Assessing the impacts of climate change on the high altitude snow- and glacier-fed hydrological regimes of Astore and Hunza, the sub-catchments of Upper Indus Basin
Author(s) -
Suhaib Bin Farhan,
Yinsheng Zhang,
Adnan Aziz,
Haifeng Gao,
Yingzhao Ma,
Syed Jamil Hasan Kazmi,
Atif Shahzad,
Iqtidar Hussain,
Muhammad Mansha,
Mudassar Umar,
Jawad Nasir,
Muhammad Shafiq,
Yasir Farhan,
Saima Shaikh,
Umair Bin Zamir,
Asad Fayyaz,
Raheel Ahmed
Publication year - 2018
Publication title -
journal of water and climate change
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.421
H-Index - 22
eISSN - 2408-9354
pISSN - 2040-2244
DOI - 10.2166/wcc.2018.107
Subject(s) - precipitation , environmental science , altitude (triangle) , glacier , snow , climate change , drainage basin , water resources , structural basin , spring (device) , hydrology (agriculture) , climatology , physical geography , geology , geography , meteorology , ecology , mechanical engineering , paleontology , oceanography , geometry , mathematics , cartography , geotechnical engineering , engineering , biology
Evaluation of the impacts of prevailing climate change on rivers and water resources is significantly important in order to successfully manage water resources, particularly in snow-fed and glacier-fed catchments. The basic aim of this research was to assess the impacts of climatic variability on Astore and Hunza river-flows by employing long-term in-situ hydro-meteorological data. Times-series analysis of highand low-altitude station data revealed consistent summer cooling, and warming in winter and spring seasons in both Karakoram and western Himalayan basins of Hunza and Astore, respectively. The intensity of these changes was not found to be identical in both basins, i.e. Hunza depicts slightly higher summer cooling rates and slightly lower annual, winter and spring warming rates as compared to Astore. Subsequently, the significant increase in annual precipitation of Hunza was also not found to be identical with Astore precipitation, which shows only a slight increase of precipitation. Notwithstanding, comparable temperature trends were observed at both highand low-altitude stations; however, on the contrary, precipitation shows a different pattern of behavior, i.e. significantly increased winter precipitation at high-altitude Astore stations was in contrast to the precipitation recorded by low-altitude stations. The study suggested that climate change is significantly influencing the characteristics and hydrological resources of this region. doi: 10.2166/wcc.2018.107 s://iwaponline.com/jwcc/article-pdf/doi/10.2166/wcc.2018.107/531045/jwc2018107.pdf Suhaib Bin Farhan (corresponding author) Yinsheng Zhang Haifeng Gao Yingzhao Ma Chinese Academy of Sciences, Institute of Tibetan Plateau Research, Beijing, China E-mail: suhaibfarhan@yahoo.com Suhaib Bin Farhan Haifeng Gao Yingzhao Ma University of Chinese Academy of Sciences, No.19A Yuquan Road, Beijing 100049, China Suhaib Bin Farhan Adnan Aziz Atif Shahzad Muhammad Mansha Mudassar Umar Jawad Nasir Muhammad Shafiq Yasir Farhan Raheel Ahmed Pakistan Space & Upper Atmosphere Research Commission, SUPARCO, Karachi, Pakistan Iqtidar Hussain Karakoram International University, Gilgit Baltistan, Pakistan Jamil Kazmi Saima Shaikh Umair Bin Zamir Department of Geography, University of Karachi, Pakistan Fayyaz Asad Department of Botany, Abdul Wali Khan University, Mardan, Pakistan
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