Sökresultat - welcome to oxelosund v2 small.pdf
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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
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
preliminary ETA to Southcoast pilots. 5/1 hours before ETA pilot station; confirmation of ETA to Oskarshamn ... Chart 6241 Distance pilotstation to berth: 5,7 nm Link to route into Oskarshamn in .rt3 format
preliminary ETA to Southcoast pilots. 5/1 hours before ETA pilot station; confirmation of ETA to Oskarshamn ... 340m Total length of the jetty: 340 m Link to “Digitala färdplaner” (Route into Jättersön in .rt3
preliminary ETA to Southcoast pilots. 5/1 hours before ETA pilot station; confirmation of ETA to Oskarshamn ... 212/032 Ro/ro Distance pilotstation to berth: 2,8 nm Link to “Digitala färdplaner” (Route into Simpevarp
preliminary ETA to Southcoast pilots. 5 hours before ETA pilot station; confirmation of ETA to Västervik pilots ... 3 90 009/189 Distance pilotstation to berth: 6,5nm Link to “Digitala färdplaner” (Route into Västervik
information contained in this documentation is subject to change without notice. Sjöfartsverket (Swedish Maritime ... http://eservices.sjofartsverket.se/PKI/policykundcert.v1.pdf
Sjökortskatalog 2025 Fo to : L ar s Jo ha ns so n/ M os tp ho to s Hej alla! Snart är det ... hämtades ut ur sjö- kortsdatabasen (Corrected up to). Ufs och sjökortsrättelser Ufs (Underrättelser
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
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
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
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
systems in the engine department. All of this made to extend the life span of the icebreaker another ... m3/h. The heeling pumps allows the ship to heel from one side to another with a maximum angle of 13° in