72 results were found for [77AGG. COM]maen slot ibox slot sgp77 slot wadah slot rj slot slot 25 xyg.

Results:

• 31. isskyrsla_14122010

  15.0W 9) 67 05.0N 21 52.0W 10) 66 57.0N 22 32.0W 11) 67 00.0N 23 00.0W 12) 66 38.0N 25 00.0W 13) 66 30.0N 26 40.0W Næst landi var ísinn á eftirfarandi stöðum: 1. 48 sjml vnv af Grímsey. 2. 46 sjml ana af Horni. 3. 34 sjml norður af Skagatá. 4. 25 sjml nnv af Sraumnesi. Kl 0003 Kallað í Remoy Viking k/m LLDM til að fá upplýsingar um ísinn sem hann er að sigla í gegnum /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf

• 32. Warning due to violent storm

  934 mb when the low approaches the southeast coast soon after midnight and 933 mb in the northeast at 7:00 UTC tomorrow morning. Then the low continues to the north and the weather moderates. Brief forecast for the evening and the night Southeast 8 - 15 m/s or patchy sleet or snow, but mainly dry in the northeastern parts. Temperatures around zero. Rapidly increasing east- and northeast winds /about-imo/news/nr/3255

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

  can be found in Huntjens et al. (2007), Chapter 4 of NeWater Deliverable 1.7.9a (http://www.newater.info). Climate change adaptation in European river basins 265 123 interactions, by private and public actors, to achieve adaptation and to enhance the capacity of processes, institutional arrangements and actors to adapt to future environmental changes (Huitema et al. 2009). Adaptive governance /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 34. 2010_005_

  Century control runs, as well as 21st Century forecast runs, submitted by various institutions to the Intergovernmental Panel on Climate Change (IPCC) for their Forth 11 Table 1. General circulation and regional climate models that were considered in this study. Model Version Model Name, Institute BCCR BCM 2.0 Bergen Climate Model, Bjerknes Centre for Climate Research, Bergen, Norway CCCMA CGCM 3.1 /media/ces/2010_005_.pdf

• 35. 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

• 36. 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

• 37. 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

• 38. 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/

• 39. CES_D2.4_VMGO

  the territories of European Russia (ER) and Europe (EU) an ensemble of 9 CMIP3 [1] comprehensive global (coupled atmosphere-ocean) climate models is used in this assessment (Table 1); so called A2 scenario is considered. Both A2 and A1B scenarios are similar in terms of resulting global mean warming up to the mid-21st century IPCC [2]. The projected changes in ER and EU in many cases continue /media/ces/CES_D2.4_VMGO.pdf

• 40. BITN_windrose_2005-2014

  15 22 32 21 3 12 3 8 4 6 6 2 1 10 5 20 29 27 24 38 37 16 52 Wind rose BITN August 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 Frequency of wind direction (%) Aerodrome Total observations: 836 Calm: 7.9% Variable winds: 8.1% Average wind speed for wind direction Wind direction /media/vedur/BITN_windrose_2005-2014.pdf