38 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja 240 Tomosiga Intan Jaya.

Results:

• 11. BIAR_windrose_2005-2014

  Wind rose BIAR 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 of wind direction (%) Aerodrome Total observations: 88640 Calm: 3.8% Variable winds: 9% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIAR_windrose_2005-2014.pdf

• 12. BIEG_windrose_2005-2014

  Wind rose BIEG 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 2 4 6 8 10 Frequency of wind direction (%) Aerodrome Total observations: 87865 Calm: 12% Variable winds: 3.4% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S W /media/vedur/BIEG_windrose_2005-2014.pdf

• 13. BIKF_windrose_2005-2014

  Wind rose BIKF 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: 176045 Calm: 1.8% Variable winds: 0.49% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S W /media/vedur/BIKF_windrose_2005-2014.pdf

• 14. BIRK_windrose_2005-2014

  Wind rose BIRK 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 Frequency of wind direction (%) Aerodrome Total observations: 88951 Calm: 1.2% Variable winds: 1.7% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S W /media/vedur/BIRK_windrose_2005-2014.pdf

• 15. BIVM_windrose_2005-2014

  Wind rose BIVM 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 8 Frequency of wind direction (%) Aerodrome Total observations: 42081 Calm: 0.58% Variable winds: 3.8% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 20 0 45 90 135 180 225 270 315 360 /media/vedur/BIVM_windrose_2005-2014.pdf

• 16. isskyrsla_2012-01-11.pdf

  BIEG 13:44 13:44 01:01 01:05 240 BIEG 13:44 13:55 BIRK 16:59 17:01 03:04 03:17 606 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 Samtals 04:05 04:22 846 Flugleið: Flugskýrsla TF-SIF 11. Janúar 2012 Flug nr. 00212.025 Kl.1520, ískönnun hefst á radar N- af Horni. N- og NV- af Straumnesi er talsverð nýmyndun. Næst landi var nýmyndunin um 11,5 sml. NNV- af /media/2012/isskyrsla_2012-01-11.pdf

• 17. Kok_et_al._TFSC_published_2011

  developed during the second scenario workshop (WS2) did not include any original GEO-4 text, except for Economy First. WS2 stories contained largely new material re
  ecting the view of the subgroups. Additionally, the title of each story was changed, indicating the increased ownership of the stakeholders. The nal scenarios were entitled: Economy First (EcF), Policy Rules (PoR), Fortress Europe (FoE /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 18. Kjellstrom_Erik_CES_2010

  is not addressed in the CES/ENSEMBLES RCM-GCM matrix • Observations Simulated • Rubel and Hantel (2001) ECHAM5 Problems with global climate models Details in precipitation are not captured: example winter (DJF) 0 30 60 90 120 150 180 210 240 mm/month Downscaling methods: Improving global climate scenarios Global Regional Regional climate models (RCMs) head2right Increased resolution /media/ces/Kjellstrom_Erik_CES_2010.pdf

• 19. Instructions for weather radar pages

  The Icelandic Meteorological Office owns a weather radar which is situated on Miðnesheiði, just outside of the Leifur Eiríksson airport. It is used to monitor real time precipitation. The weather radar has a 240 km radius, which is displayed with the highlighted dial on the image. The radar reflects signals from precipitation but also from other objects /weather/articles/nr/1221

• 20. VI_2009_006_tt

  than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf