calc_gwd | R Documentation |
This function determines the bearing from the storm's center to a grid point location and then calculates the direction of gradient winds at that grid point. Gradient winds will be perpendicular to the direction from the storm's center to the grid point. In the Northern hemisphere, cyclonic winds are counterclockwise, so you add 90 degrees to the bearing from the storm center to the grid point when using polar coordinates. In the Southern hemisphere, cyclonic winds are clockwise, so you subtract 90 degrees.
calc_gwd(tclat, tclon, glat, glon)
tclat |
A numeric value with the latitude of the tropical cyclone's center in radians |
tclon |
A numeric value with the longitude of the tropical cyclone's center in radians |
glat |
A numeric value with the latitude of the grid point in radians |
glon |
A numeric value with the longitude of the grid point in radians |
A numeric value with the the direction of gradient storm winds at a location, in polar coordinates (i.e., due East is 0 degrees, due North is 90 degrees, etc.)
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