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

Results:

• 31. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  at e (C limat e models ) GC M s X X XX X X X X RCM s X X XX X X X X Initia lco n ditions / nat ura lva riabilit y X X XX X D ow ns ca lin g/ sta tis tic al co rr ec tio n X X X X X X X X X W ate r syst em impact s (H yd ro -e co lo gi ca lm o de ls) X X X X X XX X X X X X X X X X Socio -econo m ic imp act s (So ci o- ec on om ic to ol s) X X X X X X X X X XX X X X A da pt ati on m ea su re s X X X X /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 32. 2011_005

  ....................................................................................................19 5.1.2 Shared servers ...............................................................................................19 5.2 Automated download of receiver files .....................................................................20 5.3 Processes ..................................................................................................................20 5.3.1 Data retrieval /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 33. Journal_of_Hydrology_Veijalainen_etal

  the Finnish Environment Institute, Regional Environment Centres and the Department of Geography, University of Turku. The input data sets, from which the final grids were created, consisted of photogrammetric TIN (Triangulated Irregular Network) models in Lapua (with point density of c. 20 m and ±30 cm z accuracy) and Kittilä (with point density of 10–40 m and ±20 cm z accuracy), 10 m national Digital /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 34. ces-oslo2010_proceedings

  ................................................................................................................................... 88 Melvold, K. and Laumann, T. A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate scenarios (CES) ..................................................................................................................................................... 90 Thorsteinsson, Th., Sigurðsson, O. and Einarsson, B. Monitoring changes /media/ces/ces-oslo2010_proceedings.pdf

• 35. 2010_016

  ............................................................................................................... 19 Table 4. Predicted quantitative changes from 1961–1990 to 2021–2050. ......................... 20 7 1 Abstract In order to investigate the effect of climate change on the hydrological regime in Iceland, future projections of river discharge were made for two watersheds with the WaSiM /media/ces/2010_016.pdf

• 36. VI_2015_007

  ] m ³/s l l l l l l l l l l l l l l l l l l l l l l E[Q(D=0)] vhm148 l l REF IFM−ROI IFM−CLU l IFM−WaSiM l l l l l l l l l l l l 2 4 6 8 10 12 20 0 40 0 60 0 80 0 IFM no. E[ Q] m ³/s l l l l l l l l l l l l l l l l l l l l l l l E[Q(D=0)] vhm149 l l REF IFM−ROI IFM−CLU l IFM−WaSiM l l l l l l l l l l l l 2 4 6 8 10 12 20 0 40 0 60 0 80 0 IFM no. E[ Q] m ³/s l l l l l l l l l l l l l l l l l l l l /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 37. VI_2014_006

  properly even if the sample size is increased and systematic biases may be expected. 2.2.3 Predictors Mean sea level pressure (MSLP), geopotential height (Z), specific humidity (q) and tempera- ture (T) at different pressure levels are considered in this study to describe the meteorological situations at the synoptic scale and to identify weather analogues. The MSLP and geopotential height (Z) describe /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 38. 2010_003rs

  10. Rake distribution for mapped faults/clusters in box J, Hella. ........................ 97 Figure B.11. Rake distribution for mapped faults/clusters in box K, Hraungerði. ............. 97 Figure B.12. Rake distribution for mapped faults/clusters in box L, Skeið. ........................ 98 Figure B.13. Rake distribution for mapped faults/clusters in box M, Land. ....................... 98 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 39. 2010_005_

  respec- tively. Due to limited data availability, for the SMHI-RCAO run, the 20th Century control period is restricted to the 20-year period 1971–90, and the second 21st Century reference period is limited to the years of 2070–80. For the MetNo-HIRHAM runs, no data are available during the second 21st Century reference period. 3 Spatial Variability of Climate Trends This section discusses /media/ces/2010_005_.pdf

• 40. VI_2015_005

  depression .. 18 9 Relative seasonal occurrence of mean sea level pressure modes........................ 20 10 Composite mean temporal tendencies of mean sea level pressure...................... 22 11 Composite mean 500 hPa geopotential height anomalies ................................ 25 12 Composite mean surface wind speed anomalies ............................................ 27 13 Composite /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf