Ancient Tree Rings Reveal Unprecedented Solar Storm 14,300 Years Ago, Dwarfing Carrington Event

The Carrington Event served as a stark wake-up call during a period of rapid industrialization. In September 1859, a colossal solar eruption caused widespread havoc by disrupting global telegraph systems and causing fires. Although no similar event has occurred since, evidence from ancient tree rings indicates the potential for even more powerful solar storms than the Carrington Event.

Ancient Tree Rings Reveal Unprecedented Solar Storm 14,300 Years Ago, Dwarfing Carrington Event
Ancient Tree Rings Reveal Unprecedented Solar Storm 14,300 Years Ago, Dwarfing Carrington Event Pixabay/AstroGraphix

Largest Ever Solar Storm

Around 14,300 years ago, a remarkable solar storm occurred, predating the existence of today's technological grids. Such events, surpassing the Carrington Event in magnitude, occasionally appear in the fossil record, with this one being the most potent ever identified.

Solar storms, or geomagnetic storms, occur when the Sun emits intense flares or coronal mass ejections. If these eruptions are directed toward Earth, a substantial influx of charged particles impacts our magnetosphere. While such events usually result in relatively mild effects, they can produce striking auroras and disrupt specific satellite and radio communications bands.

During exceptionally powerful and thankfully infrequent solar storms, disturbances in Earth's electromagnetic field can generate currents that affect power grids.

Solar storms also influence radioactive carbon-14, continuously descending onto Earth's surface as cosmic particles interact with atmospheric elements. Scientists employ carbon-14 decay to determine the age of organisms like trees and animals, enabling them to identify historical solar eruptions hidden in the annual rings of ancient trees.

Researchers identified the 14,300-year-old solar storm by examining subfossilized trees along the Drouzet River's eroded banks in the Southern French Alps. Subfossils are not yet fully fossilized specimens.

By analyzing slices of these trees, scientists detected a prominent radiocarbon spike around 14,300 years ago. Additional records from this period were found in Greenland ice cores, which exhibited higher concentrations of a beryllium isotope associated with radiation storms.

Miyake Events: Powerful Geomagnetic Events Greater Than the Carrington Event

Over the past 15,000 years, researchers have pinpointed nine formidable solar storms, referred to as Miyake Events, with the most recent instances noted in 993 AD and 774 AD. The recently unveiled solar storm from 14,300 years ago stands as the most massive ever observed, measuring roughly twice the magnitude of the previously verified occurrences.

Miyake Events, marked by severe geomagnetic storms, continue to elude full comprehension, as they have never been directly observed through instruments.

These occurrences highlight significant gaps in our knowledge regarding the Sun's conduct and its potential threats to Earth. The origins, occurrence frequency, and predictability of such intense solar storms remain shrouded in uncertainty.

Radiocarbon measurements derived from tree rings, complemented by beryllium data from polar ice cores, provide the most effective means to delve into the Sun's historical patterns. This is because direct instrumental monitoring of solar activity only commenced in the 17th century with the observation of sunspots.

Despite contemporary tools such as ground-based observatories, space probes, and satellites, these brief records prove insufficient for a comprehensive grasp of the Sun's behavior across extended timeframes.

The Carrington Event in 1859 caused notable disruptions on Earth, including telegraph system failures and a bright aurora at night, which even led birds to sing, mistaking it for sunrise.

In contrast, Miyake Events, including the recently uncovered 14,300-year-old storm, would have been considerably more massive, highlighting the importance of radiocarbon analysis for understanding Earth's history and predicting and managing risks associated with solar activity.


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