Thursday, 18 January 2001: 2:29 PM
Calculations of a thermal front parameter (TFP) using NCEP/NCAR reanalysis data over the period
1979-1998 reveal a relative maximum in frontal frequencies during summer along northern Eurasia from about
60-70 degrees north, best expressed over the eastern half of the continent. A similar relative maximum is found
over Alaska year-round, although best developed in summer. These high-latitude features can be clearly
distinguished from the polar frontal zone in the middle latitudes of the Pacific basin and collectively resemble
the summertime "Arctic frontal zone" discussed in several early studies. While some separation between high
and middle latitude frontal activity is observed in all seasons, the summer season is distinguished by the
development of an attendant mean baroclinic zone aligned roughly along the Arctic Ocean coastline and
associated wind maxima in the upper troposphere. The regions of maximum summer frontal frequency
correspond to preferred areas of cyclogenesis and to where the summertime contribution to annual precipitation
is most dominant. Cyclones generated in association with the Eurasian frontal zone often track into the central
Arctic Ocean, where they may impact on the sea ice circulation.
Development of the summer Eurasian frontal zone occurs in conjunction with a seasonal change in the
large-scale circulation characterized by a zonal orientation of the isotherms. Over both Eurasia and Alaska,
baroclinicity appears to be enhanced by differential heating between the Arctic Ocean and snow-free land.
Frontal activity also shows an association with orography. Several studies have argued that the location of the
summer Arctic frontal zone may be in part determined by discontinuities in energy exchange along the
tundra/boreal forest boundary. However, a vegetation forcing is not required in our conceptual model. The
potential roles of vegetation and orography are being further addressed through sensitivity studies using a
regional climate model.
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