author_facet Nakayama, Yoshihiro
Greene, Chad A.
Paolo, Fernando S.
Mensah, Vigan
Zhang, Hong
Kashiwase, Haruhiko
Simizu, Daisuke
Greenbaum, Jamin S.
Blankenship, Donald D.
Abe‐Ouchi, Ayako
Aoki, Shigeru
Nakayama, Yoshihiro
Greene, Chad A.
Paolo, Fernando S.
Mensah, Vigan
Zhang, Hong
Kashiwase, Haruhiko
Simizu, Daisuke
Greenbaum, Jamin S.
Blankenship, Donald D.
Abe‐Ouchi, Ayako
Aoki, Shigeru
author Nakayama, Yoshihiro
Greene, Chad A.
Paolo, Fernando S.
Mensah, Vigan
Zhang, Hong
Kashiwase, Haruhiko
Simizu, Daisuke
Greenbaum, Jamin S.
Blankenship, Donald D.
Abe‐Ouchi, Ayako
Aoki, Shigeru
spellingShingle Nakayama, Yoshihiro
Greene, Chad A.
Paolo, Fernando S.
Mensah, Vigan
Zhang, Hong
Kashiwase, Haruhiko
Simizu, Daisuke
Greenbaum, Jamin S.
Blankenship, Donald D.
Abe‐Ouchi, Ayako
Aoki, Shigeru
Geophysical Research Letters
Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
General Earth and Planetary Sciences
Geophysics
author_sort nakayama, yoshihiro
spelling Nakayama, Yoshihiro Greene, Chad A. Paolo, Fernando S. Mensah, Vigan Zhang, Hong Kashiwase, Haruhiko Simizu, Daisuke Greenbaum, Jamin S. Blankenship, Donald D. Abe‐Ouchi, Ayako Aoki, Shigeru 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2021gl094149 <jats:title>Abstract</jats:title><jats:p>The Totten ice shelf (TIS) in East Antarctica has received increasing attention in recent years due to high basal melt rates, which have been linked to a presence of warm modified Circumpolar Deep Water (mCDW) observed at the ice front. We show that mCDW on‐shelf intrusions towards the TIS strengthen when the Antarctic Slope Current (ASC) weakens. This demonstrates that the ASC has a blocking effect and ASC weakening leads to on‐shelf intrusions, as proposed by previous observational studies. The interannual variability of the ASC is controlled primarily by atmospheric and oceanic conditions beyond our regional model domain. We further show that heat intrusions onto the continental shelf off the TIS are not influenced by off‐shelf warming but are enhanced with coastal freshening, suggesting positive feedback whereby ice melt and freshening upstream could start a chain reaction, leading to increased melt, and further coastal freshening.</jats:p> Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier Geophysical Research Letters
doi_str_mv 10.1029/2021gl094149
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series Geophysical Research Letters
source_id 49
title Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_unstemmed Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_full Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_fullStr Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_full_unstemmed Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_short Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_sort antarctic slope current modulates ocean heat intrusions towards totten glacier
topic General Earth and Planetary Sciences
Geophysics
url http://dx.doi.org/10.1029/2021gl094149
publishDate 2021
physical
description <jats:title>Abstract</jats:title><jats:p>The Totten ice shelf (TIS) in East Antarctica has received increasing attention in recent years due to high basal melt rates, which have been linked to a presence of warm modified Circumpolar Deep Water (mCDW) observed at the ice front. We show that mCDW on‐shelf intrusions towards the TIS strengthen when the Antarctic Slope Current (ASC) weakens. This demonstrates that the ASC has a blocking effect and ASC weakening leads to on‐shelf intrusions, as proposed by previous observational studies. The interannual variability of the ASC is controlled primarily by atmospheric and oceanic conditions beyond our regional model domain. We further show that heat intrusions onto the continental shelf off the TIS are not influenced by off‐shelf warming but are enhanced with coastal freshening, suggesting positive feedback whereby ice melt and freshening upstream could start a chain reaction, leading to increased melt, and further coastal freshening.</jats:p>
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author Nakayama, Yoshihiro, Greene, Chad A., Paolo, Fernando S., Mensah, Vigan, Zhang, Hong, Kashiwase, Haruhiko, Simizu, Daisuke, Greenbaum, Jamin S., Blankenship, Donald D., Abe‐Ouchi, Ayako, Aoki, Shigeru
author_facet Nakayama, Yoshihiro, Greene, Chad A., Paolo, Fernando S., Mensah, Vigan, Zhang, Hong, Kashiwase, Haruhiko, Simizu, Daisuke, Greenbaum, Jamin S., Blankenship, Donald D., Abe‐Ouchi, Ayako, Aoki, Shigeru, Nakayama, Yoshihiro, Greene, Chad A., Paolo, Fernando S., Mensah, Vigan, Zhang, Hong, Kashiwase, Haruhiko, Simizu, Daisuke, Greenbaum, Jamin S., Blankenship, Donald D., Abe‐Ouchi, Ayako, Aoki, Shigeru
author_sort nakayama, yoshihiro
container_issue 17
container_start_page 0
container_title Geophysical Research Letters
container_volume 48
description <jats:title>Abstract</jats:title><jats:p>The Totten ice shelf (TIS) in East Antarctica has received increasing attention in recent years due to high basal melt rates, which have been linked to a presence of warm modified Circumpolar Deep Water (mCDW) observed at the ice front. We show that mCDW on‐shelf intrusions towards the TIS strengthen when the Antarctic Slope Current (ASC) weakens. This demonstrates that the ASC has a blocking effect and ASC weakening leads to on‐shelf intrusions, as proposed by previous observational studies. The interannual variability of the ASC is controlled primarily by atmospheric and oceanic conditions beyond our regional model domain. We further show that heat intrusions onto the continental shelf off the TIS are not influenced by off‐shelf warming but are enhanced with coastal freshening, suggesting positive feedback whereby ice melt and freshening upstream could start a chain reaction, leading to increased melt, and further coastal freshening.</jats:p>
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imprint_str_mv American Geophysical Union (AGU), 2021
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spelling Nakayama, Yoshihiro Greene, Chad A. Paolo, Fernando S. Mensah, Vigan Zhang, Hong Kashiwase, Haruhiko Simizu, Daisuke Greenbaum, Jamin S. Blankenship, Donald D. Abe‐Ouchi, Ayako Aoki, Shigeru 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2021gl094149 <jats:title>Abstract</jats:title><jats:p>The Totten ice shelf (TIS) in East Antarctica has received increasing attention in recent years due to high basal melt rates, which have been linked to a presence of warm modified Circumpolar Deep Water (mCDW) observed at the ice front. We show that mCDW on‐shelf intrusions towards the TIS strengthen when the Antarctic Slope Current (ASC) weakens. This demonstrates that the ASC has a blocking effect and ASC weakening leads to on‐shelf intrusions, as proposed by previous observational studies. The interannual variability of the ASC is controlled primarily by atmospheric and oceanic conditions beyond our regional model domain. We further show that heat intrusions onto the continental shelf off the TIS are not influenced by off‐shelf warming but are enhanced with coastal freshening, suggesting positive feedback whereby ice melt and freshening upstream could start a chain reaction, leading to increased melt, and further coastal freshening.</jats:p> Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier Geophysical Research Letters
spellingShingle Nakayama, Yoshihiro, Greene, Chad A., Paolo, Fernando S., Mensah, Vigan, Zhang, Hong, Kashiwase, Haruhiko, Simizu, Daisuke, Greenbaum, Jamin S., Blankenship, Donald D., Abe‐Ouchi, Ayako, Aoki, Shigeru, Geophysical Research Letters, Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier, General Earth and Planetary Sciences, Geophysics
title Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_full Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_fullStr Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_full_unstemmed Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_short Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
title_sort antarctic slope current modulates ocean heat intrusions towards totten glacier
title_unstemmed Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier
topic General Earth and Planetary Sciences, Geophysics
url http://dx.doi.org/10.1029/2021gl094149