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The optical path length from a satellite to the earth's surface is strongly dependent on the atmospheric pressure along the propagation path. Surface pressure can be measured by using a two-color laser altimeter to observe the change with wavelength in the optical path length from a satellite to the ocean surface. The statistical characteristics of the ocean-reflected pulses and the expected measurement accuracy are evaluated in terms of the altimeter parameters. The results indicate that a pressure accuracy of a few millibars is feasible.
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Gardner et al. (1983) studied this question.
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