02 September RP-C Environmental Conditions and Environmental Loads n RP-C is an updated and enhanced version of DNV. Find the most up-to-date version of DNVGL-RP-C at Engineering DNV RP C Environmental Conditions and Environmental Loads_ – DNV推荐做法,适用各种浮式结构环境载荷的计算.

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A linear random wave model is a sum of many small linear wave components with different amplitude, frequency and direction.

R is positive in stable air, i.

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The local wavelength of irregular waves can be defined as the distance between two consecutive zero up-crossings. HSE gives an indication of the accuracy which can be expected when conversions of wind speeds between different averaging periods is carried out by means of gust factors.

This is usually the case for the turbulence in homogeneous terrain. DNV is grateful for the valuable cooperation and discussions with these partners. Empirical statistical data used as a basis for design must cover a sufficiently long period of time.

For extreme mean wind speeds corresponding to specified return periods in rl of approximately 50 years, the Fr?

Note that the three parameters are not independent. This implies in particular that the expressions can be applied to winds in hurricanes. In the first approach, wind sea and swell are modelled as independent variables, which is generally a reasonable assumption with regard to the physics of combined seas.

Although such characteristics to a certain extent are of general validity, procedures established using data from a specific location should be used with c2055 when applied to other ocean areas.


The coherence decrement typically increases with increasing separation, thus indicating a faster decay of the coherence with respect to frequency at larger separations.

DNVGL-RP-C Environmental conditions and environmental loads – DNV GL

DNV does not accept any liability or responsibility for loss or damages resulting from any use of this document. Higher order terms may result in slightly higher crest heights. Usually only quantiles in the upper tail of the distribution are of interest, viz. The idea is to define contours in the environmental parameter space usually Hs, Tp along which extreme responses with given return period should lie.

Wave trough depth AT is the distance from the still water level to the trough. A cnoidal wave has crest to wave height ratio between 0. Only a few are calibrated to wind data obtained over water. Reference is made to Marthinsen and WintersteinNesteg? The coefficients Ai are calculated as?

Design of certain dynamic current sensitive structures should take into account turbulence effects. Yet, for frequencies less than approximately 0. The spectrum parameters are related to Hs and Tp according to empirical parameters.

One can replace the stochastic response by a fixed fractile level higher than the median value, or apply multipliers of the median extreme response estimates. For example year value for Hs and the conditional median for Tz — The contour line is estimated from the joint model or scatter diagram as the contour of constant probability density going through the above mentioned parameter combination.


Hydrodynamic model testing is covered in Ch.

DNV RP C Environmental Conditions and Environmental Loads__图文_百度文库

Air temperature change can be a more reliable indicator of presence of a squall, as the wind may not always change direction. The world wide scatter diagram defines the average weighted scatter diagram for the following world wide sailing route: The extreme value estimates should be compared with results from alternative methods. They generally agree in the high frequency range, whereas large differences exist in the low frequency range.

The Standards and Recommended Practices are offered within the following areas: This refers to hurricanes for which the minute mean wind speed forms a sufficient representation of the wind climate.

For the exponential distribution? The limiting values were obtained from measured data from the Norwegian Continental Shelf, but are expected to be of more general validity. For details about the von Karman coherence model, reference is made to Saranyansoontorn et al.

The Torsethaugen spectrum is given in Appendix A. Grue’s method as given above is limited to crest kinematics and valid for x205 water waves. Unstable conditions typically prevail when the surface is heated and the vertical mixing is increasing. The choice of the distribution model may depend on the application, i.

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