Enjoying EarthSky? Subscribe.

102,440 subscribers and counting ...

EarthSky // Earth, Science Wire Release Date: Jun 10, 2013

Noctilucent – or night-shining – cloud season starts early in 2013

Night-shining clouds appear early in northern summer, when water molecules are wafted up from the lower atmosphere to mix with “meteor smoke.”

Every summer, something strange and wonderful happens high above the North Pole. Ice crystals begin to cling to the smoky remains of meteors, forming electric-blue clouds with tendrils that ripple hypnotically against the sunset sky. Noctilucent clouds — aka night-shining clouds – are a delight for high-latitude sky watchers, and around the Arctic Circle their season of visibility is always eagerly anticipated.

News flash: This year, night-shining clouds are getting an early start. NASA’s AIM spacecraft, which is orbiting Earth on a mission to study noctilucent clouds, started seeing them on May 13.

“The 2013 season is remarkable because it started in the northern hemisphere a week earlier than any other season that AIM has observed,” reports Cora Randall of the Laboratory for Atmospheric and Space Physics at the University of Colorado. “This is quite possibly earlier than ever before.”

A new ScienceCast video explores the early start of the 2013 season for notilucent clouds.

The early start is extra-puzzling because of the solar cycle. Researchers have long known that noctilucent clouds tend to peak during solar minimum and bottom-out during solar maximum — a fairly strong anti-correlation. “If anything, we would have expected a later start this year because the solar cycle is near its maximum,” Randall says. “So much for expectations.”

For sky watchers, this means it’s time to pay attention to the sunset sky, where noctilucent are most often seen. An early start could herald brighter clouds and wider visibility than ever before.

Noctilucent clouds were first noticed in the mid-19th century after the eruption of super-volcano Krakatoa. Volcanic ash spread through the atmosphere, painting vivid sunsets that mesmerized observers all around the world. That was when the noctilucent clouds appeared. At first people thought they must be some side-effect of the volcano, but long after Krakatoa’s ash settled the noctilucent clouds remained.
“They’ve been with us ever since,” says Randall. “Not only that, they are spreading.”

noctilucent-clouds-solway-firth

Noctilucent clouds over the Solway Firth on May 31, 2013 thanks to EarthSky Facebook friend Adrian Strand.

When AIM was launched in 2007, the underlying cause of noctilucent, or night-shining, clouds was still unknown. Researchers knew they formed 83 kilometers above Earth’s surface where the atmosphere meets the vacuum of space – but that’s about all. AIM quickly filled in the gaps.

“It turns out that meteoroids play an important role in the formation of NLCs,” explains Hampton University Professor James Russell, the principal investigator of AIM. “Specks of debris from disintegrating meteors act as nucleating points where water molecules can gather and crystallize.”

The diagram below shows why noctilucent clouds – which are also sometimes called NLCs – are best seen at sunset or sunrise.

Illustration via NASA

Illustration via NASA

Noctilucent appear during northern summer because that is when water molecules are wafted up from the lower atmosphere to mix with the “meteor smoke.” That is also the time when the upper atmosphere is ironically coldest.

Back in the 19th century, noctilucent clouds were confined to high latitudes. You had to go to Alaska or Scandinavia to see them. In recent years, however, they have been sighted as far south as Utah, Colorado, and Nebraska. Some researchers believe that the spread of these clouds is a sign of climate change.

One of the greenhouse gases that has become more abundant in Earth’s atmosphere since the 19th century is methane. “When methane makes its way into the upper atmosphere, it is oxidized by a complex series of reactions to form water vapor,” says Russell. “This extra water vapor is then available to grow ice crystals for noctilucent clouds.”

The early start of the 2013 season appears to be caused by a change in atmospheric “teleconnections.”

“Half-a-world away from where the northern NLCs are forming, strong winds in the southern stratosphere are altering global circulation patterns,” explains Randall. “This year more water vapor is being pushed into the high atmosphere where noctilucent clouds love to form, and the air there is getting colder.”

“All of this has come as an interesting surprise for us,” notes Russell. “When we launched AIM, our interest was in the clouds themselves. But now NLCs are teaching us about connections between different layers of the atmosphere that operate over great distances. Our ability to study these connections will surely lead to new understanding about how our atmosphere works.”

Bottom line: Noctilucent clouds season – which typically begins in June – began in mid-May this year.

Via NASA

Noctilucent cloud season is here!