74 results were found for b 홈타이《Õ1Õx4889x4785》신이문역남성전용霙신이문역딥티슈σ신이문역딥티슈출장轸신이문역로미로미🎅🏽reformed.

Results:

• 41. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  on the costs of weather related delays and interruptions. Leviäkangas (2007) mentions an amount of 20 ~ 30 million euro per year. As mentioned before over time road users will start to adapt if they realize that certain delays occur too frequently. Responses could vary from shifts in departure time to switching to another mode or even relocation of activities. A note on service levels In road /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 42. VI_2009_002rs

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_002rs.pdf

• 43. Hydropower - Glacier, Snow and Ice

  of Storbreen, Norway. Journal of Glaciology, 54 (185), 245-258. (Available online at IGS: http://www.igsoc.org/journal/54/185/j07j058.pdf.). Crochet, P. (2007). A study of regional precipitation trends in Iceland using a high quality gauge network and ERA-40. J. Climate, 20(18), 4659-4677, doi: 10.1175/JCLI4255.1. Crochet P., Jóhannesson T., Jónsson T., Sigurðsson O., Björnsson H., Pálsson F. & Barstad I /ces/publications/nr/1940

• 44. ces_geus_paakitsoq_full_report

  conditions as a lower boundary condition from the driving GCM. The RCAO model-output is from a pan-arctic run for the years 1960–2080 at approx. 50 km resolution. The first 20 years of the model run must be considered as spin-up time for the ocean module. The RCAO run is experimental since the model is in a development state and the output has not yet been evaluated over Greenland (Ralf Döscher, personal /media/ces/ces_geus_paakitsoq_full_report.pdf

• 45. VI_2009_006_tt

  varð mest 123 m3 s 1 en rennsli hlaupsins við jökuljaðar varð mest 97 m3 s 1. Þetta hlaup er ekki hægt að skýra með viðteknum kenningum um jökulhlaup fremur en önnur Skaftárhlaup. Heildarrúmmál hlaupsins var 53 Gl. Geymsla vatns í hlaupfar- veginum undir jöklinum var reiknuð út frá rennslisgögnunum en hún varð mest 35 Gl, sem samsvarar tveimur þriðju af heildarrúmmáli hlaupsins. Geymslan í /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 46. 2005EO260001

  magnitudes. (b) Seismic tremor amplitude in three different frequency bands. (c) Volcanic plume height. (d) Number of lightning. Lightning and tremor amplitude roughly correlate with plume height. Intensifi ed human activity and a growing population have changed the climate and the land biosphere. One of the most widely recog- nized human perturbations is the emission of carbon dioxide (CO2 /media/jar/myndsafn/2005EO260001.pdf

• 47. VI_2017_009

  11 / 12 MPI-ESM-LR REMO2009 45 / 85 13 / 14 IHCEC-EC-Earth RCA4 45 / 85 15 / 16 IHCEC-EC-Earth COSMO-CLM4-8-17 45 / 85 17 / 18 CNRM-CERFACS-CM5 RCA4 45 / 85 19 / 20 CNRM-CERFACS-CM5 COSMO-CLM4-8-17 45 / 85 11 3 Which domain, resolution, and models of the CORDEX project should be selected for the analysis of 21st century climate change in Iceland? The subject of this chapter /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 48. glacier_mass_balance_poster

  mass balance of three small ice caps (with areas from 15 to 80 km2) over 6 to 20 years, were efficiently estimated from maps of glacier elevation changes deduced by SPOT 5 HRS, EMISAR and aerial photographs • Accuracy of estimating the elevation changes, was greatly improved by using the highly precise EMISAR DEM as a reference for co-registration and offset correction EMISAR Co-registration /media/ces/glacier_mass_balance_poster.pdf

• 49. Program

  on the afternoon of Friday, 27 August 2010 (at a time that enables catching late return flights to Norway and Denmark). Day one: 26 August 2010 9:00 opening and welcome by local representative Sigrún Karlsdóttir and by Adriaan Perrels (FMI, Fi) as NONAM coordinator 9:20 p1 Jens Christian Refsgaard (GEUS, Dk). Uncertainty and Risk - terminology and concepts 9:50 p2 Gareth James Lloyd (DHI, Dk). What /nonam/workshop/program/

• 50. RaisanenJouni_CES_2010

  not representative of present or future climate conditions? Winter mean T in Helsinki (1961-2008) 1961- 20081961- 1990 Temperature (°C) P r o b a b i l i t y d e n s i t y -12 4 Simplest case: change in mean climate, with no change in the magnitude of variability If variability changes as well, the two tails of the distribution (e.g., warm and cold) will be affected differently. IPCC (2001 /media/ces/RaisanenJouni_CES_2010.pdf