87 results were found for 【K528.COM】他趣34级账号出售 4dn8u.

Results:

• 51. 2005EO260001

  level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf

• 52. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 53. BIIS_windrose_2005-2014

  (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 28 6 85 3 223 1 339 5 367 0 315 2 161 9 89 4 34 6 11 7 18 7 9 7 7 7 15 9 8 7 7 2 14 9 7 4 22 6 36 9 69 6 148 3 183 1 148 5 96 9 45 1 21 1 9 3 7 8 2 0 1 7 2 4 1 2 1 6 7 3 11 6 Wind rose BIIS January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 /media/vedur/BIIS_windrose_2005-2014.pdf

• 54. Isskyrsla_20100407

  °26.45' 34. N66°09.51' W026°22.56' 35. N66°10.97' W026°20.13' 36. N66°11.59' W026°21.31' 37. N66°11.28' W026°31.58' 38. N66°13.34' W026°30.39' 39. N66°14.20' W026°16.63' 40. N66°15.00' W026°17.15' 41. N66°14.81' W026°21.09' 42. N66°16.86' W026°18.18' 43. N66°17.81' W026°09.01' 44. N66°19.07' W026°05.19' 45. N66°26.18' W025°59.21' 46. N66°24.31' W025°51.96' 47. N66°25.30' W025°50.48' 48. N66°25.83 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 55. Bárðarbunga 2014 - October events

  4 occurred at the caldera, an M4.6 at 17:34 yesterday and an M4.3 at 05:48 this morning, as well as a few over 3 in size. A dozen earthquakes were detected in the dike, all small. 26 October 2014 12:00 - from geoscientist on duty Approximately 80 earthquakes have been detected around the Bárðarbunga caldera. The strongest events were M5.3 today at 05:48 on the southeastern caldera rim and M4.7 /earthquakes-and-volcanism/articles/nr/3011

• 56. Bardarbunga-2014_October-events

  hours. The largest occurred at 01:05 this morning, M5.3 at the southwestern rim. Two quakes over 4 occurred at the caldera, an M4.6 at 17:34 yesterday and an M4.3 at 05:48 this morning, as well as a few over 3 in size. A dozen earthquakes were detected in the dike, all small. 26 October 2014 12:00 - from geoscientist on duty Approximately 80 earthquakes have been detected around the Bárðarbunga /media/jar/Bardarbunga-2014_October-events.pdf

• 57. Bárðarbunga 2014 - October events

  4 occurred at the caldera, an M4.6 at 17:34 yesterday and an M4.3 at 05:48 this morning, as well as a few over 3 in size. A dozen earthquakes were detected in the dike, all small. 26 October 2014 12:00 - from geoscientist on duty Approximately 80 earthquakes have been detected around the Bárðarbunga caldera. The strongest events were M5.3 today at 05:48 on the southeastern caldera rim and M4.7 /earthquakes-and-volcanism/articles/nr/3011/

• 58. 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

• 59. VI_2013_008

  systematically underestimated. The bias is not as pronounced for the non glacial rivers. Com- bining synoptic-scale and basin-scale predictors (method 3) leads to a substantial improvement compared to the use of MSLP fields alone (method 1). Analogue forecasts become similar or better than persistence, depending on catchment and lead time. Usually, persistence performs better for T=1 day and then method 3 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 60. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf