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In hatyan there is a X-factor of 0.53 for the M2 component (and other values for several other components), to account for damping of the nodal cycle by the shallow shelf. This is applied for stations along the Dutch coast. Research shows that this X-factor is actually spatially varying:
It could be considered to apply a spatially varying X-factor instead. This should already be possible with hatyan, so it is possible to investigate the impact of this improvement. However, it will be cumbersome and prone to errors to save this metadata in component files and therefore it might be inconvenient to apply it in the tidal prediction practice.
In hatyan there is a X-factor of 0.53 for the M2 component (and other values for several other components), to account for damping of the nodal cycle by the shallow shelf. This is applied for stations along the Dutch coast. Research shows that this X-factor is actually spatially varying:
It could be considered to apply a spatially varying X-factor instead. This should already be possible with hatyan, so it is possible to investigate the impact of this improvement. However, it will be cumbersome and prone to errors to save this metadata in component files and therefore it might be inconvenient to apply it in the tidal prediction practice.
Original slides by FZ:
LowFrequencyTidalModulations_20240415.pdf
FZ: Voor het testen van afwijkende M2 Xfactoren zijn de volgende locaties interessant:
Also:
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