68 results were found for S 베네치아 FC CDDC7.COM [프로모션번호 B77]평택 프로토 구매㈄마카오바카라미니멈ở1xbet 이스포츠ヷ카라바흐 FKコ베네치아 FC선정 chocolate/.


  • 11. IMO_AnnualReport2014

    computing. As a part of this development, IMO and the Danish Meteorological Institute, DMI, have signed a co-operation agree- ment on research and the operation of the next supercomputer of DMI in IMO´s premises. The partners are going to work together on climate studies, Arctic studies, development and operation of the Harmonie model and other topics of mutual interest. The benefit to IMO /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
  • 12. Guidelines2-for-rapporteurs

    Perrels)  For each session report: o start with a heading indicating session number and title o for each presentation: name of presenter(s) and title o start for each presentation summary on a new page  Try to summarize briefly the main lines of argument as well as the project results and conclusions. This can be just like a not too long bullet list. When relevant, you can notify links /media/loftslag/Guidelines2-for-rapporteurs.pdf
  • 13. VI_2015_009

    presents the study area and data. Sec- tion 3 describes the methodology. Section 4 presents the results and Section 5 concludes the report. 2 Study area and data 2.1 River basins Rivers in Iceland are often classified according to the origin of flow (Rist, 1990): direct runoff (D), spring-fed (L), glacier-fed (J) and whether they flow through lakes (S). Twelve river basins were selected for this study /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 14. Hare-2011-ParticipatoryModelling

    support ) Improv e mode l (integration) ; socia llea rnin g Farmers ,loca l aut horities , association s NO P IN D Cognitiv e mappin g HE T GM B NO P HE T Simulation - by-han d OT :Researcher s KA F F Iska r (Phas e1 ) Co n ce pt u al m o de l (D is cu ss io n su pp o rt ; Com m unication ) Improv e mode l (integration) ; socia llea rnin g Nationa l poli cy-maker s NO P IN D Cognitiv e mappin g HE /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
  • 15. VI_2009_006_tt

    the discharge in Skaftá and the temperature of the flood water close to the glacier margin were measured. The dis- charge from the subglacial lake during the jökulhlaup was calculated using a hypso- metric curve for the subglacial lake, estimated from the form of the surface cauldron after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti- mated as 123 m3 s 1 while /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 16. IPPC-2007-ar4_syr

    (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 17. Group5-Stakeholders_involvement

    /EPP 2 Stakeholders analysis 26 August 2011 PM/YZ/EPP 3 Stake h o l d e r s P u b l i c / p r i v at e P o w e r l e v e l (“ n u i s an ce” ca p a c i t y ) O r i e n tat i o n H or s t e n s m uni c ipal i t y ( c o m pe t e n t a u t h ori t y ) P u b l i c S t ron g Go v ernanc e N eighbour mun i c i p ali t y P u b l i c S t ron g Go v ernanc e Poli c y /media/loftslag/Group5-Stakeholders_involvement.pdf
  • 18. Adalgeirsdottir-etal-tc-5-961-2011

    were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
  • 19. Refsgaard_etal-2007-Uncertainty-EMS

    outcomes and/or probabilities of these outcomes is the central focus. Thus according to our definition a person is un- certain if s/he lacks confidence about the specific outcomes of an event. Reasons for this lack of confidence might include a judgement of the information as incomplete, blurred, inaccu- rate, unreliable, inconclusive, or potentially false. Similarly, a person is certain if s/he /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 20. Journal_of_Hydrology_Veijalainen_etal

    24 July 2010 This manuscript was handled by K. Georgakakos, Editor-in-Chief, with the assistance of Ercan Kahya, Associate Editor Keywords: Climate change Flood Hydrological modelling Flood inundation area Hydraulic modelling Finland s u m m a r y This paper provides a general overview of changes in flooding caused by climate change in Finland for the periods 2010–2039 and 2070–2099. Changes /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

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