65 results were found for S 외국19방송 CDDC7.COM ◆보너스번호 b77◆스페치아 칼치오Ւ마포 리딩방Ử사누키☋양천 프로토 베팅ê외국19방송선정 anthropogeny/.

Results:

• 11. VI_2009_006_tt

  the maximum discharge of jökulhlaup water at the glacier terminus is estimated as 97 m3 s 1. This jökulhlaup was a fast-rising jökulhlaup as other jökulhlaups in Skaftá and cannot be described by the traditional Nye-theory of jökulhlaups. The total volume of flood water was estimated as 53 Gl. The average propagation speed of the subglacial jökulhlaup flood front was found to be in the range 0.2–0.4 m s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 12. IPPC-2007-ar4_syr

  of significant changes consistent with warming Percentage of significant changes consistent with warming 89%94%100% 100% 100% 100% 100% 100% 99%100%98% 96% 91% 94% 94% 90%90%92%94% 355 455 53 119 NAM LA EUR AFR AS ANZ PR* TER MFW** GLO 5 2 106 8 6 1 85 7650 120 24 7645 28,115 28,586 28,671 Changes in physical and biological systems and surface temperature 1970-2004 33 Topic 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf

• 13. Group5-Stakeholders_involvement

  Knowledge gathering Proposal Testing Revision Decision- making Milestones 26 August 2011 PM/YZ/EPP 5 Phase s Du r at i o n ( mon t h s ) O V I s Problem iden t i f i ca t i on 2 A l l St a k ehol d e r s i d ent i f i ed an d selected wi t h i n 2 mo n t h s I n f o r ma t i on pro v i s i on 2 Kic k - of f m e et i n g hel d Knowled g e ga t he r i n g 6 /media/loftslag/Group5-Stakeholders_involvement.pdf

• 14. Adalgeirsdottir-etal-tc-5-961-2011

  at Hólar in Hornafjörður and precipitation at Fagurhólsmýri as an input. With a temperature gradient of 0.56 ◦C per 100 m and the degree-day factors ddfs = 4.45 mm◦w.e.C−1 d−1 and ddfi = 5.30 mm◦w.e.C−1 d−1, the model explains 92 % and 95 % of the variance of the winter and summer balance at S- Vatnajökull, respectively (Jóhannesson et al., 2007). Another model calibration of the degree-day factors /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 15. Refsgaard_etal-2007-Uncertainty-EMS

  Discrete numerical Categorical Narrative Constant in space and time A1 A2 A3 4Varies in time, not in space B1 B2 B3 Varies in space, not in time C1 C2 C3 It is noticed that the matrix is in reality three-dimensional (source, type, nature). Thus, the categories type and nature are not mutually exclusive, and it may be argued that the ma- trix should be modified in such a way that the two uncer /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 16. Journal_of_Hydrology_Veijalainen_etal

  ; fax: +358 20 490 2590. E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen). Journal of Hydrology 391 (2010) 333–350 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier .com/ locate / jhydrol Author's personal copy narios from GCMs or RCMs, and with different emission scenarios (e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 17. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 18. 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

• 19. 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

• 20. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  and to list categories of stakeholders such as water users, potential groundwater pollution sources, and autho- rities in the area including: local waterworks; water consumers; farmers; industry; anglers; the local county; and three municipalities. The stakeholder involvement process and the extension of the organisation with new Define context Collect dat a Define states Identify factors, ac tion s /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf