Search results - Route plans routes to Simpevarp1
770 hits for Route plans routes to Simpevarp1 on the whole website
1973 till maj 1974 corr: English November 1973 to May 1974 sid 49 Andra och tredje raden skall stå: ... skerries . In December new ice formed rapidly but due to rather strong winds the whole area was not ice covered
second year in succession the navigation northward to the port of Luleå could go on all winter. The ... sea . In the skerries ice of significance started to form from the 10th of January . Passage through
caused ice formation to the outer archipelagoe. Northeasterly winds and snow fall led to cooling ofthe sea ... but then increased also at the Swedish side south to the Quark. An open area was left in the central parts
formation out to the line Malören -Hailuoto. The ice grew thicker and the 17th the ice was up to 20 cm thick ... formed on inner bays and sheltered areas southwards to Kalmar. In Lake Vänern compacted slush and shuga
sea area southeast of Gotland was ice free . Due to predominant northeasterly winds the ice conditions ... the norna! hut wi- despread fog made it difficult to navigate in the ice fields. The ice breaking was
Finnish coast, however, a belt of pack ice remained to the end of May. The Bay of Bothnia: The first ... December the ice formation spread out to the outer skerries and to the sea area north of 6500N. lce formed
then also covered the skerries further southward to Kalmar and braken new ice occurred off the coast ... was rapid. 27 January the whole sea area southward to Sydostbrotten was covered by ice, more than three
thicknesses were greater than normal, ranging up to 100 cm in the northern part of the Bay of Bothnia ... time of the year. The inner archipelagos southward to Blekinge were already covered with ice by Christrnas
completely ice-covered. The cold weather also led to ice formation in the archipelagos of the Sea of ... occurred off the coasts of the Sea of Bothnia down to Gävle and elsewhere. The ice-conditions along the
Kvar- ken were covered with ice. The ice also started to spread in the skerry areas of the southern Gulf ... Baltic and in the southern part of the Sound. Due to the strong wind, the ice cover was made up of compacted
as a wide, compressed ice-belt formed an obstacle to navigation. Ice formation began in the archipelago ... occasions which, however, had soon broken up due to strong south winds and got compressed against the
ice-condi- tions were similar to those of 1991/92, with some difficulties due to ice formation only in the ... into November, where the ice rapidly beca- me 10 to 20 cm thick. South-west winds pressed the ice mostly
Navigation to Swedish harbours was possible far into the winter wit- hout ice-breaking assistance. To find ... uccession of mild winters, one has to go back to the l 930's, when up to six consecutive mild winters were
operation off the Norr- land coast, and the Ale had to assist shipping on Lake Väner for ;; few weeks. ... Otherwise, the ice-breakers "Frej" and "Tor" never had to be fully manned and remained in Stockholm and Karlskrona
were at that time almost covered with ice . Due to cold weather from mid-J anuary the ice grew worse ... middle of April the ice-conditions allowed the ODEN to fi- nish ber ice-breaking activities for the seyson
early freeze-up, even far to the south, but ice formation soon stopped, later to be followed by seve- ral ... Sea of Bothnia. In mid-February ice again began to form in the Gulf of Bothnia, which was completely
periods the ice conditions were very difficult due to heavy ice pressure and ice ridging. Partly at the ... ice belt, however, caused still some ice problems to the har- bours Göteborg and Varberg at the end of
the preceding six mild winters of the years 1988 to 1993, was very mild with easy ice-condi- tions. ... could be compared to those prevailing in January of 1993. On January 21, ice began to form slowly at sea
from off Landsort curving away across the Baltic to Ventspils on the Latvian coast. South of it there ... situation was experienced as extreme no doubt had to do with the fäet that the winters of the last six
much later than normal. Then the sea area southward to Sea of Åland were covered by ice . Gulf of Finland ... area south- ward to Högbonden (N6255) was covered by ice. After that hard southerly to southwesterly winds
Bothnia got broken and compressed. In the entrances to Luleå and Karlsborg jammed brash barriers were formed ... started to form in the inner bays about New Y ear. After that almost unchanged ice situation to 17 January
formed at the Swedish coast from Nygrån southward to open wa- ter in the Northern Quark. In a week the ... via 20 nm E Bjuröklubb to Helsingkallan. From 5 February the winter came to stay. The open areas were
land Sea and the north- ernmost Baltic southward to approximately tht , latitude 5900 N were covered ... was an ice belt off the Swedish coast southward to Öland. In The Skagerrak there was fast ice in the
Bay and Sea of Bothnia and The Åland Sea southward to Svenska Björn was then covered by ice. During 3 ... a belt of heavy ice, 10 nm wide, from Farntugrund to Brahe- stad. In a few days the whole sea area was
February the ice broke up and drifted southeastward out to sea and formed later on a compacted belt outside ... The lead became l0 nm wide in the northern part~ up to 25 nm wide in the southern part~ and was stationary