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Results:

• 31. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 32. VI_2014_005

  and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 33. Mid-Latitudes-Agenda1_nov2013EH

  Agenda *All presentations will be in the Forgardur (forecourt) underground basement room of the IMO building at Bustadavegur 7, unless otherwise noted. Wednesday, 13 November Time Agenda Item 09:00 – 09:15 Welcome and Introductions - T Jónsson and E Hanna 09:15 – 09:30 Meeting Structure and Overview - J Overland and E Hanna 09:30 – 10:40 09:30 – 09:45 09:45 – 10:05 10:05 – 10:25 /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 34. Kriauciuniene_Jurate_CES_2010

  of temperature anomaly (ºC) between 1991-2007 and 1961-1990 Variation of annual T anomaly (ºC) between 1991-2007 and 1961-1990 Seasonal differences of P anomaly (in %) between 1991-2007 and 1961-1990 Seasonal differences of Q anomaly (in %) between 1991-2007 and 1961-1990 Variation of annual P and Q anomaly (%) between 1991-2007 and 1961-1990 -40 -25 -10 5 20 35 50 1 9 2 0 1 9 4 0 1 9 6 /media/ces/Kriauciuniene_Jurate_CES_2010.pdf

• 35. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 40/ 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

• 36. Session program Thursday 13. October

  on the long- and on the short-term before large earthquakes Ragnar Stefánsson 10:10 – 10:40 Coffeebreak and poster session 10:40 – 12:10 Oral session - Chair: Peter H. Voss 10:40 – 11:00 High-rate GPS seismology in Iceland Halldór Geirsson et al. 11:00 – 11:20 Rock stress boundaries deduced from rock stress measurements /norsem/norsem2016/program/thursday

• 37. News

  News © Snorri Zóphóníasson Bridge across Ölfusá at Selfoss 26 February 2013 at 16:40. Flood due to rain and snow /about-imo/news/bigimg/2662

• 38. BIIS_windrose_2005-2014

  Wind rose BIIS 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: 33412 Calm: 12% Variable winds: 11% 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 N /media/vedur/BIIS_windrose_2005-2014.pdf

• 39. 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

• 40. Eyjafjallajokull_status_2010-04-26_IES_IMO

  (~16,000 ft) between 12:00 and 14:00 GMT; elevation of 3.9 km recorded at 17:40 GMT [From aerial observations and radar measurements] Heading: Eastwards at elevations above ~4 km (~13–14,000 ft) Colour: Mostly white (steam) to the east of the crater, but grey tephra pulses above the crater Tephra fallout: No ash-fall reported, although light ash-fall possible over Mýrdalsjökull Lightening /media/jar/Eyjafjallajokull_status_2010-04-26_IES_IMO.pdf