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• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. Sea ice in October 2009

  was observed close to the mouth of Önundarfjörður. The Cost Guard went on ice-survey the 6th of October. They observed 14 icebergs west and northwest of Westfjords, and most of them were approximately 200 nm from the cost. The iceberg closest to shore was located 77 nm westnorthwest of Bjarg. In addition to a detailed map of the icebergs location, the Cost Guard issued as well infrared (IR) images /sea-ice/monthly/2009/nr/2332

• 3. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 4. BIGJ_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 35 62 48 77 8 4 83 63 64 22 19 14 7 4 11 11 14 41 1 5 24 25 18 45 64 41 3 2 93 35 11 17 7 11 47 16 24 67 36 Wind rose BIGJ January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 12 Frequency of wind /media/vedur/BIGJ_windrose_2005-2014.pdf

• 5. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 6. Future Climate and Renewable Energy - Impacts, Risks and Adaptation 31 May - 2 June Presentations

  : model evaluation and future projections Hanna Tietäväinen Summertime precipitation in Finland under recent and projected climate Sara C. Pryor Intense and extreme wind speeds over the Nordic countries Hydrological projections, runoff Keynote Dennis Lettenmaier Runoff projections and impacts on water resources Liga Kurpniece Climate change impacts on the hydrological regime in Latvia Deborah /ces/publications/nr/2016

• 7. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 77/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas

• 8. VI_2019_009

  To distinguish between rain and snow, the volume is com- pared to the water equivalent but the volume of snow is ten times larger. Figure 1. How PWD22 determines the type of precipitation. Using the information about the changes of the backscatter signal, water equivalent and temper- ature the Vaisala Present Weather Detector can give information about the type of precipitation. It is also used /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 9. vanRoosmalen_etal-2009-WRR_2007WR006760

  marine deposits with a total thickness of generally 200–300 m. The Mio- cene layers dip slightly to the west. Beneath the Miocene sequence, Paleogene clay sediments of regional extent are found. The Paleogene unit is conceptualized as an aquitard that acts as a lower boundary to groundwater flow. [14] The Quaternary and Miocene sand formations often form large interconnected aquifers /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 10. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf