83 results were found for d 강동오피♖『dm080.com〉 강동유흥♚강동출장 강동주점 강동아로마.

Results:

• 41. TietavainenHanna_CES_2010

  versa • Very large range within the simulations • Larger number of observation stations in the study area leads to • better compatibility between different observational data sets • smaller bias in the model simulations CES Conference, Oslo 31.5.-2.6.2010 References • Haylock, M. R., Hofstra, N., Klein Tank, A. M. G., Klok, E. J., Jones, P. D. and New, M. 2008. A European daily high-resolution /media/ces/TietavainenHanna_CES_2010.pdf

• 42. Case_B___Road_transport_operation_and_infrastructure_planning

  on the Shifts of climatic zones from cooler or wetter to warmer or drier (a) 1971-2000 (b) 2010-39 A1B observational data set (0.25º grid) from Haylock et al. (2008) (b-d) Based on CMIP3 GCM runs for A1B & the delta-change method (c) 2040-69 A1B (d) 2070-99 A1B Jylhä et al. (2010) Uncertainties in climate change schematically Observed climate Future climate Natural /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 43. Climatological data

  /climatology/data/

• 44. 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

• 45. 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/

• 46. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 47. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 48. VI_2009_012

  to use the available new estimates Mw(v) to build a PGA relationship that would give very similar results as model A. Due to the more complicated relationship between Ci and Mw(v) in the acceleration case, a second order polynomial was chosen as the functional form of h and thus through the least-squares method we estimated the parameters b, c and d according to: Ci = d·Mw2(v) + b·Mw(v) + c /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 49. Lorenzoni_Pidgeon_2006

  level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 50. Volcanic plumes and tephra

  the volcanic plume due to their size and weight fall close to the volcano and constitute the proximal deposit. Smaller particles can reach higher altitudes and persist in the atmosphere for days and weeks and be advected far away by the wind. This fraction of the pyroclastic material can possibly generate a distal deposit very thin and covering wide areas.Term Size Ballistic d > 64 mm Lapilli 2 mm < d /volcanoes/volcanic-hazards/volcanic-emissions/