Recent evidence for a strengthening COâ sink in the Southern Ocean from carbonate system measurements in the Drake Passage (2002-2015)
We present a 13âyear (2002-2015) semimonthly time series of the partial pressure of COâ in surface water (pCOâsurf) and other carbonate system parameters from the Drake Passage. This record shows a clear increase in the magnitude of the sea-air pCOâ gradient, indicating strengthening of the COâ sink in agreement with recent large-scale analyses of the world oceans. The rate of increase in pCOâsurf north of the Antarctic Polar Front (APF) is similar to the atmospheric pCOâ (pCOâatm) trend, whereas the pCOâsurf increase south of the APF is slower than the pCOâatm trend. The high-frequency surface observations indicate that an absence of a winter increase in total COâ (TCOâ) and cooling summer sea surface temperatures are largely responsible for increasing COâ uptake south of the APF. Muted winter trends in surface TCOâ also provide temporary stability to the carbonate system that is already close to undersaturation with respect to aragonite.
document
https://n2t.org/ark:/85065/d7cf9rfc
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2015-09-28T00:00:00Z
Copyright 2015 American Geophysical Union.
None
OpenSky Support
UCAR/NCAR - Library
PO Box 3000
Boulder
80307-3000
name: homepage
pointOfContact
OpenSky Support
UCAR/NCAR - Library
PO Box 3000
Boulder
80307-3000
name: homepage
pointOfContact
2025-12-26T03:02:23.052362