Icing - Renewable Water Source and Resource

Abstract The icing phenomena occurs in Mongolia every winter, same places where groundwater overflow on ice on surface waterbed, create next ice sheet and create extended ice storage. This phenomenon is important parameters in hydrological cycle and surface water regime for semi-arid, cold regions....

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Published in:IOP Conference Series: Earth and Environmental Science
Main Author: Narantsogt, Nasanbayar
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2021
Subjects:
Online Access:http://dx.doi.org/10.1088/1755-1315/690/1/012046
https://iopscience.iop.org/article/10.1088/1755-1315/690/1/012046
https://iopscience.iop.org/article/10.1088/1755-1315/690/1/012046/pdf
id crioppubl:10.1088/1755-1315/690/1/012046
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spelling crioppubl:10.1088/1755-1315/690/1/012046 2024-06-02T08:08:19+00:00 Icing - Renewable Water Source and Resource Narantsogt, Nasanbayar 2021 http://dx.doi.org/10.1088/1755-1315/690/1/012046 https://iopscience.iop.org/article/10.1088/1755-1315/690/1/012046 https://iopscience.iop.org/article/10.1088/1755-1315/690/1/012046/pdf unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining IOP Conference Series: Earth and Environmental Science volume 690, issue 1, page 012046 ISSN 1755-1307 1755-1315 journal-article 2021 crioppubl https://doi.org/10.1088/1755-1315/690/1/012046 2024-05-07T13:56:11Z Abstract The icing phenomena occurs in Mongolia every winter, same places where groundwater overflow on ice on surface waterbed, create next ice sheet and create extended ice storage. This phenomenon is important parameters in hydrological cycle and surface water regime for semi-arid, cold regions. The highly continental, semi-arid and cold region has a high variability in river discharge depending on precipitation, with a general tendency towards decreasing water availability due to increasing air temperatures and thus rising potential evaporation. In this study considered understanding natural process of creating icing, due to keep water source as in ice form on surface in dry season. From March to May icing meltwater recharge groundwater and river flow while river is non-flow condition. Some year’s in April riverbed dry without ice in valley under highly mountains, but upper side is cold and water source is still in snow and ice form. Therefore, icing in river valley could recharge surface water by melting where is cold on top mountains river origin but under valley riverbed no snow, ice cover. In this paper written icing process code by MATLAB using energy change between water, air and ice. When we are promoting naturally ice storing or build icing then winter coldness creates ice storage thus artificially recharge surface water resources in dry season like April. The ice storage amount and simulation results shown that recharge groundwater in dry season is icing method one of the possibilities which creates and build huge ice storages in winter. That is new technology keep water in ice form through winter and recharge surface and groundwater in dry season. Article in Journal/Newspaper Ice Sheet IOP Publishing IOP Conference Series: Earth and Environmental Science 690 1 012046
institution Open Polar
collection IOP Publishing
op_collection_id crioppubl
language unknown
description Abstract The icing phenomena occurs in Mongolia every winter, same places where groundwater overflow on ice on surface waterbed, create next ice sheet and create extended ice storage. This phenomenon is important parameters in hydrological cycle and surface water regime for semi-arid, cold regions. The highly continental, semi-arid and cold region has a high variability in river discharge depending on precipitation, with a general tendency towards decreasing water availability due to increasing air temperatures and thus rising potential evaporation. In this study considered understanding natural process of creating icing, due to keep water source as in ice form on surface in dry season. From March to May icing meltwater recharge groundwater and river flow while river is non-flow condition. Some year’s in April riverbed dry without ice in valley under highly mountains, but upper side is cold and water source is still in snow and ice form. Therefore, icing in river valley could recharge surface water by melting where is cold on top mountains river origin but under valley riverbed no snow, ice cover. In this paper written icing process code by MATLAB using energy change between water, air and ice. When we are promoting naturally ice storing or build icing then winter coldness creates ice storage thus artificially recharge surface water resources in dry season like April. The ice storage amount and simulation results shown that recharge groundwater in dry season is icing method one of the possibilities which creates and build huge ice storages in winter. That is new technology keep water in ice form through winter and recharge surface and groundwater in dry season.
format Article in Journal/Newspaper
author Narantsogt, Nasanbayar
spellingShingle Narantsogt, Nasanbayar
Icing - Renewable Water Source and Resource
author_facet Narantsogt, Nasanbayar
author_sort Narantsogt, Nasanbayar
title Icing - Renewable Water Source and Resource
title_short Icing - Renewable Water Source and Resource
title_full Icing - Renewable Water Source and Resource
title_fullStr Icing - Renewable Water Source and Resource
title_full_unstemmed Icing - Renewable Water Source and Resource
title_sort icing - renewable water source and resource
publisher IOP Publishing
publishDate 2021
url http://dx.doi.org/10.1088/1755-1315/690/1/012046
https://iopscience.iop.org/article/10.1088/1755-1315/690/1/012046
https://iopscience.iop.org/article/10.1088/1755-1315/690/1/012046/pdf
genre Ice Sheet
genre_facet Ice Sheet
op_source IOP Conference Series: Earth and Environmental Science
volume 690, issue 1, page 012046
ISSN 1755-1307 1755-1315
op_rights http://creativecommons.org/licenses/by/3.0/
https://iopscience.iop.org/info/page/text-and-data-mining
op_doi https://doi.org/10.1088/1755-1315/690/1/012046
container_title IOP Conference Series: Earth and Environmental Science
container_volume 690
container_issue 1
container_start_page 012046
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