49 results were found for Z 리플거래「wwwͺbybͺpw」 리플매매 리플투자ิ리플리딩㊌케이엘넷 kCi.

Results:

• 21. CES_D2.4_VMGO

  deviation across the ensemble) and sign agreement (a percentage of models in the ensemble that project the same sign of changes as the entire ensemble does). Analysis In Fig.1a shown are simulated changes in the annual extreme temperature range calculated as difference between 20 yr mean absolute annual maxima and minima temperatures in baseline and future scenario periods. The range /media/ces/CES_D2.4_VMGO.pdf

• 22. 2013_001_Nawri_et_al

  the Fljótsdalsheiði region . . . . . . . 47 18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48 19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49 20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50 21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51 22 Seasonal mean /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 23. Refsgaard_etal-2007-Uncertainty-EMS

  BIOMATH, Ghent University, Gent, Belgium d Water Quality Modelling modelEAU, University Laval, Quebec, Canada Received 20 December 2005; received in revised form 5 February 2007; accepted 7 February 2007 Available online 27 April 2007 Abstract A terminology and typology of uncertainty is presented together with a framework for the modelling process, its interaction with the broader water /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 24. vonKorff_etal-2010

  ” The latter is in our case a policy decision represented by point z in Fig. 1. In European water management, typical policy decisions that involve participation include water management plans. Leading up to the policy decision is the participation process, represented by the space between points y and z, in which stakeholders interact with each other but also with the agency responsible /media/loftslag/vonKorff_etal-2010.pdf

• 25. ces-glacier-scaling-memo2009-01

  ) is considered as a sequence of steps corresponding to n individual glaciers of different sizes (with volumes vi and areas si for i = 1 to n), or using V (v) = Z v 0 1 g dS ds dx ; (7) where the slope of the area distribution function, dS=ds, is considered as a function of ice vol- TóJ 5 5.12.2009 Memo 0 50 100 150 200 0 5 10 15 20 25 Cumulative area (km2) Area (km 2 ) 0 5 10 15 0. 0 0. 5 1. 0 1. 5 2. 0 2. 5 /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 26. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  on the European level [e.g. Water Framework Directive (Directive 2000/60/EC), Common Agricultural Policy, etcetera], except for the Ukrainian part of the Tisza. However, the Ukraine shows strong incentives to enter the EU community and thus the EU acquis communautaire is used as key reference for the development of its water management principles. It was nevertheless decided to select two case-studies /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 27. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  ) of the forthcoming changes are uncertain. This uncertainty comes from three basic sources: z Scenario uncertainty: future changes in the atmospheric composition, and thus the external forcing of the climate system, depend on the magnitude of future anthropogenic emissions of greenhouse gases and other radiatively active substances such as aerosol particles and their precursor gases. z Modelling /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

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

  & 4 Y u a n g Z h e n g D e n m a r k F o r e s t r y & L a n d s c a p e 2 1 0 A t h a n a s i o s V o t s i s F i n l a n d U r b a n & r e g i o n a l p l a n n i n g 3 3 2 E i v i n d J u n k e r N o r w a y L a w 4 3 3 M i c h a e l L a i h o F i n l a n d E u r o p e a n s t u d i e s 5 2 0 H e c to r G u i n e a B a r r i e n to s S w e d e n N a t u r a l r e s o u /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 29. Paper-Olafur-Rognvaldsson_92

  Numerical simulations of precipitation in the complex terrain of Iceland—Comparison with glaciolog- ical and hydrological data. Meteorol. Z., 16(1), 71–85. Rögnvaldsson, Ó. and Ólafsson H. 2008. Dynamical downscaling of precipi- tation – Part I: Comparison with glaciological data. Proceedings of the XXV Nordic Hydrological Conference, Reykjavík, Iceland. Tómasson, H. 1982. Vattenkraft i Island och dess /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 30. 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