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Results:

• 11. VI_2009_006_tt

  cauldrons and jökulhlaups in Skaftá 3.1 The subglacial lakes There are two powerful subglacial geothermal areas under the western part of the Vatnajökull ice cap forming surface cauldrons by melting the glacier from the base. The centers of the cauldrons are approximately at N 64 29.25’ W 17 30.50’ and N 64 29.75’ W 17 37.00’ and they are called the Eastern and Western Skaftá cauldrons, respectively /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 12. VI_2015_006

  Differences in net shortwave flux due to differences in cloud cover (compare with Figure 5) are especially noticeable on 27 July and 3 August around (local) noon when, off the south and southwest coast, the net flux under clear skies is increased by up to 300 W m 2, compared with neighbouring cloud-covered regions. Although, generally, there was a more extensive cloud cover over the land on 3 August than /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 13. Perrels-CBA

  operational cost, etc.) and the annual revenues • consider an appropriate discount rate and assess NPV (net present value), IRR (internal rate of return), and net cash flows • rank alternatives by score level • SCBA: social CBA – total benefits -/- total costs for society, in this case benefits and costs often don’t accrue (entirely) to the same organisation due to the public nature of a project /media/loftslag/Perrels-CBA.pdf

• 14. ces_geus_paakitsoq_full_report

  ) is shown. At the margin the grid boxes of the RCAO RCM are visible. The area between Illulisat and Swiss camp is commonly called Paakitsôq. respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and Box, 2001). The locations of the stations are indicated in Fig. 1, further details /media/ces/ces_geus_paakitsoq_full_report.pdf

• 15. 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

• 16. IPPC-2007-ar4_syr

  a near-zero pre-industrial background concentration, primarily due to human activities. {WGI 2.3, SPM; SROC SPM} There is very high confidence that the global average net effect of human activities since 1750 has been one of warm- ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2 (Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM} The combined radiative forcing due to increases in CO2, CH4 and N2O /media/loftslag/IPPC-2007-ar4_syr.pdf

• 17. Observations - Hamarsfjörður

  Observations - Hamarsfjörður | Observations | Icelandic Meteorological office Observations - Hamarsfjörður Mon 1.05 14 GMT 4.8° WSW 10 Max wind : 11 / 14Road temp. : 13.3° 13 GMT 4.9° W 10 Max wind : 11 / 16Road temp. : 11.5° 12 GMT 5.0° W 11 Max wind : 12 / 16Road temp. : 9.5° 11 GMT 3.6° W 12 /m/observations/areas

• 18. Machguth_Horst_CES_2010

  experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf

• 19. ces-oslo2010_proceedings

  by an objective version of the Hess-Brezowsky Grosswetterlagen (OGWL; James, 2007) modified for the COST733 Action1. The OGWL has been identified as well suited for regional hydrological drought studies in north-western Europe (Fleig et al., in press 2). It is derived on a domain covering the eastern North-Atlantic and Europe (30°-76°N; 37°W-58°E) and yields 29 WTs. The WTs are characterised /media/ces/ces-oslo2010_proceedings.pdf

• 20. Reykholt-abstracts

  in sea-ice and snow sesearch Allen Pope, Ian C. Willis, Finnur Pálsson, Neil S. Arnold1, W. Gareth Rees and Lauren Grey ......................................................................................................................................... 31 Elevation change, mass balance, dynamics and surging of Langjökull, Iceland from 1997 to 2007 Peter Rieger /media/vatnafar/joklar/Reykholt-abstracts.pdf