S. Ushio et M. Wakatsuchi, A LABORATORY STUDY ON SUPERCOOLING AND FRAZIL ICE PRODUCTION PROCESSES IN WINTER COASTAL POLYNYAS, J GEO RES-O, 98(C11), 1993, pp. 20321-20328
The rates of frazil ice production and salt flux in wind-generated ope
n water were estimated on the basis of results from laboratory experim
ents that model coastal polynyas in a severe winter. The measurements
were made under various conditions of wind speed, air temperature, and
water salinity. The rate of ice production increased with increasing
wind speed and water salinity, and with decreasing air temperature. Th
e high rates of ice production are attributed to the vigorous producti
on of underwater frazil crystals. Salt fluxes due to frazil production
were also much greater than those of sheet ice growing vertically und
er calm atmospheric conditions. The important factor that governs such
a process of high ice production lies in supercooling and underwater
ice production. In the case of common seawater of salinities larger th
an 25 parts per thousand, supercooled water that formed on the surface
sinks into the underlying seawater at its freezing point by a density
instability as well as by a wind-forced convection. The sinking of th
e supercooled water and the resulting production of numerous frazil cr
ystals under the water lead to the maintenance of open water for a lon
g period. Thus large heat fluxes occur through the open water that is
continuously exposed to cold air, producing a large amount of the unde
rwater ice at high rates. This mechanism for ice production in open wa
ters is driven by a strong, cold wind and is enhanced by increasing wa
ter salinity.