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  • 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 2. „We need to control our footprint on mother Earth“

    ice and the interaction of humans and the cryosphere. There will be talks on the effect on the Himalayan mountain range and the big Asian rivers. One of the leading authors of the United Nations IPCC report will present the latest result of the scientific working group.Here you can read more about the conference and get the latest news.Group of scientists and part of the local organizing /about-imo/news/we-need-to-control-our-footprint-on-mother-earth
  • 3. IPPC-2007-ar4_syr

    at higher northern latitudes (Figure 1.2). Average Arctic tem- peratures have increased at almost twice the global average rate in the past 100 years. Land regions have warmed faster than the oceans (Figures 1.2 and 2.5). Observations since 1961 show that the aver- age temperature of the global ocean has increased to depths of at least 3000m and that the ocean has been taking up over 80 /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 4. Sitemap

    Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 80/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas
  • 5. BIGJ_windrose_2005-2014

    Wind rose BIGJ 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: 1324 Calm: 2.6% Variable winds: 0.23% 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 /media/vedur/BIGJ_windrose_2005-2014.pdf
  • 6. Sea ice in January 2011

    in the following locations: 80 nm WNW of Bjargtangar, 46 nm NW of Barði, 40 nm NW of Straumnes and 41 nm N of Kögur. No icebergs were to be seen near the ice edge. On the Greenland Strait, northeasterly wind directions were dominant to begin with, and most of the month, but at the end of the month there were a few days with southwesterly wind /sea-ice/monthly/2011/nr/2348
  • 7. Forecasts - Blönduós

    cover: 0% 15 GMT 4° NNW 6 Cloud cover: 0% 16 GMT 4° N 5 Cloud cover: 0% 17 GMT 4° N 5 Cloud cover: 50% 18 GMT 4° N 4 Cloud cover: 80% 19 GMT 4° N 4 Cloud cover: 80% 20 GMT 4° N 4 Cloud cover: 70% 21 GMT 3° NNE 3 Cloud cover: 20% 22 GMT 1° NE 2 Cloud cover: 50% 23 GMT 1° N 1 Cloud cover: 90% Wed 3.05 00 GMT 0° WNW /m/forecasts/areas
  • 8. VI_2020_005

  • 9. BIBD_windrose_2005-2014

    Wind rose BIBD 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: 18358 Calm: 9.5% Variable winds: 1.7% 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/BIBD_windrose_2005-2014.pdf
  • 10. BIGR_windrose_2005-2014

    Wind rose BIGR 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: 10329 Calm: 1.7% Variable winds: 0.34% 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/BIGR_windrose_2005-2014.pdf

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