Spatial and temporal characteristics of the daily precipitation concentration index over China from 1979 to 2015

Irregular precipitation has a nontrivial influence on hydrological processes and regional agriculture. The precipitation concentration index provides convenient quantitative characterizations of precipitation variability. To explore the spatial and temporal distribution of the precipitation concentr...

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Main Authors: Huihua Du, Yimin Wang, Zongzhi Wang, Kelin Liu, Liang Cheng
Format: Article
Language:English
Published: IWA Publishing 2020-06-01
Series:Hydrology Research
Subjects:
Online Access:http://hr.iwaponline.com/content/51/3/562
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author Huihua Du
Yimin Wang
Zongzhi Wang
Kelin Liu
Liang Cheng
author_facet Huihua Du
Yimin Wang
Zongzhi Wang
Kelin Liu
Liang Cheng
author_sort Huihua Du
collection DOAJ
description Irregular precipitation has a nontrivial influence on hydrological processes and regional agriculture. The precipitation concentration index provides convenient quantitative characterizations of precipitation variability. To explore the spatial and temporal distribution of the precipitation concentration index, the long-term concentration index (LCI) and the annual concentration index (ACI) during 1979–2015 were calculated based on the China Meteorological Forcing Dataset. The results are as follows: (1) The LCI in China ranged from 0.4571 to 0.9197, and the values between 0.6 and 0.7 accounted for 61.61% of the dataset. The highest and lowest LCI values were both recorded in Northwest China, which features low precipitation levels. Additionally, there are high LCI values (greater than 0.6) in Southeast China, which features high precipitation levels. (2) Application of the Mann-Kendall test (M-K test) and Sen's slope revealed that more than 88% of the grids exhibited nonsignificant positive or negative ACI trends and that more than 10% of the grid ACI values exhibited positive trends, with approximately 2.8% showing significant changes at the 0.1 significance level. (3) Application of the Pettitt test revealed that approximately 11.9% of the grid ACI values exhibited an abrupt change at the 0.5 significance level, with abrupt changes occurring in 1991, 1992 and 1993, together accounting for 45.89% of all grids with abrupt changes.
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spelling doaj.art-cf98a0c915434899af2a5490b3f57f7c2022-12-21T19:32:12ZengIWA PublishingHydrology Research1998-95632224-79552020-06-0151356258210.2166/nh.2020.149149Spatial and temporal characteristics of the daily precipitation concentration index over China from 1979 to 2015Huihua Du0Yimin Wang1Zongzhi Wang2Kelin Liu3Liang Cheng4 State Key Laboratory of Eco-hydraulics in Northwest Arid Region of China, Xi'an University of Technology, Jinhua Road 5, Xi'an 710048, Shaanxi, China State Key Laboratory of Eco-hydraulics in Northwest Arid Region of China, Xi'an University of Technology, Jinhua Road 5, Xi'an 710048, Shaanxi, China State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China Irregular precipitation has a nontrivial influence on hydrological processes and regional agriculture. The precipitation concentration index provides convenient quantitative characterizations of precipitation variability. To explore the spatial and temporal distribution of the precipitation concentration index, the long-term concentration index (LCI) and the annual concentration index (ACI) during 1979–2015 were calculated based on the China Meteorological Forcing Dataset. The results are as follows: (1) The LCI in China ranged from 0.4571 to 0.9197, and the values between 0.6 and 0.7 accounted for 61.61% of the dataset. The highest and lowest LCI values were both recorded in Northwest China, which features low precipitation levels. Additionally, there are high LCI values (greater than 0.6) in Southeast China, which features high precipitation levels. (2) Application of the Mann-Kendall test (M-K test) and Sen's slope revealed that more than 88% of the grids exhibited nonsignificant positive or negative ACI trends and that more than 10% of the grid ACI values exhibited positive trends, with approximately 2.8% showing significant changes at the 0.1 significance level. (3) Application of the Pettitt test revealed that approximately 11.9% of the grid ACI values exhibited an abrupt change at the 0.5 significance level, with abrupt changes occurring in 1991, 1992 and 1993, together accounting for 45.89% of all grids with abrupt changes.http://hr.iwaponline.com/content/51/3/562mann-kendall trend testpettitt testprecipitation concentration indexspatio-temporal characteristics
spellingShingle Huihua Du
Yimin Wang
Zongzhi Wang
Kelin Liu
Liang Cheng
Spatial and temporal characteristics of the daily precipitation concentration index over China from 1979 to 2015
Hydrology Research
mann-kendall trend test
pettitt test
precipitation concentration index
spatio-temporal characteristics
title Spatial and temporal characteristics of the daily precipitation concentration index over China from 1979 to 2015
title_full Spatial and temporal characteristics of the daily precipitation concentration index over China from 1979 to 2015
title_fullStr Spatial and temporal characteristics of the daily precipitation concentration index over China from 1979 to 2015
title_full_unstemmed Spatial and temporal characteristics of the daily precipitation concentration index over China from 1979 to 2015
title_short Spatial and temporal characteristics of the daily precipitation concentration index over China from 1979 to 2015
title_sort spatial and temporal characteristics of the daily precipitation concentration index over china from 1979 to 2015
topic mann-kendall trend test
pettitt test
precipitation concentration index
spatio-temporal characteristics
url http://hr.iwaponline.com/content/51/3/562
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AT zongzhiwang spatialandtemporalcharacteristicsofthedailyprecipitationconcentrationindexoverchinafrom1979to2015
AT kelinliu spatialandtemporalcharacteristicsofthedailyprecipitationconcentrationindexoverchinafrom1979to2015
AT liangcheng spatialandtemporalcharacteristicsofthedailyprecipitationconcentrationindexoverchinafrom1979to2015