32 results were found for 凯时澳门网站_50134.com.

Results:

• 21. VI_2015_005

  (97%) relative to maritime storms decreases. This relative and absolute increase in the occurrence of maritime cyclones in the central sector, with increasing time-scale, emphasises again the cli- matological significance of the Icelandic Low. During summer, the cyclone density over land increases on all time-scales and in each sector, compared with winter. There is also a relative increase /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 22. VI_2015_009

  A 1x1 km digital elevation model derived from a 500 m DEM (Icelandic Meteorological Of- fice, National Land Survey of Iceland, Science Institute, University of Iceland, and National Energy Authority. 2004), a soil map from the Agricultural University of Iceland and a map of the bedrock geology from the Icelandic Institute of Natural History (Jarðfræðikort af Íslandi - Berggrunnur - 1:600.000 - NI /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 23. 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

• 24. 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

• 25. 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

• 26. Reykholt-abstracts

  on the ground along the direction of travel) low- power laser in conjunction with single-photon sensitive detectors to measure ranges using ~532 nm (green) light. In the polar regions, the 91-day repeat orbit pattern with a roughly monthly sub-cycle is designed to monitor seasonal and interannual variations of Greenland and Antarctic ice sheet elevations and monthly sea ice thickness changes. Dense /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 27. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 28. VI_2019_009

  of the automatic station, 87% of the records show the max- imum visibility. ..................................................................................... 18 9 Records from the automatic station. The figure to the right is the visibility with- out the most frequent value....................................................................... 19 10 The visibility difference (manual observation minus /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 29. 2013_001_Nawri_et_al

  /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 30. VI_2020_004

  -based maps ............................................................................ 81 5.4.5 Probability of exceedance and accumulation rate ............................................ 87 5.5 Towards an integration of the three explosive eruptive scenarios ............................. 93 6 Main conclusions and next steps /media/vedurstofan-utgafa-2020/VI_2020_004.pdf