5 results were found for 강릉싱글〔모든톡@SECS4〕모든톡@SECS4 강릉연애어플 강릉만남어플…강릉소셜⒟강릉독신 ー袼 inaccuracy.

Results:

• 1. Windspeed

  -values, average windspeed and the median for the average windspeed in m/s, km/h, and knots. Top of page Windspeed classification To ease the understanding of the m/s measurement, the following table can be used. Windspeed IN m/s Description <5 Very slow wind 5-10 Rather slow wind 10-20 Considerable wind, may lead to difficulties 20-30 Very windy, caution is advised >30 /weather/articles/nr/1283

• 2. Windspeed

  -values, average windspeed and the median for the average windspeed in m/s, km/h, and knots. Top of page Windspeed classification To ease the understanding of the m/s measurement, the following table can be used. Windspeed IN m/s Description <5 Very slow wind 5-10 Rather slow wind 10-20 Considerable wind, may lead to difficulties 20-30 Very windy, caution is advised >30 /weather/articles/nr/1283/

• 3. ces-glacier-scaling-memo2009-01

  volume towards a new steady state of the glacier in the case of a “moderate” step change in climate. The relative importance of the mass-balance–elevation feedback and the reduction in ice- covered area may be analysed with reference to the perturbation equation d(DV ) dt = B0+beDA+GeDV = B 0 DV tV ; (3) where the volume time-scale tV is given by tV = 1 ( be=H) Ge ; (4) (Harrison and others, 2001 /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 4. VI_2009_006_tt

  the maximum discharge of jökulhlaup water at the glacier terminus is estimated as 97 m3 s 1. This jökulhlaup was a fast-rising jökulhlaup as other jökulhlaups in Skaftá and cannot be described by the traditional Nye-theory of jökulhlaups. The total volume of flood water was estimated as 53 Gl. The average propagation speed of the subglacial jökulhlaup flood front was found to be in the range 0.2–0.4 m s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 5. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  tg ui da n ce fo rt ra ns bo un da ry w at er s, pr ep ar ed an d P. van der Keur et al. (floo dmanag ement )an d wat er qualit y ag re ed u po n in co m m o n u n de rs ta nd in g, creat ed th e bas is fo rth e formul atio n o f joi nt m ea su re s (Fr ijte rs an d Le en tv aa r 200 3) Mo del s (na tural ,te chnica l an d so ci al sy ste m s): Uncert aint y ha s to be incorp orated : 1: Ep ist /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf