51 results were found for 【┋添加扣46⒋1⒍85〓】杏彩登录3.

Results:

• 31. 2010_012rs

  ), 3) samband milli skjálftaáhrifa og mesta hraða og hröðunar, 4) þróun sjálfvirkra, rauntíma „alert“ korta og hristingskorta (ShakeMap) fyrir jarðskjálfta, 5) undirbúning rauntímakortlagningar á eftirskjálftavá, og 6) rauntímakortlagningu spennuútlausnaskjálfta. Upplýsingar um SAFER verkefnið má finna á vefsíðunni: http:// www.saferproject.net/. 7 1. Development /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 32. BIHN_windrose_2005-2014

  Wind rose BIHN 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 Frequency of wind direction (%) Aerodrome Total observations: 28301 Calm: 5.3% Variable winds: 1.6% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIHN_windrose_2005-2014.pdf

• 33. Lettenmaier_Dennis_CES_2010pdf

  25 30 35 40 1950 1960 1970 1980 1990 2000 B C M Current Use + Reservoir Evap: 18.0 BCM Simulated Historical: 19.7 BCM Control: 17.8 BCM Periods 1-3: 16.0 - 16.9 BCM Storage Reservoirs Run of River Reservoirs CRRM • Basin storage aggregated into 4 storage reservoirs – Lake Powell and Lake Mead have 85% of basin storage • Reservoir evaporation = f(reservoir surface area, mean /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 34. VI_2013_008

  ) 555 535 391 753 664 480 % Glacierized area 0 0 0 11 20 12 % Grassland <1 43 25 15 10 25 % Woodland <1 0 0 0 2 2 % Moss 59 25 0 9 14 13 % Little or no vegetation 35 27 30 63 47 36 % Wetland 0 5 46 <1 6 7 % Lakes 6 <1 <1 <1 <1 3 10 3 Data Various meteorological and hydrological parameters were extracted and used to select ana- logues. 3.1 Hydrological data A set of six river basins of various /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 35. BIVO_windrose_2005-2014

  S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 26 8 27 9 44 9 36 0 111 1 173 2 39 3 24 9 20 7 9 0 2 9 4 7 1 0 1 4 3 3 1 6 2 6 3 5 6 8 10 1 27 3 39 0 86 7 209 6 71 4 25 7 21 5 8 2 5 4 9 4 2 9 7 7 11 8 7 1 16 0 21 5 Wind rose BIVO January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIVO_windrose_2005-2014.pdf

• 36. 2010_003rs

  place in the same area on 5 December in 1968 (Tryggvason, 1973; Erlendsson and Einarsson, 1996; Halldórsson, 2004). A quite large event also occurred on the RP on 10 June 1933. Its best known location is near to Fagradalsfjall, at 63.9°N and 22.2°W, and it was probably of magnitude M 5.5 (Tryggvason, 1973; Halldórsson, 2004). 8 F ig ure 1 .3 . A m a p s h o w in g e p ice n tr e lo /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 37. BIBD_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 36 2 69 4 138 2 187 3 151 2 106 7 83 1 58 1 36 0 20 3 17 6 14 5 14 9 11 0 10 6 13 0 16 7 29 8 55 2 73 0 95 6 140 7 98 9 41 9 20 2 17 7 8 1 6 4 4 8 3 7 5 7 4 4 4 5 7 3 9 2 18 5 Wind rose BIBD January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIBD_windrose_2005-2014.pdf

• 38. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  AVAILABLE FROM: http://www.atm.helsinki.fi/~jaraisan/CES_D2.3/CES_D2.3.html 2 Table of Contents Abstract 1 1. Introduction 2 2. Model simulations 4 3. Methods used for deriving probabilistic climate change forecasts 7 3.1 Resampling and variance correction 9 3.2 Relationship between local and large-scale climate changes in ENSEMBLES simulations 10 3.3 Comparison of large-scale /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 39. Forecasts - Öxnadalsheiði

  GMT -3° SSW 3 Cloud cover: 10% 05 GMT -3° SSW 4 Cloud cover: 10% 06 GMT -3° SSW 4 Cloud cover: 10% 07 GMT -2° SSW 4 Cloud cover: 20% 08 GMT -1° SW 3 Cloud cover: 10% 09 GMT -1° WSW 2 Cloud cover: 40% 10 GMT -0° WSW 3 Cloud cover: 90% 11 GMT 0° WSW 3 Cloud cover: 80% 12 GMT 1° WSW 3 Cloud cover: 70% 13 GMT 2° W 3 /m/forecasts/areas

• 40. Lorenzoni_Pidgeon_2006

  findings from various surveys and studies, which highlight both the distinctiveness and some shared perspectives at a generalised level. We reflect upon these in relation to trust and responsibility for climate change action, and risk communication, supporting the call for discourses about climate change to also be situated in people’s locality, as a means of increasing its saliency. 1 /media/loftslag/Lorenzoni_Pidgeon_2006.pdf