As a result, the phenomena I describe above, with the rapid
changes in circulation regimes, are not represented in the climate models at all except as gridcell sized averages...
Not exact matches
It results
in step
changes and
regimes in upwelling
in the eastern Pacific and
in overturning
circulation in the Atlantic.
What science is suggesting is that there are multi-decadal
regimes that are related to
changes in ocean and atmospheric
circulation in the broader Earth system.
It is seen
in regime changes in cloud, ice, ocean and atmospheric
circulation, hydrology and biology that are evident
in climate records and that are best described as shifts
in state space on the multi-dimensional climate strange attractor at 20 to 30 year intervals.
Changes in the upwelling or
circulation regimes could affect dissolved oxygen (DO)
in these regions [4], [27].