56 results were found for 99贵宾汇开户(3266-409-932薇Q).adw.

Results:

• 31. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 32. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 33. aerodrome_summaries_20140603

  M (171FT ) FRE Q UENCIE S (PE R CENT ) O F OCCU R RENC E O F CONCURREN T WIN D DIRECTIO N (I N 30 0 SEC T ORS ) AN D SPEE D (I N KN O TS ) WITHI N SPECIFIE D RANGE S ANN U A L WIN D WIN D SPEE D (KT) ) DIRECTIO N CAL M 1– 5 6–1 0 11–1 5 16–2 0 21–2 5 26–3 0 31–3 5 36–4 0 41–4 5 46–5 0 >5 0 T O T A L V ARIABL E 0 0 0 0 0 0 0 0 0 0 0 0 0 35-36-0 1 3 2 3 3 2 1 1 0 0 0 0 0 14 02-03-0 4 0 2 4 4 3 1 0 0 /media/vedur/aerodrome_summaries_20140603.pdf

• 34. FMI_-_Disaster_Mitigation

  Disaster Mitigation Kevin M. Simmons, Ph.D. Austin College Fulbright Research Scholar International Centre for Geohazards Oslo, Norway Economic and Societal Impacts of Tornadoes By Kevin M. Simmons and Daniel Sutter © 2010, 296 pages in paperback ISBN: 978-1-878220-99-8 AVAILABLE NOVEMBER 2010 from the American Meteorological Society and the University of Chicago Press Research Agenda /media/loftslag/FMI_-_Disaster_Mitigation.pdf

• 35. VI_2009_012

  Different kinds of weights were tried in the regression process in which case the least squares problem becomes the problem of minimizing { }2102 ,...),()(log∑ − i iiii rMfPGXw , with respect to the parameters of the model f. The weights wi were generally of the form ),( rMq p wi = , where p was a normalization constant and usually q(M,r) was a discrete density distribution made to correct /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 36. Protective measures

  experiments for evaluating the effectiveness of avalanche defence structures in Iceland. Main results and future programme (pdf 0,8 Mb) (Í: Proceedings of the International Seminar on Snow and Avalanches Test Sites, Grenoble, France, 22−23 November 2002, F. Naaim-Bouvet, ed., s. 99−109, Grenoble, Cemagref, 2003, author T. Jóhannesson) [abstract] (html) Stálgrindur eða snjóflóðanet? Val á tegund /avalanches/imo/protective/

• 37. Mid-Latitudes-Agenda1_nov2013EH

  Thursday, 14 November Time Agenda Item 09:00 – 10:30 09:00 – 09:20 09:20 – 09:40 09:40 – 10:00 10:00 – 10:30 Potential Arctic / Mid-Latitude Linkages - East Asia (Chair: Jim Overland) Rapid Arctic Warming in Recent Decades and Its Impact on Climate Change over East Asia - S-J Kim Extreme weather in northern mid-latitudes linked to cryosphere loss - Q Tang A cause of the AO /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 38. ces-glacier-scaling-memo2009-01

  of melt water from glaciated areas in long integrations for a warming climate. Glacier dynamics This problem can be qualitatively analysed by considering the continuity equation for ice vol- ume, which may be expressed as ¶h ¶t + ¶q ¶x = b or ¶h ¶t +~ ~q = b ; (1) for a one-dimensional ice flow channel or an ice cap that flows in two horizontal dimensions, respectively. h is ice thickness, q or ~q /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 39. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 40. raisanen_ruosteenoja_CES_D2.2

  in Table 2.1. Some potential limitations of using the CMIP3 ensemble for probabilistic climate change forecasting should be mentioned. First, current GCMs still have a relatively coarse horizontal resolution. Within the CMIP3 ensemble, the grid spacing varies from 1.1 q latitude × 1.1q longitude to 4 q latitude × 5q longitude (for the analysis presented here, all the model results were /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf