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• 51. The weather in Iceland 2006

  © Sigvaldi Árnason. Back to top The spring (April and May) was very sunny in the South, the sunniest since 1924. April was rather cold, not least in comparison with the preceding five months of April, which were all very warm. There was some snow in the North during the first half of the month. The first 10 days of May were very warm, temperatures in sheltered areas in the Southwest reached 20°C /about-imo/news/nr/1206/

• 52. The weather in Iceland 2010

  was unusually light. The barometric pressure reached the highest annual value on record. The climate was very favourable and windstorms markedly fewer than usual. Temperature Thermometer screen at IMO's grounds in Reykjavík. Photo by Jón Gunnar Egilsson, 15 September 2010. Temperature The average temperature in Reykjavík was 5.9°C, 1.6°C above the 1961 to 1990 mean, and has only once /about-imo/news/2011/nr/2112

• 53. The weather in Iceland 2010

  was unusually light. The barometric pressure reached the highest annual value on record. The climate was very favourable and windstorms markedly fewer than usual. Temperature Thermometer screen at IMO's grounds in Reykjavík. Photo by Jón Gunnar Egilsson, 15 September 2010. Temperature The average temperature in Reykjavík was 5.9°C, 1.6°C above the 1961 to 1990 mean, and has only once /about-imo/news/nr/2112

• 54. ved-eng-2010

  The average temperature in Reykjavík was 5.9°C, 1.6°C above the 1961 to 1990 mean, and has only once been higher, 6.0°C in 2003. It has twice before been equally high as now, in 1939 and 1941. The temperature has now been above average (1961-1990) for 15 years in a row. Nine months registered above average temperatures, three were below. January had the largest positive anomaly, almost 3°C /media/vedurstofan/utgafa/skylduskil/ved-eng-2010.pdf

• 55. CES_D2.4_VMGO

  size. References 1. Meehl, G.A., C. Covey, T. Delworth, M. Latif, B. McAvaney, J.F.B. Mitchell, R.J. Stouffer and K.E. Taylor, 2007: The WCRP CMIP3 Multimodel Dataset: A New Era in Climate Change Research, BAMS, 88, 1383-1394, DOI: 10.1175/BAMS-88-9-1383. 2. Naki �enovi � N., J. Alcamo, G. Davis, B. de Vries, J Fenhann, S. Gaffin, K. Gregory, A.Grübler, T.Y. Jung, T. Kram, E.L. La Rovere /media/ces/CES_D2.4_VMGO.pdf

• 56. The weather in Iceland in 2019

  4.8 1.1 17 147 -0.1 Höfn í Hornaf. 5.3 # -0.1 Fagurhólsmýri 5.5 0.9 24 til 25 117 -0.1 Vatnsskarðshólar 6.2 1.1 8 80 0.2 Stórhöfði 5.9 1 15 til 16 143 0.2 Árnes 5 1.4 6 140 0.3 Hjarðarland 4.7 # 4 29 0.3 Hveravellir 0.7 1.8 5 /about-imo/news/the-weather-in-iceland-in-2019

• 57. VI_2020_004

  .................... 85 8 Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86 Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87 Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88 Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 58. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  Journal of Environmental Management 88 Heid , Øste d e A broad range of tools are available for integrated water resource management (IWRM). In the EU research project NeWater, a Human dependence on water leaves us vulnerable to climate change, flood and drought hazards, and poverty dynamic element of vulnerable groups and their relation- ship to water resources, and to represent the decisions /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 59. A new absolute minimum temperature record

  temperature record for May in Iceland 6.5.2013 On 2 May the automatic weather station at Brúarjökull registered a minimum temperature of -21.7°C. This is the lowest temperature ever measured in Iceland in May. However, it should be kept in mind, that the station /about-imo/news/nr/2691

• 60. VI_2020_005

  flooding, sea level, sea level rise, risk assessment, natural hazard This work was carried out for the Icelandic Meteorological Office and is a part of Masters Thesis ISSN 1650-6553 No. 470, published by the Department of Earth Sciences at Uppsala University in 2019. The Masters Thesis is available as a whole at www.diva-portal.org. Copyright c Guðrún Elín Jóhannsdóttir Contents 1 Introduction /media/vedurstofan-utgafa-2020/VI_2020_005.pdf