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Автор: Grafiati
Опубліковано: 18 травня 2024

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Статті в журналах з теми "Himalaya watershed"

1

Kamboj, Nitin, A. K. Chopra, D. S. Malik, and G. P. Juyal. "Watershed characteristics of Shiwalik torrents at Sabhawala in Doon Valley." Environment Conservation Journal 11, no. 1&2 (June 18, 2010): 115–18. http://dx.doi.org/10.36953/ecj.2010.1223.

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In the foothills of Shiwalik Himalaya, torrents are the prominent seasonal land features and characterized by high sediment ladder flash flow during monsoon period. These torrents have low banks and thus the flow frequently over tops the banks and causes floods in foot hill region to agricultural plain area. In present study, morphological, water and soil characteristics were studied with special references to torrential behavior and flow mechanics of torrent at Sabhawala watershed in Doon Valley of Garhwal Himalaya. The torrent gradient had varied from 1-75 to 2-62 % with flow velocity was 0.30 - 0.95 ms-1, occurred in Sabhawala watershed. Different forms of soil texture of torrent were observed and pH slightly alkaline consisting organic matter (%) as 0.24-0.95 in different zones of torrent The present study will provide resource based data for remedial measurement of torrent in other watersheds of Himalayan region.
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2

Gurung, Sher Bahadur. "Soil Erosion Status of Nepal." NUTA Journal 8, no. 1-2 (December 31, 2021): 112–23. http://dx.doi.org/10.3126/nutaj.v8i1-2.44109.

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Soil erosion is one of the problems in Nepal because about 73 percent of the land surface is mountainous and still tectonically active where 60.43 percent people involved in agricultural activities. The paper assesses the soil erosion status based on ecological region and watershed boundary with population density. The ecological region determined based on elevation and the watershed boundary of Nepal was generated using the Advanced Spaceborne Thermal Emission and Reflection Radiometer–ASTER, 30m resolution Digital Elevation Model (DEM) of NASA's Earth Observing System (EOS) on May 14, 2010. The DEM data was processed using remote sensing technique then hydrological analysis conducted using remote sensing and geographic information system to delineate the watershed boundary. The study generates 19 watersheds based on available soil erosion data. The soil erosion rate of ecological zone and watershed are assessed with population data of Nepal from central bureau of statistic, 2011. There is below 50 people per square kilometer watersheds have average soil erosion rate (about 20 t ha-1/ y-1) and 100 to 500 people per square kilometer watersheds have high soil erosion rate ranges from 27 to 102 t ha-1/ y-1 . These scenarios partial follow the theory of Himalayan degradation. So that there is still environmental degradation is observed and it is needed in detail field based study of Himalaya degradation
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3

Rai, Suresh Chand, Eklabya Sharma, and Rakesh Chandra Sundriyal. "Conservation in the Sikkim Himalaya: Traditional Knowledge and Land-use of the Mamlay Watershed." Environmental Conservation 21, no. 1 (1994): 30–34. http://dx.doi.org/10.1017/s0376892900024048.

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The ecological problems, including degradation of fragile ecosystems, of the Himalaya are quite conspicuous. A rapid depletion of forest resources is the main cause of environmental degradation and economic deterioration. Watersheds are considered as a unit for natural resource management and development in hilly areas; therefore a case-study of Mamlay watershed of Sikkim is presented in this paper.The Mamley watershed presents a viable system having a gradient of altitude where almost all types of land-uses that are common in the eastern Himalaya are found. All the ethno-cultural groups of Sikkim are present in this watershed, although the agricultural sector provides the main land-use, followed by forestry. Most of the forested areas in the Himalaya have been purportedly destroyed for the expansion of agricultural land. A similar situation was experienced in the Mamlay watershed, where an increase of 12.79% of the land-area used for agriculture has been recorded in the past 40 years. The watershed being fragile, 62% of the area is under intensive agricultural practice. Land-use and spatial relationships in the perspective of conservation are presented in this paper.Great genetic diversity of agricultural crops and trees has been recorded in this small watershed. Conservation ethics of optimum utilization/production of the resources, following traditional practices without much degrading of the system which is believed to be sustainable, was practised earlier in the watershed. But recently, due to population pressure and fragmentation of farm-owning families, the balance of land-use, natural resource utilization, and conservation, has become perturbed. Examples of traditional adaptation, indigenous knowledge, and perception of conservation amongst farm-owning families, are also presented in the paper.
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4

Thayyen, R. J., and J. T. Gergan. "Role of glaciers in watershed hydrology: ''Himalayan catchment'' perspective." Cryosphere Discussions 3, no. 2 (July 15, 2009): 443–76. http://dx.doi.org/10.5194/tcd-3-443-2009.

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Abstract. A large number of Himalayan glacier catchments are under the influence of humid climate with snowfall in winter (November–April) and South-West monsoon in summer (June–September) dominating the regional hydrology. Such catchments are defined as ''Himalayan catchment'', where the glacier melt water contributes to the river flow during the period of annual high flows produced by the monsoon. Other two major glacio-hydrological regimes of the Himalaya are winter snow dominated Alpine catchments of the Kashmir and Karakoram region and cold-arid regions of the Ladakh mountain range. Factors influencing the river flow variations in a ''Himalayan catchment'' were studied in a micro scale glacier catchment in the Garhwal Himalaya, covering an area of 77.8 km2. Discharge data generated from three hydrometric stations established at different altitudes of the Din Gad stream during the summer ablation period of 1998, 1999, 2000, 2001, 2003 and 2004. These data has been analysed along with winter/summer precipitation, temperature and mass balance data of the Dokriani glacier to study the role of the glacier and precipitation in determining the runoff variations along the stream continuum from the glacier snout to 2360 m a.s.l. Study shows that the inter-annual runoff variations in a ''Himalayan glacier catchment'' is directly linked with the precipitation rather than mass balance changes of the glacier. Study suggest that warming induced initial increase of glacier degraded runoff and subsequent decline is a glaciers mass balance response and cannot be translated as river flow response in a ''Himalayan catchment'' as suggested by the IPCC, 2007. Study also suggest that the glacier runoff critically influence the headwater river flows during the years of low summer discharge and proposes that the Himalayan catchment could experience higher river flows and positive glacier mass balance regime together in association with strong monsoon. This paper intended to highlight the importance of creating credible knowledge on the Himalayan cryospheric processes to develop a global outlook on river flow response to cryospheric change and locally sustainable water resources management strategies.
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5

Bartarya, S. K. "Watershed management strategies in Central Himalaya." Land Use Policy 8, no. 3 (July 1991): 177–84. http://dx.doi.org/10.1016/0264-8377(91)90029-i.

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6

Parihar, DS. "Disaster events and management in the Himalayan Watershed Gori Ganga, Kumaun Himalaya." International Journal of Geography, Geology and Environment 4, no. 1 (January 1, 2022): 89–100. http://dx.doi.org/10.22271/27067483.2022.v4.i1b.87.

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7

Kothyari, U. C., Raaj Ramsankaran, D. Sathish Kumar, S. K. Ghosh, and Nisha Mendiratta. "Geospatial-based automated watershed modeling in Garhwal Himalaya." Journal of Hydroinformatics 12, no. 4 (January 28, 2010): 502–20. http://dx.doi.org/10.2166/hydro.2010.024.

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An automated GIS tool and its computational outcomes on the spatial distribution of runoff and soil erosion are presented. The developed tool, named Automated Soil Erosion Assessment Tool (ASEAT), simulates runoff and soil erosion rates based on the concept of erosion processes suggested by Morgan–Morgan–Finney (MMF) in 1984. ASEAT is provided with a user-friendly graphical user interface (GUI) to interact with the users. The computational algorithms used are made fully automated and have been developed using the ERDAS Macro Language (EML) and Spatial Macro Language (SML). The developed modelling methodology is applied to the data of an experimental watershed of Pathri Rao in the Indian lower Himalayan region. Generated spatial distribution of runoff potential and soil erosion rates for the studied watershed using ASEAT are depicted by maps. The model-computed surface runoff potential (145.63 mm) available in the watershed seems fair when compared with the runoff depth (176.07 mm) observed at the watershed outlet. The derived estimates of soil erosion are validated, albeit qualitatively, with field observations and seem reliable for making decisions on the adoption of soil erosion conservative measures in the watershed.
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8

Negi, Raghuveer, Sarswati Prakash Sati, Ashish Rawat, Tripti Jayal, Vikram Sharma, Parvendra Kumar, and Gambhir Singh Chauhan. "Assessment of soil erosion using WSA and SPR techniques for Giri watershed, Himachal Pradesh, NW Himalaya, India." Disaster Advances 16, no. 6 (May 15, 2023): 18–44. http://dx.doi.org/10.25303/1606da18044.

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A watershed is the result of several geomorphic processes such as weathering, erosion, degradation and aggradation which are influenced by several factors viz. tectonics, lithology, climate, landslides and mass wasting processes etc. In a tropical climate, watersheds contribute a significant amount of eroded material which is reflecting the impact of lithology, precipitation, tectonics, relief and anthropogenic activities. In the Himalayan region besides significant heterogeneity in lithology, stratigraphy, structure and tectonics, it is observed that variability is exhibited in climatic conditions over a small region. These factors contribute to the development of geomorphic landforms and are best studied in watersheds or river basins. In the present study, Giri Watershed (GW) is assessed to contemplate susceptibility to erosion for 66 sub-watersheds using geomorphic parameters. The prioritization of subwatersheds has been done using Weighted Sum Analysis (WSA) and Sediment Production Rate (SPR) methods. The quantitative analysis of subwatersheds is categorized into different priority classes viz. very high, high, moderate, low and very low, among which 27 subwatersheds have very high to high susceptibility to erosion.
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9

Meraj, Gowhar, Tanzeel Khan, Shakil A. Romshoo, Majid Farooq, Kumar Rohitashw, and Bashir Ahmad Sheikh. "An Integrated Geoinformatics and Hydrological Modelling-Based Approach for Effective Flood Management in the Jhelum Basin, NW Himalaya." Proceedings 7, no. 1 (November 15, 2018): 8. http://dx.doi.org/10.3390/ecws-3-05804.

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In the present study, using static land system parameters, such as geomorphology, land cover, and relief, we calculated the water yield potential (RP) of all the watersheds of the Jhelum basin (Kashmir Valley) using the analytical hierarchy process (AHP) based watershed evaluation model (AHP-WEM). The results revealed that among the 24 watersheds of the Jhelum basin, the Vishav watershed, with the highest RP, is the fastest water yielding catchment of the Jhelum basin followed by Bringi, Lidder, Kuthar, Sind, Madhumati, Rembiara, Sukhnag, Dal, Wular-II, Romshi, Sandran, Ferozpur, Viji-Dhakil, Ningal, Lower Jhelum, Pohru, Arin, Doodganga, Arapal, Anchar, Wular-I, Gundar, and Garzan in the case of a same intensity storm event. The results were validated with the mean annual peak discharge values of the watersheds and a strong positive correlation of 0.71 was found. Further, for the forecasting of the floods in the watersheds that had a small lag time, such as in the case of Vishaw, Bringi, and Lidder, we evaluated the performance of the HEC-GeoHMS hydrological model to simulate stream discharge during storm events. It was observed that the model performs well for August-September period with a strong positive correlation (0.94) between the observed and simulated discharge and hence could be used as a flood forecasting model for this period in the region.
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10

Ahmad, Sarfaraz, and Khatib Khan. "Impact of Elevation - Glaciation - Tectonics on landscape characteristics of the watersheds in Bhagirathi valley, Garhwal Himalaya." Journal of The Indian Association of Sedimentologists 37, no. 2 (December 31, 2020): 141–47. http://dx.doi.org/10.51710/jias.v37i2.110.

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Terrain attributes of watersheds i.e., mean , maximum, minimum elevation, mean slope elevation, mean aspect, HI (Hypsometrical Integral), Plan and Profile curvature index were determined using ASTER DEM in Bhagirathi basin, Uttaarakhand. These attributes are used in determine the impact of elevation, glaciations and tectonic processes on terrain characteristics of the watersheds. The scatter diagrame between altitude and terrain attribute were used to analyse th impact of altitude and impact of glacition is revealed through Box Whisker diagram using moderate and fully glacier watersheds. The results indicated that permanent snowline altitude is important that determine the watershed density in particular elevation and bear direct relationship with area and degree of glaciations. It is found that slope, STD of elevation in glacier basin, profile and plan curvature, relief influenced by glaciations.
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Дисертації з теми "Himalaya watershed"

1

Sharma, Purnima. "Ecological linkages of carbon dynamics in relation to land-use/cover change in a Himalaya watershed." Thesis, University of North Bengal, 2003. http://hdl.handle.net/123456789/842.

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2

Asay, Maria Nicole. "Quantification of glacier melt volume in the Indus River watershed." BYU ScholarsArchive, 2011. https://scholarsarchive.byu.edu/etd/2684.

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Quantifying the contribution of glaciers to water resources is particularly important in locations where glaciers may provide a large percentage of total river discharge. In some remote locations, direct field measurements of melt rates are difficult to acquire, so alternate approaches are needed. Positive degree-day modeling (PDD) of glacier melt is a valuable tool to making first order approximations of the volume of melt coming from glaciers. In this study, a PDD-melt model is applied to glaciers in the Indus River watershed located in Afghanistan, China, India, and Pakistan. Here, millions of people rely on the water from the Indus River, which previous work suggests may be heavily dependent on glacier melt from high mountain regions in the northern part of the watershed. In this region, the PDD melt model calculates the range of melt volumes from more than 45,000 km2 of glaciated area. It relies on a limited suite of input variables for glaciers in the region: elevation, temperature, temperature lapse rate, melt factor, and surface area. Three global gridded climate datasets were used to determine the bounds of temperature at each glacier: UEA CRU CL 2.0, UEA CRU TS 2.1, and NCEP/NCAR 40 year reanalysis. The PDD melt model was run using four different melt scenarios: mean, minimum, maximum, and randomized. These scenarios account for differences in melt volume not captured by temperature, and take uncertainties in all input parameters into account to bound the possible melt volume. The spread in total melt volume from the model scenarios ranges between 27 km3 and 439 km3. While the difference in these calculations is large, it is highly likely the real value falls within this range. Importantly, even the smallest model volume output is a significant melt water value. This suggests that even when forcing the absolute smallest volume of melt, the glacier contribution to the Indus watershed is significant. In addition to providing information about melt volume, this model helps to highlight glaciers with the greatest contribution to total melt. Despite differences in the individual climate models, the spatial pattern in glacier melt is similar, with glaciers contributing the majority of total melt volume occurring in similar geographic regions regardless of which temperature dataset is used. For regions where glacier areas are reasonably well-constrained, contributions from individual glaciers can be quantified. Importantly, less than 5% of glaciers contribute at least 70% of the total melt volume in the watershed. The majority of these glaciers are in Pakistan, the region with the largest percentage of known glaciers with large surface areas at lower elevations. In addition to calculating current melt volumes over large glaciated areas, this model can also be used to determine future melt rates under differing climate scenarios. By applying suggested future regional temperature change to the temperature data, the impact on average melt rate over the watershed was found to increase from 3.02 m/year to 4.69 m/year with up to 2 °C temperature increase. Assuming glacier area remains relatively constant over short time periods, this would amount to a 145 km3 increase in melt volume.
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3

Zokaib, Suhail. "Rainfall, runoff and soil degradation in the Hindu Kush-Himalayas - a case study in Hilkot watershed Pakistan." Thesis, University of British Columbia, 2011. http://hdl.handle.net/2429/36646.

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Surface runoff and sediment transport are often considered as the two most important hydrological parameters in water resources engineering. Surface soil erosion from most of the areas is a serious threat to sustainable agriculture and sediment accumulation in reservoirs. An extensive runoff and soil erosion study was conducted in Hilkot watershed, Pakistan. The watershed consists of four major land uses including degraded, forests, agricultural, and pasture lands. The main objective of this dissertation was to provide a better understanding of the hydrologic and land use behavior of the watershed. Moreover, the goals were: 1) to calculate and compare annual rainfall, runoff and soil losses with their seasonal distribution from different land uses; 2) to establish rainfall, runoff and soil loss relationships; and 3) to develop a calibrated mathematical model for runoff and soil loss estimation. Overall, the results obtained from this research demonstrated that the Hilkot watershed falls in the monsoon region with about 38% rainfall occurred in the monsoon period (July to September). The average annual rainfall found in the study area was 1160 mm. In all the erosion plots, almost 50% of the runoff and soil loss occurred during the monsoon period. The mean maximum runoff was from the degraded plot (674 m³/ha/y), while the minimum was observed at the pasture plot (310 m³/ha/y). The average runoffs on other land uses were 529 and 460 m³/ha/y from the forest and agriculture plots, respectively. The average maximum soil loss was recorded from the degraded plot (6.5 t/ha/y) and the average minimum (1.8 t/ha/y) was on the pasture plot. Similarly, the average soil losses were 3.3 and 3.4 t/ha/y measured from the forest and agricultural plots, respectively. Polynomial regression analyses were developed for predicting rainfall, runoff and soil loss relationships and showed a reasonable correlation among the parameters. A mathematical model was also developed and calibrated with field data (using a genetic algorithm approach) to estimate the total runoff and soil loss for various land uses. The model reproduced the measured field data reasonably well and it indicated the highest and lowest runoff and soil loss for degraded and pasture lands, respectively.
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4

Shams, El Din Ahmed. "Human occupation development in the High Mountains of Sinai Peninsula, Egypt with Alpine and Himalayan reflections in the light of rural-urban development ‘socio-economy’, semi-arid watershed management ‘cocio-ecology’ and land use policy ‘governance’." Thesis, IMT Alti Studi Lucca, 2013. http://e-theses.imtlucca.it/101/1/Shams_el_din_ahmed_phdthesis.pdf.

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In theory and practice, centralization, sub-optimization, and transborder crisscross culture have been extensively discussed over decades with limited progress on the interdisciplinary level in the developing countries (precisely in the remote semi-arid highland regions: the High Mountains of Sinai Peninsula). Post the Egyptian National Reforms Revolution of January 25, 2011 CE, the need for a decentralized governance structure in the Arab Republic of Egypt surfaced once again as one of the very demanding reforms for socio-economic and socio-ecological sustainable development., accounting to several domestic (e.g. social strategy, behaviour and stratification; traditional tribal system ‘kinship seniority’ and alliances; social homogeneity subdivisions; survival strategies and interaction; urbanization, trade and mobility; productivity and resources exploitation) and external ones (e.g. cross political and economic interest, and warfare). A Comparative Corporate Governance Model ‘CCGM’ based on three integrated sub-models is conducted to identify, address, and feasibly resolve the previously discussed issues: 1 a newly modified timeline-based version of Quality Function Deployment ‘QFD’, addressing the socioeconomic aspects and needs (i.e. issues of interest; domestic and global practice); 2 heritage-based arid/semi-arid watershed management model, utilizing the heritage economic-conservation and experimental archeology methodologies and techniques as the core for a low cost model; 3 dynamic sub-monitoring model, enabling multilevel decision making actions (i.e. predictive/preventive); all under routine and breaking governance events In practice, the high mountains act as a system under pre-defined criteria. The CCGM resolves the legislative and administrative constraints (e.g. land use and ownership) by decentralizing the planning and decision making process on the micro-local/municipal and macro-regional/governorate levels. It is an interdisciplinary approach towards natural-cultural heritage conservation and preservation under the sustainability and decrease theories while being subjected to a domestic profit maximization trend. It is conducted inSinai Peninsula with reflections on the Alpine and Himalayan contexts.
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5

Verdhen, Anand. "Snow and glacier melt simulation for hydrology in a typical himalayan watershed." Thesis, 2013. http://localhost:8080/iit/handle/2074/6722.

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Книги з теми "Himalaya watershed"

1

Negi, Sharad Singh. Integrated watershed development in the Himalaya. Dehra Dun: Bishen Singh Mahendra Pal Singh, 2010.

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2

1957-, Pandey B. P., and Uttaranchal (India). Water Management Directorate., eds. Watershed management in Himalaya: Concept and strategy. Nainital: Published for Watershed Management Directorate, Uttaranchal by Gyanodaya Prakashan, 2002.

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3

E, Sharma, and G.B. Pant Institute of Himalayan Environment & Development., eds. Integrated watershed management: A case study in Sikkim Himalaya. Nainital: Published for the G.B. Pant Institute of Himalayan Environment & Development by Gyanodaya Prakashan, 1992.

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4

L, Dhyani H., and Central Soil & Water Conservation Research & Training Institute., eds. Socio-economic analysis of a participatory integrated watershed management in Garhwal Himalaya: Fakot watershed. Dehradun, India: Central Soil and Water Conservation Research and Training Institute, 1997.

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5

Environmental geomorphology and watershed management: A study from central Himalaya. New Delhi: Concept Pub. Co., 2011.

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6

Seminar, on Action Research in Khulgad Micro Watershed of Kosi Catchment in Central Himalaya (1992 Naini Tal India). Sustainable & replicable eco-development in Central Himalaya/Uttarakhand: Proceedings of the Seminar on Action Research in Khulgad Micro Watershed of Kosi Catchment in Central Himalaya. Almora: Shri Almora Book Depot, 1997.

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7

Regmi, Ganga Ram, and Falk Huettmann, eds. Hindu Kush-Himalaya Watersheds Downhill: Landscape Ecology and Conservation Perspectives. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36275-1.

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8

1964-, Pathak J. K., ed. Himalayan environment, water quality of the drainage basins. Almora: Shree Almora Book Depot, 1992.

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9

Anu, Kapur, ed. Resource use and environmental degradation in the Himalayas: The Kali Watershed. New Delhi: Mudrit, 1999.

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10

Balla, Mohan K. Natural resources management: Reviews and research in the Himalayan watersheds. Edited by Tribhuvana Viśvavidyālaya. Institute of Forestry, Norwegian Programme for Higher Education, Research, and Training, and HIMUNET Project. Pokhara: Tribhuvan University, Institute of Forestry, 2009.

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Частини книг з теми "Himalaya watershed"

1

Baral, Hem Sagar, and Carol Inskipp. "Birds of Nepal: Their Status and Conservation Especially with Regards to Watershed Perspectives." In Hindu Kush-Himalaya Watersheds Downhill: Landscape Ecology and Conservation Perspectives, 435–58. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36275-1_22.

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2

Pant, N. C., Meenaxi, Anand Kumar, and Upasana Choudhury. "Detecting Vegetation and Timberline Dynamics in Pinder Watershed Central Himalaya Using Geospatial Techniques." In Geospatial Modeling for Environmental Management, 213–21. Boca Raton: CRC Press, 2022. http://dx.doi.org/10.1201/9781003147107-14.

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3

Prajapati, Jamuna, Falk Huettmann, Tashi Rapte Ghale, and Ganga Ram Regmi. "The Annapurna Conservation Area Project (ACAP): Towards a Success Story in Landscape Feature and Watershed Conservation Management." In Hindu Kush-Himalaya Watersheds Downhill: Landscape Ecology and Conservation Perspectives, 473–96. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36275-1_24.

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4

Kumar, Manish, and Pankaj Kumar. "Snow Cover Dynamics and Timberline Change Detection of Yamunotri Watershed Using Multi-temporal Satellite Imagery." In Climate Change, Glacier Response, and Vegetation Dynamics in the Himalaya, 391–99. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-28977-9_20.

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5

Sati, Vishwambhar Prasad. "Garhwal Himalaya—Potential of Cash Crops in Attaining Food Security and Enhancing Livelihoods—Khanda Gad Watershed Case Study." In Perspectives on Geographical Marginality, 289–99. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-50998-3_18.

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6

Paul, James Xavier, and Daya Shanker. "Use of GIS for Hypsometric Analysis for Determining Erosion Proneness of Mandakini Watershed, Lesser Himalaya, Uttarakhand, North India." In Lecture Notes in Civil Engineering, 613–24. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-99-1459-3_49.

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7

Rawat, Ashish, M. P. S. Bisht, Y. P. Sundriyal, Pranaya Diwate, and Swapnil Bisht. "Prioritization and Quantitative Assessment of Dhundsir Gad Using RS and GIS: Implications for Watershed Management, Planning and Conservation, Garhwal Himalaya, Uttarakhand." In Geospatial Technology for Landscape and Environmental Management, 165–89. Singapore: Springer Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-7373-3_8.

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8

Rawat, J. S., and Geeta Rawat. "Dying and Dwindling of Non-glacial Fed Rivers Under Climate Change (A Case Study from the Upper Kosi Watershed, Central Himalaya, India)." In Geoecology of Landscape Dynamics, 53–74. Singapore: Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-2097-6_5.

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9

Rawat, J. S., M. Kumar, V. Viswas, V. S. Rawat, and N. Gahlaut. "The Impact of Climate Change on the Shifting of the Vegetation Line in the Indian Himalaya: A Case Study from the Kutiyangti Watershed." In Globalization and Marginalization in Mountain Regions, 191–98. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-32649-8_14.

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Merz, Juerg, Rolf Weingartner, Pradeep M. Dangol, Madhav P. Dhakal, Bhawani S. Dongol, Gopal Nakarmi, and Pravakar B. Shah. "Water Management Issues in Middle Mountain Catchments of the Nepal Himalayas: The Downstream Perspective." In Integrated Watershed Management, 160–75. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3769-5_14.

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Тези доповідей конференцій з теми "Himalaya watershed"

1

Rana, Samagra, and Vaibhav Gupta. "Watershed Management in the Indian Himalayan Region: Issues and Challenges." In World Environmental and Water Resources Congress 2009. Reston, VA: American Society of Civil Engineers, 2009. http://dx.doi.org/10.1061/41036(342)527.

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2

Verdhen, Anand, Bhagu R. Chahar, and Om P. Sharma. "Snowmelt Runoff Simulation Using HEC-HMS in a Himalayan Watershed." In World Environmental and Water Resources Congress 2013. Reston, VA: American Society of Civil Engineers, 2013. http://dx.doi.org/10.1061/9780784412947.317.

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3

Majumdar, Sayantan, Praveen K. Thakur, Ling Chang, Shashi Kumar, and Ryan G. Smith. "SPACEBORNE POLARIMETRIC SAR INTERFEROMETRY FOR SNOW DEPTH RETRIEVAL IN THE NORTHWESTERN HIMALAYAN WATERSHED." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338916.

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4

Saran, Sameer, Geert Sterk, and Suresh Kumar. "Optimal land use/cover classification using remote sensing imagery for hydrological modelling in a Himalayan watershed." In Remote Sensing, edited by Christopher M. U. Neale, Manfred Owe, and Guido D'Urso. SPIE, 2007. http://dx.doi.org/10.1117/12.769056.

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5

Majumdar, Sayantan, Praveen K. Thakur, Ling Chang, and Shashi Kumar. "X-Band Polarimetric Sar Copolar Phase Difference for Fresh Snow Depth Estimation in the Northwestern Himalayan Watershed." In IGARSS 2019 - 2019 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2019. http://dx.doi.org/10.1109/igarss.2019.8898884.

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6

Nautiyal, Nanda, and Vir Singh. "Carbon-Nitrogen Ratios in Rangeland Soils in Various Agriculture Response Units in Three Watersheds in the Central Himalayas, India." In XXV International Grassland Congress. Berea, KY 40403: International Grassland Congress 2023, 2023. http://dx.doi.org/10.52202/071171-0069.

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7

Pandey, Shachi, Parmanand Kumar, and Vijendra Pal Panwar. "Remote sensing for assessing soil erosion susceptibility of the lesser Himalayan watershed by Multi Criteria Analysis (MCA) of morphometry, hypsometry, and land cover." In Remote Sensing for Agriculture, Ecosystems, and Hydrology, edited by Christopher M. Neale and Antonino Maltese. SPIE, 2018. http://dx.doi.org/10.1117/12.2325313.

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Звіти організацій з теми "Himalaya watershed"

1

Kotru, R., S. Sharma, E. Sharma, and T. Hofer. Everybody Lives Upstream- The Watershed Approach for the Changing Climate of the Hindu Kush Himalaya; ICIMOD Working Paper 2017/11. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2017. http://dx.doi.org/10.53055/icimod.662.

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2

Kotru, R., S. Sharma, E. Sharma, and T. Hofer. Everybody Lives Upstream- The Watershed Approach for the Changing Climate of the Hindu Kush Himalaya; ICIMOD Working Paper 2017/11. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2017. http://dx.doi.org/10.53055/icimod.662.

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3

Panday, K. K. Watershed Management Experiences In The Hindu Kush-Himalayas; An Overview. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1991. http://dx.doi.org/10.53055/icimod.107.

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4

Panday, K. K. Watershed Management Experiences In The Hindu Kush-Himalayas; An Overview. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1991. http://dx.doi.org/10.53055/icimod.107.

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5

Ali, A., B. Bhadra, S. M. Ruhulamin, P. Alirol, K. G. Tejwani, M. M. D. Joshi, and G. M. Khattak. Watershed Management Experiences In The Hindu Kush-Himalayan Region; Summaries of Review Country Studies. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1991. http://dx.doi.org/10.53055/icimod.106.

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Ali, A., B. Bhadra, S. M. Ruhulamin, P. Alirol, K. G. Tejwani, M. M. D. Joshi, and G. M. Khattak. Watershed Management Experiences In The Hindu Kush-Himalayan Region; Summaries of Review Country Studies. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1991. http://dx.doi.org/10.53055/icimod.106.

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7

White, R., and S. K. Bhuchar. Resource Constraints and Management Options in Mountain Watersheds of the Himalayas; Proceedings of a Regional Workshop held 8-9 December, 2003, in Kathmandu, Nepal. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 2005. http://dx.doi.org/10.53055/icimod.435.

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8

Watershed Management; Proceedings of the International Workshop on Watershed Management in the Hindu Kush-Himalaya Region. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1986. http://dx.doi.org/10.53055/icimod.26.

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9

Watershed Management; Proceedings of the International Workshop on Watershed Management in the Hindu Kush-Himalaya Region. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1986. http://dx.doi.org/10.53055/icimod.26.

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10

Managing Mountain Watersheds; Report of the International Workshop on Watershed Management in the Hindu Kush-Himalayan Region. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD), 1985. http://dx.doi.org/10.53055/icimod.18.

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