoples R China; 3.Nanjing Inst Environm Sci, Minist Environm Protect, Nanjing 210042, Jiangsu, Peoples R China; 4.Baoji Univ Arts & Sci, Key Lab Disaster Monitoring & Mech Simulating Sha, Boaji 721013, Shaanxi, Peoples R China; 5.Gen Inst Water Resources & Hydropower Planning &, Minist Water Resources, Beijing 100120, Peoples R China |
推荐引用方式 GB/T 7714 | Sun, Wenyi,Mu, Xingmin,Song, Xiaoyan,et al. Changes in extreme temperature and precipitation events in the Loess Plateau (China) during 1960-2013 under global warming[J]. 西北农林科技大学,2016,168:33-48. |
APA | Sun, Wenyi,Mu, Xingmin,Song, Xiaoyan,Wu, Dan,Cheng, Aifang,&Qiu, Bing.(2016).Changes in extreme temperature and precipitation events in the Loess Plateau (China) during 1960-2013 under global warming.ATMOSPHERIC RESEARCH,168,33-48. |
MLA | Sun, Wenyi,et al."Changes in extreme temperature and precipitation events in the Loess Plateau (China) during 1960-2013 under global warming".ATMOSPHERIC RESEARCH 168(2016):33-48. |
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