midlatitudes

Re 222 - At least in the transient response (as opposed to equilibrium), it is expected that warming will be greater in the Northern Hemisphere, especially at higher latitudes because of albedo feedbacks, but in general because of the greater land area - minimal warming will occur in Southern midlatitudes because of the dominance of water, and also because of a ring of upwelling water (it takes considerable time for the warming of upper oceanic water to partly fill the deep ocean and come back up in areas of upwelling deep water) - this upwelling is driven by winds from storm activity that will tend to be enhanced when there is greater warming equatorward.

RealClimate 2009

Re 222 - At least in the transient response (as opposed to equilibrium), it is expected that warming will be greater in the Northern Hemisphere, especially at higher latitudes because of albedo feedbacks, but in general because of the greater land area - minimal warming will occur in Southern midlatitudes because of the dominance of water, and also because of a ring of upwelling water (it takes considerable time for the warming of upper oceanic water to partly fill the deep ocean and come back up in areas of upwelling deep water) - this upwelling is driven by winds from storm activity that will tend to be enhanced when there is greater warming equatorward.

RealClimate 2009

Re 222 - At least in the transient response (as opposed to equilibrium), it is expected that warming will be greater in the Northern Hemisphere, especially at higher latitudes because of albedo feedbacks, but in general because of the greater land area - minimal warming will occur in Southern midlatitudes because of the dominance of water, and also because of a ring of upwelling water (it takes considerable time for the warming of upper oceanic water to partly fill the deep ocean and come back up in areas of upwelling deep water) - this upwelling is driven by winds from storm activity that will tend to be enhanced when there is greater warming equatorward.

RealClimate 2009

Re 222 - At least in the transient response (as opposed to equilibrium), it is expected that warming will be greater in the Northern Hemisphere, especially at higher latitudes because of albedo feedbacks, but in general because of the greater land area - minimal warming will occur in Southern midlatitudes because of the dominance of water, and also because of a ring of upwelling water (it takes considerable time for the warming of upper oceanic water to partly fill the deep ocean and come back up in areas of upwelling deep water) - this upwelling is driven by winds from storm activity that will tend to be enhanced when there is greater warming equatorward.

RealClimate 2009

Re 222 - At least in the transient response (as opposed to equilibrium), it is expected that warming will be greater in the Northern Hemisphere, especially at higher latitudes because of albedo feedbacks, but in general because of the greater land area - minimal warming will occur in Southern midlatitudes because of the dominance of water, and also because of a ring of upwelling water (it takes considerable time for the warming of upper oceanic water to partly fill the deep ocean and come back up in areas of upwelling deep water) - this upwelling is driven by winds from storm activity that will tend to be enhanced when there is greater warming equatorward.

RealClimate 2009

Re 222 - At least in the transient response (as opposed to equilibrium), it is expected that warming will be greater in the Northern Hemisphere, especially at higher latitudes because of albedo feedbacks, but in general because of the greater land area - minimal warming will occur in Southern midlatitudes because of the dominance of water, and also because of a ring of upwelling water (it takes considerable time for the warming of upper oceanic water to partly fill the deep ocean and come back up in areas of upwelling deep water) - this upwelling is driven by winds from storm activity that will tend to be enhanced when there is greater warming equatorward.

RealClimate 2009

Re 222 - At least in the transient response (as opposed to equilibrium), it is expected that warming will be greater in the Northern Hemisphere, especially at higher latitudes because of albedo feedbacks, but in general because of the greater land area - minimal warming will occur in Southern midlatitudes because of the dominance of water, and also because of a ring of upwelling water (it takes considerable time for the warming of upper oceanic water to partly fill the deep ocean and come back up in areas of upwelling deep water) - this upwelling is driven by winds from storm activity that will tend to be enhanced when there is greater warming equatorward.

RealClimate 2009

It has been shown very clearly that the large scale, slowly evolving in time solution of the atmosphere in the midlatitudes is a fully three dimensional beast.

Exponential Growth in Physical Systems #2 « Climate Audit 2007

In a "positive phase", the pattern is reversed, with lower pressure in the polar region, and higher pressure in the midlatitudes.

The winter the Arctic shifted south Andrew Freedman 2011

Here we have an Arctic region that is being literally transformed by warming and melting ice, and yet in the northern midlatitudes, that translates to colder and snowier winters?

The winter the Arctic shifted south Andrew Freedman 2011