نتایج جستجو برای: himalayan river

تعداد نتایج: 87130  

2005
Mikaël Attal Jérôme Lavé

Understanding and quantifying fluvial transport and bedrock abrasion processes have become major concerns in modeling landform response to tectonic and climatic forcing. Recent theoretical and experimental investigations have in particular stressed the importance of sediment supply and size in controlling bedrock incision rate. Many studies on the downstream evolution of pebble size have focuse...

2007
Babar A. Shah

Arsenic contamination in groundwater affecting West Bengal (India) and Bangladesh is a serious environmental problem. Contamination is extensive in the low-lying areas of Bhagirathi–Ganga delta, located mainly to the east of the Bhagirathi River. A few isolated As-contaminated areas occur west of the Bhagirathi River and over the lower parts of the Damodar river fan-delta. The Damodar being a P...

2002
Beth Pratt Douglas W. Burbank Arjun Heimsath

The steep-walled bedrock gorges of the Greater Himalayan rivers currently lack significant stored sediment, suggesting that fluvial erosion and transport capacity outpace the supply of sediment from adjacent hillsides. Despite this appearance of sustained downcutting, such rivers can become choked with sediments and aggrade during intervals of higher precipitation. Cosmogenic dating (10Be and 2...

Journal: :Hydrology and Earth System Sciences 2022

Abstract. Streamflow regimes are rapidly changing in many regions of the world. Attribution these changes to specific hydrological processes and their underlying climatic anthropogenic drivers is essential formulate an effective water policy. Traditional approaches hydrologic attribution rely on ability infer through development catchment-scale models. However, such challenging implement practi...

2015
NAMRATA SAXENA

Department of Obstetric and Gynaecology, Himalayan Institute of Medical Science, Dehradun, Pin code248140 Associate Professor, Department of Obstetric and Gynaecology, Himalayan Institute of Medical Science, Dehradun Pin code248140 Associate Professor, Department of Microbiology, Himalayan Institute of Medical Science, Dehradun-Pin code248140 PG resident , Department of Obstetric and Gynaecolog...

1998
Albert Galy Christian France-Lanord Louis A. Derry

Himalayan rivers have very unusual Sr characteristics and their budget cannot be achieved by simple mixing between silicate and carbonate even if carbonates are radiogenic. We present Sr, O, and C isotopic data from river and rain water, bedload and bedrock samples for the western and central Nepal Himalaya and Bangladesh, including the monsoon season. Central Himalayan rivers receive Sr from s...

2012
H. Wulf B. Bookhagen

The sediment flux through Himalayan rivers directly impacts water quality and is important for sustaining agriculture as well as maintaining drinking-water and hydropower generation. Despite the recent increase in demand for these resources, little is known about the triggers and sources of extreme sediment flux events, which lower water quality and account for extensive hydropower reservoir fi...

2005
Bodo Bookhagen Rasmus C. Thiede Manfred R. Strecker

The interplay between topography and Indian summer monsoon circulation profoundly controls precipitation distribution, sediment transport, and river discharge along the Southern Himalayan Mountain Front (SHF). The Higher Himalayas form a major orographic barrier that separates humid sectors to the south and arid regions to the north. During the Indian summer monsoon, vortices transport moisture...

Hydrological components in a river basin can get adversely affected by climate change in coming future. Manipur River basin lies in the extreme northeast region of India nestled in the lesser Himalayan ranges and it is under severe pressure from anthropogenic and natural factors. Basin is un-gauged as it lies in remote location and suffering from large data scarcity. This paper explores the imp...

2000
J. Lavé J. P. Avouac

We analyze geomorphic evidence of recent crustal deformation in the subHimalaya of central Nepal, south of the Kathmandu Basin. The Main Frontal Thrust fault (MFT), which marks the southern edge of the sub-Himalayan fold belt, is the only active structure in that area. Active fault bend folding at the MFT is quantified from structural geology and fluvial terraces along the Bagmati and Bakeya Ri...

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