65 results were found for z 구미휴게텔㎰《dm080.com』✼구미주점□구미업소□구미타이✗구미안마.

Results:

• 21. raisanen_ruosteenoja_CES_D2.2

  that increases in atmospheric greenhouse gases will lead to substantial changes in the global climate during this century (IPCC 2007), estimates of the magnitude (and for some aspects of climate, the direction) 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 /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 22. 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

• 23. 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

• 24. Guidelines2-for-rapporteurs

  ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 25. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  o t o - a g e n d a D e f i n e a n d i n v i t e s t a k e h o l d e r s T e c h n i c a l i n p u t a n d v i s i o n s - I n t e r n a l e x p e r t s - s t a k e h o l d e r e x p e r t s F r am e p r o b l e m - t r p s e r v i c e ( q u a l i t y ) l e v e l s - t y p e s o f s c e n a r i o s A n a l y z e p r o b l e m T e c h n i c a l i n p u t f r /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 26. Paper-Olafur-Rognvaldsson_91

  Pálsson F., Rögnvaldsson Ó., Sigurðsson O., Snorrason Á., Sveinsson Ó. G. B., Thorsteinsson Th. 2007. Effect of climate change on hydrology and hydro-resources in Iceland. Rep. OS-2007/011, National Energy Authority, Reykjavík. Liang, X.-Z., Li L. and Kunke K. E. 2004 Regional climate model simulation of U.S. precipitation during 1982–2002. Part I: Annual cycle. J. Climate, 17, 3510–3529. Pálsson, F /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 27. CES_D2.4_VMGO

  L. Michaelis, S. Mori, T. Morita, W.Pepper, H. Pitcher, L. Price, K. Raihi, A. Roehrl, H.-H. Rogner, A. Sankovski, M.Schlesinger, P.Shukla, S. Smith, R. Swart, S. van Rooijen, N. Victor, Z. Dadi, 2000: IPCC Special Report on Emission Scenarios. Cambridge University Press, United Kingdom and New York, NY, USA. a) b) c) Fig.1 Change of annual extreme temperature range /media/ces/CES_D2.4_VMGO.pdf

• 28. 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

• 29. 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

• 30. 2010_005_

  which are significantly lower com- pared with similar beginning and end years. Consequently, for the 2004–50 period, the average RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are somewhat larger than for the reduced IPCC ensemble mean. Additionally, the tabulated values of SAT differences between the 1961–90 control period and either the 2021–50 /media/ces/2010_005_.pdf