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68 results were found for AG包杀网 130—0687—8615 包abwer纱.


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  • 11. 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
  • 12. 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
  • 13. 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
  • 14. 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
  • 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. VI_arsskyrsla2020

    til 2000. Mest snjódýpt á árinu mældist 130 cm við Skeiðsfossvirkjun þ. 23., 24. og 25. desember. Sólskinsstundir, loftþrýstingur og vindhraði Árið var óvenjusólríkt á suðvesturhluta landsins á árinu. Sólskinsstundir í Reykjavík mældust 1582,2 sem er 314 fleiri en í meðalári 1961 til 1990. Árið var það þriðja sólrík- asta frá upphafi sólskinsstundamælinga í Reykjavík. Á Akureyri mældust /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
  • 17. skyrsla-rannshops-eldfraedi-natturuvar_JHI_20150304

    Kvikugösin eru bláleit á meðan vatnsblandan er hvít. Hitamælingar sýna að hiti í sprungum í botni gígsins fer upp í 550 til 600 °C. Það gefur ástæðu til að ætla að fljótandi kviku sé að finna á um 3 til 5 metra dýpi undir gígyfirborði. Yfirborð á gasbreiðum sem einkennast af kvikugasa virkni er um 250 til 300 °C heitt á meðan yfirborð sem gufuaugu rísa af er um 100 til 130 °C. Hraunið var í morgun í /media/jar/skyrsla-rannshops-eldfraedi-natturuvar_JHI_20150304.pdf
  • 18. Eyjafjallajokull_status_2010-04-26_IES_IMO

    : No detections over the eruption site since 19 April 2010 Noises: Report from ~20 km SE of the volcano of booming sounds (02:30 GMT) Meltwater: Continuing discharge of water from Gígjökull due to ice-melt at the eruption site. Discharge at the old Markarfljót bridge, 18 km from Gígjökull, is estimated at 110–130 m3 s–1, of which 30–40 m3 s–1 is baseflow. Conditions at eruption site: No visual /media/jar/Eyjafjallajokull_status_2010-04-26_IES_IMO.pdf
  • 19. New article on glacier changes in

    New article on glacier changes in Iceland over the past 130 years A scientific article by Icelandic glaciologists is an important contribution to global studies and assessments of climate change. The average mass loss of the Icelandic glaciers per unit area in recent decades is among the highest on Earth. 7.12.2020 /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years
  • 20. Arctic cooperation

    hydrology, glaciology, climatology, seismology and volcanology, and staff are involved in projects relating to natural hazards, such as volcanic ash, extreme weather and flooding. The IMO's headquarters are in Reykjavik but other offices are in Ísafjörður and at the international airport in Keflavík. IMO has a staff of 130 people, in addition to about 120 people who work on research-related /about-imo/arctic/

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