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• 41. GA_2009_91A_4_Andreassen

  net balances are wellcorrelated and (obviously) best modelled as the sum of bw measured and bs modelled (bs-m2). Thebest obtained correlations of modelled bw (0.86), bs(0.87) and bn (0.94) for 1949–2006, show that themodel could explain 73, 76 and 88% of the variance over this period.From each year we also extracted the day with maximum bw (bwd) and minimum bs (bsd, mini-mum values as bs is negative /media/ces/GA_2009_91A_4_Andreassen.pdf

• 42. Warning due to violent storm

  during the evening, 18 - 23 in places by midnight, but 23 - 28 and severe rain or sleet in the southeast- and eastern parts. South 25 - 33 m/s in the east parts late tonight and during morning, windiest in the easternmost parts. Veering southwest 15 - 25 tomorrow, strongest in the north. Rain or sleet, later becoming showery. Temperatures mostly 0 to 5 °C. Warning Violent storms to hurricane /about-imo/news/nr/3255

• 43. 2010_005_

  and total precipitation in the RCMs during the 1961–90 control period in winter (DJF) and summer (JJA). 25 4 Differences between summer (JJA) and winter (DJF) mean seasonal surface air temperature in degrees centigrade during the 1961–90 control period, for the re- analyses and the RCMs. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26 5 Dependence on terrain elevation of linear trends /media/ces/2010_005_.pdf

• 44. Reykholt-abstracts

  .................................................................... 24 SURFMAP? – integrating lidar measurements into an Antarctic surface DEM Gary M. Llewellyn .................................................................................................................. 25 An overview of past and future surveys of Iceland conducted by the NERC ARSF Eric Lutz, Bob Hawley, Michelle Hofton, John Sonntag, Kelly /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 45. Largest earthquakes during the last 48 hours

  2.030.04 14:11:0730.63.5 km NE of Básar 1.830.04 00:26:13Check.33.1 km ESE of Grímsey 1.730.04 02:16:01Check.3.8 km ESE of Bárðarbunga 1.630.04 13:25:0090.04.1 km W of Dreki 1.529.04 16:47:58Check.5.7 km ENE of Goðabunga 1.329.04 16:13:22Check.17.5 km E of Grímsey 1.230.04 00:49:27Check.33.9 km ESE of Grímsey Sitemap Front page /m/earthquakes/largest

• 46. Sea ice in October 2008

  but somewhat of icebergs and one dispatch regarding a possible iceberg was received on October 9th at 67°24N and 25°41W. On the 21st sea ice was clearly noticable on satellitepictures, which by then had moved into the Greenland Strait and bordered the Blosseville coast of Greenland. Sea ice was considerably more than average for October. Harsh northerly winds were on the Greenland Strait until /sea-ice/monthly/2008/nr/2319

• 47. Sea ice in June 2009

  that sparse ice was to be found within the ice-edge. The information also indicated that the ice-edge came closest to shore about 55-75 nm westnorthwest of the Westfjords. A dispatch regarding icebergs was received by the end of the month, but they were at 66°40N and 25°30W. Information regarding the ice-edge was issued four times by the Met office and the Office also received a photograph, taken from /sea-ice/monthly/2009/nr/2328

• 48. Eyjafjallajökull

  volcanic system is located on the Eastern Volcanic zone, approximately 25 km west of Katla volcano. Eyjafjallajökull volcano is a 1666 m high stratovolcano with an east-west elongated direction, the system is about 25 km long and 15 km wide. The volcano is mostly covered by ice and has an ice-filled caldera of about 2.5 km wide.In the last 8000 years Eyjafjallajökul has been moderately active /volcanoes/about-volcanoes/eyjafjallajokull/

• 49. Journal_of_Hydrology_Veijalainen_etal

  Terrain Models (DTM) in Kokemäenjoki and 25 m national DTM in Salo. The DTM in Salo was enhanced with point elevation data measured by the University of Turku, Southwest Finland Regional Environ- ment Centre and the City of Salo (Selin, 2006). Contour lines (i.e. 2.5 m or 5 m interval, and accuracy of 5–20 m depending on the area) were also used in Salo and Kittilä for interpolation of the DTM /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 50. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  269 123 Tabl e 2 continue d Dimensio n Variabl e Indicato r Literatur e (G )Finance s an d cos t recover y 25 .Resourc e availabilit y Sufficien t(publi can d private )resource s ar e availabl e Leac h an d Pelke y (200 1) 26 .Cos trecover y Cost s ar e recovere d fro m th e ‘users ’ by publi c an d privat e financia linstrument s (charges ,prices ,insuranc e etc. ) Pahl-Wos te t al .( 2007 c) 27 /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf