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Trough depth did not influence any of the variables recorded.
The trough depth increases with increasing F107 and with decreasing incidence angle of solar flux.
The trough depth increased as F107 increased and as the incidence angle of solar flux decreased.
The trough depth increases with increasing F107 and with decreasing incidence angle of solar flux. 3.
The trough depth depends primarily on F107 and, to a lesser degree, on MLT.
The red lines denote the variation in the trough depth with respect to F107.
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wave trough depths distribution model, and the accuracy of the new method has been once again substantiated.
This paper deals with the calculation of wave trough depths exceedance probabilities for stochastic ocean waves, and a Transformed Rayleigh method is proposed for carrying out the calculation.
It is demonstrated that the proposed new method can offer better predictions than those from using the theoretical Rayleigh wave trough depths distribution model.
The proposed new method has been applied for calculating the wave trough depths exceedance probabilities of two sea states, one with the surface elevation data measured at the coast of Yura in the Japan Sea, and another one with the surface elevation data measured at the North Sea.
Indeed, in our study we found post-fixation to be a strategic step because the fixative-to-protein binding is slow and largely completed within 24 h (Helander 1994) required for the penetration of the antibodies trough slices' depth.
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