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Scientists use X-rays to remotely measure magnetic reconnection in near-Earth space

Using x-rays as a new diagnostic tool for monitoring space weather
This image depicts the X-ray emission intensity distribution (keyed in colors) calculated by the proposed model and Earth's magnetic field (lines). The sphere in the center of the figure represents the Earth, and the left-hand side of the figure is the sun side. Credit: Dr. Yosuke Matsumoto from Chiba University, Japan

The magnetosphere, formed by Earth's magnetic field, acts as a protective shield that deflects solar wind鈥攖he flow of charged particles constantly streaming from the sun toward our planet. This magnetic barrier protects our atmosphere and the technology we increasingly depend on in near-Earth space, such as communication satellites.

However, the magnetosphere isn't impenetrable, as a fundamental process called "" can temporarily strip this barrier during intense and cause violent energy fluctuations in near-Earth space. As human activity in this region increases, understanding and forecasting such space weather becomes critical.

A key to understanding these breaches lies in measuring what's known as the " rate," which quantifies energy efficiency in magnetic reconnection processes. For decades, scientists have attempted to measure this rate using various methods, including spacecraft flying directly through reconnection zones and observations of solar flares by remote imaging.

However, these traditional approaches provide only local snapshots of the magnetic reconnection process or are limited by specific, often unsteady conditions. Obtaining a comprehensive and consistent picture that bridges the gap between local and global reconnection rates remains a challenge.

Against this backdrop, a research team led by Associate Professor Yosuke Matsumoto from the Institute for Advanced Academic Research at Chiba University, Japan, is testing an innovative approach using soft X-ray imaging to measure the reconnection rates. The study, co-authored by Mr. Ryota Momose from Chiba University and Prof. Yoshizumi Miyoshi from Nagoya University, was made available online on June 23, 2025, and was published in Volume 52, Issue 12 of the journal on June 28, 2025.

Soft X-ray emission occurs through a charge exchange process between the heavy ions in the solar wind and the hydrogen neutral atoms originating from Earth. In this study, the researchers propose leveraging the soft X-rays that are naturally emitted when solar wind particles interact with the boundaries of the magnetosphere to remotely measure reconnection rates across much larger regions than previously possible.

The team conducted on the Fugaku supercomputer, combining high-resolution global magnetohydrodynamic simulations of Earth's magnetosphere with a model of soft X-ray emission. From the simulations, they analyzed how reconnection-related X-rays can be viewed from a satellite positioned at a lunar distance during intense solar wind conditions. This vantage point roughly matches that of an upcoming X-ray imaging satellite like GEO-X, which is scheduled for launch in the near future.

After analyzing the , the researchers found that the brightest X-ray emissions form distinct cusp-shaped patterns that directly reflect the magnetic field structure around reconnection zones. By measuring the opening angle of these bright regions, they calculated the global reconnection rate to have a value of 0.13, which closely matches theoretical predictions and previous laboratory measurements.

Therefore, the results demonstrate that the geometry of bright X-ray features correlates with the reconnection rate, offering a new method to estimate this important parameter. "Imaging X-rays from the sun-facing magnetospheric boundary can now potentially quantify solar wind energy inflow into the magnetosphere, making X-rays a novel space weather diagnostic tool," highlights Dr. Matsumoto.

By providing a new way to measure and understand magnetic reconnection, this research contributes directly to improving space weather forecasting. Being able to predict how solar activity influences the near-Earth space is vital for protecting astronauts and ensuring the reliability of communication systems and space missions, especially in the face of potentially devastating events like magnetic storms.

Notably, this study also has broader scientific implications for understanding magnetic reconnection in other contexts, as Dr. Matsumoto explains, "Magnetic reconnection is not only responsible for breaching Earth's magnetic shield but is also the underlying process behind explosive events in plasma devices, the sun, and black holes. Understanding this process is essential for advancing technologies like plasma confinement in fusion reactors and investigating the origin of high-energy cosmic rays."

As humanity prepares for an era of space exploration and commercial space activities, this newly proposed method could pave the way to accurate space weather predictions, helping ensure the safety and success of our ventures beyond Earth's atmosphere.

More information: Ryota Momose et al, Estimation of Reconnection Rate From Soft X鈥怰ay Emission at the Earth's Dayside Magnetopause, Geophysical Research Letters (2025).

Journal information: Geophysical Research Letters

Provided by Chiba University

Citation: Scientists use X-rays to remotely measure magnetic reconnection in near-Earth space (2025, July 22) retrieved 24 July 2025 from /news/2025-07-scientists-rays-remotely-magnetic-reconnection.html
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