72 results were found for 杏彩国际娱乐2平台【┃稳定２17⒋31┃扣】】.

Results:

• 21. BIHU_windrose_2005-2014

  Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 31 32 1 2 1 5 3 4 3 5 7 4 48 1 3 23 4 7 2 5 5 5 1 4 12 9 16 68 29 Wind rose BIHU September 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 /media/vedur/BIHU_windrose_2005-2014.pdf

• 22. BIAR_windrose_2005-2014

  (knots ) 0 2 4 6 8 12 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 31 3 15 8 11 0 7 4 6 0 6 9 6 0 7 2 5 1 5 7 4 6 4 6 8 5 15 8 27 0 37 0 36 0 41 9 55 4 61 3 43 6 20 9 13 2 7 3 5 7 4 3 3 8 3 2 5 4 7 4 14 0 21 7 23 7 28 5 41 1 34 7 Wind rose BIAR April 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 /media/vedur/BIAR_windrose_2005-2014.pdf

• 23. Future Climate and Renewable Energy: Impacts, Risks and Adaptation

  ? Oslo, Norway, 31 May - 2 June 2010 At the Nordic and Baltic conference on “Future Climate and Renewable Energy ? Impacts, Risks and Adaptation”, you will meet stakeholders from the energy sector and researchers to exchange views and acquire information about current research results regarding the: past and present changes in climate /ces/events/nr/1739

• 24. Earthquakes last 48 hours

  Earthquakes last 48 hours | Latest | Icelandic Meteorological office Quake list | View Earthquakes last 48 hours Number of earthquakes SizeNumber Size 3 and greater0 earthquakes Size 2 to 34 earthquakes Size 1 to 222 earthquakes Size less than 167 earthquakes All quakes SizeTimeQualityLocation /m/earthquakes/latest

• 25. Factsheet_Bardarbunga_20141103

  207 earthquakes have been detected in the caldera. Two earthquakes were bigger then M5,0, on 31. October at 21:32 an M5,2 earthquake was detected and M5,3 on 2. November at 16:02. In total 27 earthquakes between M4 and 5 were detected and 8 between M3 and 4. • The GPS station in the centre of Bardarbunga show that the subsidence of the caldera continues with similar rate as it has done over /media/jar/Factsheet_Bardarbunga_20141103.pdf

• 26. 16910025

  Flugskýrsla TF-SIF 30. nóvember 2010 Flug nr. 16910.025 Áhöfn: Flugstjóri Benóný Ásgrímsson Flugmaður Hafsteinn Heiðarsson Flugmaður 2 / Þjálfunarfl. Yfirstýrimaður Auðunn F. Kristinsson Stýrimaður Gunnar Örn Arnarson Stýrimaður Stýrimaður Aðrir Flugtími: Flugvöllur Hreyfing Flugtak Flugvöllur Lending Stöðvað Flugtími Blokktími Sjml. BIRK 08:31 08:35 /media/hafis/skyrslur_lhg/16910025.pdf

• 27. Climate and Modeling Scenarios

  climate. Nat. Hazards Earth Syst. Sci., 10, 1563-1574, doi: 10.5194/nhess-10-1563-2010. Other international Benestad, R.E. (2010). A study of storms and winds in the North-Atlantic, met.no report no 7/2010. Benestad, R.E. (2010). An analysis if simulated and observed storm characteristics, In Proc. of Future climate and renewable energy: Impacts, risks and adaptation, Oslo, 31 May-2 June 2010 /ces/publications/nr/1680

• 28. BIVM_windrose_2005-2014

  ) Icelandic Met Office 02. júl. 2015 3 4 4 7 1 7 1 7 9 3 4 2 7 7 9 14 2 36 3 34 2 31 2 24 6 13 5 17 7 14 2 6 9 5 0 7 9 7 3 10 4 10 9 9 8 12 7 13 8 15 7 14 8 14 3 16 3 9 2 5 6 5 9 3 2 4 5 6 5 Wind rose BIVM 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 6 7 Frequency /media/vedur/BIVM_windrose_2005-2014.pdf

• 29. BIGR_windrose_2005-2014

  ) 0 5 10 15 20 25 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 52 49 35 28 30 23 20 42 5 2 34 61 48 31 35 17 15 19 15 9 7 10 9 11 22 43 2 1 8 10 20 4 5 16 6 9 17 3 3 Wind rose BIGR December 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 /media/vedur/BIGR_windrose_2005-2014.pdf

• 30. CES_D2.4_task2_CMIP3_winds

  the windiest part of the year from November to January, the observed Vg is approximately 1 m/s higher than the 10-GCM mean. 2 Fig. 1. The seasonal cycle of the geostrophic wind speeds at the grid point (60°N, 25°E), as averaged over the years 1971-2000. The solid line shows the 10-GCM average and the shading the mean ± one standard deviation between the model simulations. The red squares /media/ces/CES_D2.4_task2_CMIP3_winds.pdf