Event-Based Time Distribution Patterns, Return Levels, and Their Trends of Extreme Precipitation across Indus Basin

被引:27
作者
Zaman, Muhammad [1 ,2 ]
Ahmad, Ijaz [3 ]
Usman, Muhammad [4 ]
Saifullah, Muhammad [5 ]
Anjum, Muhammad Naveed [6 ]
Khan, Muhammad Imran [1 ]
Uzair Qamar, Muhammad [2 ]
机构
[1] Jiangsu Univ, Res Ctr Fluid Machinery Engn & Technol, Zhenjiang 212013, Jiangsu, Peoples R China
[2] Univ Agr Faisalabad, Dept Irrigat & Drainage, Faisalabad 380000, Pakistan
[3] Univ Engn & Technol, Ctr Excellence Water Resources Engn, Lahore 54600, Pakistan
[4] Univ Halle Wittenberg, Inst Geosci & Geog, Dept Geoecol, Seckendorff Pl 4, D-06120 Halle, Saale, Germany
[5] Muhammad Nawaz Shareef Univ Agr, Dept Agr Engn, Multan 66000, Pakistan
[6] Pir Mehr Ali Shah Arid Agr Univ, Fac Agr Engn & Technol, Dept Land & Water Conservat Engn, Rawalpindi 46000, Pakistan
关键词
extreme precipitation; precipitation indices; time distribution patterns; Northern Highlands of Pakistan; REGIONAL FREQUENCY-ANALYSIS; SUMMER MONSOON RAINFALL; DURATION SERIES METHODS; ANNUAL MAXIMUM SERIES; RIVER-BASIN; HYDROLOGIC EVENTS; CLIMATE EXTREMES; NON-STATIONARITY; DIURNAL CYCLE; YANGTZE-RIVER;
D O I
10.3390/w12123373
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study presented the spatio-temporal characteristics of extreme precipitation events in the Northern Highlands of Pakistan (NHPK). Daily precipitation observations of 30 in situ meteorological stations from 1961 to 2014 were used to estimate the 11 extreme precipitation indices. Additionally, trends in time distribution patterns (TDPs) and return periods were also investigated for event based extreme precipitations (EEP). Results found that the precipitation events with an amount of 160-320 mm and with a concentration ratio of 0.8-1.0 and a duration of 4-7 consecutive days were dominant. The frequency of heavy, very heavy and extremely heavy precipitation days decreased, whereas the frequency of wet, very wet and extremely wet days increased. Most of the indices, generally, showed an increasing trend from the northeast to middle parts. The extreme precipitation events of the 20 and 50-year return period were more common in the western and central areas of NHPK. Moreover, the 20 and 50-year return levels depicted higher values (up to 420 mm) for an event duration with all daily precipitation extremes dispersed in the first half (TDP1) in the Chitral, Panjkora and Jhelum Rivers basins, whilst the maximum values (up to 700 mm) for an event duration with all daily precipitation extremes dispersed in the second half (TDP2) were observed in the eastern part of the NHPK for 20-year and eastern and south-west for 50-year, respectively.
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页数:29
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