TY - JOUR
T1 - Deciphering Patterns and Drivers of Heat and Carbon Storage in the Southern Ocean
AU - Chen, Haidi
AU - Morrison, Adele K.
AU - Dufour, Carolina O.
AU - Sarmiento, Jorge Louis
N1 - Publisher Copyright:
©2019. American Geophysical Union. All Rights Reserved.
PY - 2019/3/28
Y1 - 2019/3/28
N2 - The storage of anomalous heat and carbon in the Southern Ocean in response to increasing greenhouse gases greatly mitigates atmospheric warming and exerts a large impact on the marine ecosystem. However, the mechanisms driving the ocean storage patterns are uncertain. Here using recent hydrographic observations, we compare for the first time the spatial patterns of heat and carbon storage, which show substantial differences in the Southern Ocean, in contrast with the conventional view of simple passive subduction into the thermocline. Using an eddy-rich global climate model, we demonstrate that redistribution of the preindustrial temperature field is the dominant control on the heat storage pattern, whereas carbon storage largely results from passive transport of anthropogenic carbon uptake at the surface. Lastly, this study highlights the importance of realistic representation of wind and surface buoyancy flux in climate models to improve future projection of circulation change and thus heat and carbon storage.
AB - The storage of anomalous heat and carbon in the Southern Ocean in response to increasing greenhouse gases greatly mitigates atmospheric warming and exerts a large impact on the marine ecosystem. However, the mechanisms driving the ocean storage patterns are uncertain. Here using recent hydrographic observations, we compare for the first time the spatial patterns of heat and carbon storage, which show substantial differences in the Southern Ocean, in contrast with the conventional view of simple passive subduction into the thermocline. Using an eddy-rich global climate model, we demonstrate that redistribution of the preindustrial temperature field is the dominant control on the heat storage pattern, whereas carbon storage largely results from passive transport of anthropogenic carbon uptake at the surface. Lastly, this study highlights the importance of realistic representation of wind and surface buoyancy flux in climate models to improve future projection of circulation change and thus heat and carbon storage.
KW - Southern Ocean
KW - excess carbon storage
KW - excess heat storage
KW - residual overturning circulation
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U2 - 10.1029/2018GL080961
DO - 10.1029/2018GL080961
M3 - Article
AN - SCOPUS:85063342094
SN - 0094-8276
VL - 46
SP - 3359
EP - 3367
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 6
ER -