Modeling Lake Temperature Response to Climate Change in the Alaskan Arctic
This thesis study focuses on simulating lake temperature and ice duration for four lakes at the Arctic Long-Term Ecological Research site, near the Toolik Field Station in Alaska. Model projections were driven by the representative global climate model outputs under different carbon emission scenari...
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ftutahsudc:oai:digitalcommons.usu.edu:gradreports-2449 2023-06-11T04:08:33+02:00 Modeling Lake Temperature Response to Climate Change in the Alaskan Arctic Balkcom, Thomas 2019-12-01T08:00:00Z application/pdf https://digitalcommons.usu.edu/gradreports/1423 https://doi.org/10.26076/3054-3650 https://digitalcommons.usu.edu/context/gradreports/article/2449/viewcontent/Plan_B_Balkcom_A02239920.pdf unknown DigitalCommons@USU https://digitalcommons.usu.edu/gradreports/1423 doi:10.26076/3054-3650 https://digitalcommons.usu.edu/context/gradreports/article/2449/viewcontent/Plan_B_Balkcom_A02239920.pdf Copyright for this work is held by the author. Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Works not in the public domain cannot be commercially exploited without permission of the copyright owner. Responsibility for any use rests exclusively with the user. For more information contact the Institutional Repository Librarian at digitalcommons@usu.edu. All Graduate Plan B and other Reports climate change arctic lake temperature Alaska Environmental Indicators and Impact Assessment text 2019 ftutahsudc https://doi.org/10.26076/3054-3650 2023-05-04T17:45:49Z This thesis study focuses on simulating lake temperature and ice duration for four lakes at the Arctic Long-Term Ecological Research site, near the Toolik Field Station in Alaska. Model projections were driven by the representative global climate model outputs under different carbon emission scenarios. Results show that my simple lake model can reproduce historical lake temperature and ice duration observations, indicating the reliability of the model for future projections. Model projections show that JuneSeptember lake temperatures would increase by 4.3-5.8 °C from the historical period with most progressive carbon emission scenarios, but by 0.7-2.2 °C in the conservative scenarios. Results also indicate that in all carbon emission scenarios, the ice-off period would increase in duration by at least 10 days by 2100, but by as much as 25-30 days in the most progressive scenarios. In addition, while the timing of mixed lake conditions would shift with the timing of ice-off, the duration of mixing and onset of stratification would be unaffected by warming temperatures. This study provides important knowledge for modeling and predicting lake thermal processes for the Arctic region. Text Arctic Climate change Alaska Utah State University: DigitalCommons@USU Arctic Arctic Lake ENVELOPE(-130.826,-130.826,57.231,57.231) Four Lakes ENVELOPE(-126.826,-126.826,54.858,54.858) |
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Utah State University: DigitalCommons@USU |
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unknown |
topic |
climate change arctic lake temperature Alaska Environmental Indicators and Impact Assessment |
spellingShingle |
climate change arctic lake temperature Alaska Environmental Indicators and Impact Assessment Balkcom, Thomas Modeling Lake Temperature Response to Climate Change in the Alaskan Arctic |
topic_facet |
climate change arctic lake temperature Alaska Environmental Indicators and Impact Assessment |
description |
This thesis study focuses on simulating lake temperature and ice duration for four lakes at the Arctic Long-Term Ecological Research site, near the Toolik Field Station in Alaska. Model projections were driven by the representative global climate model outputs under different carbon emission scenarios. Results show that my simple lake model can reproduce historical lake temperature and ice duration observations, indicating the reliability of the model for future projections. Model projections show that JuneSeptember lake temperatures would increase by 4.3-5.8 °C from the historical period with most progressive carbon emission scenarios, but by 0.7-2.2 °C in the conservative scenarios. Results also indicate that in all carbon emission scenarios, the ice-off period would increase in duration by at least 10 days by 2100, but by as much as 25-30 days in the most progressive scenarios. In addition, while the timing of mixed lake conditions would shift with the timing of ice-off, the duration of mixing and onset of stratification would be unaffected by warming temperatures. This study provides important knowledge for modeling and predicting lake thermal processes for the Arctic region. |
format |
Text |
author |
Balkcom, Thomas |
author_facet |
Balkcom, Thomas |
author_sort |
Balkcom, Thomas |
title |
Modeling Lake Temperature Response to Climate Change in the Alaskan Arctic |
title_short |
Modeling Lake Temperature Response to Climate Change in the Alaskan Arctic |
title_full |
Modeling Lake Temperature Response to Climate Change in the Alaskan Arctic |
title_fullStr |
Modeling Lake Temperature Response to Climate Change in the Alaskan Arctic |
title_full_unstemmed |
Modeling Lake Temperature Response to Climate Change in the Alaskan Arctic |
title_sort |
modeling lake temperature response to climate change in the alaskan arctic |
publisher |
DigitalCommons@USU |
publishDate |
2019 |
url |
https://digitalcommons.usu.edu/gradreports/1423 https://doi.org/10.26076/3054-3650 https://digitalcommons.usu.edu/context/gradreports/article/2449/viewcontent/Plan_B_Balkcom_A02239920.pdf |
long_lat |
ENVELOPE(-130.826,-130.826,57.231,57.231) ENVELOPE(-126.826,-126.826,54.858,54.858) |
geographic |
Arctic Arctic Lake Four Lakes |
geographic_facet |
Arctic Arctic Lake Four Lakes |
genre |
Arctic Climate change Alaska |
genre_facet |
Arctic Climate change Alaska |
op_source |
All Graduate Plan B and other Reports |
op_relation |
https://digitalcommons.usu.edu/gradreports/1423 doi:10.26076/3054-3650 https://digitalcommons.usu.edu/context/gradreports/article/2449/viewcontent/Plan_B_Balkcom_A02239920.pdf |
op_rights |
Copyright for this work is held by the author. Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Works not in the public domain cannot be commercially exploited without permission of the copyright owner. Responsibility for any use rests exclusively with the user. For more information contact the Institutional Repository Librarian at digitalcommons@usu.edu. |
op_doi |
https://doi.org/10.26076/3054-3650 |
_version_ |
1768381853332406272 |