Non-singular calculation method for vertical components of external disturbing gravity of flow points in sea area
A technology of external disturbance and calculation method, which is applied in the field of ocean gravity to achieve the effect of high-precision calculation
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[0015] The present invention is described in further detail below by way of examples.
[0016] A non-singular calculation method for the vertical component of the external disturbance gravitational force of the floating point in the sea area, comprising the following steps:
[0017] Step 1. Using the local integral domain identity transformation to realize the non-singularity calculation of the vertical component of the external disturbance gravitational force of the grid points in the sea area. The specific implementation method is:
[0018] The integral formula for calculating the vertical component of the earth’s external disturbance gravitational force using the surface layer method is:
[0019]
[0020] in:
[0021]
[0022]
[0023] r=R+h
[0024] In the formula, T p Compute the perturbation bit at point P for the external space; and Represent the geocentric radius, geocentric latitude, and geocentric longitude of the calculation point and the spherica...
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