Sentences with phrase «amoc decadal variability»

Sevellec, F., and A. V. Fedorov, 2014b: Optimal excitation of AMOC decadal variability: links to the subpolar ocean.

Not exact matches

In a recent paper, Sanchez - Franks and Zhang show that the underlying physical driver for the decadal variability in the Gulf Stream path and the regional biogeochemical cycling is linked to the low - frequency variability of the large - scale ocean circulation in the Atlantic, also known as Atlantic meridional overturning circulation (AMOC).
Further, AMOC - induced decadal variability in chlorophyll and nutrient concentrations in the Gulf Stream region might be important for changes in the localized carbon cycle and fisheries at decadal timescales.
How can the CMIP6 decadal MIPs be used to understand AMOC variability and related climate impacts?
Specific attention is given to variability of the Atlantic Meridional Overturning Circulation (AMOC), which is likely the origin of a considerable part of decadal variability and predictability in the Atlantic Sector.
Buoyancy anomalies on the western boundary are key to decadal AMOC variability, but the origin of these buoyancy anomalies and how they are communicated meridionally is not clear.
On decadal timescales, AMOC variability involves a complex interplay between wind - driven and thermohaline (buoyancy - driven) processes.
If the transition zone indeed controls decadal AMOC variability, monitoring this region may enable scientists to measure and perhaps predict AMOC variability, with potential impacts for interannual - to - decadal climate predictions.
I linked studies showing a link of SAM and NAM to AMOC and the IPO and thus to a decadal to millennial scale climate variability.
And there are a bunch of different time - scales to consider (decadal to multi-centennial variability for the AMOC alone).
Translate the knowledge developed about AMOC variability and predictability mechanisms into reliable decadal climate forecasts.
Models and reconstructions seem to agree that the AMOC has substantial natural variability on decadal (10 - 100 years) time scales.
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