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The idea is to switch off (or modify) winds in particular basin(s). For eg: The ocean circulation in North Atlantic is a lot more dependent on the global ocean circulation than the North Pacific, as can be seen in all the experiments we have done so far (see here). By switching off winds in the North Pacific, we expect the basin to not affect (or be affected) by global circulation.
However, the meridional transport of heat flux will be reduced in the North Pacific, and it will be interesting to see whether in equilibrium, the total heat flux into the ocean reduces or whether the Atlantic ocean transfers more heat to high latitudes than in the control run.
The text was updated successfully, but these errors were encountered:
The idea is to switch off (or modify) winds in particular basin(s). For eg: The ocean circulation in North Atlantic is a lot more dependent on the global ocean circulation than the North Pacific, as can be seen in all the experiments we have done so far (see here). By switching off winds in the North Pacific, we expect the basin to not affect (or be affected) by global circulation.
However, the meridional transport of heat flux will be reduced in the North Pacific, and it will be interesting to see whether in equilibrium, the total heat flux into the ocean reduces or whether the Atlantic ocean transfers more heat to high latitudes than in the control run.
The text was updated successfully, but these errors were encountered: