35 results were found for 킹덤홀덤〔trrt2-com〕 킹덤홀덤모바일 타임바카라‡타짜슬롯⑭타짜홀덤 RTh/.

Results:

• 21. VI_2009_006_tt

  farvegarins undir jöklinum út frá rúmmáli vatns sem þar hefur safnast fyrir benda til þess að viðnám gegn vatnsrennsli við jökul- botn minnki eftir því sem líður á hlaupið. Undir lok hlaupsins runnu á bilinu 80– 90 m3 s 1 um farveg sem var einungis einn þriðji hluti af rúmmáli farvegar sem flutti svipað vatnsmagn á fyrsta eða öðrum degi eftir að hlaupið hófst við jökuljaðar. Þessi niðurstaða er /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 22. IPPC-2007-ar4_syr

  of significant changes consistent with warming Percentage of significant changes consistent with warming 89%94%100% 100% 100% 100% 100% 100% 99%100%98% 96% 91% 94% 94% 90%90%92%94% 355 455 53 119 NAM LA EUR AFR AS ANZ PR* TER MFW** GLO 5 2 106 8 6 1 85 7650 120 24 7645 28,115 28,586 28,671 Changes in physical and biological systems and surface temperature 1970-2004 33 Topic 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf

• 23. 2010_005_

  respec- tively. Due to limited data availability, for the SMHI-RCAO run, the 20th Century control period is restricted to the 20-year period 1971–90, and the second 21st Century reference period is limited to the years of 2070–80. For the MetNo-HIRHAM runs, no data are available during the second 21st Century reference period. 3 Spatial Variability of Climate Trends This section discusses /media/ces/2010_005_.pdf

• 24. VI_2015_005

  depression .. 18 9 Relative seasonal occurrence of mean sea level pressure modes........................ 20 10 Composite mean temporal tendencies of mean sea level pressure...................... 22 11 Composite mean 500 hPa geopotential height anomalies ................................ 25 12 Composite mean surface wind speed anomalies ............................................ 27 13 Composite /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 25. VI_2015_009

  M A M J J A l ll l l l l l l l lll l l lll 0 100 200 300 60 0 80 0 100 0 Days since Sept. 1st Q (m ³/s ) vhm102 S O N D J F M A M J J A l l l ll l l l l l l l l l l l l l ll l l l l l l 0 100 200 300 30 40 50 60 70 Days since Sept. 1st Q (m ³/s ) vhm116 S O N D J F M A M J J A l l l l l l l l l l l l l l l l l l l l l l l l l l 0 100 200 300 20 0 30 0 40 0 50 0 Days since Sept. 1st Q (m ³/s /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 26. Hare-2011-ParticipatoryModelling

  ; mayo ran d governmen t of cer s F M (si m u lat ion m od el) M F Tabl e2 . Ca te go riz at io n ta bl e fo r th e ex am pl es o fF AB E ap pr o ac he s to pa rt ic ip at o ry m o de llin g. A ce ll in th e ‘ pa rt ic ip at o ry m o de llin g st ag e’ ca n be interprete d in th e fo llo w in g m an n er : w he re th er e is n o st ak eh o ld er in vo lve m en t, N O P is w rit te n . W he re th /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 27. Kok_JGEC658_2009

  scenario development, with an example from Brazil Kasper Kok * Land Dynamics, Department of Environmental Sciences, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands 1. Introduction The world is undergoing rapid changes while globalising constantly, which gives the consideration of the future new urgency and importance. Scenario development has emerged as a key method when taking /media/loftslag/Kok_JGEC658_2009.pdf

• 28. 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

• 29. Reykholt-abstracts

  Twin-Otter as survey aircraft. Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 Guðmundsson and others 15 Post-Little Ice Age (1891–2011 AD) volume loss of Kotárjökull glacier, southeastern Iceland, as established from historical photography and lidar Snævarr Guðmundsson*, Hrafnhildur Hannesdóttir and Helgi Björnsson Institute of Earth Sciences, University /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 30. VI_2016_006_rs

  wide and 1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf