Every year, for a period of between five to 10 days, the night skies over Antarctica and the Arctic Circle are visited by an unusual phenomenon known as noctilucent clouds (NLCs) or polar mesospheric clouds (PMCs). Residing at an altitude between 47 to 53 miles, these electric-blue clouds are the highest in Earth’s atmosphere and can only be observed well after the sun has dipped below the horizon at twilight.
In July 2018, NASA launched a balloon from Sweden across the Arctic towards Canada to observe the clouds. The balloon captured 6 million high-resolution images over the course of five days. The video above is the first look at this footage.
“This is the first time we’ve been able to visualize the flow of energy from larger gravity waves to smaller flow instabilities and turbulence in the upper atmosphere,” said Dave Fritts, principal investigator of the PMC Turbo mission at Global Atmospheric Technologies and Sciences in Boulder, Colorado, in a NASA press release. “At these altitudes you can literally see the gravity waves breaking — like ocean waves on the beach — and cascading to turbulence.”
According to NASA, night clouds are a relatively new phenomenon, with the first observations occurring a couple years after the eruption of Krakatoa sent tons of volcanic ash high into the atmosphere. They increased again after the Tunguska meteor event over Siberia in 1908. In 2007, NASA launched the AIM satellite (Aeronomy of Ice in the Mesosphere) to specifically study noctilucent clouds and discover the conditions that favor their formation.
“AIM and other research has shown that in order for the clouds to form, three things are needed: very cold temperatures, water vapor and meteoric dust,” James Russell, an atmospheric and planetary scientist at Hampton University, said in a NASA article. “The meteoric dust provides sites that the water vapor can cling to until the cold temperatures cause water ice to form.”
The Krakatoa event, says Thomas, likely “seeded” the upper atmosphere with dust, allowing noctilucent clouds to be seen over more populated areas. In its most recent observations, however, NASA is reporting that the blue cloud formations are not only starting earlier than normal, but also once again spreading beyond the polar regions.
Noctilucent clouds can only be observed well after the sun has dipped below the horizon. (Photo: Juhku/Shutterstock)
Researchers believe the beautiful twilight displays, observed as far south as Colorado and Utah, could be due to an increased abundance of methane in the upper atmosphere.
“When methane makes its way into the upper atmosphere, it is oxidized by a complex series of reactions to form water vapor,” Russell added. “This extra water vapor is then available to grow ice crystals for NLCs.”
Because methane is roughly 30 times more potent a heat-trapping greenhouse gas compared to carbon dioxide, its theorized that noctilucent clouds could potentially serve as a kind of “canary in a coal mine” on climate change. For now, however, the connection remains tenuous.
“I think the jury is still out,” SpaceWeather.com’s Tony Phillips told the SFGate in 2015. “But it is undeniable that increasing levels of methane favor the formation of NLCs at very high altitudes.”
Editor’s note: This article has been updated since it was originally published in December 2016.
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