91 results were found for Y アイリス〈ωωω,RTЗЗ,TOP〉コード:B77〉ミップスロット༿トラットfc🤞サッカートトサイト💛マカオベネシアン╜ソマリアの国家戦㍁パワーボールピクスター∿ジョージアサッカー␇プロトライブスコア∔.adq/.

Results:

• 61. Bárðarbunga 2014 - December events

  ). The largest one, M4.1 occurred at 7:14, another, M4.0 at 18:11 and the third, M4.0 at 09:45 this morning. Ca 15 earthquakes between M3 and M4 were detected in Bárðarbunga. Yesterday evening at 23:18 an earthquake M4.4 was detected in the ocean, ca 20 km north of Kolbeinsey and some smaller followed. Similar pattern is common in the area. The lava almost 83 square kilometers? An overview map /earthquakes-and-volcanism/articles/nr/3055/

• 62. Bardarbunga-2014_December-events

  pattern is common in the area. The lava almost 83 square kilometers? An overview map last midnight (28 - 29 Dec.). The lava was estimated 82,8 km² (82,4 km² + 0,4 km²); possibly an overestimate. A field excursion on the 28th, organised from Húsavík, measured the whole length of the northern margin at 5 - 20 km distance but in places it was impossible to be so close and they had to make loops /media/jar/Bardarbunga-2014_December-events.pdf

• 63. ces_geus_paakitsoq_full_report

  conditions as a lower boundary condition from the driving GCM. The RCAO model-output is from a pan-arctic run for the years 1960–2080 at approx. 50 km resolution. The first 20 years of the model run must be considered as spin-up time for the ocean module. The RCAO run is experimental since the model is in a development state and the output has not yet been evaluated over Greenland (Ralf Döscher, personal /media/ces/ces_geus_paakitsoq_full_report.pdf

• 64. Kok_and_Veldkamp_editorial_ES-2011-4160

  ? Methodological reflections on scalar structuration. Progress in Human Geography 25:591-614. Bryan, B. A., N. D. Crossman, D. King, W. S. Meyer. 2011. Landscape futures analysis: assessing the impacts of environmental targets under alternative spatial policy options and future scenarios. Environmental Modelling and Software 26(1):83-91. Buizer, M., B. Arts, and K. Kok. 2011. Governance, scale /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 65. ces-oslo2010_proceedings

  Resources and Energy Directorate Edited by: Heidi H. Pikkarainen Print: Norwegian Water Resources and Energy Directorate Number printed: 130 Cover design: Rune Stubrud Prepared for: The CES project Norwegian Water Resources and Energy Directorate Middelthunsgate 29 P.O. Box 5091 Majorstua N-0301 OSLO NORWAY Telephone: +47 22 95 95 95 Fax: +47 22 95 90 00 /media/ces/ces-oslo2010_proceedings.pdf

• 66. VI_2014_006

  ˚ 55˚ 55˚ 60˚ 60˚ 65˚ 65˚ 70˚ 70˚ 75˚ 75˚ Figure 2. Analogy domains AD1 (blue polygon) and AD2 (red polygon). 20 Figures 3 and 4 present the performances of each analogue method (cf. Table 2), considering a deterministic prediction obtained by taking the weighted mean of the ensemble precipitation or temperature predictions. The weight was defined according to the rank of the analogue. Some /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

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

  Av. Ed. Belin, 31400 Toulouse, France Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011 Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011 Abstract. The Little Ice Age maximum extent of glaciers in Iceland was reached about 1890 AD and most glaciers in the country have retreated during the 20th century. A model for the surface mass balance /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 68. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 69. Kok_et_al._TFSC_published_2011

  17 24 64 Sustainability Eventually 5 3 30 28 66 Fortress Europe 18 11 30 23 72 Policy Rules 6 5 13 17 41 Total 44 27 80 92 243 844 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy sector. The presence of various climate-related strategies is a consequence of the presence of climate-related obstacles and opportunities. 3.4.6. Robust elements Results /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 70. Journal_of_Hydrology_Veijalainen_etal

  A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf