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  • 21. Outline_for_the_case_Road_maintenance_in_a_changing_climate

    NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011 …………………………………………………………………………………………………………………………………………………………………… 1 Outline for the case Road maintenance in a changing climate Introduction Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010 /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
  • 22. Sea ice in June 2010

    an ice strip at 66°42'N and 24°15' W up to 66°59'N and 22°24'W. On the 14th an observation was also received from the weather station „Hraun á Skaga“ on an iceberg 10-11 nm northwest of Skagatá. On the 22nd an ice strip was observed at 66°49'N and 22°22'W until 66°51'N and 22°09'W. On the 29th two icebergs were observed in Þverál. IMO issued information and an image of the ice edge 16th June. Wind /sea-ice/monthly/2010/nr/2341
  • 23. Joining forces in weather forecasting and climate research

    of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research
  • 24. Sea ice in May 2010

    An ice edge was observed in the area from 67°31'N and 023°35'W to 66°41'N and 23°43'W. Westerlies were a little more prevailing in the Greenland Strait and north of Iceland than on average /sea-ice/monthly/2010/nr/2340
  • 25. Sea ice in August 2010

    reported on a floe on 66°12,67'N 27°38,17'W and on the 30th a ship observed a large iceberg in location 66°56'N 24°44,4'W. Wind directions were close to the average on the Greenland Strait this month /sea-ice/monthly/2010/nr/2343
  • 26. vhmkerfi_mars_2012

    W W W W W W W D DD DD DD CB CA CB CA CA CB CB CB CA CA CB CA CA CA CBCB CB CA CB CB CB CBCBCB CB CB CA CA CACA CA CA CACACB CA CA CA CA CB CA CA CA CA CA CB CA CA CA CACA CA CB CA CA CA CA CA CA CB CA CA CA CBCA CA CACA CA CA CA CA CA CA CA CB CA CA CA CBCB CB C CA CA CB CB CA CA CB CA CB CA CA CB CA CA CA CACA CA CB B CA CA CA CA CA CB CA CA CA CA CB CA CA CAC CACB CA CBCB CB CB CB CACA CBCA C B /media/vatnafar/maelar/vhmkerfi_mars_2012.pdf
  • 27. Sea ice in April 2010

    to land 52 nm NW of Barði and 48 nm NW of Straumnes. Two observations were received on icebergs, the 4th and the 5th. An observation from a ship on the 18th reported sea ice from 66°31´N and 26°08´W to 66°26´N and 25°47´W. Northeasterlies were somewhat less prevalent on the Greenland Strait than the average this month /sea-ice/monthly/2010/nr/2339
  • 28. Sea ice in November 2010

    WNW of Straumnes and the ice was scattered. Two observations from ships were received 29th November, on a strip at location 66°50´N - 24°36´W and at 67°00´N - 24°02´W. Wind directions were mostly from the northeast and the east, however southwesterlies occurred for a few days at the Greenland Strait /sea-ice/monthly/2010/nr/2346
  • 29. Sea ice in July 2011

    which implies the need of caution for passing ships. Two observations were received on icebergs from ships: 21st July in location 66°40.23‘N 025°13.34‘W 31st July in location 66°48.6‘N 023°03.7‘W In the Greenland Strait northeasterly wind directions were predominant but there were also a few days with southwesterlies /sea-ice/monthly/2011/nr/2403
  • 30. Eyjafjallajokull_status_2010-05-07_IES_IMO

    recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

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