49 results were found for z 토토디비업자㎨〔ㅌ그sEin07】 토토DB업체е토토DB판매사이트←토토디비판매❁토토DB업자.

Results:

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

  /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 32. 2011_005

  in the CGPS network. Receiver model Number of receivers Trimble 4000 2 Trimble 4700 5 Trimble 5700 / R7 4 Trimble NetRS 39 Septentrio PolaRX2e 10 Ashtech Z-12 CGRS 2 Ashtech μZ-12/Martec Mira-Z 1 2.4 Communication Remote communication with stations is mainly IP-based but some stations still rely on dial- up modems. The dial-up modem technology is slowly being phased out /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

  snow depth and winter precipitation. Darker (lighter) colors indicate negative (positive) correlations. Engeset, R.V., Tveito, O.E., Alfnes, E., Mengistu, Z., Udnæs, H.C., Isaksen, K. and Førland, E.J., 2004: Snow map system for Norway. Proceedings XXIII Nordic Hydrological Conference 2004, 8-12 August 2004, Tallinn, Estonia Hanssen-Bauer, I., Drange, H., Førland, E.J., Roald, L.A /media/ces/ces-oslo2010_proceedings.pdf

• 35. 2010_016

  /media/ces/2010_016.pdf

• 36. VI_2015_007

  catchment altitude (Z) Catchment perimeter (L) Ratio between actual catchment area and area of circular catchment of perimeter L Percentage of glaciated area (G) Mean annual precipitation (1961-2006) (P) Mean annual maximum snowpack (1961-2006) (SWEm) Mean annual maximum daily input water supply (1961-2006) (WSm) Normalized mean monthly input water supply (1961-2006) (NWS( j); j = 1; ::;12 /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

  ca ti o n s fo r th e la rg est e a rt h q u a ke s w it h in t h e S IS Z b et w ee n 1 7 0 6 a n d 2 0 0 8 d en o te d b y w h ite fil le d c ir cles. E stim a te d f a u lt p la n es o f h is to ric a l ea rt h q u a ke s a re s h o w n a s w h ite , th ick li n es ( fr o m R o th , 2 0 0 4 ). F a u lt p la n es f ro m 1 9 9 8 ( V o g fj ö rd et a l. , 2 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 39. 2010_005_

  /media/ces/2010_005_.pdf

• 40. VI_2015_005

  /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf