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• 11. Windspeed

  to a slight inaccuracy in the calculations. The figure on the right loosely shows the relationship between m/s and a few Beaufort-values. The prerequisites of the calculations above are: The equation: W = 0.836B3/2 where W is windspeed in m/s and B is value on the Beaufort-scale. 1 m/s = 3.6 km/h = 1.944 knots (2.237 miles per hour) Below is a detailed table with comparison between Beaufort /weather/articles/nr/1283/

• 12. Material from the Workshop in Reykjavík 2010

  /nonam/workshop/material/

• 13. VI_2016_006_rs

  and in the uppermost rows of houses below Botnabrún. The most effective mitigation options to improve the landslide hazard situation in southern Seyðisfjörður is draining of the main source areas in Neðri-Botnar in the lower part of the mountainside as well as a construction of a moderately high catching dam above the top row of houses below Botnabrún, and debris retention basins and guiding dams at the lateral /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 14. VI_2009_012

  -20.367 6.35 6.4 6.5 6.2 6.4 -1.3 -2.1 20000621 005147.0 63.972 -20.711 5.00 6.6 6.5 6.6 6.5 -1.3 -2.2 A second advantage of the two step regression applied is that when the Mi are known, errors in the magnitude estimate do not affect the estimation of the distance parameter a. When both the distance (a) and the magnitude (b) parameters are fitted in a one step regression, a positive /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 15. Bárðarbunga earthquakes 3D

  of ten days. An unusual presentation in the sense that the surface location is shown on a topographic map at the bottom, instead of at the top, in order to improve visibility and clarify the connection between location and depth. The gray planes represent depths at 0 km, 5 km and 10 km from the true surface. The colour code of the earthquakes indicates days as counting from 16th August which /earthquakes-and-volcanism/articles/nr/2948

• 16. 2010_003rs

  on the Reykjanes Peninsula on 17 June ............................ 41 3.3 Other faults in SW-Iceland .................................................................................... 43 3.3.1 Geysir region (box A) .................................................................................. 43 3.3.2 Reykjanes Peninsula (boxes B-F /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 17. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  and top–down governance. Finally, this research shows that in a basin where one type of extreme is dominant—like droughts in the Alentejo (Portugal) and floods in Rivierenland (Netherlands)—the potential impacts of other extremes are somehow ignored or not perceived with the urgency they might deserve. Keywords Standardized comparative analysis  Adaptive and integrated water management (AIWM /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 18. VI_2015_009

  (Crochet, 2012a, b; Crochet & Þórarinsdóttir, 2014) and in eastern Iceland (Crochet & Þórarinsdóttir, 2015). This study is a continuation of this work. The capacity of the IFM to estimate design floods at ungauged locations is now evaluated for river basins having substantial glacier coverage and/or substantial groundwater contribution to streamflow. The report is organized as follows. Section 2 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 19. VI_2015_007

  The idea is to compensate for the lack of temporal data by spatial data, taken within a homogeneous region with respect to flood characteristics, and transfer information regarding flood characteristics from gauged sites to the target site. The IFM has already been evaluated in northern Iceland (Crochet, 2012a,b). Results are very encouraging but indicate that a limited number of gauged sites can /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 20. Glossary

  We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208