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• 31. ved-eng-2014

  or about 20 percent above the 1961 to 1990 mean. The precipitation was especially heavy in the North and East. At Akureyri 743.7 mm, or 50 percent above the mean. This is the highest annual sum since the beginning of registration in 1928 (although it is only a few mm more than measured in 1989). Table 2. Precipitation overview 2014 station total mm 1961-1990 % 2004-2013 % max /media/vedurstofan/utgafa/skylduskil/ved-eng-2014.pdf

• 32. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  extensively used in experimental economics over the past 20 years. One robust result is that a considerable percentage of individuals voluntar- ily cooperate, even though the Nash equilibrium is to contribute nothing to the public good (see Anderson 2001 and Ledyard 1995, for reviews).3 Once we drop the homo-œconomicus hypothesis, by assuming that either all agents have social preferences or agents /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 33. Factsheet_Bardarbunga_20141210

  into the small island in the centre of the lava field. This change can be seen from web cameras.  Seismic activity in Bardarbunga continues to be strong. The strongest earthquake since noon on Monday, 8. December, was magnitude M4,9 on Tuesday at 18:00. About 20 earthquakes larger then M3,0 were detected since Monday. In total about 180 earthquakes were detected in Bardarbunga since noon on Monday /media/jar/Factsheet_Bardarbunga_20141210.pdf

• 34. Eriksson_Garvill_Nordlund_2006

  to influence freedom to choose travel mode, own ways. Air pollution through emissions, the use of household traveling, policy measures such as laws and regulations, economic incentives and disincentives, as well soft strategies, such as information and education, aim to (Loukopoulos, 2005). Collectively, strategies aiming to change travel behavior are often referred to as travel demand management (TDM /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 35. Kurpniece_Liga_CES_2010

  From 1925 to 1938, Aiviekste HPP was the largest in Latvia. Daugava and Aiviekste Basins Study area After Plavinas HPP was constructed in 1967, territories near Plavinas city and above river to Jekabpils city almost every spring are endangered by floods caused mostly by ice jams. Hydrological model • since year 1994, HBV model is used at LVGMC • HBV 96 model (version 4.5) was used to simulate /media/ces/Kurpniece_Liga_CES_2010.pdf

• 36. Bardarbunga_Daily_status_report_260814

  draining from Vatnajökull regions affected by the unrest is normal for this time of the year. At the Upptyppingar hydrometric station on Jökulsá á Fjöllum, discharge has averaged 180 m3/s in recent days and conductivity is close to 180 uS/cm. A sensor in Rjúpnabrekkukvísl (Skjálfandafljót water divide, NW part of Bárðarbunga) shows 60 uS/cm today and Köldukvísl (receiving meltwater from W-Bárðarbunga /media/jar/Bardarbunga_Daily_status_report_260814.pdf

• 37. ces-oslo2010_proceedings

  ............................................................................... 20 Räisänen, J. Probability distributions of monthly-to-annual mean temperature and precipitation in a changing climate ......... 22 Nikulin, G., Kjellström, E., Hansson, U., Strandberg G. and Ullerstig A. Nordic weather extremes as simulated by the Rossby Centre Regional Climate Model: Model evaluation and future projections /media/ces/ces-oslo2010_proceedings.pdf

• 38. Lorenzoni_Pidgeon_2006

  their lifestyles for this purpose. Of those who would be prepared to change their way of living, most (92% to 96%) favoured options that could be easily undertaken in the home, and that would cost almost nothing, like recycling and using less energy. Fewer favoured reducing their private transport (68% would use the car less; 62% would take fewer flights), whilst price increases were not popular (only 37 /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 39. Isskyrsla_20100407

  - W022°51' 12.N67°42' -W022°10' 13.N67°42'- W022°20' 14.N67°47' -W022°08' 15.N67°46'- W021°40' 16.N67°46' -W021°37' 17.N67°38' -W021°05' 18.N67°43' -W021°02' Næst landi: 52 sml NV af Barða. 48 sml NV af Straumnesi. Hér að neðan er nákvæm staðsettning ísjaðarsins ________________________ Friðrik Höskuldsson Yfirstýrimaður 1. N65°49.46' W028°04.81' 2. N65°44.19' W027°49.00' 3. N65°42.85' W027°38.41 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 40. VI_2015_005

  depression .. 18 9 Relative seasonal occurrence of mean sea level pressure modes........................ 20 10 Composite mean temporal tendencies of mean sea level pressure...................... 22 11 Composite mean 500 hPa geopotential height anomalies ................................ 25 12 Composite mean surface wind speed anomalies ............................................ 27 13 Composite /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf