Seasonal source water and flow path insights from a year of sampling in the Chamkhar Chhu basin of Central Bhutan
Hydrologic processes that control river flow in Bhutan’s Chamkhar Chhu basin are important for understanding water supply vulnerability to downstream populations in a changing climate. Seasonal source waters and flow paths of streamflow of the basin were determined using isotopic and geochemical tra...
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ftdoajarticles:oai:doaj.org/article:868c3c0547dc48c88d143a9197a39940 2023-05-15T14:14:31+02:00 Seasonal source water and flow path insights from a year of sampling in the Chamkhar Chhu basin of Central Bhutan Dendup Tshering Tshewang Dendup Holly A. Miller Alice F. Hill Alana M. Wilson 2020-01-01T00:00:00Z https://doi.org/10.1080/15230430.2020.1743148 https://doaj.org/article/868c3c0547dc48c88d143a9197a39940 EN eng Taylor & Francis Group http://dx.doi.org/10.1080/15230430.2020.1743148 https://doaj.org/toc/1523-0430 https://doaj.org/toc/1938-4246 1523-0430 1938-4246 doi:10.1080/15230430.2020.1743148 https://doaj.org/article/868c3c0547dc48c88d143a9197a39940 Arctic, Antarctic, and Alpine Research, Vol 52, Iss 1, Pp 146-160 (2020) stable isotopes brahmaputra headwaters two-component hydrograph separation groundwater glacier outflow eastern himalaya Environmental sciences GE1-350 Ecology QH540-549.5 article 2020 ftdoajarticles https://doi.org/10.1080/15230430.2020.1743148 2022-12-31T04:50:30Z Hydrologic processes that control river flow in Bhutan’s Chamkhar Chhu basin are important for understanding water supply vulnerability to downstream populations in a changing climate. Seasonal source waters and flow paths of streamflow of the basin were determined using isotopic and geochemical tracers for water year 2016. Samples including surface water, groundwater, glacier meltwater, and precipitation were collected in premonsoon, monsoon, and postmonsoon seasons along an elevation transect from 2,538 to 5,158 m. Solute trends in surface waters demonstrate the major influence that tributaries can have on main stem hydrochemistry and the increasingly important role of groundwater below 3,500 m. Groundwater’s role in flow is supported by a two-component hydrograph separation using SO42− as a tracer and shows that groundwater is especially important to river flow in the premonsoon. Source waters to river flow were calculated using δ18O as a tracer, indicating that rain and meltwater are more evenly important across the elevation transect in the early monsoon period than in the postmonsoon period when ice melt contributions rapidly wane with distance from the glacier. Article in Journal/Newspaper Antarctic and Alpine Research Arctic Directory of Open Access Journals: DOAJ Articles Arctic, Antarctic, and Alpine Research 52 1 146 160 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
stable isotopes brahmaputra headwaters two-component hydrograph separation groundwater glacier outflow eastern himalaya Environmental sciences GE1-350 Ecology QH540-549.5 |
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stable isotopes brahmaputra headwaters two-component hydrograph separation groundwater glacier outflow eastern himalaya Environmental sciences GE1-350 Ecology QH540-549.5 Dendup Tshering Tshewang Dendup Holly A. Miller Alice F. Hill Alana M. Wilson Seasonal source water and flow path insights from a year of sampling in the Chamkhar Chhu basin of Central Bhutan |
topic_facet |
stable isotopes brahmaputra headwaters two-component hydrograph separation groundwater glacier outflow eastern himalaya Environmental sciences GE1-350 Ecology QH540-549.5 |
description |
Hydrologic processes that control river flow in Bhutan’s Chamkhar Chhu basin are important for understanding water supply vulnerability to downstream populations in a changing climate. Seasonal source waters and flow paths of streamflow of the basin were determined using isotopic and geochemical tracers for water year 2016. Samples including surface water, groundwater, glacier meltwater, and precipitation were collected in premonsoon, monsoon, and postmonsoon seasons along an elevation transect from 2,538 to 5,158 m. Solute trends in surface waters demonstrate the major influence that tributaries can have on main stem hydrochemistry and the increasingly important role of groundwater below 3,500 m. Groundwater’s role in flow is supported by a two-component hydrograph separation using SO42− as a tracer and shows that groundwater is especially important to river flow in the premonsoon. Source waters to river flow were calculated using δ18O as a tracer, indicating that rain and meltwater are more evenly important across the elevation transect in the early monsoon period than in the postmonsoon period when ice melt contributions rapidly wane with distance from the glacier. |
format |
Article in Journal/Newspaper |
author |
Dendup Tshering Tshewang Dendup Holly A. Miller Alice F. Hill Alana M. Wilson |
author_facet |
Dendup Tshering Tshewang Dendup Holly A. Miller Alice F. Hill Alana M. Wilson |
author_sort |
Dendup Tshering |
title |
Seasonal source water and flow path insights from a year of sampling in the Chamkhar Chhu basin of Central Bhutan |
title_short |
Seasonal source water and flow path insights from a year of sampling in the Chamkhar Chhu basin of Central Bhutan |
title_full |
Seasonal source water and flow path insights from a year of sampling in the Chamkhar Chhu basin of Central Bhutan |
title_fullStr |
Seasonal source water and flow path insights from a year of sampling in the Chamkhar Chhu basin of Central Bhutan |
title_full_unstemmed |
Seasonal source water and flow path insights from a year of sampling in the Chamkhar Chhu basin of Central Bhutan |
title_sort |
seasonal source water and flow path insights from a year of sampling in the chamkhar chhu basin of central bhutan |
publisher |
Taylor & Francis Group |
publishDate |
2020 |
url |
https://doi.org/10.1080/15230430.2020.1743148 https://doaj.org/article/868c3c0547dc48c88d143a9197a39940 |
genre |
Antarctic and Alpine Research Arctic |
genre_facet |
Antarctic and Alpine Research Arctic |
op_source |
Arctic, Antarctic, and Alpine Research, Vol 52, Iss 1, Pp 146-160 (2020) |
op_relation |
http://dx.doi.org/10.1080/15230430.2020.1743148 https://doaj.org/toc/1523-0430 https://doaj.org/toc/1938-4246 1523-0430 1938-4246 doi:10.1080/15230430.2020.1743148 https://doaj.org/article/868c3c0547dc48c88d143a9197a39940 |
op_doi |
https://doi.org/10.1080/15230430.2020.1743148 |
container_title |
Arctic, Antarctic, and Alpine Research |
container_volume |
52 |
container_issue |
1 |
container_start_page |
146 |
op_container_end_page |
160 |
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1766286939145633792 |