Abstract
Climate change is a common concern globally and the Kabul River Basin, a transboundary basin between Pakistan and Afghanistan, is no exception. Rising temperatures cause snow and glaciers to melt rapidly, which increases the variability of river flows that may affect the water resource management between the two countries. For this purpose, it is necessary to study snow and glaciers, the main source of river flow. The goal of this research is to assess and analyze the basin-scale and elevation-zonal variation in the areal extent of snow and glacier cover for the years 2001–2016, on daily, monthly, seasonal and yearly basis. The basin was distributed into eight elevation zones; and snow cover for the whole basin and each elevation zone was then extracted by utilizing the Moderate Resolution Imaging Spectroradiometer (MODIS), Onboard TERRA Satellite, 8-daily, 500 m resolution images. As per average climatology of the basin, snow cover is minimum in August because of higher summer temperatures and maximum in February owing to lower winter temperatures and higher westerly precipitation in solid form. Based on the basin-scale analysis of changes in the daily snow-covered areal extents, it is found that snow cover significantly increases in the three lowest elevation zones, whereas in the mid elevation zones (Zone 4 and 5) and the highest elevation zone (Zone 8) a negligible decreasing trend is found. Moreover, non-significant but decreasing trend in Zone 8 may hint either at decrease in solid precipitation in the high elevation region or a slight retreat of the glaciers which may become significant in the coming years. In addition, there is a significant decreasing trend of snow covered area in Zones 6 and 7 which gives a similar indication. Our seasonal and annual analysis indicates that there is an overall slight increasing trend in the basin for all analyzed seasons and also on annual basis. The results concluded that a detailed hydro-climate modeling analysis should be carried out for this basin to find the changes in water availability under the future climate scenarios.
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References
Archer DR, Fowler Hayley J (2004) Spatial and temporal variations in precipitation in the Upper Indus Basin, global teleconnections and hydrological implications. Hydrol Earth Syst Sci Discuss 8(1):47–61
Bolch T et al (2017) Brief communication: glaciers in the Hunza catchment (Karakoram) have been nearly in balance since the 1970s. Cryosphere 11(1):531
Brun F et al (2017) A spatially resolved estimate of High Mountain Asia glacier mass balances from 2000 to 2016. Nat Geosci 10(9):668–673
Chu D (2018) Spatiotemporal variability of snow cover on Tibet, China using MODIS remote-sensing data. Int J Remote Sens. https://doi.org/10.1080/01431161.2018.1466075
Cogley JG (2011) Present and future states of Himalaya and Karakoram glaciers. Ann Glaciol 52(59):69–73
Hall DK, Riggs GA, Salomonson VV, Digirolamo NE, Bayr KJ (2002) MODIS snow-cover products. Remote Sens Environ 83:181–194
Hasson S, Lucarini V, Khan MR, Petitta M, Bolch T, Gioli G (2014) Early 21st century snow cover state over the western river basins of the Indus River system. Hydrol Earth Syst Sci 18:4077–4100. https://doi.org/10.5194/hess-18-4077-2014
Hewitt K, Wake CP, Young GJ, David C (1989) Hydrological investigations at Biafo Glacier, Karakoram Himalaya, Pakistan: an important source of water for the Indus River. Ann Glaciol 13:103–108
Immerzeel WW, Bierkens MFP (2012) Asia’s water balance. Nat Geosci 5(12):841
Immerzeel WW et al (2009) Large-scale monitoring of snow cover and runoff simulation in Himalayan river basins using remote sensing. Remote Sens Environ 113(1):40–49
Immerzeel WW et al (2015) Reconciling high-altitude precipitation in the upper Indus basin with glacier mass balances and runoff. Hydrol Earth Syst Sci 19(11):4673
Lashkaripour GR, Hussaini SA (2007) Water resource management in Kabul river basin, easternAfghanistan. Environmentalist 2008(28):253–260
Lin H et al (2017) A decreasing glacier mass balance gradient from the edge of the Upper Tarim Basin to the Karakoram during 2000–2014. Scientific Rep. 7(1):6712
Lutz AF, Immerzeel WW, Kraaijenbrink PDA, Shrestha AB, Bierkens MFP (2016) Climate change impacts on the upper indus hydrology: sources, shifts and extremes, shifts and extremes. PLoS ONE. https://doi.org/10.1371/journal.pone.0165630
Malmrosa JK, Mernild SH, Wilson R, Tagesson T, Fensholta R (2018) Snow cover and snow albedo changes in the central Andes of Chile and Argentina from daily MODIS observations (2000–2016). Remote Sens Environ 209:240–252
Mukhopadhyay B, Khan A (2015) A reevaluation of the snowmelt and glacial melt in river flows within Upper Indus Basin and its significance in a changing climate. J Hydrol 527:119–132
Pellicciotti F et al (2012) Challenges and uncertainties in hydrological modeling of remote Hindu Kush–Karakoram–Himalayan (HKH) basins: suggestions for calibration strategies. Mountain Res Dev 32(1):39–50
Pfeffer TW, Arendt AA, Bliss A, Bolch T, Cogley J, Gardner AS, Hagen JO, Hock R, Kaser G, Kienholz C et al (2014) The Randolph Glacier inventory. J Glaciol 60:537–552
Shafiq MU, Ahmed P, Islam ZU, Joshi PK, Bhat WA (2018) Snow cover area change and its relations with climatic variability in Kashmir Himalayas India. Geocarto International. https://doi.org/10.1080/10106049.2018.1469675
Shrestha M, Koike T, Hirabayashi Y, Xue Y, Wang L, Rasul G, Ahmad B (2015) Integrated simulation of snow and glacier melt in water and energy balance-based, distributed hydrological modeling framework at Hunza River Basin of Pakistan Karakoram region. J Geophys Res Atmos 120(10):4889–4919
Tahir AA, Chevallier P, Arnaud Y, Ahmad B (2011) Snow cover dynamics and hydrological regime of the Hunza River Basin, Karakoram Range, Northern Pakistan. Hydrol Earth Syst Sci 15(7):2275–2290
Tahir AA, Adamowski JF, Chevallier P, Haq AU, Terzago S (2016) Comparative assessment of spatiotemporal snow cover changes and hydrological behavior of the Gilgit, Astore and Hunza River Basins (Hindukush–Karakoram–Himalaya region, Pakistan). Meteorol Atmos Phys 128(6):1–19
Tunnemeier T, Houben G (2005) Hydrogeology of the Kabul river basin, Part 1, Geology, aquifer characteristics, climate and hydrology. Federal Institute for Geosciences and Natural Resources (BGR), Hannover, Germany
Wi S, Yang YCE, Steinschneider S, Khalil A, Brown CM (2015) Calibration approaches for distributed hydrologic models in poorly gaged basins: implication for streamflow projections under climate change. Hydrol Earth Syst Sci 19:857–876
Wijngaard RR, Lutz AF, Nepal S, Khanal S, Pradhananga S, Shrestha AB, Immerzeel WW (2017) Future changes in hydro-climatic extremes in the Upper Indus, Ganges, and Brahmaputra River Basins. PLoS ONE 12(12):e0190224
Yao T, Thompson LG, Mosbrugger V, Zhang F, Ma Y, Luo T, Xu B, Yang X, Joswiak DR, Wang W, Joswiak ME (2012) Third pole environment (TPE). Environ Dev 3:52–64
Zhou Y, Li Zhiwei, Li JIA (2017) Slight glacier mass loss in the Karakoram region during the 1970s to 2000 revealed by KH-9 images and SRTM DEM. J Glaciol 63(238):331–342
Acknowledgements
The authors acknowledge with thanks the LEAD Pakistan for collaboration in this research work. The authors are also thankful to MODIS and SRTM DEM teams for providing snow covered and DEM data, respectively, free of cost.
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Masood, A., Hashmi, M. & Mushtaq, H. Spatio-Temporal Analysis of Early Twenty-First Century Areal Changes in the Kabul River Basin Cryosphere. Earth Syst Environ 2, 563–571 (2018). https://doi.org/10.1007/s41748-018-0066-6
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DOI: https://doi.org/10.1007/s41748-018-0066-6