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Results:

• 11. VI_2015_005

  and about 900 km based on NCEP reanalyses. Using NCEP-NCAR reanalyses, Rudeva and Gulev (2007) and Rudeva and Gulev (2011) defined effective cyclone radius as the distance from the low-pressure centre to the point, at which the radial derivative of MSLP goes to zero. They found that effective radii varied between 200 – 1000 km, with 50% of radii between 400 – 800 km. Based on these results, a low /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 12. VI_2015_009

  vhm145 Vestari-Jökulsá D+J+L 844 751 11.3 924 1971–2014 vhm167 Austari-Jökulsá D+J 553 916 28.8 1208 1985–2014 8 vhm59 vhm64 vhm66 vhm102 vhm116 vhm162 vhm233 vhm235 vhm238 vhm144 vhm145 vhm167 Figure 1. Location of river basins. 9 l l l l l l l l l l l l l l l l l l ll l l l l l l l l l l l l l ll l l l l l 0 100 200 300 50 15 0 25 0 35 0 Days since Sept. 1st Q (m ³/s ) vhm59 S O N D J F M A M J /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 13. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 14. event_numbers_17022015

  Earthquakes since 16. August 2014 00:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 35.000 - - - - - - - checked ~ 20.000 ~ 8.000 ~ 9.000 ~ 200 ~ 300 ~ 1.800 ~ 600 ~ 20 M3.0-3.9 1208 99 1089 6 2 4 7 1 M4.0-4.9 655 7 646 1 1 0 0 0 M>5.0 79 0 79 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell cluster north /media/jar/myndasafn/frodleikur/event_numbers_17022015.pdf

• 15. IPPC-2007-ar4_syr

  (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf

• 16. 2010_005_

  which are significantly lower com- pared with similar beginning and end years. Consequently, for the 2004–50 period, the average RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are somewhat larger than for the reduced IPCC ensemble mean. Additionally, the tabulated values of SAT differences between the 1961–90 control period and either the 2021–50 /media/ces/2010_005_.pdf

• 17. 2005EO260001

  in addition to real-time access to locations deter- mined by the United Kingdom’s Met Offi ce. IMO’s C-band weather-radar can be used to monitor and track tephra plumes [Lacasse et al., 2004], and over 200 weather stations monitor weather conditions throughout the country. Plume-trajectory predictions are calculated for eruption sites by using current meteorological data. Geophysical Precursors /media/jar/myndsafn/2005EO260001.pdf

• 18. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 19. IMO_AnnualReport2014

  is the largest in Iceland in over 200 years. The progression of the rifting occurred in sequences of varia- ble rates and was o?and on accompanied by low-frequency tremor. This tremor was presumed of volcanic origin, particularly after the appearance of four cauldrons above the dyke. Shortly after the earthquake swarm began, the Bárðarbunga caldera began to sub- side, totalling over 60 m. The rate /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 20. VI_2020_004

  -laid with the deposit isopach for the 1362 eruption. ................ 74 Figure 46 Vertical velocity profile for the eruptive mixture (Öræfajökull) ............................. 75 Figure 47 Probabilistic hazard map for a load ≥1.0 kg/m2 (Öræfajökull) ............................... 76 Figure 48 Probabilistic hazard map for a load ≥100 kg/m2 (Öræfajökull) ............................. 77 Figure /media/vedurstofan-utgafa-2020/VI_2020_004.pdf