12 results were found for 〔대호지면불륜〕 WWWͺP82ͺSHOP 근흥면연하 근흥면원나잇근흥면원나잇톡♞근흥면유부❻ㄅ緒quaternary.

Results:

• 1. Moberg_Anders_CES_2010

  Past changes in climate and hydrology Anders Moberg Department of Physical Geography and Quaternary Geology Stockholm University Conference on Future Climate and Renewable Energy: Impacts, Risks and Adaptation Oslo, 31 May 2010 http://data.giss.nasa.gov/gistemp/ This year so far (Jan – Apr) ... Temperature anomaly (°C) from 1951-80 mean http://www.metoffice.gov.uk/climatechange/science /media/ces/Moberg_Anders_CES_2010.pdf

• 2. Recent publications

  Oddur Sigurðsson, Óðinn Þórarinsson, Philippe Crochet, Tómas Jóhannesson & Þorsteinn Þorsteinsson (2012). Floods in Iceland. In: Z. W. Kundzewicz (ed), Changes in Flood Risk in Europe. Oxfordshire: IAHS Special Publication 10, 257-276. Hálfdán Ágústsson & Haraldur Ólafsson (2012). The bimodal downslope windstorms at Kvisker. Meteorology and Atmospheric Physics 116(1-2), 27-42, doi:10.1007/s00703 /about-imo/arctic/completed-projects/publications/

• 3. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Irrigationa Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Current 101 85 59 13
  6
  4
  1 6 39 79 84 97 A2 145 132 73 10
  10
  7
  6
  8 4 75 92 123 B2 137 119 75 16
  6
  6
  6
  5 21 74 110 141 aValues are in millimeters. 10 of 18 W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15 time and larger area where groundwater levels rise above the drain levels. Table 6 shows the mean discharges /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 4. GA_2009_91A_4_Andreassen

  (alb: AWS) MODELLING LONG-TERM SUMMER AND WINTER BALANCES ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241 ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature /media/ces/GA_2009_91A_4_Andreassen.pdf

• 5. VI_2009_006_tt

  was therefore formed by ice lifting and deformation induced by subglacial water pressures higher than ice overburden pressure. The discharge data and the derived size of the subglacial flood path, as indicated by the volume of water stored subglacially, indicates a development towards more efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the iii range 80–90 m3 s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 6. VI_2020_005

  (Quante and Colijn, 2016). Work on risk analysis and adaptation is in different stages in the countries of the world. Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the probability of such events can rise with climate change (Almannavarnir, 2011 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 7. 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

• 8. VI_arsskyrsla2020

  meteorological services for large areas of the North Atlantic and Green- land. It is the second largest aviation service region in the world. Over the course of a decade IMO was modernized and sta?ed to meet the highest international requirements. The Icelandic public and economic sectors, in particular the fisheries, transportation and agriculture, benefitted hugely from this development making /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 9. VI_2020_004

  .................... 85 8 Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86 Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87 Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88 Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 10. VI_Arsskyrsla_2018_vef

  Nesjum 0-5 5-10 10 15 20-15 2008-2018 1979-1989 Dæmi um ólíkt rennslismynstur. 100 90 80 70 60 50 40 30 20 10 0 Júní mánaðarmeðaltal Ársmeðaltal Rennsli m 3 /s Sigurvegarinn í getraun Veðurstofunnar á Vísindavöku Rannís hlaut heimsókn á Veðurstofuna að launum. Salka Elín Sæþórsdóttir ásamt vinum sínum, Ými og Bjarti. Með þeim á myndinni er Ragnar Heiðar Þrastarson, fagstjóri landfræðilegra /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf