Relevant bibliographies by topics / Upper Indus Basin

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers

Academic literature on the topic 'Upper Indus Basin'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Upper Indus Basin"

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Ali, S. H., I. Bano, R. B. Kayastha, and A. Shrestha. "COMPARATIVE ASSESSMENT OF RUNOFF AND ITS COMPONENTS IN TWO CATCHMENTS OF UPPER INDUS BASIN BY USING A SEMI DISTRIBUTED GLACIO-HYDROLOGICAL MODEL." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLII-2/W7 (September 14, 2017): 1487–94. http://dx.doi.org/10.5194/isprs-archives-xlii-2-w7-1487-2017.

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The hydrology of Upper Indus basin is not recognized well due to the intricacies in the climate and geography, and the scarcity of data above 5000 m a.s.l where most of the precipitation falls in the form of snow. The main objective of this study is to measure the contributions of different components of runoff in Upper Indus basin. To achieve this goal, the Modified positive degree day model (MPDDM) was used to simulate the runoff and investigate its components in two catchments of Upper Indus basin, Hunza and Gilgit River basins. These two catchments were selected because of their different glacier coverage, contrasting area distribution at high altitudes and significant impact on the Upper Indus River flow. The components of runoff like snow-ice melt and rainfall-base flow were identified by the model. The simulation results show that the MPDDM shows a good agreement between observed and modeled runoff of these two catchments and the effects of snow and ice are mainly reliant on the catchment characteristics and the glaciated area. For Gilgit River basin, the largest contributor to runoff is rain-base flow, whereas large contribution of snow-ice melt observed in Hunza River basin due to its large fraction of glaciated area. This research will not only contribute to the better understanding of the impacts of climate change on the hydrological response in the Upper Indus, but will also provide guidance for the development of hydropower potential and water resources assessment in these catchments.
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Archer, David. "Contrasting hydrological regimes in the upper Indus Basin." Journal of Hydrology 274, no. 1-4 (April 2003): 198–210. http://dx.doi.org/10.1016/s0022-1694(02)00414-6.

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Fowler, H. J., and D. R. Archer. "Conflicting Signals of Climatic Change in the Upper Indus Basin." Journal of Climate 19, no. 17 (September 1, 2006): 4276–93. http://dx.doi.org/10.1175/jcli3860.1.

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Abstract Temperature data for seven instrumental records in the Karakoram and Hindu Kush Mountains of the Upper Indus Basin (UIB) have been analyzed for seasonal and annual trends over the period 1961–2000 and compared with neighboring mountain regions and the Indian subcontinent. Strong contrasts are found between the behavior of winter and summer temperatures and between maximum and minimum temperatures. Winter mean and maximum temperature show significant increases while mean and minimum summer temperatures show consistent decline. Increase in diurnal temperature range (DTR) is consistently observed in all seasons and the annual dataset, a pattern shared by much of the Indian subcontinent but in direct contrast to both GCM projections and the narrowing of DTR seen worldwide. This divergence commenced around the middle of the twentieth century and is thought to result from changes in large-scale circulation patterns and feedback processes associated with the Indian monsoon. The impact of observed seasonal temperature trend on runoff is explored using derived regression relationships. Decreases of ∼20% in summer runoff in the rivers Hunza and Shyok are estimated to have resulted from the observed 1°C fall in mean summer temperature since 1961, with even greater reductions in spring months. The observed downward trend in summer temperature and runoff is consistent with the observed thickening and expansion of Karakoram glaciers, in contrast to widespread decay and retreat in the eastern Himalayas. This suggests that the western Himalayas are showing a different response to global warming than other parts of the globe.
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Hassan, Syed, and Hamza Khan. "Stochastic River Flow Modelling and Forecasting of Upper Indus Basin." Journal of Basic & Applied Sciences 11 (December 17, 2015): 630–36. http://dx.doi.org/10.6000/1927-5129.2015.11.84.

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Pomee, Muhammad Saleem, Moetasim Ashfaq, Bashir Ahmad, and Elke Hertig. "Modeling regional precipitation over the Indus River basin of Pakistan using statistical downscaling." Theoretical and Applied Climatology 142, no. 1-2 (June 23, 2020): 29–57. http://dx.doi.org/10.1007/s00704-020-03246-9.

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Abstract Complex processes govern spatiotemporal distribution of precipitation within the high-mountainous headwater regions (commonly known as the upper Indus basin (UIB)), of the Indus River basin of Pakistan. Reliable precipitation simulations particularly over the UIB present a major scientific challenge due to regional complexity and inadequate observational coverage. Here, we present a statistical downscaling approach to model observed precipitation of the entire Indus basin, with a focus on UIB within available data constraints. Taking advantage of recent high altitude (HA) observatories, we perform precipitation regionalization using K-means cluster analysis to demonstrate effectiveness of low-altitude stations to provide useful precipitation inferences over more uncertain and hydrologically important HA of the UIB. We further employ generalized linear models (GLM) with gamma and Tweedie distributions to identify major dynamic and thermodynamic drivers from a reanalysis dataset within a robust cross-validation framework that explain observed spatiotemporal precipitation patterns across the Indus basin. Final statistical models demonstrate higher predictability to resolve precipitation variability over wetter southern Himalayans and different lower Indus regions, by mainly using different dynamic predictors. The modeling framework also shows an adequate performance over more complex and uncertain trans-Himalayans and the northwestern regions of the UIB, particularly during the seasons dominated by the westerly circulations. However, the cryosphere-dominated trans-Himalayan regions, which largely govern the basin hydrology, require relatively complex models that contain dynamic and thermodynamic circulations. We also analyzed relevant atmospheric circulations during precipitation anomalies over the UIB, to evaluate physical consistency of the statistical models, as an additional measure of reliability. Overall, our results suggest that such circulation-based statistical downscaling has the potential to improve our understanding towards distinct features of the regional-scale precipitation across the upper and lower Indus basin. Such understanding should help to assess the response of this complex, data-scarce, and climate-sensitive river basin amid future climatic changes, to serve communal and scientific interests.
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Afzal, Jawad, Mark Williams, and Richard J. Aldridge. "Revised stratigraphy of the lower Cenozoic succession of the Greater Indus Basin in Pakistan." Journal of Micropalaeontology 28, no. 1 (May 1, 2009): 7–23. http://dx.doi.org/10.1144/jm.28.1.7.

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Abstract. A refined stratigraphy for the lower Cenozoic succession of the Greater Indus Basin in Pakistan is presented. This region preserves an important East Tethyan marine succession through the Paleocene–Eocene, but its interpretation in terms of regional (tectonic) and global (climatic) effects has been inhibited by poor stratigraphy. Established dinoflagellate, nannofossil, planktonic foraminiferal and shallow benthonic foraminiferal biostratigraphical data for the Greater Indus Basin in Pakistan are collated, reinterpreted (where necessary) and correlated with the global standard chronostratigraphy and biostratigraphy of the early Palaeogene. Inter-regional stratigraphical correlations for the Upper Indus Basin and Lower Indus Basin are resolved. Age-diagnostic larger benthonic foraminifera from the Late Paleocene Lockhart Formation are illustrated. These collective biostratigraphical data provide a means of interpreting the lithostratigraphy and physical stratigraphical relationships of the Palaeogene succession in terms of the interplay between local tectonics (India–Asia collision) and global sea-level change. The timing of the Tethys closure, initial and final contact of the Indian–Asian plates, and dispersal of land mammals on the Indian Plate are discussed and correlated in the stratigraphical record of the basin.
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Karki, Madhav Bahadur, Arun Bhakta Shrestha, Hans Hurni, Anne B. Zimmermann, and Susanne Wymann von Dach. "Focus Issue: Water Resources in the Upper Indus Basin and Beyond." Mountain Research and Development 32, no. 1 (February 2012): 3. http://dx.doi.org/10.1659/mrd.3201.

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Khattak, MS, MS Babel, and M. Sharif. "Hydro-meteorological trends in the upper Indus River basin in Pakistan." Climate Research 46, no. 2 (February 22, 2011): 103–19. http://dx.doi.org/10.3354/cr00957.

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Latif, Yasir, Ma Yaoming, and Muhammad Yaseen. "Spatial analysis of precipitation time series over the Upper Indus Basin." Theoretical and Applied Climatology 131, no. 1-2 (December 9, 2016): 761–75. http://dx.doi.org/10.1007/s00704-016-2007-3.

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Shrestha, Arun Bhakta, Debabrat Shukla, Neera Shrestha Pradhan, Sharmila Dhungana, Fayezurahman Azizi, Nisar Memon, Khalid Mohtadullah, et al. "Developing a science-based policy network over the Upper Indus Basin." Science of The Total Environment 784 (August 2021): 147067. http://dx.doi.org/10.1016/j.scitotenv.2021.147067.

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Dissertations / Theses on the topic "Upper Indus Basin"

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Forsythe, Nathan. "Investigating the impact of climate change on hydro-climatological variability and water resources in the Upper Indus Basin." Thesis, University of Newcastle upon Tyne, 2013. http://hdl.handle.net/10443/1886.

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The Indus is crucial for Pakistan; economically and for water and food security. This thesis makes substantial contributions to fundamental understanding of local hydro-climatological processes in the Upper Indus Basin (UIB), essential as changes to water resources potentially affect millions of people. Drawing on a range of available data sources, complex vertical gradients are identified in several climate variables including cloud cover. The study confirms previously identified seasonally and diurnally asymmetrical temperature trends, which result in year round increasing diurnal temperature range, continue to the recent record, and describes some of the underlying causal mechanisms. Furthermore, for the first time, a stochastic weather generator is used to provide downscaled time series for 2071-2100 for two contrasting “climate scenarios” for the UIB: (i) using change factors from a Regional Climate Model (RCM) under the SRES A2 emissions scenario, (ii) extrapolating from recent observed climatic trends. A new semi-distributed basin-scale hydrological model is assembled using existing and adapted model algorithms to simulate cryosphere-hydrology interactions, including snowmelt and basic glacial mechanics. Calibrated catchment models – one glacial (Hunza) and one snowmelt-dominated (Astore) regime – are run to provide probabilistic estimates of potential hydrological changes. The RCM-derived scenario – featuring strong summer warming (> 5°C) – projects large decreases in glacial volumes (>90% and >80% mass loss in Astore and Hunza respectively) and one month earlier peak flows. The historical trends-based scenario – featuring net annual warming (0.7°C) but moderate summer cooling (~1.5°C) – also projects earlier peak flows but stable glacial areas and suppression of summer runoff from energy input constraints on melting.
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Khan, Asim Jahangir [Verfasser]. "Estimating the Effects of Climate Change on the Water Resources in the Upper Indus Basin (UIB) / Asim Jahangir Khan." Kassel : Universitätsbibliothek Kassel, 2018. http://d-nb.info/1174850035/34.

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BAIG, MUHAMMAD SOHAIB. "IMPACTS OF CLIMATE CHANGE ON THE QUANTITY AND TIMING OF RIVER FLOW IN THE UPPER INDUS BASIN, KARAKORAM-HIMALAYA, PAKISTAN." Doctoral thesis, Kyoto University, 2021. http://hdl.handle.net/2433/265201.

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京都大学
新制・課程博士
博士(工学)
甲第23429号
工博第4884号
新制||工||1763(附属図書館)
京都大学大学院工学研究科社会基盤工学専攻
(主査)教授 田中 茂信, 准教授 田中 賢治, 准教授 佐山 敬洋
学位規則第4条第1項該当
Doctor of Philosophy (Engineering)
Kyoto University
DFAM
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Bashir, Furrukh, and Furrukh Bashir. "Quantified Assessment of the Meteorological Variables Facilitating the Establishment of the Karakoram Anomaly." Thesis, The University of Arizona, 2016. http://hdl.handle.net/10150/622832.

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Lofty Hindukush, Karakoram and Himalayan (HKH) mountain ranges centered in the Northern Pakistan are host to some of the world’s largest glaciers outside the Polar Regions and are a source of water for drinking and irrigation to the millions of people living downstream. With the increase in the global temperatures, glaciers are reported as retreating globally. However, some of the glaciers in the Karakoram mountain ranges are reported as surging with positive mass balance, especially since the 1990s. This phenomenon is described as "The Karakoram Anomaly". Various efforts have been made to explain the state and fate of the HKH glaciers in the recent past. However, they are limited to quantification of the change in temperature, precipitation and river runoff, or through their impact on future climate projections. For the HKH region, temperature fluctuations have been out of the phase with hemispheric trends for past several centuries. Therefore, climate change in this region is not solely the temperature effect on melting as compared to other glaciated regions. To identify the reasons for the establishment of the Karakoram Anomaly, monthly mean climatic variables for last five decades, reported from meteorological observatories at the valley floors in HKH region, are analyzed. In addition to the climatic variables of temperature and precipitation, monthly mean synoptic observations reported by meteorological observatories in both morning and afternoon, along with monthly mean radiosonde data are used. From these data the role of different near-surface and upper atmospheric meteorological variables in maintaining the positive mass balance of the glaciers and the development of the Karakoram Anomaly can be explained. An overall warming in the region is observed. The trends in the summer temperatures, which were reported as decreasing a decade ago, are now found as increasing in updated time series. However, the overall gradient is still negative. The winter mean and maximum temperatures are increasing with accelerated trends. Both maximum and minimum temperatures in summer are not diverging anymore and the diurnal temperature range is decreasing in the most recent decade. The afternoon cloudiness is found as increasing throughout the year except for spring, which is indicative of an increase in convective uplifting. Moreover, humidity is increasing all over the region; due to evaporation in the spring, from monsoon moisture advection in summer, and due to the recycling of monsoon moisture in autumn. Furthermore, near-surface wind speed and net radiation in the region are decreasing, explaining the decrease in the summer minimum temperature and the presence of the cloudy skies. The decrease in near-surface wind speed, and net radiation, and increase in water vapor pressure put a limit on the evapotranspiration process. In addition, winter and summer precipitation is increasing. The aridity index, which is based on the ratio of precipitation and reference evaporation, indicates that region is turning moisture surplus and energy deficient. Surface atmospheric pressure and 700 hPa geopotential height is increasing due to warming in the bottom layers of the troposphere. Nighttime inversion in the lower tropospheric layers is decreasing due to warming. Analysis of gridded observed and reanalysis datasets indicates that they are not presenting a signal of change in accordance with the instrumental record. Furthermore, it is found that meteorological conditions during the summer season are still favorable for the sustenance of glaciers whereas more melting may occur in the spring season that may increase the early season river flows and may affect lower lying portions of the debris-free glaciers.
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Ul, Hussan Waqas [Verfasser], and F. [Akademischer Betreuer] Nestmann. "Assessment of climate change and development of data based prediction models of sediment yields in Upper Indus Basin / Waqas Ul Hussan ; Betreuer: F. Nestmann." Karlsruhe : KIT-Bibliothek, 2020. http://d-nb.info/1215190719/34.

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Tahir, Adnan Ahmad. "Impact of climate change on the snow covers and glaciers in the Upper Indus River basin and its consequences on the water reservoirs (Tarbela reservoir) – Pakistan." Thesis, Montpellier 2, 2011. http://www.theses.fr/2011MON20056/document.

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L'économie du Pakistan, fondée sur l'agriculture, est hautement dépendante de l'approvisionnement en eau issu de la fonte de la neige et des glaciers du Haut Bassin de l'Indus (UIB) qui s'étend sur les chaînes de l'Himalaya, du Karakoram et de l'Hindukush. Il est par conséquent essentiel pour la gestion des ressources en eau d'appréhender la dynamique de la cryosphère (neige et glace), ainsi que les régimes hydrologiques de cette région dans le contexte de scénarios de changement climatique. La base de données satellitaire du produit de couverture neigeuse MODIS MOD10A2 a été utilisée de mars 2000 à décembre 2009 pour analyser la dynamique du couvert neigeux de l'UIB. Les données journalières de débits à 13 stations hydrométriques et de précipitation et température à 18 postes météorologiques ont été exploitées sur des périodes variables selon les stations pour étudier le régime hydro-climatique de la région. Les analyses satellitaires de la couverture neigeuse et glaciaire suggèrent une très légère extension de la cryosphère au cours de la dernière décade (2000‒2009) en contradiction avec la rapide fonte des glaciers observée dans la plupart des régions du monde. Le modèle « Snowmelt Runoff » (SRM), associé aux produits neige du capteur MODIS a été utilisé avec succès pour simuler les débits journaliers et étudier les impacts du changement climatique sur ces débits dans les sous-bassins à contribution nivo-glaciaire de l'UIB. L'application de SRM pour différents scénarios futurs de changement climatique indique un doublement des débits pour le milieu du siècle actuel. La variation des écoulement de l'UIB, la capacité décroissante des réservoirs existants (barrage de Tarbela) à cause de la sédimentation, ainsi que la demande croissante pour les différents usages de l'eau, laissent penser que de nouveaux réservoirs sont à envisager pour stocker les écoulements d'été et répondre aux nécessités de l'irrigation, de la production hydro-électrique, de la prévention des crues et de l'alimentation en eau domestique
Agriculture based economy of Pakistan is highly dependent on the snow and glacier melt water supplies from the Upper Indus River Basin (UIB), situated in the Himalaya, Karakoram and Hindukush ranges. It is therefore essential to understand the cryosphere (snow and ice) dynamics and hydrological regime of this area under changed climate scenarios, for water resource management. The MODIS MOD10A2 remote-sensing database of snow cover products from March 2000 to December 2009 was selected to analyse the snow cover dynamics in the UIB. A database of daily flows from 13 hydrometric stations and climate data (precipitation and temperature) from 18 gauging stations, over different time periods for different stations, was made available to investigate the hydro-climatological regime in the area. Analysis of remotely sensed cryosphere (snow and ice cover) data during the last decade (2000‒2009) suggest a rather slight expansion of cryosphere in the area in contrast to most of the regions in the world where glaciers are melting rapidly. The Snowmelt Runoff Model (SRM) integrated with MODIS remote-sensing snow cover products was successfully used to simulate the daily discharges and to study the climate change impact on these discharges in the snow and glacier fed sub-catchments of UIB. The application of the SRM under future climate change scenarios indicates a doubling of summer runoff until the middle of this century. This variation in the Upper Indus River flow, decreasing capacity of existing reservoirs (Tarbela Dam) by sedimentation and the increasing demand of water uses suggests that new reservoirs shall be planned for summer flow storage to meet with the needs of irrigation supply, increasing power generation demand, flood control and water supply
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Book chapters on the topic "Upper Indus Basin"

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Ali, Nahida, and Shakil A. Romshoo. "Stream Flow Changes and Glacier Recession in the Upper Indus Basin." In Geostatistical and Geospatial Approaches for the Characterization of Natural Resources in the Environment, 905–8. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-18663-4_140.

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Soncini, Andrea, Daniele Bocchiola, G. Confortola, E. Nana, A. Bianchi, R. Rosso, G. Diolaiuti, et al. "Hydrology of the Upper Indus Basin Under Potential Climate Change Scenarios." In Engineering Geology for Society and Territory - Volume 1, 43–49. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09300-0_9.

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Banerjee, Soumyadeep, Muhammad Zubair Anwar, Giovanna Gioli, Suman Bisht, Saleem Abid, Nusrat Habib, Sanjay Sharma, Sabarnee Tuladhar, and Azeem Khan. "An Index Based Assessment of Vulnerability to Floods in the Upper Indus Sub-Basin: What Role for Remittances?" In Migration, Risk Management and Climate Change: Evidence and Policy Responses, 3–23. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-42922-9_1.

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Forsythe, Nathan, David R. Archer, David Pritchard, and Hayley Fowler. "A Hydrological Perspective on Interpretation of Available Climate Projections for the Upper Indus Basin." In Indus River Basin, 159–79. Elsevier, 2019. http://dx.doi.org/10.1016/b978-0-12-812782-7.00008-4.

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Yu, Winston, Yi-Chen Yang, Andre Savitsky, Donald Alford, Casey Brown, James Wescoat, Dario Debowicz, and Sherman Robinson. "Hydrology and Glaciers in the Upper Indus Basin." In The Indus Basin of Pakistan, 57–76. The World Bank, 2013. http://dx.doi.org/10.1596/9780821398746_ch03.

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Mahmood, Shakeel, and Razia Rani. "Extent of 2014 Flood Damages in Chenab Basin Upper Indus Plain." In Natural Hazards - Risk Assessment and Vulnerability Reduction. IntechOpen, 2018. http://dx.doi.org/10.5772/intechopen.79687.

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Farooqi, A., N. Mushtaq, J. A. Khattak, I. Hussain, and A. van Geen. "Geographical controls on arsenic variability in groundwater of Upper Indus Basin, Punjab, Pakistan." In Environmental Arsenic in a Changing World, 36–38. CRC Press, 2019. http://dx.doi.org/10.1201/9781351046633-12.

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"A Geographic Information System (GIS) Based Assessment of Hydropower Potential within the Upper Indus Basin Pakistan." In Geospatial Technology for Water Resource Applications, 53–64. Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742: CRC Press, 2016. http://dx.doi.org/10.1201/9781315370989-5.

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Conference papers on the topic "Upper Indus Basin"

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Amin Khan, Khalid. "Regional 3D velocity model building: An Upper Indus Basin case study." In First International Meeting for Applied Geoscience & Energy. Society of Exploration Geophysicists, 2021. http://dx.doi.org/10.1190/segam2021-3595009.1.

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"Challenges on modelling a large river basin with scare data: a case study of the Indus upper catchment." In 20th International Congress on Modelling and Simulation (MODSIM2013). Modelling and Simulation Society of Australia and New Zealand (MSSANZ), Inc., 2013. http://dx.doi.org/10.36334/modsim.2013.l1.sugiura.

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Anwar Saleem, W. "Predicting Liquid Loading in a Gas Condensate Well by Using a Systematic Approach (Case Study – Upper Indus Basin)." In 6th Saint Petersburg International Conference and Exhibition. Netherlands: EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20140243.

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Lone, Suhail, and Gh Jeelani. "Stable water isotopic evidence for the moisture source and composition of surface runoff in Ladakh, upper Indus river basin (UIRB)." In 5th International Electronic Conference on Water Sciences. Basel, Switzerland: MDPI, 2020. http://dx.doi.org/10.3390/ecws-5-07903.

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Forsythe, N., C. G. Kilsby, H. J. Fowler, and D. Archer. "Assessment of climate pressures on glacier-melt and snowmelt-derived runoff in the Hindu Kush-Karakoram sector of the Upper Indus Basin." In BHS 3rd International Conference. British Hydrological Society, 2010. http://dx.doi.org/10.7558/bhs.2010.ic10.

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