Projected Changes of Future Extreme Drought Events under Numerous Drought Indices in the Heilongjiang Province of China
Muhammad Imran Khan (),
Dong Liu (),
Qiang Fu (),
Qaisar Saddique (),
Muhammad Abrar Faiz (),
Tianxiao Li (),
Muhammad Uzair Qamar (),
Song Cui () and
Chen Cheng ()
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Muhammad Imran Khan: Northeast Agricultural University
Dong Liu: Northeast Agricultural University
Qiang Fu: Northeast Agricultural University
Qaisar Saddique: Northwest A&F University
Muhammad Abrar Faiz: Northeast Agricultural University
Tianxiao Li: Northeast Agricultural University
Muhammad Uzair Qamar: University of Agriculture
Song Cui: Northeast Agricultural University
Chen Cheng: Northeast Agricultural University
Water Resources Management: An International Journal, Published for the European Water Resources Association (EWRA), 2017, vol. 31, issue 12, No 14, 3937 pages
Abstract:
Abstract Effective drought prediction methods are essential for the mitigation of adverse effects of severe drought events. This study utilizes the Reconnaissance Drought Index, Standardized Precipitation Index and Standardized Precipitation Evapotranspiration Index to assess the occurrence of future drought events in the study area of the Heilongjiang province of China over a period of 2016–2099. The drought indices were computed from the meteorological data (temperature, precipitation) generated by the global climate model (HadCM3A2). Moreover, Mann-Kendall trend test was applied for the assessment of future climatic trends and detecting probable differences in the behaviour of various drought indices. Drought forecasting periods has been divided into three categories: the early phase (1916–2030), middle phase (2031–2060) and late phase (2061–2099). The occurrence of future droughts is also ranked according to their intensity (mild, moderate, severe and extreme drought). Based on the drought results, more number of drought events are expected to occur during 12-month drought analysis are, RDI during 2084–2098 (DD = 14, DS = −1.38), SPEI during 2084–2098 (DD = 14, DS = −1.33) and SPI during 2084–2095 (DD = 12, DS = −1.19). The 1st and 2nd months of the years studied predicted a warming trend, while the 7th, 8th, and 9th months predicted a wetter trend. Finally, it was observed that RDI is more sensitive to drought and indicated a high percentage of years under severe and extreme drought conditions during the drought frequency analysis. Conclusively, this study provides a strategies for water resources management and monitoring of droughts, in which drought indices like RDI can play a central role.
Keywords: Reconnaissance drought index; Warming trend; Projected changes; Drought extremes; GCMs (search for similar items in EconPapers)
Date: 2017
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DOI: 10.1007/s11269-017-1716-4
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