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2018 (v1)PublicationUploaded on: April 14, 2023
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2020 (v1)Publication
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Uploaded on: April 14, 2023 -
2018 (v1)Publication
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Uploaded on: April 14, 2023 -
2023 (v1)Publication
The Antarctic continental shelf is a significant sink for anthropogenic CO2 (Cant) due to its cold waters, high primary productivity, and unique circulation that allows it to store large amounts of organic and inorganic carbon into the deep ocean. However, climate change is currently altering the Antarctic marine carbon cycle, making...
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2018 (v1)Publication
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Uploaded on: April 14, 2023 -
2020 (v1)Publication
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Uploaded on: April 14, 2023 -
2023 (v1)Publication
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Uploaded on: February 14, 2024 -
2023 (v1)Publication
The production of Antarctic Bottom Water (AABW) is a crucial factor in determining the strength of the Meridional Overturning Circulation, and therefore plays a significant role in the ocean's contribution to the global climate. AABW is primarily formed in the Ross and Weddell Seas, with unique thermohaline characteristics. In recent years, a...
Uploaded on: February 14, 2024