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Open AccessJournal ArticleDOI

A gravity-driven electric current in the Earth's ionosphere identified in CHAMP satellite magnetic measurements

TLDR
In this article, the authors present the first observational evidence for a gravity-driven current system in the Earth's low-latitude ionosphere, which is clearly visible in CHAMP satellite magnetic measurements.
Abstract
[1] A gravity field acting on a collisionless, magnetized space plasma causes electrons and ions to drift into opposite directions, in addition to gyrating around the magnetic field lines. This sets up an electric current which flows perpendicular to the gravity and magnetic fields in the eastward direction. Here we present the first observational evidence for such a gravity-driven current system in the Earth's low-latitude ionosphere. Its magnetic field signal, although 10,000 times smaller than the ambient Earth's magnetic field, is clearly visible in CHAMP satellite magnetic measurements. We find a current ribbon of more than 50 kA, about 66° wide in latitude, which moves with the sun northward in summer and southward in winter. Correcting magnetic measurements for this current's signature should lead to a better agreement between low-orbiting satellite and ground-based observations.

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Citations
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Journal ArticleDOI

Third generation of the Potsdam Magnetic Model of the Earth (POMME)

TL;DR: The Potsdam Magnetic Model of Earth (POMME) as discussed by the authors is a geomagnetic field model providing an estimate of the Earth's core, crustal, magnetospheric, and induced magnetic fields.
Journal ArticleDOI

The Magnetic Field of the Earth’s Lithosphere

TL;DR: In this paper, the authors review the difficulties encountered in measuring, extracting, interpreting and even defining the magnetic field of the Earth's lithosphere, and illustrate the lessons learned in measuring and processing Earth's magnetic field data may prove fruitful in planetary exploration.
Journal ArticleDOI

Fifth-generation lithospheric magnetic field model from CHAMP satellite measurements

TL;DR: In this paper, the authors describe the fifth-generation satellite-only magnetic field model MF5, which extends to spherical harmonic degree 100 and is particularly suited for inferring large-scale structure and composition of the lithosphere.
Journal ArticleDOI

Sources of low-latitude ionospheric E × B drifts and their variability

TL;DR: In this article, the authors examined the contribution of gravity and plasma pressure gradient driven current, the geomagnetic main field, and longitudinal variation in the conductivities to the vertical drift.
Book ChapterDOI

The Present Field

TL;DR: In this article, the authors introduce the various sources that contribute to the Earth's magnetic field as measured either from space or on ground and report on the progress that have been made, both in terms of methodology and success, in identifying and understanding the magnetic signal produced on a planetary scale by each type of source since 1999, when magnetic field measurements from space became available in a continuous manner.
References
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Journal ArticleDOI

International Reference Ionosphere 2000

Dieter Bilitza
- 01 Mar 2001 - 
TL;DR: The International Reference Ionosphere (IRI) is the international standard for the specification of ionospheric densities and temperatures as mentioned in this paper, which was developed and is being improved-updated by a joint working group of the International Union of Radio Science (URSI) and the Committee on Space Research (COSPAR).
Book

The earth's ionosphere

Journal ArticleDOI

CHAMP mission status

TL;DR: The German small satellite CHAMP is on the final track for launch on July 15, 2000 into a circular, near-polar and 460 km altitude orbit as discussed by the authors, with synergetic use for precise orbit determination, global gravity and magnetic field recovery, and GPS atmosphere and ionosphere profiling.
Journal ArticleDOI

Ionospheric Electrodynamics Using Magnetic Apex Coordinates.

TL;DR: In this paper, the equations of ionospheric electrodynamics are developed for a geomagnetic field of general configuration, with specific application to coordinate systems based on Magnetic Apex Coordinates.
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