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

Results:

• 1. Windspeed

  boxes, the Beaufort-box will display the approximated Beaufort-value. This approximation inevitable leads to a slight inaccuracy in the calculations. The figure on the right loosely shows the relationship between m/s and a few Beaufort-values. The prerequisites of the calculations above are: The equation: W = 0.836B3/2 where W is windspeed in m/s and B is value on the Beaufort-scale. 1 m/s = 3.6 /weather/articles/nr/1283

• 2. Windspeed

  boxes, the Beaufort-box will display the approximated Beaufort-value. This approximation inevitable leads to a slight inaccuracy in the calculations. The figure on the right loosely shows the relationship between m/s and a few Beaufort-values. The prerequisites of the calculations above are: The equation: W = 0.836B3/2 where W is windspeed in m/s and B is value on the Beaufort-scale. 1 m/s = 3.6 /weather/articles/nr/1283/

• 3. ces-glacier-scaling-memo2009-01

  determined, some inaccuracy in the area distribution of individual glaciers can be accepted without causing a large error in the estimate of the total volume of ice stored in glaciers within the watershed. A procedure for estimating the total ice volume in a watershed is outlined in Figure 3. A statistical estimate of the distribution of ice bodies of different areas within the watershed in question /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 4. VI_2009_006_tt

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 5. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  and with absolute certainty, an ideal that is never achieved in policy relevant sciences due to the complexity of the problem dealt with (Krayer von Krauss 2005). In this range, statistical uncertainty can be described in statistical terms, e.g. measurement error due to sampling error, inaccuracy or imprecision. In contrast, scenario uncertainty cannot be described statistically. Scenarios are common /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf