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

    During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 2. Bárðarbunga and Holuhraun - overview

    dispersion model AVCC Aviation colour code map Prohibited area Prohibited area around the Holuhraun lava field Prohibited area Preliminary assessment of the risk of flooding Short articles on the subject The latest articles are on top of the list: Steam plumes from Holuhraun lava field End of eruption - photos Bárðarbunga - decay of seismic activity /earthquakes-and-volcanism/articles/nr/2947
  • 3. The Bárdarbunga/Holuhraun eruption 2014-2015

    chapter on BárðarbungaBárðarbunga system, a pre-publication extract from the Catalogue of Icelandic Volcanoes (pdf 0.9 Mb). NewsIn reversed order.2016 On the Bárðarbunga gradual caldera collapse - An article in Science Activity in the Bárðarbunga system since the end of the eruption2015Bárðarbunga AVCC now green The eruption has come to an endNew equipment at HoluhraunMonitoring device rescued /volcanoes/about-volcanoes/bardarbunga/the-bardarbungaholuhraun-eruption/
  • 4. Bárðarbunga and Holuhraun - overview

    dispersion model AVCC Aviation colour code map Prohibited area Prohibited area around the Holuhraun lava field Prohibited area Preliminary assessment of the risk of flooding Short articles on the subject The latest articles are on top of the list: Steam plumes from Holuhraun lava field End of eruption - photos Bárðarbunga - decay of seismic activity /earthquakes-and-volcanism/articles/nr/2947/
  • 5. VI_2015_006

    m 2 or less, compared with losses of 80 W m 2 or more over neigh- bouring cloud-free regions. The conditions around midnight, off the southeast coast on 27 July, and along the north coast on 3 September, clearly show the limited ability (in the model) of even a complete high-level cloud cover to affect the longwave radiation balance at the surface. Mid- level clouds are usually simulated together /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
  • 6. VI_2020_005

    and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 7. Refsgaard_1-Welcome

    Geological Survey of Denmark and Greenland Ministry of Climate and Energy Nordic Network on Adaptive Management in relation to climate change (NONAM) PhD course: “Adaptive management in relation to climate change” Copenhagen, August 22-26, 2011 Jens Christian Refsgaard Welcome NONAM •Adriaan Perrels FIVA •Frederik Uldall Geocenter Copenhagen/GEUS •Jens Christian Refsgaard Geocenter Copenhagen /media/loftslag/Refsgaard_1-Welcome.pdf
  • 8. Machguth_Horst_CES_2010

    experiments with different RCM’s • explore RCM biasesapply 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
  • 9. 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
  • 10. IPPC-2007-ar4_syr

    Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf

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