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• 41. 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

• 42. 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/

• 43. 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

• 44. Reykholt-abstracts

  – from LiDAR DEM, aerial images and historical photographs Michelle Hofton, B. Blair, D. Rabine, and S. Luthcke ........................................................ 19 Using NASA's LVIS wide-swath, full-waveform laser altimeter system to precisely and accurately image ice surfaces from high altitude Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 2 Tómas /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 45. Linnet_Ulfar_CES_2010

  2015, 2025, 2035 and 2050 North (Blanda) East (Karahnjukar) South (Thorisvatn) Change in average inflow to the main storage reservoirs Watershed A v e r a g e i n f l o w [ m 3 / s ] 0 2 0 4 0 6 0 8 0 1 0 0 1 2 0 Last 50 years Last 20 years Last 15 years Last 10 years Last 5 years Temperature corrected Transformation of climate measurements •Change in temperature • 0.75 °C/100y 1950-1975 • 1.55 /media/ces/Linnet_Ulfar_CES_2010.pdf

• 46. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  /lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13 April 2009. [2] WTO, World Tourism Organization (2008): “Climate Change and Tourism - Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain. Available at: http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7 March 2010. [3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for sustainable /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

• 47. Hydropower, Hydrology

  Hydrological Sciences Journal, 53, 100-111. Kriauciuniené, J., Meilutyté-Barauskiené, D., Rimkus, E., Kays, J., Vincevicius, A. (2008). Climate change impact on hydrological processes in Lithuanian Nemunas river basin. Baltica, Vol. 21 (1-2), pp. 1-61. Vilnius. ISSN 3067-3064. Lawrence, D., Haddeland, I. (2010). Uncertainty in hydrological modelling of climate change impacts in four Norwegian /ces/publications/nr/1938

• 48. Case_B___Road_transport_operation_and_infrastructure_planning

  variability Models Emission scenarios 2000 2100 LEVEL OF UNCERTAINTY Near future End of the century Natural climate variability + + Climate model sensitivity (+) ++ Emission scenarios ++ Source: J. Räisänen (Univ. of Helsinki) Probabilistic forecasts of temperature change in southern Finland (1971-2000 barb2right 2011-2020) Temperature change (ºC) P r o b a b i l i t y d e n s i t y ( 1 / º C /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 49. Kok_and_Veldkamp_editorial_ES-2011-4160

  -473. Gabriel, D., S. M. Sait, J. A. Hodgson, U. Schmutz, W. E. Kunin, and T. G. Benton. 2010. Scale matters: the impact of organic farming on biodiversity at different spatial scales. Ecology Letters 13 (7):858-869. Gibson, C. C., E. Ostrom, and T. K. Ahn. 2000. The concept of scale and the human dimensions of global change: a survey. Ecological Economics 32:217-239. Hare, M., and P. Deadman /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 50. VI_2009_012

  +⋅+= (6) and the parameters g and e are given by: g = - b/a and e = -d/a. The parameters of M and M2 in model (5) are thus directly linked with the parameters of form (6) to better constrain the behavior in the near-field, and to provide PGA independence of magnitude very close to the epicenter (see Appendix B). As in model B we use a second order term M2 for the saturation of the PGA /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf