83 results were found for 【K528.COM】Match 男性账户 年龄50-65岁 2zd5x.

Results:

• 41. Observations - Vatnsskarðshólar

  / 7Sunny (3/8)Visibility 65 kmSea surf.: slight 08 GMT 4.1° ENE 4 Max wind : 4 / 5 07 GMT 2.9° NNE 2 Max wind : 2 / 2 06 GMT -0.7° SE 1 Max wind : 6 / 7Sunny (3/8)Visibility 65 kmSea surf.: moderate 05 GMT 0.4° NNE 3 Max wind : 5 / 6 04 GMT 1.0° NE 5 Max wind : 6 / 7 03 GMT 0.8° NE 6 Max wind : 6 / 7 02 GMT 1.1° NE 3 Max /m/observations/areas

• 42. 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

• 43. VI_2015_009

  vhm145 Vestari-Jökulsá D+J+L 844 751 11.3 924 1971–2014 vhm167 Austari-Jökulsá D+J 553 916 28.8 1208 1985–2014 8 vhm59 vhm64 vhm66 vhm102 vhm116 vhm162 vhm233 vhm235 vhm238 vhm144 vhm145 vhm167 Figure 1. Location of river basins. 9 l l l l l l l l l l l l l l l l l l ll l l l l l l l l l l l l l ll l l l l l 0 100 200 300 50 15 0 25 0 35 0 Days since Sept. 1st Q (m ³/s ) vhm59 S O N D J F M A M J /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 44. 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

• 45. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  ). NeWater is based on the hypothesis that IWRM cannot be realised unless current management regimes undergo a transition towards more 0301-4797/$ - see front matter r 2007 Elsevier Ltd. All rights reserved. doi:10.1016/j.jenvman.2007.05.009 Corresponding author. Tel.: +45 38 14 27 71; fax: +45 38 14 20 50. E-mail address: hjh@geus.dk (H.J. Henriksen). (Downing et al., 2005). Vulnerability /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 46. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  /lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13 April 2009. [2] WTO, World Tourism Organization (2008): “Climate Change and Tourism - Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain. Available at: http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7 March 2010. [3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for sustainable /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

• 47. 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

• 48. 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

• 49. 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

• 50. 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