Processes governing seasonal and interannual change of the Antarctic sea-ice area

Seasonal and interannual variabilities of sea-ice area in the Southern Ocean were examined using daily sea-ice concentration and ice velocity products for 2003–2019, derived from Advanced Microwave Scanning Radiometer for EOS (AMSR-E) and AMSR2 data. This study quantified the contributions to change...

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Published inJournal of oceanography Vol. 79; no. 2; pp. 109 - 121
Main Authors Kimura, Noriaki, Onomura, Tomoyuki, Kikuchi, Takashi
Format Journal Article
LanguageEnglish
Published Singapore Springer Nature Singapore 01.04.2023
Springer Nature B.V
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Abstract Seasonal and interannual variabilities of sea-ice area in the Southern Ocean were examined using daily sea-ice concentration and ice velocity products for 2003–2019, derived from Advanced Microwave Scanning Radiometer for EOS (AMSR-E) and AMSR2 data. This study quantified the contributions to changes in the sea-ice area due to sea-ice transport and local processes, including ice formation/melting and ice deformation. Regional differences in the processes of seasonal advance and retreat of sea ice were elucidated. In most regions, sea-ice area increases mainly due to new ice formation in the marginal ice zone during autumn and winter. However, in the Amundsen–Bellingshausen seas, ice melting occurs in the marginal ice zone, even during winter, and expansion of the ice cover is attributable mainly to off-ice transport. With regard to interannual variability, the maximum ice area for each year is highly correlated with increase of ice area attributable to the ice formation in the marginal ice zone. Revealed processes that controls sea-ice changes could help improve our understanding of the sea-ice response to climate change.
AbstractList Seasonal and interannual variabilities of sea-ice area in the Southern Ocean were examined using daily sea-ice concentration and ice velocity products for 2003–2019, derived from Advanced Microwave Scanning Radiometer for EOS (AMSR-E) and AMSR2 data. This study quantified the contributions to changes in the sea-ice area due to sea-ice transport and local processes, including ice formation/melting and ice deformation. Regional differences in the processes of seasonal advance and retreat of sea ice were elucidated. In most regions, sea-ice area increases mainly due to new ice formation in the marginal ice zone during autumn and winter. However, in the Amundsen–Bellingshausen seas, ice melting occurs in the marginal ice zone, even during winter, and expansion of the ice cover is attributable mainly to off-ice transport. With regard to interannual variability, the maximum ice area for each year is highly correlated with increase of ice area attributable to the ice formation in the marginal ice zone. Revealed processes that controls sea-ice changes could help improve our understanding of the sea-ice response to climate change.
Author Kikuchi, Takashi
Kimura, Noriaki
Onomura, Tomoyuki
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  givenname: Noriaki
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  surname: Kimura
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  email: kimura_n@aori.u-tokyo.ac.jp
  organization: Atmosphere and Ocean Research Institute, The University of Tokyo
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  givenname: Tomoyuki
  surname: Onomura
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  surname: Kikuchi
  fullname: Kikuchi, Takashi
  organization: Graduate School of Frontier Sciences, The University of Tokyo, Japan Agency for Marine-Earth Science and Technology
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CitedBy_id crossref_primary_10_1016_j_marpolbul_2024_116820
crossref_primary_10_5194_tc_17_701_2023
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Antarctic sea ice
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Snippet Seasonal and interannual variabilities of sea-ice area in the Southern Ocean were examined using daily sea-ice concentration and ice velocity products for...
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SubjectTerms Climate change
Deformation
Earth and Environmental Science
Earth Sciences
Freshwater & Marine Ecology
Ice cover
Ice formation
Ice melting
Melting
Oceanography
Original Article
Radiometers
Sea ice
Transport
Winter
Title Processes governing seasonal and interannual change of the Antarctic sea-ice area
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