Warning
Variable wind 3-10 m/s and widely fair, but isolated showers of snow or sleet near the coast. Frost 0 to 7 deg. C. Increasing easterly wind in the south and west by evening and becoming warmer.

East 13-20 m/s tomorrow morning and intermittent rain, sleet or snow, but slower wind in the east parts. Decreasing wind throughout the day, 8-15 m/s by afternoon, but gale with snow in the northwest. Temperature widely 0 to 7 deg. C, mildest in the far south. Valid to 18.12.2025 00:00 More
Yellow alert for weather: Westfjords and Northwest Iceland More

78 results were found for WA 0812 2782 5310 Bengkel Las Atap Canopy Baja Ringan Atap Go Green Kajoran Kab Magelang.

Results:

11. Sea ice in January 2009

attention to the proceedings on satellite images and put information in that regard three times on the web. Easterly and northeasterly winds were dominant in the Greenland Strait. No dispatches were received from ships and the Coast Guard did not go on an exploration flight. By the end of the month sea ice maps from the Norwegian Met Office were made accessible on the IMO's web site (originally hafis /sea-ice/monthly/2009/nr/2323
12. Sea ice in February 2009

northnorthwest of Straumsnesviti and about 60 nm northwest of Barði. Easterly and northeasterly winds were dominant in the Greenland Strait and the sea ice was far off shore the whole month. No dispatches from ships were received from ships and the Coast Guard did not go on an exploration flight /sea-ice/monthly/2009/nr/2324
13. VI_2009_006_tt

Special thanks go to Gwenn E. Flowers at the Simon Fraser University in Vancou- ver for providing me with her Matlab code for the coupled sheet–conduit model, for her comments and assistance with model calibration and discussions of model results. I thank Finnur Pálsson and Helgi Björnsson at the Institute of Earth Sciences at the University of Iceland for providing profiles of the subglacial flood /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
14. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

requires an appropriate monitoring system and the use of integrated or more simple models for the prediction of future scenarios including effects of implemented measures. Such integrated models should also include socio-economic aspects. In the Netherlands for the Major sources of uncertainty in current IWRM practice Tabl e 1 St ep 1: Es ta bl ish st at us an d go al s Pr oces s in Ste p 1 Es tablis /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
15. Factsheet_Bardarbunga_140914

breaking out from the main lava stream towards the east and west. The largest one of these lava tongues stretches towards the east and had become 300 m wide and 2 km long at 18:00 yesterday. An eruption cloud reaches 4 km in height but lowers with distance from the eruption site.  Seismic activity is similar to what it has been in the past days but earthquakes are starting to go down in numbers /media/jar/myndsafn/Factsheet_Bardarbunga_140914.pdf
16. Hare-2011-ParticipatoryModelling

or system dynamics models, provide benets which go beyond the production of the model itself. The discussions and negotiations between the groupmembers during themodel building, for example, improve the group’s shared understanding of the management problem and its solutions. As such, participatory modelling can be a tool for supporting the type of social learning currently being promoted for water /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
17. VI_2020_011_en

scenarios might be constrained by these observations. Moreover, the simulation results and maps might be updated to reflect new sources of information and the usage of the maps would go more towards assisting the response planning. During an eruption, the methodology would change again, and the hazard assessment would be revisited continually based on the real-time monitoring. The scenarios would /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
18. Reporting floods well appreciated

-explanatory. Please have a go and comment in English, that would be well appreciated.Participation is considered as a consent to further publishing of the individual reports.Assistance with the filling of the form provided through Contact us or in +354 522 6000 during office hours. News /about-imo/news/reporting-floods-well-appreciated
19. Sea ice in October 2008

the 26th and the ice edged south. From the 26th and for the rest of the month, westerly winds were predominant and the ice edged therefore closer to Iceland. On satellite images taken on the 30th, pretty dense ice was noticable about 70n.m. from Barði but single icebergs and rips were closer, or 50n.m. from Barði. The Coast Guard did not go on an exploration flight during the month. Norherly /sea-ice/monthly/2008/nr/2319
20. Sea ice in November 2008

this period. From the 21st until the 24th of November, 4 dispatches regarding sea ice were received from ships. The Coast Guard did not go on an exploration flight during the month /sea-ice/monthly/2008/nr/2320