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. ❋ Unknown (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. ❋ Unknown (2007)
In a "positive phase", the pattern is reversed, with lower pressure in the polar region, and higher pressure in the midlatitudes. ❋ 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? ❋ Andrew Freedman (2011)
It also tends to push the weather in midlatitudes toward certain configurations (like one with an upper-level trough near eastern North America, or another with an upper ridge similarly positioned). ❋ Unknown (2010)
We are reviewing a paper by S Koumoutsaris et al. "Influence of El-Nino-Southern Oscillation on the Interannual Variability of tropospheric ozone in the northern midlatitudes". ❋ HayleyM (2008)
Trends in lower stratospheric zonal winds, Rossby wave breaking behavior, and column ozone at northern midlatitudes. ❋ Unknown (2009)
Satellite retrievals of erythemal UV dose compared with ground-based measurements at northern and southern midlatitudes. ❋ Unknown (2009)
The most rapid expansion will occur in the midlatitudes, where yields are higher and production costs lower. ❋ Unknown (2008)
Looking more closely, the models have SW forcing in the Tropics that is too negative, but not negative enough in the midlatitudes. ❋ Unknown (2007)
This manuscript is based on the earlier theoretical manuscript by Browning and Kreiss and is a practical example of the concept of balanced mesoscale motions in the midlatitudes. ❋ Unknown (2007)
In the midlatitudes at the smaller scales, evaporative cooling and condensational heating play a major role in the vertical velocity of the mesoscale storms see articles referenced above. ❋ Unknown (2007)
In our 1986 manuscript we mathematically prove that the new system accurately describes the large scale motions of the atmosphere in the midlatitudes. ❋ Unknown (2007)
