Climate Change Impacts and Adaptation to Flow of Swat River and Glaciers in Hindu Kush Ranges, Swat District, Pakistan (2003-2013)

This work aims at the climate change impacts and adaptation to surface flow of Swat river and glacier resources in Swat river catchments area, Hindu Kush ranges, Northwest Pakistan. The data about temperature and precipitation have been collected from the Pakistan Meteorological Department, Karachi,...

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Main Authors: Saifullah Khan, Mahmood-Ul-Hasan
Format: Article
Language:English
Published: Society of Economic Geologists and Mineral Technologists 2016-06-01
Series:International Journal of Economic and Environment Geology
Subjects:
Online Access:http://www.econ-environ-geol.org/pdf/jan2016/3.pdf
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author Saifullah Khan
Mahmood-Ul-Hasan
author_facet Saifullah Khan
Mahmood-Ul-Hasan
author_sort Saifullah Khan
collection DOAJ
description This work aims at the climate change impacts and adaptation to surface flow of Swat river and glacier resources in Swat river catchments area, Hindu Kush ranges, Northwest Pakistan. The data about temperature and precipitation have been collected from the Pakistan Meteorological Department, Karachi, whereas the Swat River flow data from the Irrigation Department, Peshawar, Khyber Pukhtunkhwa. Two types of climate that is humid and undifferentiated highlands prevail over the area. The total precipitation recorded has been 41.8inches (1061.7 millimeters) with mean monthly precipitation of 3.5 inches (88.9 millimeters) having a decrease of -0.1 inch (-2.8 millimeters). The area has been humid during 2004 and currently at the threshold of the sub-humid climates (20-40 inches). Kalam valley experiences cold long winters (7 months) and short warm summers (5 months). The mean temperature reveals an increase of 0.90C, maximum temperature 0.40C and mean minimum temperature 0.50Celsius. This increase in the temperature of the area has caused water stress and retreat of glaciers and affected the permafrost condition at higher altitudes in the area. The annual flow of the Swat river is 192.2 cubic meter/seconds with a decline of -0.03 cubic m/sec from 2003 to 2013. The annual trend of water flow is directly proportional to precipitation and contrary to maximum temperature during 2003 to 2012 and shows converse condition till 2013. The decrease in the flow of Swat river seems both in winter and summer season. The glaciers and snow covered area of the Kalam valley decreases with passage of time and required mitigation. The vulnerability of the study area to climate change can be minimized by the construction of small reservoirs, river embankments, improvement in sewerage and sanitation, planning for flood water, and revision of the water management policy, implementation, and establishment of research and development funds.
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spelling doaj.art-8dab2dc134e842eeab73607456fb740d2022-12-21T18:11:30ZengSociety of Economic Geologists and Mineral TechnologistsInternational Journal of Economic and Environment Geology2223-957X2223-957X2016-06-01712435Climate Change Impacts and Adaptation to Flow of Swat River and Glaciers in Hindu Kush Ranges, Swat District, Pakistan (2003-2013)Saifullah Khan0Mahmood-Ul-Hasan1Institute of Social Sciences and Directorate of Distance Education. Bahauddin Zakariya University, Multan, Punjab, Pakistan.Department of Geography, University of Peshawar, KP, Pakistan.This work aims at the climate change impacts and adaptation to surface flow of Swat river and glacier resources in Swat river catchments area, Hindu Kush ranges, Northwest Pakistan. The data about temperature and precipitation have been collected from the Pakistan Meteorological Department, Karachi, whereas the Swat River flow data from the Irrigation Department, Peshawar, Khyber Pukhtunkhwa. Two types of climate that is humid and undifferentiated highlands prevail over the area. The total precipitation recorded has been 41.8inches (1061.7 millimeters) with mean monthly precipitation of 3.5 inches (88.9 millimeters) having a decrease of -0.1 inch (-2.8 millimeters). The area has been humid during 2004 and currently at the threshold of the sub-humid climates (20-40 inches). Kalam valley experiences cold long winters (7 months) and short warm summers (5 months). The mean temperature reveals an increase of 0.90C, maximum temperature 0.40C and mean minimum temperature 0.50Celsius. This increase in the temperature of the area has caused water stress and retreat of glaciers and affected the permafrost condition at higher altitudes in the area. The annual flow of the Swat river is 192.2 cubic meter/seconds with a decline of -0.03 cubic m/sec from 2003 to 2013. The annual trend of water flow is directly proportional to precipitation and contrary to maximum temperature during 2003 to 2012 and shows converse condition till 2013. The decrease in the flow of Swat river seems both in winter and summer season. The glaciers and snow covered area of the Kalam valley decreases with passage of time and required mitigation. The vulnerability of the study area to climate change can be minimized by the construction of small reservoirs, river embankments, improvement in sewerage and sanitation, planning for flood water, and revision of the water management policy, implementation, and establishment of research and development funds.http://www.econ-environ-geol.org/pdf/jan2016/3.pdfPrecipitationtemperaturewater resourcesglacierspermafrostadaptation.
spellingShingle Saifullah Khan
Mahmood-Ul-Hasan
Climate Change Impacts and Adaptation to Flow of Swat River and Glaciers in Hindu Kush Ranges, Swat District, Pakistan (2003-2013)
International Journal of Economic and Environment Geology
Precipitation
temperature
water resources
glaciers
permafrost
adaptation.
title Climate Change Impacts and Adaptation to Flow of Swat River and Glaciers in Hindu Kush Ranges, Swat District, Pakistan (2003-2013)
title_full Climate Change Impacts and Adaptation to Flow of Swat River and Glaciers in Hindu Kush Ranges, Swat District, Pakistan (2003-2013)
title_fullStr Climate Change Impacts and Adaptation to Flow of Swat River and Glaciers in Hindu Kush Ranges, Swat District, Pakistan (2003-2013)
title_full_unstemmed Climate Change Impacts and Adaptation to Flow of Swat River and Glaciers in Hindu Kush Ranges, Swat District, Pakistan (2003-2013)
title_short Climate Change Impacts and Adaptation to Flow of Swat River and Glaciers in Hindu Kush Ranges, Swat District, Pakistan (2003-2013)
title_sort climate change impacts and adaptation to flow of swat river and glaciers in hindu kush ranges swat district pakistan 2003 2013
topic Precipitation
temperature
water resources
glaciers
permafrost
adaptation.
url http://www.econ-environ-geol.org/pdf/jan2016/3.pdf
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