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It is found that the most prominent nonmigrating diurnal tidal modes at 95 km are: the eastward propagating tide with zonal wavenumber s = -3, the standing tide (s = 0), and the westward propagating tides with s = 2 and s = 3.
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A comparison of the results indicates that there is good quantitative agreement between TIDI and the model predictions during equinox, but the latter tend to underestimate the westward 2 diurnal tide and standing diurnal tide during solstice.
It is shown that the westward propagating diurnal tide with zonal wavenumber s = 2 is mainly excited by nonlinear interactions between the migrating diurnal tide and the stationary planetary wave with zonal wavenumber s = 1, while the nonlinear excitation of the standing diurnal tide with zonal wavenumber s = 0 is less important than the excitation by tropospheric heating.
But, with strength in numbers, we started wondering if we ought to be standing athwart the tide of Tim's love.
It usually began with standing water: a tide pool or pond or salty shallow, wet enough to breed bacteria but not so wet as to wash them away.
Standing against the tide of popular opinion makes you cling to it more tightly, this thing that you, and only you, know to be true.
Among the democratic defectors, standing against the tide with his metaphorical fist in the air, was Washington State delegate and Puyallup tribal member Robert Satiacum Jr.
Blair praised Miliband for standing against the tide on the EU, and said Eurosceptics "need to get real about how difficult it would be for Britain to negotiate a new relationship with the EU.
Look back at any period of rapid technological progress and you'll find two groups of individuals: Pioneers tirelessly charting new territory for the benefit of the species and members of the old order standing against the tide to fight back the phantom of their own perceived obsolescence.
Vertical isopycnal displacement observations at different stations fit a one-dimensional model of partly standing semidiurnal internal tides – comprised of a major, incident wave propagating up the canyon limbs and a minor wave reflected back down-canyon by steep, supercritical bathymetry near the canyon heads.
They attributed the eastward propagation of these features as being the result of the dominant diurnal standing (D0 tide) and the eastward wavenumber 1 (DE1 tide), both of which appear to have eastward phase velocities when viewed in local time.
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CEO of Professional Science Editing for Scientists @ prosciediting.com