81 results were found for 【K06.CC】Match 男性账户 年龄50-65岁 4f5it.

Results:

• 41. BIGR_windrose_2005-2014

  Wind rose BIGR 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: 10329 Calm: 1.7% Variable winds: 0.34% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S W /media/vedur/BIGR_windrose_2005-2014.pdf

• 42. Sea ice in April 2011

  was seen just within the jurisdiction of Greenland. No large floes were seen on radar beyond the ice edge. No observations were received from ships but 3rd April one observation was received from land, reporting an ice berg in location 65°42' N 32°07'W. On the Greenland Straight easterlies were predominant but occasionally strong southwesterly wind prevailed for a few days /sea-ice/monthly/2011/nr/2375

• 43. 2010_016

  The trend analysis of future climate eliminates the direct use of a past baseline period in the derivation of the scenarios and provides a consistent match with the recent climate development. The statistical matching of the past climate observations with the trend lines of the future climate, furthermore, provides an implicit bias correction. This is important near Iceland because the RCM /media/ces/2010_016.pdf

• 44. VI_2019_009

  a71 a71a71a71a71a71 a71 a71 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 0 1 2 3 4 5 6 7 8 9 10 12 13 14 15 16 17 18 20 22 23 24 25 26 28 30 35 40 45 50 55 60 65 70 75 Visibility (Manual) Visibility ( Automatic ) Proportion of records a71 a71 a71 a71 0.1 0.2 0.3 0.4 0.1 0.2 0.3 0.4 Proportion of records Figure 12. Automatic records as a function of manual observations. 20 Present weather /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 45. CES_D2.4_task1

  the shifts in the probability distributions, Fig. 1.1 divides December mean temperatures to four classes based on the distribution observed in 1961-1990: “very cold” (below the 10th percentile in 1961-1990), “cold” and “warm” (below and above the median), and “very warm” (above the 90th percentile). By definition, the probabilities of these classes in 1961-1990 were 10%, 50%, 50% and 10 /media/ces/CES_D2.4_task1.pdf

• 46. Isskyrsla_20100407

  Ísskýsla 7.apríl Flug 03410.025 Miðvikudaginn 7 apríl var farið í ískönnunarflug á TF-SIF úti fyrir vestfjörðum. Kl.1115 var komið að ísröndini sem lá til NA um eftirtalda staði: 1. N65°50'- W028°05' 2. N65°44' -W027°49 ' 3. N65°56'- W027°08' 4. N66°12' -W026°21' 5. N66°31'- W025°57' 6. N66°43'- W025°49' 7. N66°40'- W025°24' 8. N67°05'- W024°32' 9. N67°14' -W023°56' 10.N67°19'- W023°32' 11.N67°40 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 47. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 48. VI2010-006_web

  1971–2000 var 1367mm í Siglufirði og 885mm á Kálfsárkoti í Ólafsfirði. Innan Ólafsfjarðarmúla minnkar hún ört og var 509mm á Tjörn í Svarfaðardal, 518mm á Akureyri og 473mm á Torfufelli, framarlega í firðinum. Árs- meðalúrkoma á Akureyri 1961–1990 var 490mm. Á bilinu 65% til 75% úrkomu í Eyjafirði fell- ur í norðlægum vindáttum. Úrkomuákefðin á Akureyri er mest þegar norðaustanátt er ríkjandi. Sama /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 49. BIVM_windrose_2005-2014

  N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 114 8 128 7 84 9 36 1 26 0 13 9 24 3 65 4 136 4 250 3 366 4 298 8 189 6 146 9 99 9 160 6 111 5 83 5 86 1 86 4 80 0 82 6 92 4 96 3 97 5 124 9 109 5 127 7 122 4 115 3 88 0 61 9 52 3 55 3 96 0 109 9 Wind rose BIVM January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 /media/vedur/BIVM_windrose_2005-2014.pdf

• 50. Refsgaard_2-uncertainty

  -6 0 60 -6 5 65 -7 0 70 -7 5 75 -8 0 Nedbørsintensitet (mm/dag) A n ta l h æ n d el se r RCM Delta Change Direkte 0 10 20 30 40 50 30 -3 5 35 -4 0 40 -4 5 45 -5 0 50 -5 5 55 -6 0 60 -6 5 65 -7 0 70 -7 5 75 -8 0 A nt al h æ nd el se r Future climate Down scaling Bias correction Global 100-250 km Scale Regional 10-25 km Hydrological 50-500 m Present climate Climate change impacts on hydrology /media/loftslag/Refsgaard_2-uncertainty.pdf