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Ionospheric correction for single frequency GPS receivers using three satellites

  • US 6,169,958 B1
  • Filed: 04/09/1999
  • Issued: 01/02/2001
  • Est. Priority Date: 04/09/1999
  • Status: Active Grant
First Claim
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1. A method using satellite signal transmission for determining the geographic location of a receiver on the earth'"'"'s surface, comprising:

  • receiving a first signal transmitted at a known frequency from a first satellite having a known orbital position;

    receiving a second signal transmitted at the same frequency as the first signal from a second satellite having a known orbital position;

    receiving a third signal transmitted at the same frequency as the first signal from a third satellite having a known orbital position;

    calculating measured distances λ

    1, λ

    2 and λ

    3 of the respective first, second and third satellites from the receiver based at least in part on the transmission time of the respective first, second and third signals; and

    calculating actual distances ρ

    1, ρ

    2 and ρ

    3 of the respective first, second and third satellites from the receiver based on the measured distances λ

    1, λ

    2 and λ

    3, according to the relationships Fpp1Fpp2

    (λ

    2
    -ρ

    2
    )
    =λ

    1
    -ρ

    1
    ,

    Fpp1Fpp3

    (λ

    3
    -ρ

    3
    )
    =λ

    1
    -ρ

    1
    ,and
    Fpp2Fpp3

    (λ

    3
    -ρ

    3
    )
    =λ

    2
    -ρ

    2
    ,
    where Fpp1, Fpp2, and Fpp3 are obliquity factors for the respective first, second and third satellites based on the respective angles φ

    1, φ

    2 and φ

    3 they form with a plane tangent to the earth'"'"'s surface at the geographic location of the receiver, with Fpp1=-[1-(Re

    cos





    φ

    1
    Re+Hr
    )
    2
    ]
    -12
    ,

    Fpp2=-[1-(Re

    cos





    φ

    2
    Re+Hr
    )
    2
    ]
    -12
    ,and
    Fpp3=[1-(Re

    cos





    φ

    3
    Re+Hr
    )
    2
    ]
    -12
    ,
    where Re is the radius of the earth and Hr is the height of maximum electron density in the ionosphere surrounding the earth'"'"'s surface.

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