Earth gravitational field strength

May 24, 2015

1 August 2015 Unit 4.1: Mass

The geoid is a hypothetical Earth surface that represents the mean sea level in the absence of winds, currents, and most tides. The geoid is a useful reference surface. It defines the horizontal everywhere and gravity acts perpendicular to it. A carpenter’s level aligns itself along the geoid and a carpenter’s plumb bob points down the vertical or perpendicular to the geoid. Water will not flow in aqueducts if the pipes are perfectly aligned along the geoid. Surveyors use knowledge of the geoid and the horizontal when they lay out highways and boundaries.

Producing a precise model of the geoid has proven to be a challenge. Until recently, there was no single source for producing a geoid map. Data from several dozen satellites, along with surface measurements over land and from ships at sea, had to be combined to produce a model of the gravitational field. Traditionally, the models have done a fairly good job reproducing large-scale features of the gravity field, but have fallen short when it comes to reproducing finer-scale features or accurately describing time-variable gravity effects like those associated with the hydrologic cycle.

GRACE provides, for the first time, global coverage of the Earth’s gravity field every 30 days from a single source. GRACE is already able to measure the gravity field with a level of precision that is at least 100 times greater than any existing measurement, and continued improvements are expected as the mission progresses. The finer details of the geoid that have evaded scientists for so long are on the verge of being revealed. GRACE also gives us our best opportunity to date to study time-variable gravity effects. As the mission progresses and more data are added to the model, the resolution of the geoid will improve even further.

These “gravity anomaly” maps show where models of the Earth’s gravity field based on GRACE data differ from a simplified mathematical model that assumes the Earth is perfectly smooth and featureless. Areas colored yellow, orange, or red are areas where the actual gravity field is larger than the featureless-Earth model predicts—such as the Himalayan Mountains in Central Asia (top left of the left-hand globe)—while the progressively darker shades of blue indicate places where the gravity field is less—such as the area around Hudson Bay in Canada (top center of right-hand globe).

As the geoid map becomes more detailed, the accuracy of satellite altimetry, synthetic aperture radar interferometry, and digital terrain models covering large land and ice areas — all used in remote sensing applications and cartography — will improve. These techniques provide critical input to many scientific models used in oceanography, hydrology, geology, and related disciplines, and will be used for a variety of applications including:

  • measuring the changing mass of polar ice caps;
  • measuring changes in water resources on land
  • understanding shallow and deep ocean current transport;
  • understanding sea level change resulting from ocean temperature and water mass changes;
  • understanding atmosphere-ocean mass exchange;
  • understanding the forces that generate Earth’s geomagnetic field; and
  • understanding internal Earth forces that move tectonic plates and result in earthquakes and volcanic eruptions.

This enhanced knowledge should lead to a better understanding of the forces that drive El Niño and La Niña, more accurate seasonal forecasts of Earth’s weather patterns, an ability to track the changing distribution of water resources in critically important land aquifers, and improved forecasting of natural hazards.

next: The Workings of GRACE
back: Gravity 101

The Earth’s gravity signal changes day-to-day, even minute by minute. The image above shows how the average variability in Earth’s gravity field in August 2002 compared to the yearly average of 2001. The red and pink areas show where the variation measured in August 2002 is the most different from the variation measured for the year 2001, while the blue and purple areas show where the variation measured in August 2002 is just about the same as the variation measured for the year 2001. The variability has to be accounted for using models in order to produce a mean gravity field that is useful for hydrologic applications. (Image credit: Paul Thompson / UT-CSR)

Gravitational Field Notes
Gravitational Field Notes
A Level Physics - Gravitational Field Strength
A Level Physics - Gravitational Field Strength
Gravitational Field Strength
Gravitational Field Strength

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