98 results were found for [77AGG. COM]2d slot dhk4d slot slot woles pbb4 slot 8278 slot japan slot wht.

Results:

• 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. CES_D2.4_VMGO

  the territories of European Russia (ER) and Europe (EU) an ensemble of 9 CMIP3 [1] comprehensive global (coupled atmosphere-ocean) climate models is used in this assessment (Table 1); so called A2 scenario is considered. Both A2 and A1B scenarios are similar in terms of resulting global mean warming up to the mid-21st century IPCC [2]. The projected changes in ER and EU in many cases continue /media/ces/CES_D2.4_VMGO.pdf

• 3. norsem_giulia

  a major source of hazard for people and infrastructure. Due to the flank instability of volcanic edifices, landslides, or flank collapses, at active volcanoes can trigger major eruptions or produce tsunami waves when the material enters open or enclosed water bodies. A large landslide occurred at Askja Volcano, Iceland, on July 21st, 2014. The landslide had a total volume between 30 and 50 /media/norsem/norsem_giulia.pdf

• 4. Journal_of_Hydrology_Veijalainen_etal

  A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 5. Mid-Latitudes-Agenda1_nov2013EH

  11:20 – 11:35 11:35 – 11:55 11:55 – 12:15 12:15 – 12:35 12:35 – 12:45 Jet Stream Especially the North Atlantic (Chair: Robert Erdelyi) A long perspective on Atlantic jet variability – T Woollings A comparison of North Atlantic Jet Stream Representation in ERA-Interim and 20th Century Reanalysis Data - R Hall Frozen assets: what can ships' logbooks tell us about Arctic climate change /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 6. Aurora and the Earth's magnetic field

  currents in its outer core. At the surface, about 90% of the field can be described by a simple dipole field tilting about 10° from the rotation axis. The currents in the Earth's core are slowly varying causing slow changes of the magnetic field, typically on timescales of years and ages. A flow of charged particles from the sun, called the solar wind, hits steadily the magnetic field and bends /weather/articles/nr/2549

• 7. Reports and publications

  et al. 3 2005 Seismic hazard in the Hengill area based on the SIL earthquake catalogue - First results (PDF) Kristján Ágústsson, Páll Halldórsson 42 0,8 2005 A model of the release of the two June 2000 earthquakes based on all available observations (PDF) Sigurlaug Hjaltadóttir, Kristín S. Vogfjörð, Þóra Árnadóttir, Páll Einarsson, Peter Suhadolc 8 8,2 2005 /earthquakes-and-volcanism/reports-and-publications/

• 8. Markarfljót outwash plain and Öræfajökull

  was funded mainly by the National Avalanche and Landslide Fund, with additional financial contributions from the Icelandic Road and Coastal Administration and the National Power Company. Published material Under the link below, each of the chapters can be downloaded or short summaries read. Pagneux, E., Gudmundsson, M. T., Karlsdóttir, S., & Roberts, M. J. (Eds.) (2015). Volcanogenic floods /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 9. 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

• 10. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  Institution BCCR-BCM2.0 Bjerknes Centre for Climate Research, Norway CGCM3.1 (T47) Canadian Centre for Climate Modelling and Analysis CGCM3.1 (T63) same as previous CNRM-CM3 Météo-France CSIRO-MK3.0 CSIRO Atmospheric Research, Australia ECHAM5/MPI-OM Max Planck Institute (MPI) for Meteorology, Germany ECHO-G University of Bonn and Model & Data Group, Germany; Korean Meteorological Agency GFDL /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf