Note
Volcanic eruption is ongoing on the Sundhnúksgígaröð crater row. Gas pollution hazard in the area. More

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Results:

11. GA_2009_91A_4_Andreassen

). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf
12. Refsgaard_1-Welcome

Organisers NONAM •Finnish Meteorological Institute, FMI (Adriaan Perrels) •Geological Survey of Denmark and Greenland, GEUS (Jens Christian Refsgaard and Hans Jørgen Henriksen) •Icelandic Meteorological Office, IMO (Sigrún Karlsdóttir) FIVA - International Research School of Water Resources •University of Copenhagen, KU (Frederik Uldall) Course objectives • To introduce students to the concept /media/loftslag/Refsgaard_1-Welcome.pdf
13. Gudmundsson-etal-2011-PR-7282-26519-1-PB

-corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1 N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
14. Group4

); new long-term investment strategy prioritizing low- or zero-net carbon forms of mobility 2040 Modal shift in logistics chains, especially within heavy industry. 3.3 Backcasting scenario narrative Low-Impact Mobility Project Evaluation (LIMPE) Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even though the future is inherently uncertain, one certainty /media/loftslag/Group4.pdf
15. vanRoosmalen_etal-2009-WRR_2007WR006760

1998] and RCM output such as incoming and outgoing, short- and long-wave radiation, temperature, water vapor pressure, and wind speed: ETref ¼ 0:408D Rn Gð Þ þ g 900T þ 273 u2 es eað Þ Dþ g 1þ 0:34u2ð Þ ð3Þ where ETref is reference evapotranspiration (mm d1), Rn is net radiation at the crop surface (MJ m2 d1), G is soil heat flux density (MJ m2 d1), T is mean daily air temperature at 2 m /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
16. ces-oslo2010_proceedings

anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf
17. Keranen_Jaana_CES_2010

ilmiö W inter Sprin g SummerA utumn Kosteus Lauha t talve t Talvitulvat Jäätävä sade Hyyde Kova tuu li … Aikaisempi kevät ja tu lvat Ku ivuus Ku ivuvat vesiva rastot … Ku ivuus Rankkasa teet sa lamointi Rakeet … Myrskyt Rankkasateet Rou ta Jääkannen muodostaminen … yli y €yli y €Merkittävät3 x - y €x – y €Keskinkertaiset2 alle x €alle x €Vähäiset1 Mahdollisuuden tunnisteväriRiskin /media/ces/Keranen_Jaana_CES_2010.pdf
18. Adalgeirsdottir-etal-tc-5-961-2011

(DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
19. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

increased net precipitation and increased rainfall intensity put pressure on the sewage system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding storms could be as high as 2,5 meters. The challenges have been divided into two main themes: sea level change and rainfall. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
20. Case_A___Horsens_Fjord

increased net precipitation and increased rainfall intensity put pressure on the sewage system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding storms could be as high as 2,5 meters. The challenges have been divided into two main themes: sea level change and rainfall. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop /media/loftslag/Case_A___Horsens_Fjord.pdf