Temporal and spatial variability of surface fluxes over the ice edge zone in the northern Baltic Sea

• Published in: Journal of Geophysical Research
• Main Authors: Brümmer, B., Schroeder, David, Launiainen, J., Vihma, T., Smedman, A.-S., Magnusson, M.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2002
• Subjects: Aranda; Breaker; Sea ice
• Online Access: https://centaur.reading.ac.uk/55443/; https://centaur.reading.ac.uk/55443/1/03_BSLVSM_2002.pdf; https://doi.org/10.1029/2001JC000884

Three land-fast ice stations (one of them was the Finnish research ice breaker Aranda) and the German research aircraft Falcon were applied to measure the turbulent and radiation fluxes over the ice edge zone in the northern Baltic Sea during the Baltic Air-Sea-Ice Study (BASIS) field experiment from 16 February to 6 March 1998. The temporal and spatial variability of the surface fluxes is discussed. Synoptic weather systems passed the experimental area in a rapid sequence and dominated the conditions (wind speed, airsurface temperature difference, cloud field) for the variability of the turbulent and radiation fluxes. At the ice stations, the largest upward sensible heat fluxes of about 100 Wm�2 were measured during the passage of a cold front when the air cooled faster (�5 K per hour) than the surface. The largest downward flux of about �200 Wm�2 occurred during warm air advection when the air temperature reached +10�C but the surface temperature remained at 0�C. Spatial variability of fluxes was observed from the small scale (scale of ice floes and open water spots) to the mesoscale (width of the ice edge zone). The degree of spatial variability depends on the synoptic situation: during melting conditions downward heat fluxes were the same over ice and open water, whereas during strong cold-air advection upward heat fluxes differed by more than 100 Wm�2. A remarkable amount of grey ice with intermediate surface temperature was observed. The ice in the Baltic Sea cannot be described by one ice type only.