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• 41. “The small eruption” in

  and deformation may precede many eruptions this is not always the case and depends on how much stress has already been released and the strength of the upper crust”, says Michelle.Figure 2. A) GPS data from the station KRI in Krísuvík. The blue line indicates the beginning of the eartquake swarm (24.02) and the red line shows the beginning of the eruption (19.03). A rapid deformation was detected /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

• 42. IMO_AnnualReport2014

  of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 43. VI_2014_001

  for the largest ones. For these catchments, the index flood model is ex- trapolated far beyond the range of characteristics for which it was developed and the estimation of µi(D) may not be valid. This is in line with Crochet (2012a,b). This is the case in Region 1 for catchment vhm200, for which the index flood is usually strongly understimated. This catchment is by far the largest and much larger than /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 44. VI_2020_008

  leading to the selection of the Peak-over- Threshold method as it shows more similarities when applied to both sets of data. Intensity– duration–frequency (IDF) graphs are presented for each station, based on simulated precipitation values and station observations. The project results in two 1M5 maps: one based on daily values from midnight to midnight in line with the earlier 1M5 map, and the other /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 45. ces-glacier-scaling-memo2009-01

  2008) together with a regression line through this data set and a regression line derived for a data set of more than a hundred valley glaciers (Bahr and others, 1997). The regression lines are of the form v = csg ; (5) where v and s are glacier volume and area, respectively. The coefficient and exponent for the Icelandic ice caps are c = 0:048, g = 1:23, when the area and volume are expressed /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 46. VI_2015_009

  by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 47. Past temperature conditions in Iceland

  temperature trend, 1.2°C per century. Figure 3. Winter (Dec to March) temperatures at Stykkishólmur. The red line corresponds to a linear trend of 1.2°C per century. We also see that the individual warm and cold winter periods are similar to the corresponding annual ones in temporal behaviour. There are a few warm winters during the 19th century warm period with temperatures /climatology/articles/nr/1213

• 48. Past temperature conditions in Iceland

  temperature trend, 1.2°C per century. Figure 3. Winter (Dec to March) temperatures at Stykkishólmur. The red line corresponds to a linear trend of 1.2°C per century. We also see that the individual warm and cold winter periods are similar to the corresponding annual ones in temporal behaviour. There are a few warm winters during the 19th century warm period with temperatures /climatology/articles/nr/1213/

• 49. On the micro-earthquake activity at Mýrdalsjökull

  cannot rule-out a sudden escalation in seismicity in connection with a hazardous flood. On-line overview of seismicity levels within the caldera is available. An overview of the Katla volcanic system is given in the Catalogue of Icelandic Volcanoes. News 2023 2022 /about-imo/news/micro-earthquake-activity-at-myrdalsjokull

• 50. More

  On Thursday the 26th of March an on-line Scientific Advisory Board meeting was held to discuss the ongoing unrest in the Reykjanes peninsula. Scientists from IMO, University of Iceland, ISOR and representatives from Civil Protection, HS-Orka, ISAVIA-ANS, and the Environment Agency of Iceland attended the meeting.Magmatic intrusion still the most likely explanation for the ongoing /about-imo/news/more-research-is-needed-to-decipher-the-on-going-activity-at-the-reykjanes-peninsula-as-a-whole