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February the was almost stationary and new-formed small leads were rapidly covered by ice. In the beginning ... ridges, From the middle 'of April some cracks and small leads begun to form in the icefield. Later a typical
- Farstugrund. During February only cracks and small leads were formed. Even during March the sea area ... the inner parts of the archipelagoes while some small floes occurred in the outer until the end of May
During Febru- ary the ice was rather stationary. Small leads., which opened we.Y'e rapidly covered by ... normal. The ice field broke up into large and small floes and from the middle of the month the ice
Below shows brash ice. lce in form of small or very small floes. It is formed when ice is wrecked
out. The ice field was broken up into large and small floes. The ice melting started slowly, especially ... grounded floebits occurred further some days on small rocks in outer parts of the archipelagoes. 7
sea-approach to Umeå, however, was blocked by a fairly small compac- ted ice-belt. The ice disappeared in many ... southern parts of the Bay of Bothnia a relati- vely small area with open water occurred at the end of March
situated offUmeå. In the Gulf of Bothnia, cracks and small leads appeared in the ice-field. Varying winds and ... ice-field broke up into vast floes interspersed with small and big ones. Some of the floes drifted out into
slowly due to the cold weather but cracks and small areas of open water formed by the weak variable ... March the ice drifted northwards and leads and small open areas was formed . Large open areas were formed
assistance
pack ice (1-6/10), big or small floes Close pack ice (7-8/10), big er small floes Very close or cornpact
working life onboard and on professionals in a small minority. A consistent theme is investing in preventive
days after the first one, right? No, start with small steps, and you'll probably find that you don't
Where cofferdams are provided over integral tanks, small trunks may be used to penetrate the cofferdam.
navigation in the district until 24 May in spite of the small ice area. First on 31 May there was no ice in sight
part of the ice field consisted of partly rotten small floes. Northeast of the line Norströmsgrund - Ulkokalla ... latitude 61 lON. The ice was ratten and braken into small floes in the southem parts of the ice field, otherwise
melting. a t the end of the month there were only small areas with rotten ice left at sea in the bay of
Delvis små vallar av sammanfrusen issörja (Partly small ridges av frozen sludge) Dödmanskär - Vännskär
ice field was broken up into vast floes mixed by small. A large area of open water was formed in the northeastern
paper chart covering the same area, ranging from “small scale charts” to “large scale plans”. As shown
in capsize; .8 pitch instability of SWATH (small waterplane area twin hull) craft due to the hydrodynamic
in general north- erly winds the ice broke into small floes and the ice melting started early, in spite
northern coast of the Sea of Bothnia eased off and small systems of leads were formed. Mild weather and
normal. The area with larger ice extent may look small but approximately corresponds ... with the area
coast and broke up more and more in !arge and small floes. Tempo- rarily, ice drifted down into the