84 results were found for X 홈타이{ㄲr톡 gttg5}新원미구아로마출장烆원미구아로마테라피訮원미구아줌마출장骶원미구알바녀출장📞evasively/.

Results:

• 51. Paper-Olafur-Rognvaldsson_91

  The role of orography was found to be crucial in determining the precipitation dis- tribution and amount. Atmospheric flow over Iceland was simulated for the period January 1961 through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale model (Grell et al., 1995). The domain used is 123× 95 points, centered at 64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 52. Kok_2-scenarios-lecture-2

  research VIII. Resources: extensive vs limited IX. Institutional conditions: open vs constrained C Scenario content - complex vs simple: X. Temporal nature: chain vs snapshot XI. Variables: heterogeneous vs homogenous XII. Dynamics: peripheral vs trend XIII. Level of deviation: alternative vs conventional XIV. Level of integration: high vs low Scenarios - types EXAMPLE 1 – EXPLORATORY SCENARIOS /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 53. 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

• 54. VI_2014_001

  6 0 20 40 60 80 10 0 12 0 14 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm51 heM 95?bh ??Obs 95?bh ??W aSiM 95?bh heM Annual max. Q : GEV Distributions for vhm51 Index flood model no. 6 l l l l l l l l l l l l l l l l l l −2 0 2 4 6 0 50 10 0 15 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm52 heM 95?bh Obs 95?bh /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 55. 2010_003rs

  and May. ............................................................................... 94 Figure B.8. Rake distribution for mapped faults/clusters in box H, Hengill, active between June and December. .......................................................................... 95 Figure B.9. Rake distribution for mapped faults/clusters in box I, Flói. ............................. 96 Figure B /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 56. VI_2009_013

  Volcanol. 68: 377–393. Doi:10.1007/s00445-005-0020-y. Rögnvaldsson, S. Th. and R. Slunga (1993). Routine fault plane solutions for local networks: a test with synthetic data. Bull. Seism. Soc. Am., 83, 4, 1232–1247. Rögnvaldsson, S. Th. and R. Slunga (1994). Single and joint fault plane solutions for microearthquakes in South Iceland. Tectonophysics, 237, 73–86. Scholz, C. H. (1988 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 57. ces_geus_paakitsoq_full_report

  conditions as a lower boundary condition from the driving GCM. The RCAO model-output is from a pan-arctic run for the years 1960–2080 at approx. 50 km resolution. The first 20 years of the model run must be considered as spin-up time for the ocean module. The RCAO run is experimental since the model is in a development state and the output has not yet been evaluated over Greenland (Ralf Döscher, personal /media/ces/ces_geus_paakitsoq_full_report.pdf

• 58. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 59. Case_A___Horsens_Fjord

  is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/Case_A___Horsens_Fjord.pdf

• 60. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  %) 14 (26%) 39 (74%) Gender Number (%) E I S N T F P J Male 100 (48%) 47 (47%) 53 (53%) 15 (15%) 85 (85%) 59 (59%) 41 (41%) 29 (29%) 71 (71%) Female 109 (52%) 66 (61%) 43 (39%) 22 (20%) 87 (80%) 43 (39%) 66 (61%) 21 (19%) 88 (81%) Climatic Change (2012) 112:233–242 237 symposia participants were not significantly different from the preferences of the U.S. general population, which was 49 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf