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Numerical models have shown that mangroves are better at reducing surge heights during faster moving storms (~40 km/hr).
The Army Corps of Engineers examined the elevation of water at the shoreline, and estimated the potential dangers from larger and slower moving storms, particularly at high tide.
It is found that downstream moving storms with Ls/L<1.0 increase the peak discharges to a limited extent compared to stationary storms, and the kinematic-wave model overstates the increase in the peak flows resulting from downstream moving storms with Ls/L<1.0.
However, the TRCM often underestimates the rainfall amount in cases of slowing moving storms with strong southwest monsoon supply of water vapor flux.
The kinematic-wave model simulates the upstream moving storms pretty well, i.e. Nash Sutcliffe coefficient of model fit efficiency equal to 0.948 and 0.831 for storms lengths equal to and not equal to the watershed length, respectively.
The hypothesis that downstream moving storms with storm length less than watershed length (Ls/L<1.0) magnify the peak discharges as indicated by kinematic-wave models in previous studies was evaluated in an analysis of the dimensionless peak discharge and dimensionless storm velocity.
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The dynamic response of the coastal and shelf seas to a moving storm is complex.
"This is an incredibly slow moving storm," said Brandon Smith, a meteorologist for the National Weather Service in Upton, N.Y.
Tang, C. L., Gui, Q. & DeTracey, B. M. Barotropic response of the Labrador/Newfoundland Shelf to a moving storm.
In some cases the rainbands are stationary relative to the centre of the moving storm, and in other cases they seem to rotate around the centre.
Tang et al.6 using a linear model investigated the barotropic response of shelf circulation to an idealized moving storm off Newfoundland and Labrador.
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