Availability of fresh water in cold climate regions
Abstract Challenges related to the availability of fresh water in cold climate regions are discussed with emphasis on possible degradation of the quality of drinking water. The permafrost in this region has been consistent in making sure there is little drainage in the ground. This is important, as...
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2023
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crioppubl:10.1088/1757-899x/1294/1/012034 2024-06-02T08:04:12+00:00 Availability of fresh water in cold climate regions Awong, A D Gudmestad, O T 2023 http://dx.doi.org/10.1088/1757-899x/1294/1/012034 https://iopscience.iop.org/article/10.1088/1757-899X/1294/1/012034 https://iopscience.iop.org/article/10.1088/1757-899X/1294/1/012034/pdf unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining IOP Conference Series: Materials Science and Engineering volume 1294, issue 1, page 012034 ISSN 1757-8981 1757-899X journal-article 2023 crioppubl https://doi.org/10.1088/1757-899x/1294/1/012034 2024-05-07T14:04:02Z Abstract Challenges related to the availability of fresh water in cold climate regions are discussed with emphasis on possible degradation of the quality of drinking water. The permafrost in this region has been consistent in making sure there is little drainage in the ground. This is important, as fresh water is mainly supplied through melting water from snow and ice in the many winter months. Climate change and warmer weather plays a role in heating up the permafrost and increasing the rate of the melting snow. This has an impact on both the amount of water and potentially the drinking quality. In certain cold region areas, fresh water sources are located not far from the shore. With increased shorline erosion due to warming climate, the fresh water supply is in danger of being contaminated by salt water during large storm events. Furthermore, human activities such as road transport and sewage contamination do also have a significant impact on the water’s quality. A bowtie diagram will be used to illustrate the different risk factors and suggestions on how to maintain the quality of fresh water supplies in cold climate areas. The primary focus areas will be Isdammen, near Longyearbyen on Svalbard and Utqiagvik (formerly Barrow), Alaska. Article in Journal/Newspaper Barrow Ice Longyearbyen permafrost Svalbard Alaska IOP Publishing Longyearbyen Svalbard IOP Conference Series: Materials Science and Engineering 1294 1 012034 |
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Abstract Challenges related to the availability of fresh water in cold climate regions are discussed with emphasis on possible degradation of the quality of drinking water. The permafrost in this region has been consistent in making sure there is little drainage in the ground. This is important, as fresh water is mainly supplied through melting water from snow and ice in the many winter months. Climate change and warmer weather plays a role in heating up the permafrost and increasing the rate of the melting snow. This has an impact on both the amount of water and potentially the drinking quality. In certain cold region areas, fresh water sources are located not far from the shore. With increased shorline erosion due to warming climate, the fresh water supply is in danger of being contaminated by salt water during large storm events. Furthermore, human activities such as road transport and sewage contamination do also have a significant impact on the water’s quality. A bowtie diagram will be used to illustrate the different risk factors and suggestions on how to maintain the quality of fresh water supplies in cold climate areas. The primary focus areas will be Isdammen, near Longyearbyen on Svalbard and Utqiagvik (formerly Barrow), Alaska. |
format |
Article in Journal/Newspaper |
author |
Awong, A D Gudmestad, O T |
spellingShingle |
Awong, A D Gudmestad, O T Availability of fresh water in cold climate regions |
author_facet |
Awong, A D Gudmestad, O T |
author_sort |
Awong, A D |
title |
Availability of fresh water in cold climate regions |
title_short |
Availability of fresh water in cold climate regions |
title_full |
Availability of fresh water in cold climate regions |
title_fullStr |
Availability of fresh water in cold climate regions |
title_full_unstemmed |
Availability of fresh water in cold climate regions |
title_sort |
availability of fresh water in cold climate regions |
publisher |
IOP Publishing |
publishDate |
2023 |
url |
http://dx.doi.org/10.1088/1757-899x/1294/1/012034 https://iopscience.iop.org/article/10.1088/1757-899X/1294/1/012034 https://iopscience.iop.org/article/10.1088/1757-899X/1294/1/012034/pdf |
geographic |
Longyearbyen Svalbard |
geographic_facet |
Longyearbyen Svalbard |
genre |
Barrow Ice Longyearbyen permafrost Svalbard Alaska |
genre_facet |
Barrow Ice Longyearbyen permafrost Svalbard Alaska |
op_source |
IOP Conference Series: Materials Science and Engineering volume 1294, issue 1, page 012034 ISSN 1757-8981 1757-899X |
op_rights |
http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining |
op_doi |
https://doi.org/10.1088/1757-899x/1294/1/012034 |
container_title |
IOP Conference Series: Materials Science and Engineering |
container_volume |
1294 |
container_issue |
1 |
container_start_page |
012034 |
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1800748838437257216 |