Global meridional overturning circulation inferred from a data-constrained ocean & sea-ice model
Our current understanding of the global meridional overturning circulation (GMOC) is revisited using a surface-forced ocean model simulation constrained by global hydrographic data. The derived GMOC is qualitatively consistent with previous observation-based studies and further provides enhanced spatial details in the sources, transformations, and transports of major global water masses including in poorly observed regions. Several important but relatively underexplored aspects of the GMOC are highlighted, including complex but vigorous heavy-to-light water mass transformation that occurs in the Indo-Pacific and Southern Oceans, and the role of the equatorial Pacific upwelling in closing the GMOC circuit. These and other key aspects of the GMOC are poorly captured in a surface-forced ocean model simulation without the temperature and salinity corrections, suggesting that current climate models do not realistically simulate the GMOC and the associated global heat, salt, and carbon balances.
document
http://n2t.net/ark:/85065/d7cn76zs
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2019-02-16T00:00:00Z
Copyright 2019 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
2023-08-18T18:26:44.030115