amentum.space – gravity

OpenAPI apis-guru locationopen_data

The gravitational field of the earth is non-uniform. The is the shape the ocean surface would take if only gravity and the rotation of the Earth were considered. The geoid is the surface that defines zero elevation.

The geoid height is the difference between an ideal reference ellipsoid and the geoid.

The gravity anomaly is the difference between the acceleration due to gravity on the Earth's surface and the value calculated assuming the reference ellipsoid.

The official Earth Gravitational Model <a href= was developed and released to the public by the National Geospatial-Intelligence Agency (NGA).

Our EGM2008 API provides on-demand access to the EGM2008 model, as implemented by the open-source GeographicLib <a href= library.

API requests must contain a key "API-Key" in the header (see code samples). Obtain a key from .

Amentum Pty Ltd is not responsible nor liable for any loss or damage of any sort incurred as a result of using the API.

Copyright 2021.

Homepage: https://api.apis.guru/v2/specs/amentum.space:gravity/1.1.1.json
Provider: amentum.space:gravity / gravity
OpenAPI version: 3.0.0
Spec (JSON): https://api.apis.guru/v2/specs/amentum.space/gravity/1.1.1/openapi.json
Spec (YAML): https://api.apis.guru/v2/specs/amentum.space/gravity/1.1.1/openapi.yaml

Tools (4)

Extracted live via the executor SDK.

egm2008.appApiEgm2008EndpointsEgM2008CalculateAnomaly

for a given latitude / longitude.
egm2008.appApiEgm2008EndpointsEgM2008CalculateHeight

for a given latitude / longitude.
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