The Effects of Sea-Ice Movement on Adélie Penguin Winter Migration Within the Ross

Global warming is disproportionately impacting polar regions, making it increasingly important to understand how and when wildlife depend on sea ice for their movements. Movement patterns within sea-ice fields have been much less studied compared to wind and ocean currents, even though sea ice is an...

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Bibliographic Details
Main Author: Dennis Jongsomjit
Other Authors: Ellen Hines, Jerry Davis, Grant Ballard
Format: Master Thesis
Language:English
Published: San Francisco State University 2022
Subjects:
Online Access:https://hdl.handle.net/20.500.12680/xg94hw31b
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spelling ftcalifstateuniv:oai:scholarworks:xg94hw31b 2024-09-30T14:26:41+00:00 The Effects of Sea-Ice Movement on Adélie Penguin Winter Migration Within the Ross Dennis Jongsomjit Ellen Hines Jerry Davis Grant Ballard 2022 https://hdl.handle.net/20.500.12680/xg94hw31b English eng San Francisco State University Science & Engineering Geographic Information Science http://hdl.handle.net/20.500.12680/xg94hw31b Copyright by Dennis Jongsomjit 2022 Masters Thesis 2022 ftcalifstateuniv https://doi.org/20.500.12680/xg94hw31b 2024-09-10T17:06:15Z Global warming is disproportionately impacting polar regions, making it increasingly important to understand how and when wildlife depend on sea ice for their movements. Movement patterns within sea-ice fields have been much less studied compared to wind and ocean currents, even though sea ice is an integral part of polar ecology. Adélie penguins (Pygoscelis adeliae) in the southern Ross Sea, Antarctica undergo the longest winter migration known for the species. Within and north of the Ross Sea, the Ross Gyre drives ocean circulation and the large-scale movement of sea-ice. We used remotely sensed ice movement data together with geolocation-based penguin movement data to test the hypothesis that penguins take advantage of sea-ice movement to aid their migration. We found that penguins travelled longer distances when their movement and sea ice-movement were aligned. Distances traveled were in part explained by which of two routes ("east" or "west") a penguin took. We found favorable sea-ice movement conditions occurred when penguins moved northward but ice support decreased through the winter. We also found that higher velocity of the Ross Gyre resulted in penguins being advected farther north, potentially into less productive waters and farther from their breeding colony. Changes in sea ice will have implications related to energy expenditure and ecological interactions and our findings provide further evidence that ice/ocean circulation patterns are important drivers of wildlife movement and life history patterns within the Ross Sea. https://doi.org/10.46569/20.500.12680/xg94hw31b Master Thesis Antarc* Antarctica Pygoscelis adeliae Ross Sea Sea ice Scholarworks from California State University Ross Sea
institution Open Polar
collection Scholarworks from California State University
op_collection_id ftcalifstateuniv
language English
description Global warming is disproportionately impacting polar regions, making it increasingly important to understand how and when wildlife depend on sea ice for their movements. Movement patterns within sea-ice fields have been much less studied compared to wind and ocean currents, even though sea ice is an integral part of polar ecology. Adélie penguins (Pygoscelis adeliae) in the southern Ross Sea, Antarctica undergo the longest winter migration known for the species. Within and north of the Ross Sea, the Ross Gyre drives ocean circulation and the large-scale movement of sea-ice. We used remotely sensed ice movement data together with geolocation-based penguin movement data to test the hypothesis that penguins take advantage of sea-ice movement to aid their migration. We found that penguins travelled longer distances when their movement and sea ice-movement were aligned. Distances traveled were in part explained by which of two routes ("east" or "west") a penguin took. We found favorable sea-ice movement conditions occurred when penguins moved northward but ice support decreased through the winter. We also found that higher velocity of the Ross Gyre resulted in penguins being advected farther north, potentially into less productive waters and farther from their breeding colony. Changes in sea ice will have implications related to energy expenditure and ecological interactions and our findings provide further evidence that ice/ocean circulation patterns are important drivers of wildlife movement and life history patterns within the Ross Sea. https://doi.org/10.46569/20.500.12680/xg94hw31b
author2 Ellen Hines
Jerry Davis
Grant Ballard
format Master Thesis
author Dennis Jongsomjit
spellingShingle Dennis Jongsomjit
The Effects of Sea-Ice Movement on Adélie Penguin Winter Migration Within the Ross
author_facet Dennis Jongsomjit
author_sort Dennis Jongsomjit
title The Effects of Sea-Ice Movement on Adélie Penguin Winter Migration Within the Ross
title_short The Effects of Sea-Ice Movement on Adélie Penguin Winter Migration Within the Ross
title_full The Effects of Sea-Ice Movement on Adélie Penguin Winter Migration Within the Ross
title_fullStr The Effects of Sea-Ice Movement on Adélie Penguin Winter Migration Within the Ross
title_full_unstemmed The Effects of Sea-Ice Movement on Adélie Penguin Winter Migration Within the Ross
title_sort effects of sea-ice movement on adélie penguin winter migration within the ross
publisher San Francisco State University
publishDate 2022
url https://hdl.handle.net/20.500.12680/xg94hw31b
geographic Ross Sea
geographic_facet Ross Sea
genre Antarc*
Antarctica
Pygoscelis adeliae
Ross Sea
Sea ice
genre_facet Antarc*
Antarctica
Pygoscelis adeliae
Ross Sea
Sea ice
op_relation http://hdl.handle.net/20.500.12680/xg94hw31b
op_rights Copyright by Dennis Jongsomjit 2022
op_doi https://doi.org/20.500.12680/xg94hw31b
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