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Tidal Gravity Correction Solid Earth Tide Estimate Calculator

Estimate degree-two solid-Earth tidal gravity from supplied external-body GM/distances/zeniths and gravimetric factor 1+h2-1.5k2; downward-positive gravity and opposite removal correction, not full IERS tides or ephemerides.

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Description

Estimate degree-two tidal gravity from supplied body geometry and Love numbers, retaining the gravity/correction sign distinction.

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.

Estimate degree-two tidal gravity from supplied body geometry and Love numbers, retaining the gravity/correction sign distinction.

When to use this tool

Use this tool when you need to estimate degree-two tidal gravity from supplied body geometry and Love numbers, retaining the gravity/correction sign distinction.

How to use the tool and how it works

  1. Enter bodyGm, bodyDistanceMeters, bodyZenithDegrees, earthRadiusMeters, loveH2, loveK2 using the definitions below.
  2. Run the operation. Resolve input-format errors before interpreting an output.
  3. Read result.gravimetricFactor, result.tidalDownGravityChangeMicrogal, result.correctionToObservedMicrogal, using the stated boundary, ordering, sign and absence conventions.

For each supplied body, accumulate outward degree-two acceleration GM×R/r³×(3cos²(zenith)−1). Multiply by 1+h2−1.5k2, negate for down-positive gravity change, and convert m/s² to microgal by 10⁸. Return the opposite sign as the correction to observed gravity.1

Input fieldMeaning and unitsAccepted input
bodyGmOne to eight positive body gravitational parameters GM in m³/s², each at most 2×10²⁰.Dense list of at most 128 finite numbers, under the stated integer/range rules.
bodyDistanceMetersBody-center distances in meters, aligned to bodyGm, each from 10 Earth radii through 10¹³.Dense list of at most 128 finite numbers, under the stated integer/range rules.
bodyZenithDegreesBody zenith angles in degrees, zero through 180, aligned to bodyGm.Dense list of at most 128 finite numbers, under the stated integer/range rules.
earthRadiusMetersExplicit spherical reference radius in meters, 10⁶–10⁷.Finite numeric value satisfying the stated comparisons.
loveH2Dimensionless degree-two displacement Love number h2, zero through one.Finite numeric value satisfying the stated comparisons.
loveK2Dimensionless degree-two potential Love number k2, zero through 0.5.Finite numeric value satisfying the stated comparisons.
Output fieldInterpretation
resultObject containing the fields below.
result.gravimetricFactorDimensionless 1+h2−1.5k2 applied to the supplied degree-two body contributions.
result.tidalDownGravityChangeMicrogalModeled down-positive gravity change in microgal.
result.correctionToObservedMicrogalOpposite-signed correction to remove the modeled gravity change, in microgal.
json
{
  "input": {
    "bodyGm": [
      100000000000000
    ],
    "bodyDistanceMeters": [
      100000000
    ],
    "bodyZenithDegrees": [
      0
    ],
    "earthRadiusMeters": 1000000,
    "loveH2": 0.6,
    "loveK2": 0.3
  },
  "output": {
    "result": {
      "gravimetricFactor": 1.1500000000000001,
      "tidalDownGravityChangeMicrogal": -23000.000000000004,
      "correctionToObservedMicrogal": 23000.000000000004
    }
  }
}

Limitations and assumptions

  • One to eight bodies use GM in m³/s², distance at least 10 Earth radii and at most 10¹³ m, and zenith in [0,180] degrees. Love numbers h2∈[0,1], k2∈[0,0.5] must yield a positive factor. No ephemerides, ocean loading or full tidal spectrum are included.
  • 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

  1. Tool behavior and example: Tidal Gravity Correction Solid Earth Tide Estimate Calculator — tool.io

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