NASA Confirms Existence of Earth’s Long-Sought Ambipolar Electric Field

A suborbital rocket ascends through the upper atmosphere against the backdrop of the Earth's curvature and the blackness of space.The Endurance mission launched from Svalbard to measure the faint electric field governing atmospheric escape.The Endurance mission launched from Svalbard to measure the faint electric field governing atmospheric escape.

NASA’s Endurance mission has confirmed the existence of the ambipolar electric field, a weak planet-wide force that drives atmospheric particles into space. This discovery solves a 60-year-old mystery regarding the “polar wind” and establishes the field as a fundamental component of Earth’s atmospheric dynamics.

TLDR: NASA scientists have measured Earth’s ambipolar electric field for the first time, confirming a theoretical force that lifts the atmosphere into space. Using a suborbital rocket launched from Norway, researchers detected a subtle voltage that counteracts gravity, explaining how particles escape the planet at the poles.

NASA scientists have successfully confirmed the existence of a planet-wide electric field that has remained a theoretical mystery for over sixty years. This discovery, achieved through the Endurance suborbital rocket mission, validates the presence of the “ambipolar field,” a weak but fundamental force that serves as a primary driver of atmospheric escape. With this confirmation, the ambipolar field joins gravity and magnetism as one of the core physical properties governing Earth’s environment and its interaction with space.

The quest to find this field began in the late 1960s when early satellite observations over Earth’s poles detected a phenomenon known as the “polar wind.” This was a steady stream of particles flowing out of the atmosphere into space at supersonic speeds. While some atmospheric loss is expected, the polar wind presented a paradox: the particles were “cold,” meaning they lacked the thermal energy required to reach such high velocities. Scientists hypothesized that an invisible electric field was providing the necessary acceleration, but the field was expected to be so faint that it would be nearly impossible to detect with the technology of the era.

The ambipolar field is generated at the subatomic level within the ionosphere. As ultraviolet radiation from the sun strikes atoms in the upper atmosphere, it strips away electrons, creating a plasma composed of negatively charged electrons and positively charged ions. Because electrons are incredibly light, they attempt to zip away into space. However, the much heavier ions are held back by Earth’s gravity. This creates a charge separation that generates an electric field. The field acts like a tether, pulling the ions upward while holding the electrons back, effectively “hitching” them together. This is why it is called “ambipolar”—it works in both directions to maintain the plasma’s neutrality.

To measure this elusive force, NASA launched the Endurance mission from Svalbard, Norway. This remote archipelago, located deep within the Arctic Circle, is the only place on Earth where the planet’s magnetic field lines are “open,” allowing the polar wind to flow directly into space rather than being trapped in a closed loop. On May 11, 2022, the rocket reached a peak altitude of 477 miles, carrying a suite of specialized instruments, including the Photoelectron Spectrometer. This device was designed to detect a voltage change across hundreds of miles that was previously beyond the reach of scientific sensors.

The data returned by Endurance revealed a potential change of only 0.55 volts across a 322-mile altitude range. While this is roughly the strength of a single watch battery, its impact on the atmosphere is profound. For hydrogen ions—the most abundant component of the polar wind—this field exerts an upward force ten times stronger than gravity, launching them into the magnetosphere. Even for heavier oxygen ions, the field provides a significant “lift,” increasing the “scale height” of the ionosphere. Without this field, the upper atmosphere would be significantly thinner; with it, the atmosphere remains 271% denser at high altitudes than it would be otherwise.

The discovery of the ambipolar field provides a more complete picture of how Earth’s atmosphere has evolved over billions of years. It acts as a “conveyor belt,” lifting the ionosphere and influencing how our planet interacts with the solar wind. This mechanism is likely a universal feature for any planet with an atmosphere, offering a new lens through which to study the evolution of Mars and Venus. By understanding the strength and fluctuations of this field, scientists can better predict which exoplanets might be capable of retaining their atmospheres and supporting life, marking a major milestone in our understanding of planetary habitability.

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