Scientific Computation Platform for Geophysical Geodesy

Fortran codes for numerical integral of terrain Helmert condensation effects on Fortran codes for numerical integral of terrain Helmert condensation effects on all-element gravity field

Issuing time:2024-11-21 14:42Author:Chuanyin ZhangLink:http://www.zcyphygeodesy.com
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[Algorithm purpose]

Using the rigorous numerical integral algorithm, from the ground digital elevation model and ground ellipsoidal height grid, compute the terrain Helmert condensation effects on the height anomaly (m), gravity (anomaly/disturbance, mGal), vertical deflection (ʺ, to south, to west) or (disturbing) gravity gradient (E, radial) on or outside the geoid.

Since the normal gravity field keeps unchanged, the terrain Helmert condensation effect on the gravity disturbance and gravity anomaly is always equal to the terrain Helmert condensation effect on gravity.

Compared with local terrain effects, terrain Helmert condensation has more ultrashort wave components. Affected by the continental topography, there is terrain Helmert condensation in the nearshore sea area, and the terrain Helmert condensation in the deep ocean area is equal to zero.

[Main program for test entrance]

    TerrainHelmertintgrl.f90

    The record format of the input calculation point file: ID (point no / point name), longitude (decimal degrees), latitude (decimal degrees), ellipsoidal height (m)......

    The record format of the output file reslt.txt: Behind the record of the calculation point file, appends 5 columns of terrain Helmert condensation effects on the height anomaly (m), gravity (anomaly/disturbance, mGal), vertical deflection (ʺ, to south, to west) or (disturbing) gravity gradient (E, radial) on or outside the geoid.

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[Main modules]

(1) Algorithm module for numerical integral of local terrain effects on various field elements

    LTerAllBLH(BLH,dtm,sfh,nlat,nlon,hd,dr,GRS,ter)

    Input parameters:BLH(3)-longitude (decimal degrees), latitude (decimal degrees), ellipsoidal height (m) of the calculation point.

    Input parameters:dtm(nlat,nlon) - the ground digital elevation model (normal /orthometric height) grid, which is employed to indicate terrain relief.

    Input parameters: sfh(nlat,nlon) - the ground ellipsoidal height grid, which represents the terrian surface position employed to calculate the integral distance.

    Input parameters: dr, hd(6) - the integral radius (m) and grid specification parameters (minimum and maximum longitude, minimum and maximum latitude, longitude and latitude intervals of a cell grid).

    Input parameters: GRS(6) - gm, ae, j2, omega, 1/f, default value

    Return parameters: ter(5) - local terrain effects (in unit of SI) on the height anomaly, gravity (anomaly/disturbance), vertical deflection (to south, to west) or (disturbing) gravity gradient (radial).

(2) Algorithm module for numerical integral of local terrain compensation effects on various field elements

    TercmpnBLH(BLH,mu,sfh,nlat,nlon,hd,dr,GRS,ter)

    Input parameters: mu(nlat,nlon) - the terrain compensation density grid.

    Input parameters: sfh(nlat,nlon) - the ground ellipsoidal height grid, which represents the terrian surface position employed to calculate the integral distance.

    Return parameters: ter(5) - local terrain compensation effects (in unit of SI) on the height anomaly, gravity (anomaly/disturbance), vertical deflection (to south, to west) or (disturbing) gravity gradient (radial).

(3) Calculation module for the normal gravity field

    normdjn(GRS,djn); GNormalfd(BLH,NFD,GRS)

    Return parameters: NFD(5) - the normal geopotential (m²/s²), normal gravity (mGal), normal gravity gradient (E), normal gravity line direction (', expressed by its north declination relative to the center of the Earth center of mass) or normal gravity gradient direction (', expressed by its north declination relative to the Earth center of mass).

(4) Calculation module for Legendre functions and their derivatives to ψ

    LegPn_dt2(pn,dp1,dp2,n,t) ! t=cos ψ

(5) Algorithm library for transforming of geodetic coordinates

    BLH_RLAT(GRS, BLH, RLAT); BLH_XYZ(GRS, BLH, XYZ)

    RLAT_BLH(GRS, RLAT, BLH)

(6) Algorithm library for interpolation point value from numerical grid

    CGrdPntD(lon,lat,dt,row,col,hd);CGrdPntD2(lon,lat,dt,row,col,hd)

    CShepard(lon,lat,dt,row,col,hd);Gauss2D(lon,lat,dt,row,col,hd)

(7) Other auxiliary modules

    PickRecord(str0, kln, rec, nn)

[For compile and link]

    Fortran90, 132 Columns fixed format. Fortran compiler for any operating system. No external link library required.

[Algorithmic formula] PAGravf4.5 User Reference

    1.4.1 Format convention for geodetic data file

    7.7 Local terrain compensation and terrain Helmert condensation

    7.5.2 Integral formula of local terrain effect outside the Earth

    7.1(4) Low-dgree Legendre function and its first and second derivative algorithms


The rar compression package in the attachment includes the test project in visual studio 2017 - intel fortran integrated environment, DOS executable file and all input and output data.


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