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Results:

• 21. The weather app

  News The weather app The ever changing /about-imo/news/nr/2812

• 22. The weather app improved

  News The weather app improved The ever /about-imo/news/nr/3224

• 23. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 24. Reykholt-abstracts

  of Norwegian glaciers – an overview Liss M. Andreassen*, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen Section for glaciers, snow and ice, Norwegian Water Resources and Energy Directorate (NVE) * Corresponding author, e-mail: lma (at) nve.no ABSTRACT The current glacier monitoring programme in mainland Norway includes direct mass balance investigations on 14 glaciers. Accurate maps /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 25. 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

• 26. 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

• 27. Kok_JGEC658_2009

  to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf

• 28. Lorenzoni_Pidgeon_2006

  PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN AND USA PERSPECTIVES IRENE LORENZONI and NICK F. PIDGEON∗ Centre for Environmental Risk and Tyndall Centre for Climate Change Research, Zuckerman Institute for Connective Environmental Research, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK E-mail: i.lorenzoni@uea.ac.uk Abstract. If uncontrolled, human influences /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 29. VI_2015_005

  Franz Josef Land. The western boundary at 71 W excludes Hudson Bay and Foxe Basin, both associated with their own storm climate. Baffin Bay is included in its entirety, since storm activity in that region is closely linked to that over the western North Atlantic (Dacre & Gray, 2009). The eastern boundary at 55 E is chosen to completely include the Barents Sea. This results in an area of 21,625,566 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 30. News

  News © Examples from the weather app /about-imo/news/bigimg/2812