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

Results:

• 51. 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

• 52. 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

• 53. 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

• 54. Kok_JGEC658_2009

  to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf

• 55. The weather in Iceland 2010

  except in January and September. The annual total was only 74% of the mean. In Stykkishólmur the precipitation has been measured almost continuously since 1856 (a few months in 1919 are missing). 2010 was the fifth driest of the series; it was driest 1881, 1915, 1916 and 1998. The annual total was only 65% of the annual average. In the North and East the total precipitation in 2010 was slightly /about-imo/news/2011/nr/2112

• 56. The weather in Iceland 2010

  except in January and September. The annual total was only 74% of the mean. In Stykkishólmur the precipitation has been measured almost continuously since 1856 (a few months in 1919 are missing). 2010 was the fifth driest of the series; it was driest 1881, 1915, 1916 and 1998. The annual total was only 65% of the annual average. In the North and East the total precipitation in 2010 was slightly /about-imo/news/nr/2112

• 57. ved-eng-2010

  ; it was driest 1881, 1915, 1916 and 1998. The annual total was only 65% of the annual average. In the North and East the total precipitation in 2010 was slightly above the average (5 to 16%). January and June were almost completely dry in the northeast. Monthly precipitation anomalies 2010 in Reykjavík og Akureyri Monthly precipitation anomalies in Reykjavík (blue /media/vedurstofan/utgafa/skylduskil/ved-eng-2010.pdf

• 58. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  *** (0.637) (0.638) Contribution of the first mover −0.040** (0.020) No. observations 1180 1180 Prob > χ2 0.0000 0.0000 Wald χ2 48.51 52.26 Log Likelihood 439.69 437.63 same contribution as the first mover, was chosen to keep the design simple and to identify types. Only advantageous inequity aversion should affect second movers’ decisions. The number of times that second movers match the public good /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 59. VAT_newsletter_2018_06

  Sporðar/te rmini (% ) 0 20 40 60 80 10 0 1930 1940 1950 1960 1970 1980 1990 2000 2010 2020 Hopa/Retreat Ganga fram Advance Engin breyting Stationary Gögn/Data: Jörfi/Icel. Glaciol. Soc. 1900 1920 1940 1960 1980 2000 2020 6 7 8 9 10 11 Hiti/ Tempe rature (°C ) Rúmmál/ Volume (km³ ) 50 55 60 65 70 Sumarhiti/Summer temperature Stykkishólmur ... 10−ára/year meðaltal/average Rúmmál/Volume /media/Eplicanámskeið/VAT_newsletter_2018_06.pdf

• 60. Bardarbunga_kafli20140825

  eruption: The large explosive basaltic eruption in 1477 CE took place on a ~65 km long volcanic fissure on the southwestern part of the Veiðivötn fissure swarm where ground water level is high, and deposited about 10 km3 of tephra on land affecting 50% of the country (Figures 4 and 5b). Heavy proximal tephra fall clogged water ways and volcanic craters dammed river Tungnaá resulting /media/jar/Bardarbunga_kafli20140825.pdf