60 results were found for 【K528.COM】82接码平台 fwroq.

Results:

• 31. BIIS_windrose_2005-2014

  50 Frequency of wind direction (%) Aerodrome Total observations: 82 Calm: 0% Variable winds: 0% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 10 20 30 40 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 3 13 41 12 1 1 6 1 2 2 BIIS gusts exceeding 70 knots (2005−2014) 90 80 70 60 /media/vedur/BIIS_windrose_2005-2014.pdf

• 32. BITN_windrose_2005-2014

  Wind direction (°) Wind speed (knots ) 0 5 10 15 20 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 25 20 34 20 20 18 23 16 24 12 1 5 17 9 24 19 14 9 18 3 1 58 82 5 2 43 30 25 5 12 7 4 18 15 19 11 23 13 28 BITN gusts exceeding 40 knots (2005−2014) 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BITN_windrose_2005-2014.pdf

• 33. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 34. VI_2014_005

  in an overall cold bias, compared with station measurements. To test, whether this is due to the HARMONIE model core or the external surface scheme, biases of 2-m temperature from SURFEX are com- pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is found that the negative temperature biases are due to shallow inversion layers near the ground, which are introduced /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 35. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 36. Journal_of_Hydrology_Veijalainen_etal

  ; fax: +358 20 490 2590. E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen). Journal of Hydrology 391 (2010) 333–350 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier .com/ locate / jhydrol Author's personal copy narios from GCMs or RCMs, and with different emission scenarios (e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 37. Bardarbunga_kafli20140825

  basaltic eruptions. Dominant type for the ice covered part of the volcanic system (Figure 2). The number of verified eruptions in the last 1000 years is 22. However, only one eruption out of every four left a tephra layer in the soils outside the Vatnajökull ice. During the preceding 6600 years at least 82 tephra layers were deposited in the soils outside Vatnajökull which could indicate that up /media/jar/Bardarbunga_kafli20140825.pdf

• 38. 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

• 39. VI2010-006_web

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 27 5.2 Hamrar . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 28 5.3 Fjaran, Aðalstræti 34–82 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 30 5.4 Brekka sunnan Búðargils, Aðalstræti 10–32 . . . . . . . . . . . . . . . . . . . 31 5.5 Búðargil . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 33 /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 40. Adalgeirsdottir-etal-tc-5-961-2011

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf