83 results were found for d 구리건마а〔optop5.com｝✈구리휴게텔 구리휴게텔 구리립카페 구리안마.

Results:

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

  –averaged modeled ice velocity corresponding to the simulated 2002 ice sur- face geometry, using A= 6.8× 10−15 s−1 kPa−3 implicitly includ- ing the basal sliding (in B), and using A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3 (in (C)). (D) The contribution of the modeled basal sliding to the velocity shown in (C). Table 2. Average annual (September 2002 to September 2003; accuracy ∼2 m a−1 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 32. Lawrence_Deborah_CES_2010

  
  
                                !  !   0 20 40 60 80 100 120 140 jan feb mar apr mai jun jul aug sep okt nov des m m / m å n e d 55550 Hafslo 60 80 100 120 140 jan feb ar apr ai j j l t m m / m å n e d 55550 Hafslo 54130 Lærdal Ensemble approach for probabilistic hydrological projections Catchment /media/ces/Lawrence_Deborah_CES_2010.pdf

• 33. 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

• 34. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf

• 35. 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

• 36. ces_risk_flyer

  and distribution network are all identified a section at a time. In some cases, however, it might be more valuable to focus only on a certain part of functional model. Fig.1. Functional Model. The results of the risk analysis are represented visually in a fourfold table. (Fig.2) The main idea of the table is to provide a readily interpretable overview of h hi hli h d i k d i i i l i Having already been /media/ces/ces_risk_flyer.pdf

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

  inty in decision making linking pluriform uncertainty combining certified and tacit knowledge Tommy Chan Mich el Laiho Patrick Driscoll Kare Lundgren Hector Guin a Barrientos Eivind Junker Jussi Ylhäisi Athanasios Votsis Karoliina Pilli-Sihvola Yuang Zheng Väi ö Nurmi Jiao Xi nj Wejs a p p l i c a n t n o . a b s t r a c t n o . n a m e c o u n t r y d i s c i p l i n e ( M S c . ) 1 3 /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 38. Hydropower, Hydrology

  Hydrological Sciences Journal, 53, 100-111. Kriauciuniené, J., Meilutyté-Barauskiené, D., Rimkus, E., Kays, J., Vincevicius, A. (2008). Climate change impact on hydrological processes in Lithuanian Nemunas river basin. Baltica, Vol. 21 (1-2), pp. 1-61. Vilnius. ISSN 3067-3064. Lawrence, D., Haddeland, I. (2010). Uncertainty in hydrological modelling of climate change impacts in four Norwegian /ces/publications/nr/1938

• 39. TietavainenHanna_CES_2010

  versa • Very large range within the simulations • Larger number of observation stations in the study area leads to • better compatibility between different observational data sets • smaller bias in the model simulations CES Conference, Oslo 31.5.-2.6.2010 References • Haylock, M. R., Hofstra, N., Klein Tank, A. M. G., Klok, E. J., Jones, P. D. and New, M. 2008. A European daily high-resolution /media/ces/TietavainenHanna_CES_2010.pdf

• 40. Case_B___Road_transport_operation_and_infrastructure_planning

  on the Shifts of climatic zones from cooler or wetter to warmer or drier (a) 1971-2000 (b) 2010-39 A1B observational data set (0.25º grid) from Haylock et al. (2008) (b-d) Based on CMIP3 GCM runs for A1B & the delta-change method (c) 2040-69 A1B (d) 2070-99 A1B Jylhä et al. (2010) Uncertainties in climate change schematically Observed climate Future climate Natural /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf