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The clouds form when summertime wisps of water vapor waft up and crystallize around specks of meteor smoke.

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This means observers on the ground could begin to see them not long after AIM does.

Here is what a well-developed display of NLCs looks like, photographed on August 5, 2017, by Catalin Tapardel in Alberta, Canada: Early-season NLCs are usually faint and always found in high latitude places such as Canada, the British isles, Siberia and Scandinavia.

Now, however, the solar cycle is swinging toward Solar Minimum, allowing cosmic rays to return.

Another reason could be the weakening of Earth's magnetic field, which helps protect us from deep-space radiation.

High-latitude sky watchers should be alert for auroras, especially in the southern hemisphere where autumn darkness favors visibility. NASA's Aeronomy of Ice in the Mesosphere (AIM) spacecraft has spotted its first noctilucent clouds (NLCs) of the 2018 season.

They are the electric-blue puffs circled in this image of the Arctic taken by AIM's CIPS instrument on May 27th: "The summer season for noctilucent clouds has begun," says Cora Randall, AIM science team member at the University of Colorado.

We've been working to streamline our data reduction, allowing us to post results from balloon flights much more rapidly, and we have developed a new data product, shown here: This plot displays radiation measurements not only in the stratosphere, but also at aviation altitudes. For instance, we see that boarding a plane that flies at 25,000 feet exposes passengers to dose rates ~10x higher than sea level. These measurements are made by our usual cosmic ray payload as it passes through aviation altitudes en route to the stratosphere over California. Approximately once a week, and the students of Earth to Sky Calculus fly space weather balloons to the stratosphere over California.

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