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• 31. Outline of the earthquake fault in Ölfus

  of faulting took place during the June 2000 earthquake sequence in southern Iceland. The star denotes the source of the large earthquake that occurred south-west of Ingólfsfjall. Significant earthquake activity has taken place west of the main fault; this is the location where a magnitude 5 earthquake occurred in November 1998, making it unlikely that a large earthquake will occur in this region /about-imo/news/nr/1312

• 32. A new absolute maximum temperature for March

  was broken by an astounding 1,7 degree margin, the former record being 18.8 degrees, measured in Eskifjörður in the Eastern Fjords on 28 March 2000. Many local maximum temperature records where also exceeded, amongst those at Teigarhorn in the Eastern Fjords where the maximum rose to 18.2 degrees. The daily recording of maximum temperature at Teigarhorn began in 1872 and the new record exceeded /about-imo/news/nr/2459

• 33. Dataseries and components

  ), quantity (mm), pH Heavy metals in aerosol: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/m3) Cl, NO3-N, SO4-S (µg/m3) Hg (pg/m3) Persistent organic pollutants (POPs), same for precipitation (ng/l) and air (pg/m3): alfa-HCH, beta-HCH, gamma-HCH p,p'-DDE p,p'-DDD o,p'-DDT p,p'-DDT dieldrin HCB cis-chlordan, trans-chlordan, trans-nonachlor, PCB-28, -31, -52, -101, -105, -118, -138, -153, -156 /pollution-and-radiation/pollution/components/

• 34. VI_2009_006_tt

  max Qm Qb Vm Vm Vb (m3 s 1) (m3 s 1) (Gl) (Gl) 1968 09 110 1971 07 658 532 450 230 1973 12 238 191 151 72 1975 09 307 210 172 53 1977 08 545 390 277 134 1980 01 444 351 214 121 1981 08 472 250 360 110 1983 09 222 138 177 99 1986 07 418 275 242 102 1988 08 394 301 188 106 1990 10 129 101 129 75 1994 08 968 726 330 162 1996 08 672 521 249 147 1997 07 335 169 197 60 1998 09 292 149 323 116 2000 08 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 35. VI_2020_004

  height and was introduced by Newhall and Self in 1982 (Newhall & Self, 1982). Over the last decades it erupted with almost regular interval every 10 years with the last five eruptions occurring in the 1970, 1980–1981, 1991 and 2000. All these events have been characterized by a short-lived explosive phase prolonged over a couple of hours followed by an effusive phase. Despite this apparent /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 36. 2010_017

  vhm 26 Without g.w. module 100 35–80 2000 150–350 0.47 0.18 -10.3 2.3 -1.4 8.5 With g.w. module 50 35–80 300 150–350 0.65 0.69 1.6 1.3 7.1 6.9 Figure 11. Scatter plots of the modelled and measured annual discharges for Austari- Jökulsá, vhm 144, 1990–2005. Former calibration without the groundwater module active to the left, and new calibration with the groundwater /media/ces/2010_017.pdf

• 37. Glaciers in Iceland

  of a warming climate in the country.The Icelandic Meteorological Office, The Institute of Earth Sciences, University of Iceland and the Southeast Iceland Nature Centre have published a newsletter briefly describing glacier changes since about 1900 along with the results of monitoring of glacier termini, glacier mass balance and crustal movements induced by glacier changes in recent years.Since 2000 /about-imo/news/glaciers-in-iceland-continue-to-retreat

• 38. IMO at the Arctic Circle Assembly 2017

  IMO at the Arctic Circle Assembly 2017 17.10.2017 The Fifth Arctic Circle Assembly was held in the Harpa Conference Center in Reykjavík on October 13-15. The symposium was attended by 2000 delegates from more /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 39. Map of the glaciers of Iceland

  at the peak of the so called Little Ice Age during the 1890s and also the outlines as they were around the year 2000. The map distinguishes surging glaciers from other outlet glaciers, and identifies all known sub-glacial volcanic calderas. Featured are the names of all named glaciers and the map includes a brochure and a list of glacier names. The Map of Glaciers can be used for both tourism /about-imo/arctic/map-of-glaciers/

• 40. SVALI

  The western cauldron in Vatnajökull ice cap on 19 August 2000, shortly after jökulhlaup in river Skaftá which originated in the cauldron. Photo: Oddur Sigurðsson. The SVALI project examines the complex effects of climate change on the Arctic environment, especially as glaciers, ice and snow. The projects main research questions are as follows: How fast is land ice volume in the Arctic /about-imo/arctic/svali/