SYNOPTIC AND MESOSCALE ATMOSPHERIC FEATURES OVER THE ICE-COVERED PORTION OF THE FRAM-STRAIT IN SPRING

Data obtained during the Coordinated Eastern Arctic Experiment (CEAREX ) from March 31 to April 20, 1989, from two ice camps in the pack ice region in the Fram Strait have been analyzed. The data show that the t otal period can be divided into two periods or regimes divided by a tr ansition period. The first period was a radiative type, characterized by very low surface temperatures and low wind speeds. Fairly regular o scillations between southerly and northerly winds were caused by small -scale disturbances in the surface pressure field, associated with upp er level waves of large amplitude. During a transition period toward a n ''advective weather type'' on April 11 a sharp frontal zone passed b oth ice camps. The front was associated with a small-scale low which h ad formed over the ice on the shallow but intense baroclinic zone alon g the northeastern Greenland coast. Mesoscale vortices of this type ma y, if numerous enough, affect the horizontal transfer of heat from low er latitudes toward Arctic regions as well as the ice drift through th e Fram Strait.