Dense water production in the seas around Antarctica is a key process for century-scale carbon storage, slowing global warming. Results from an advanced new model reveal the prospect of system changes that may greatly reduce the efficiency of this carbon storage by the end of this century
Carbon capture and storage by southern polar benthos is potentially the largest negative feedback on...
Antarctic coastal polynyas produce Dense Shelf Water, a precursor to Antarctic Bottom Waters that su...
During the last termination (from ~18 000 years ago to ~9000 years ago), the climate significantly w...
Antarctic Bottom Water formation, such as in the Weddell Sea, is an efficient vector for carbon sequ...
Antarctic Bottom Water formation, such as in the Weddell Sea, is an efficient vector for carbon sequ...
Palaeo-oceanographic reconstructions indicate that the distribution of global ocean water masses has...
All authors acknowledge support from the National Science Foundation. R.F. acknowledges support from...
Feedbacks on climate change so far identified are predominantly positive, enhancing the rate of chan...
The Southern Ocean plays a critical role in the uptake, transport, and storage of carbon by the glob...
The ocean's ability to store large quantities of carbon, combined with the millennial longevity over...
© 2020 National Academy of Sciences. All rights reserved.The Southern Ocean (SO) played a prominent ...
The Antarctic Ice Sheet stores water equivalent to 58 m in global sea-level rise. We show in simulat...
International audienceDuring glacial periods, atmospheric CO 2 concentration increases and decreases...
The ocean carbon cycle plays a fundamental role in the Earth’s climate system, on decadal to multi-m...
The prevailing hypothesis for lower atmospheric carbon dioxide (CO2) concentrations during glacial p...
Carbon capture and storage by southern polar benthos is potentially the largest negative feedback on...
Antarctic coastal polynyas produce Dense Shelf Water, a precursor to Antarctic Bottom Waters that su...
During the last termination (from ~18 000 years ago to ~9000 years ago), the climate significantly w...
Antarctic Bottom Water formation, such as in the Weddell Sea, is an efficient vector for carbon sequ...
Antarctic Bottom Water formation, such as in the Weddell Sea, is an efficient vector for carbon sequ...
Palaeo-oceanographic reconstructions indicate that the distribution of global ocean water masses has...
All authors acknowledge support from the National Science Foundation. R.F. acknowledges support from...
Feedbacks on climate change so far identified are predominantly positive, enhancing the rate of chan...
The Southern Ocean plays a critical role in the uptake, transport, and storage of carbon by the glob...
The ocean's ability to store large quantities of carbon, combined with the millennial longevity over...
© 2020 National Academy of Sciences. All rights reserved.The Southern Ocean (SO) played a prominent ...
The Antarctic Ice Sheet stores water equivalent to 58 m in global sea-level rise. We show in simulat...
International audienceDuring glacial periods, atmospheric CO 2 concentration increases and decreases...
The ocean carbon cycle plays a fundamental role in the Earth’s climate system, on decadal to multi-m...
The prevailing hypothesis for lower atmospheric carbon dioxide (CO2) concentrations during glacial p...
Carbon capture and storage by southern polar benthos is potentially the largest negative feedback on...
Antarctic coastal polynyas produce Dense Shelf Water, a precursor to Antarctic Bottom Waters that su...
During the last termination (from ~18 000 years ago to ~9000 years ago), the climate significantly w...
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