Description
Calculate an ideal annular-sector terrain gravity correction from supplied geometry, relief and density.
Geodesy distinguishes a mathematical reference ellipsoid, a realized coordinate datum and the physical gravity field. Geodetic latitude follows the ellipsoid normal; geocentric latitude follows a radius from the center. Ellipsoidal height, orthometric height and geoid undulation are separate signed quantities. Keep the declared ellipsoid, coordinate axes, angular units and time scale with a result.
Calculate an ideal annular-sector terrain gravity correction from supplied geometry, relief and density.
When to use this tool
Use this tool when you need to calculate an ideal annular-sector terrain gravity correction from supplied geometry, relief and density.
How to use the tool and how it works
- Enter innerRadiusMeters, outerRadiusMeters, reliefMeters, densityKgPerM3, angularWidthDegrees using the definitions below.
- Run the operation. Resolve input-format errors before interpreting an output.
- Read result.terrainCorrectionMgal, using the stated boundary, ordering, sign and absence conventions.
Treat the terrain as one constant-relief annular sector of positive density. Use absolute relief h and evaluate 2πGρ×(angularWidth/360)×[rOuter−rInner+sqrt(rInner²+h²)−sqrt(rOuter²+h²)], using an algebraically stable equivalent and converting to mGal.1
| Input field | Meaning and units | Accepted input |
|---|---|---|
| innerRadiusMeters | Nonnegative inner radius of the terrain sector in meters, below outerRadiusMeters. | Finite numeric value satisfying the stated comparisons. |
| outerRadiusMeters | Outer terrain-sector radius in meters, greater than inner and at most 100,000. | Finite numeric value satisfying the stated comparisons. |
| reliefMeters | Signed sector relief in meters, within ±10,000; its absolute value is used. | Finite numeric value satisfying the stated comparisons. |
| densityKgPerM3 | Positive terrain density in kg/m³, at most 10,000. | Finite numeric value satisfying the stated comparisons. |
| angularWidthDegrees | Sector width in degrees, strictly positive and at most 360. | Finite numeric value satisfying the stated comparisons. |
| Output field | Interpretation |
|---|---|
| result | Object containing the fields below. |
| result.terrainCorrectionMgal | Nonnegative modeled annular-sector terrain correction in mGal. |
{
"input": {
"innerRadiusMeters": 0,
"outerRadiusMeters": 4,
"reliefMeters": 3,
"densityKgPerM3": 1000,
"angularWidthDegrees": 360
},
"output": {
"result": {
"terrainCorrectionMgal": 0.08387172739141742
}
}
} Limitations and assumptions
- Require 0≤inner<outer≤100,000 m, abs(relief)≤10,000 m, 0<density≤10,000 kg/m³ and 0<width≤360°. The name does not select a preset Hammer zone; supply the actual sector geometry. This is one idealized sector, not a DEM terrain correction.
- All quantities are finite and retain the units stated for this operation. Ellipsoid-parameter tools use semi-major axis 1–10⁸ m and dimensionless flattening 0–0.02; explicit-axis tools use 0.9a≤b≤a unless a tighter bound is stated. These tools do not fetch datums, geoid grids, satellite observations or Earth-orientation updates.
- Every declared outer field is required and unknown outer fields are rejected. Strings and JSON text have size limits, lists are bounded to 128 entries, and JSON nesting/node counts are bounded. Tighter operation-specific bounds stated above take precedence.
- Numeric results must be finite. Large physical magnitudes are allowed by the output evidence checks, while integer fields and source schemas retain their exactness rules. Source indexes are zero-based. Floating-point residues can remain even where an ideal formula gives an exact zero.
Alternative or Complementary methods
Use a coordinate transform for a change of representation and explicit datum parameters for a change of reference frame. Preserve model and convergence metadata, and use observation and datum information appropriate to a real survey before interpreting a computed tolerance as accuracy.
References
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