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• 51. The weather in Iceland in 2019

  168 138 Írafoss 1947.1 # 98.8 98.3 140 134 Keflavíkurflugvöllur 984.2 88.2 94.1 29.1 219 155 The annual total precipitation in Reykjavík was 876.8 mm, 6 percent above the 1971 to 2000 mean. In Akureyri the total was 692.8 mm, 34 percent above the 1971 and 2000 mean. This is the fourth highest annual sum in Akureyri since /about-imo/news/the-weather-in-iceland-in-2019

• 52. The weather in Iceland 2015

  consecutive year above this mean in Reykjavík. But, it was also the coldest since 2000. In Stykkishólmur the average temperature was 4.1°C, 0.6 above the mean, and 3.8°C in Akureyri, also 0.6°C above the mean. In Vestmannaeyjar the mean was 4.8°C, equal to the 1961-1990 mean. In the country as a whole the temperature was 0.5°C above the 1961-1990 mean, but -0.6°C below the mean of the last ten /about-imo/news/nr/3273

• 53. VI_2009_012

  Mw(v) plotted against log distance. The coefficient of correlation between Mw(v) and log distance is 0.24. High correlation coefficients have been shown to affect parameter estimates in one step regression methods (see Fukushima and Tanaka, 1990). The Ci values were also calculated from the derived PGA values. Instead of constructing another magnitude scale based on acceleration it was decided /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 54. Recent publications

  The Icelandic Meteorological Office annually publishes a variety of reports, journals and articles. Below are examples of recent publications, most of which contribute to Arctic issues in general. Large-scale atmospheric conditions associated with major avalanche cycles and cold season weather hazards in Iceland (2013) The wind energy potential of Iceland (2013) Surface wind and air temperature over /about-imo/arctic/completed-projects/publications/

• 55. CES_D2.4_task1

  is projected to approach 90%. The impact of anthropogenic climate change on precipitation is still estimated to be very small at present. In the middle of this century, typically about 60% of all months are projected to have above-median precipitation in northern Europe, although with a substantial variation with the time of the year. An on-line appendix of this report provides detailed tables /media/ces/CES_D2.4_task1.pdf

• 56. GA_2009_91A_4_Andreassen

  (alb: AWS) MODELLING LONG-TERM SUMMER AND WINTER BALANCES ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241 ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature /media/ces/GA_2009_91A_4_Andreassen.pdf

• 57. Publications 2012

  Nawri, Halldór Björnsson, Guðrún Nína Petersen & Kristján Jónasson 44 pp 3,1 Mb 2012-009 Empirical Terrain Models for Surface Wind and Air Temperature over Iceland Nikolai Nawri, Halldór Björnsson, Guðrún Nína Petersen & Kristján Jónasson 33 pp 1,8 Mb 2012-008 Surface Wind and Air Temperature over Iceland based on Station Records and ECMWF Operational Analyses Nikolai Nawri /about-imo/publications/2012/

• 58. Eyjafjallajokull_status_2010-05-20_IES_IMO

  radar measurements, web cameras, ATDnet – UK Met. Offices lightning detection system, NOAA satellite images and web-based ash reports from the public. Eruption plume: Height (a.s.l.): According to radar obersvations, the plume has been at around 5 km/18,000ft. today. Over the volcano, winds blow from the south at 10 m/s, but at the top of the plume the wind is south-southwesterly at 13 /media/jar/Eyjafjallajokull_status_2010-05-20_IES_IMO.pdf

• 59. Update on activity in Eyjafjallajökull 2010

  not exceeded since 16 April 2010. Meltwater draining beneath the old Markarfljót bridge, ~18 km downstream from Gígjökull, had a temperature of over 11°C. The above is based on status report issued collectively by IMO and the Institute of Earth Sciences. The ash cloud will be analysed - 28 April 2010 17:45 Tomorrow and Friday, scientists from the German Aerospace Center (DLR) will do a measurement /earthquakes-and-volcanism/articles/nr/1884

• 60. Journal_of_Hydrology_Veijalainen_etal

  A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf