Sökresultat - welcome to oxelosund v2 small.pdf
1415 träffar på welcome to oxelosund v2 small.pdf inom hela webbplatsen
provides pilotage and assistance in the navigation to vessels within Swedish territorial waters. SMA ... quality, safe and efficient pilotage service in order to minimize risks for the shipping industry.
NYNÄSHAMN PASSAGE PLAN INFORMATION SHEET AGENT TO - Eastcoastpilot@sjofartsverket.se REQUESTED PILOT ... CALCULATED MAX. WINDLOAD :________________ts___(formula: v2/18=kp/m2x windarea) WATER LEVEL:_________________
Normal FORMCHECKBOX Small FORMCHECKBOX Large FORMCHECKBOX Unequal Reactive to light? FORMCHECKBOX ... with medical expertise. It is intended to enable officers onboard to provide detailed information about an
Connect Tug(s) 8-10 kn 30 minutes notice to connect harbour tug(s). POB POB 6-8 kn Gothenburg ... turns 0.5-1.0M (radius and speed to be agreed). Vessel to be prepared to use either North or South Channel
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
characterized as more severe than normal especially owing to the ice conditions at the westcoast. The ice formation ... anormal date. A more permanent ice layer started to form 23 November in inner bays and archipelagoes
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
February to 20 nm west of Skagen, 30 nm west of Smögen and along the Norwegian coast westward to Kristiansand ... the Baltic and in the Belts the ice was difficult to force during some weeks and obstructed especially
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
the month ice occurred in the skerries south- ward to Piteå . The ice situation was unchanged until the ... major parts of the sea area was again open. Due to the winds the ice north of a line Röd- kallen - Hailuoto
of view this ice winter was unique as the channel to the port of Luleå for the first time was open for ... part. The ice formation continued in the skerries to the middle of November, but thereafter the weather
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
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