30 results were found for 电子竞技押注平台平台平台-登录网址注册网址-【✔️输入㊙️700bet.net✔️】-电子竞技押注平台平台平台-万博max客户端官方苹果-(✔️网址sogou7.com✔️)-电子竞技押注平台平台平台-电子竞技押注平台平台平台-电子竞技押注平台平台平台-【✔️输入㊙️315bet.net✔️】.

Results:

• 21. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 22. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 23. Observations - Gagnheiði II

  Observations - Gagnheiði II | Observations | Icelandic Meteorological office Observations - Gagnheiði II Mon 1.05 14 GMT NNE 10 Max wind : 11 / 13 13 GMT NW 5 Max wind : 5 / 10 12 GMT NW 5 Max wind : 5 / 9 11 GMT WNW 4 Max wind : 4 / 9 10 GMT NW 4 Max wind : 6 / 9 09 GMT N 6 Max wind : 6 /m/observations/areas

• 24. VI_2013_008

  point of the domain under study: S1(u) = n i=1 jEij+ n j=1 jE jj ni=1 Gi+ n j=1 G j (1) with El = (MSLP(l 1;u) MSLP(l+1;u)) (MSLP(l 1; t) MSLP(l+1; t)) (2) and Gl = max(jMSLP(l 1;u) MSLP(l+1;u)j; jMSLP(l 1; t) MSLP(l+1; t)j) (3) where El is the difference around a given grid point l, between the MSLP gradient at current time t and time u (i.e. candidate analogue), and Gl is the maximum /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 25. 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

• 26. VI_2015_005

  This is also the case with cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are cyclones in the neighbouring sector, in which case pressure tendencies are reversed. 21 Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com- posite mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 27. Hare-2011-ParticipatoryModelling

  support ) Improv e mode l (integration) ; socia llea rnin g Farmers ,loca l aut horities , association s NO P IN D Cognitiv e mappin g HE T GM B NO P HE T Simulation - by-han d OT :Researcher s KA F F Iska r (Phas e1 ) Co n ce pt u al m o de l (D is cu ss io n su pp o rt ; Com m unication ) Improv e mode l (integration) ; socia llea rnin g Nationa l poli cy-maker s NO P IN D Cognitiv e mappin g HE /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 28. 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

• 29. Lorenzoni_Pidgeon_2006

  level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 30. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf