A method and apparatus for estimating the sea state beneath a platform using a radar altimeter is provided. The method includes dividing a received wide angle radar beam into a plurality of Doppler bins. Ranges to a sea surface is tracked for at least one Doppler bin over time. Wave spectrum information associated with the sea state is estimated based on at least one tracked range. The estimated wave spectrum information includes at least one of a primary peak period estimation and a significant wave height estimation.
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