23 results were found for IM体育 微信号BET99688 菲律宾直营官网范尤.

Results:

• 1. Climate and Modeling Scenarios

  Clausen, N.-E., Pryor, S. C., Guo Larsén, X., Hyvönen, R., Venäläinen, A., Suvilampi, E., Kjellström, E., Barthelmie, R. (2009). Are we facing increasing extreme winds in the future? EWEC 2009 Marseille session DT2A, 19 March 2009. Engen-Skaugen,T & Førland, E.J. (2010). Future change in return values and extreme precipitation at selected catchments in Norway, met.no Report 20/2010 (draft). Engen /ces/publications/nr/1680

• 2. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  The Rhine River Basin The Rhine basin (Fig. 3) covers an area of approximately 185,000 km2, distributed between nine countries. Two third of the basin is located in Germany, whereas the alpine countries of which Switzerland is the most important form 20% of the area (Buck et al. 1993). With its 1,320 km, of which 880 km is navigable, the Rhine is one of the longest rivers in Europe (Frijters /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 3. 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

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

  Av. Ed. Belin, 31400 Toulouse, France Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011 Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011 Abstract. The Little Ice Age maximum extent of glaciers in Iceland was reached about 1890 AD and most glaciers in the country have retreated during the 20th century. A model for the surface mass balance /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 5. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  e in relatio n to climat echang eadapt ation .X ,X X ,XX X is a ge n era lguid eo n th e relativ e imp ortanc e leve lo fth e sourc es , alth oug h it mus tb e em phasise d tha tth e imp ortanc e o fth e indi vidua lsou rce s o fun certaint y is co n tex tspe cifi c St ep si n cl im at e ch an ge ad ap tat io n an al ys es (ch ain in u n ce rta in ty ca sc ad e, Fi g. 2) So ur ce s o fu n ce rta /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 6. Statistical Analysis

  ISBN 978-9979-68-238-7. NHP Report No. 50, P. 638-645. Kriauciuniene J. & Kovalenkovienė M. (2008). Dependence of Lithuanian river runoff extremes on atchment area. XII Biennal International Conference. Hydrological extremes in small basins, 18-20 September, 2008, Cracow, Poland. ISBN-978-83-88424-38-0. P.183-186. Kriauciuniene, J., Kovalenkovienë, M., and Meilutytë-Barauskienë D. (2007). Changes /ces/publications/nr/1943

• 7. 2005EO260001

  im- proved by a double-difference location meth- od [Slunga et al., 1995], and supported by P - wave particle-motion analysis at GRF, reveal a northerly trending event distribution, centered at the southern caldera rim, ~1 km east of the main eruption site (Figure 1b). Focal depths mostly concentrate above 4 km and decrease by ~2 km near the eruption onset. The detection threshold /media/jar/myndsafn/2005EO260001.pdf

• 8. Hare-2011-ParticipatoryModelling

  ) Domai n expert s NO P NO P NO P HO M Proto typin g (co nceptua l m o de ls) NO P OT :Researcher s M KA M (conceptua l m od els ;s im u lat ion sub-model ) M/K A M 5Participatory Modelling in the Water Sector Copyright © 2011 John Wiley & Sons, Ltd and ERP Environment Env. Pol. Gov. (2011) DOI: 10.1002/eet 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 9. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  aversion should influence the first mover’s decision. The 98 Public Choice (2012) 151:91–119 Fi g. 1 O pt im al co n tr ib u tio n de pe nd in g o n α , r an d p Public Choice (2012) 151:91–119 99 Table 1 The predicted effect of intrinsic preferences on first and second movers’ contributions 1st mover 2nd mover Disadvantageous Negative None inequity aversion Advantageous None Positive inequity /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 10. IMO_AnnualReport2014

  kg/s. Plume compo- sition measurements were made by FTIR, MultiGAS and DOAS dur- ing multiple campaigns early in the eruption. IMO is collecting precipitation samples at ~20 meteorological observation sites. IMO performs the estimation of pH and amount of sulphates and other pollutants (HF, HCl) to identify potential are- as a?ected by acid rain. These samples are then analysed in cooper /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf