Radar altimetry: introduction and application to air-sea interaction

David Kevin Woolf, Christine Gommenginger

    Research output: Chapter in Book/Report/Conference proceedingChapter (peer-reviewed)

    4 Citations (Scopus)

    Abstract

    Radar altimeters are among the more common satellite-borne Earth Observation instruments with a long history including continuous data since 1991. They are also exceptionally versatile providing information on sea level, ocean dynamics, wind speed and a number of wave parameters. Radar altimetry is a “point” rather than a “swath” instrument so that sampling resolution by a single altimeter is relatively poor in both space and time. Also the sizeable footprint restricts use of altimetry to greater than 10km from any coast, with some restrictions at a greater distance. The sampling limitations do not negate the usefulness of altimetry, either in isolation or in combination with other instruments or modelling. Climatologies of sea level and wave parameters built from altimetry provide a unique perspective on both a regional and global scale. Measurements of individual storm events provide a test for both wave and storm-surge modelling and could be useful in Near Real Time applications. New interpretations of satellite altimeter waveforms and dual-frequency data, and new advanced altimeter concepts, continuously present new products to broaden the geophysical applications of radar altimetry.
    Original languageEnglish
    Title of host publicationRemote sensing of the European seas
    EditorsVittorio Barale, Martin Gade
    PublisherSpringer
    Pages283-294
    Number of pages12
    ISBN (Electronic)9781402067723
    ISBN (Print)9781402067716
    DOIs
    Publication statusPublished - 2008

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