By its very nature, interpolation in a vector field is ambiguous, owing to the somewhat arbitrary nature of the vector norm. Since a 2-dimensional vector field can be specified by 2 scalar quantities, which can be separately interpolated, the ambiguity can be resolved by forcing the interpolated wind field to preserve the vorticity and divergence fields associated with the raw data. A method to calculate divergence and vorticity directly from randomly spaced wind observations is developed and, using analytically generated data, shown to produce more accurate results than conventional computations. 2 methods of retrieving the wind field from the analyzed scalar fields are presented and also tested on the analytic field. Finally, total analysis, from wind observations to gridded wind fields, is demonstrated on real meteorological data. -Authors
CITATION STYLE
Schaefer, J. T., & Doswell, C. A. (1979). On the interpolation of a vector field. Monthly Weather Review, 107(4), 458–476. https://doi.org/10.1175/1520-0493(1979)107<0458:OTIOAV>2.0.CO;2
Mendeley helps you to discover research relevant for your work.