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• W1986236687 abstract "[1] Observations indicate that midlatitude weather systems are organized into “storm tracks” near oceanic frontal zones with pronounced sea-surface temperature (SST) gradients. A pair of atmospheric general circulation model experiments with zonally uniform SST profiles prescribed show that their observed collocation is not fortuitous. In one experiment, a storm track is anchored around a midlatitude SST front that maintains near-surface thermal gradients and energizes eddies. Westerly momentum transport by eddies produces a well-defined polar-front jet along the front, even in winter when a subtropical jet stream intensifies. In the other experiment, removal of the SST front leads to a substantial weakening in eddy activity and the PFJ especially in winter. It also leads to a weakening of the annular mode —the dominant mode of westerly-jet variability— and its notable structural distortion in winter. Though idealized, our experiments suggest the importance of midlatitude oceanic fronts for the tropospheric circulation and its variability." @default.
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• W1986236687 date "2008-08-13" @default.
• W1986236687 modified "2023-10-09" @default.
• W1986236687 title "On the importance of midlatitude oceanic frontal zones for the mean state and dominant variability in the tropospheric circulation" @default.
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• W1986236687 doi "https://doi.org/10.1029/2008gl034010" @default.
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