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  • 41. Bárðarbunga 2015 - March, April, May

    to reduce risk in the area will be taken and decisions on further opening of the area will then be made. The Aviation Colour Code for Bárðarbunga was changed from orange to yellow when the eruption ended. 5 March 2015 - field trip yesterday Burn out From Holuhraun lava field 4 March 2015. The photo is taken from the central part of crater Baugur, view to the North along the crater /earthquakes-and-volcanism/articles/nr/3122/
  • 42. Bardarbunga-2015_MarchAprMay-events

    and May. New material is added to the top of the article. In combination, the monthly articles give an overview of events: August, September, October, November, December, January, February, March-April-May and the overview article (list of links). Calendar Below is a short-cut to additions in March, April and May plus an announcement 1st June. March: 2-3-4-5-9-12-16-24-26. April: 1-3-8-11 /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf
  • 43. BIGJ_windrose_2005-2014

    1 2 1 1 Wind rose BIGJ April 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: 114 Calm: 0.88% Variable winds: 0% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 /media/vedur/BIGJ_windrose_2005-2014.pdf
  • 44. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

    RM, Capraro MM (2002) Myers-Briggs Type Indicator score reliability across studies: a meta-analytic reliability generalization study. Educ Psychol Meas 62:590–602 Carlson JG (1985) Recent assessments of the Myers-Briggs Type Indicator. J Personal Assess 49:356–365 Carlyn M (1977) An assessment of the Myers-Briggs Type Indicator. J Personal Assess 41:461–473 Clack GB, Allen J, Cooper D et al (2004 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf
  • 45. Lorenzoni_Pidgeon_2006

    for people to conceptualise and to relate to their daily activities, arguably because it cannot be easily translated into the language of popular culture (Ungar, 2000; see also mental models of cli- mate change by Bostrom et al., 1994; Kempton, 1997; discussed later). Secondly, the various datasets available detailing public opinions and attitudes on climate PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
  • 46. The weather in Iceland in 2022

    was particularly cold; the temperature was 5 °C below average in both places. It hasn't been this cold in Reykjavík in December for over 100 year. Precipitation The year 2022 was unusually wet in Reykjavík. It was relatively wet in the capital in the beginning of the year, with March exceptionally wet. It was the wettest March on record, with total precipitation almost triple the average precipitation /about-imo/news/the-weather-in-iceland-in-2022
  • 47. The weather in Iceland in 2020

    to the 10-year average. It was relatively warmer in coastal areas but colder in the inland.JuneJune was warm and favorable. It was relatively warmest in the Northeast but cooler in the southwestern part. Wind and precipitation were close to average.July July was rather cold compared to recent years, although the mean was above the 1961 to 1990 average. Yet the weather was not unfavorable /about-imo/news/the-weather-in-iceland-in-2020
  • 48. BIHN_windrose_2005-2014

    9 3 2 2 7 1 6 8 6 12 9 13 2 15 8 Wind rose BIHN March 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: 2200 Calm: 6% Variable winds: 0.73% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 /media/vedur/BIHN_windrose_2005-2014.pdf
  • 49. 2005EO260001

    ) by fossil fuel burning and land-use change. As the terrestrial bio- sphere is an active player in the global carbon cycle, changes in land use feed back to the climate of the Earth through regulation of the content of atmospheric CO2, the most impor- tant greenhouse gas, and changing albedo (e.g., energy partitioning). Recently, the climate modeling community has started to develop more /media/jar/myndsafn/2005EO260001.pdf
  • 50. BIAR_windrose_2005-2014

    1 8 1 7 1 9 4 1 7 5 21 5 27 2 32 5 48 9 68 4 82 1 Wind rose BIAR September 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: 7233 Calm: 3.5% Variable winds: 8.7% Average wind speed for wind direction Wind direction (°) Wind /media/vedur/BIAR_windrose_2005-2014.pdf

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