globalchange  > 全球变化的国际研究计划
DOI: 10.5194/hess-23-3081-2019
WOS记录号: WOS:000476504500001
论文题名:
Spatiotemporal changes in aridity of Pakistan during 1901-2016
作者: Ahmed, Kamal1,2; Shahid, Shamsuddin1; Wang, Xiaojun3,4; Nawaz, Nadeem2; Khan, Najeebullah1
通讯作者: Wang, Xiaojun
刊名: HYDROLOGY AND EARTH SYSTEM SCIENCES
ISSN: 1027-5606
EISSN: 1607-7938
出版年: 2019
卷: 23, 期:7, 页码:3081-3096
语种: 英语
WOS关键词: CLIMATE VARIABILITY ; SEMIARID REGIONS ; TREND DETECTION ; MANN-KENDALL ; DROUGHT ; PRECIPITATION ; RAINFALL ; CHINA ; EVAPOTRANSPIRATION ; IRRIGATION
WOS学科分类: Geosciences, Multidisciplinary ; Water Resources
WOS研究方向: Geology ; Water Resources
英文摘要:

The changing characteristics of aridity over a larger spatiotemporal scale have gained interest in recent years due to climate change. The long-term (1901-2016) changes in spatiotemporal patterns of annual and seasonal aridity during two major crop growing seasons of Pakistan, Kharif and Rabi, are evaluated in this study using gridded precipitation and potential evapotranspiration (PET) data. The UNESCO aridity index was used to estimate aridity at each grid point for all the years between 1901 and 2016. The temporal changes in aridity and its associations with precipitation and PET are evaluated by implementing a moving window of 50 years of data with an 11-year interval. The modified Mann-Kendall (MMK) trend test is applied to estimate unidirectional change by eliminating the effect of natural variability of climate, and Pettitt's test is used to detect year of change in aridity. The results revealed that the climate over 60% of Pakistan (mainly in southern parts) is arid. The spatial patterns of aridity trends show a strong influence of the changes in precipitation on the aridity trend. The increasing trend in aridity (drier) is noticed in the southwest, where precipitation is low during Kharif, while there is a decreasing trend (wetter) in the Rabi season in the region which receives high precipitation due to western disturbances. The annual and Kharif aridity is found to decrease (wetter) at a rate of 0.0001 to 0.0002 per year in the northeast, while Kharif and Rabi aridity are found to increase (drier) at some locations in the south at a rate of -0.0019 to -0.0001 per year. The spatial patterns of aridity changes show a shift from arid to the semi-arid (wetter) climate in annual and Kharif over a large area while showing a shift from arid to hyper-arid (drier) region during Rabi in a small area. Most of the significant changes in precipitation and aridity are observed in the years between 1971 and 1980. Overall, aridity is found to increase (drier) in 0.52 %, 4.44% and 0.52% of the area and decrease (wetter) in 11.75 %, 7.57% and 9.66% of the area for annual, Rabi and Kharif seasons respectively during 1967-2016 relative to 1901-1950.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/143566
Appears in Collections:全球变化的国际研究计划

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作者单位: 1.Univ Teknol Malaysia, Fac Civil Engn, Johor Baharu 81310, Malaysia
2.Lasbela Univ Agr Water & Marine Sci, Fac Water Resource Management, Balochistan 90150, Pakistan
3.Nanjing Hydraul Res Inst, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210029, Jiangsu, Peoples R China
4.Minist Water Resources, Res Ctr Climate Change, Nanjing 210029, Jiangsu, Peoples R China

Recommended Citation:
Ahmed, Kamal,Shahid, Shamsuddin,Wang, Xiaojun,et al. Spatiotemporal changes in aridity of Pakistan during 1901-2016[J]. HYDROLOGY AND EARTH SYSTEM SCIENCES,2019-01-01,23(7):3081-3096
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