Icepicks (9/22/22)

Good afternoon, and happy Thursday! Welcome to Parallax #3. Whether you’re just joining us or you’re a Day 1 sign-up, it’s great to have you here.

On Monday, Jupiter will reach the point in its orbit when it’s closest to Earth. This happens every 13 months or so, but this time around, the gas giant will draw closer to Earth than it’s been in 59 years, offering savvy stargazers a good chance to see its rings and its biggest moons.

If you snap any good photos of the king of planets this weekend, send ‘em my way!

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Seeing Through the Glare

Each year, seawater in the Arctic freezes, melts, and re-freezes with the changing of the seasons. And each year, brave researchers trek out into the cold to stick poles into the snow and float buoys on the sea to measure just how thick that ice is.

Why not just measure the ice thickness with satellites?

In-situ vs. on-orbit

To be sure, a few satellites do provide radar data over the polar regions. In the winter, when the ice and snow are dry and frozen solid, these satellites can record accurate readings of the ice. But in the summer, when the snow melts and forms pools of water on top of the ice, the satellites are blinded by the brilliant reflection off the water. That means they can only gather accurate data for about half the year.

A study published last week in Nature addresses how researchers could fill in the gaps in Arctic ice thickness data and make it trackable via satellite throughout the year.

The researchers used data from ESA’s CryoSat-2, a science mission that records data with synthetic aperture radar (SAR) and an altimeter, to develop a machine learning model to accurately measure the thickness of Arctic sea ice year-round.

“These beautiful ponds of meltwater that sit on top of the ice surface look amazing, but it's difficult for our radars to properly measure that,” Jack Landy, lead author of the paper, told Parallax. “Basically, these ponds provide a really strong blinding response to the radar.”

Why measure the ice?

Reasonable minds—and ML models—disagree on the variance of Arctic ice change over the course of the next century. That delta, in part, is due to the lack of high-quality summer data.

Better summer data would help to improve those models, giving climate researchers a better understanding of climate change’s effects at the Earth’s outer edges.

“Now that we've produced this dataset, there's a chance to actually calibrate the models against a better or more comprehensive dataset,” Landy said. “And maybe we can narrow down some of these projections for how the ice is going to change in the next decades.”

When it comes to seasonal forecasting, there are commercial applications for accurate sea thickness measurements, Landy said. One example: Shipping companies want to steer vessels through the Arctic regions, so they’re very interested in accurate ice thickness forecasting.

A kink in the data

The CryoSat-2 satellite’s SAR sensor sends a microwave signal down to the Earth, which reflects off the target area and back up to the satellite.

“As that radar pulse comes down from our CryoSat-2 satellite and hits cold, snow-covered ice, it tends to scatter and reflect the energy in many directions,” said Landy. “When it hits the ocean, the ocean acts like a bit of a mirror to it, and it just reflects all of that energy straight back to the satellite.”

The ponds of meltwater dazzle the satellite in the same way the ocean does, keeping CryoSat-2 from distinguishing between the two.

Building the algorithm: Landy and his team have been working for years to figure out how to fill in these yearly gaps in the data. They began by combing through CryoSat-2 data since 2011 and classifying images of water based on whether they depicted the ocean or ponds on top of ice. Using these images, the team trained an algorithm to spot the differences between meltwater ponds and the ocean.

The algorithm also pulls in information from related datasets, including data about the roughness of the ice and thickness of the snow on top, to produce its estimates of ice thickness.

Up next...Right now, the program that the researchers developed takes several months to produce data. This is in part because of the many layers of data cleaning and the slow analysis of auxiliary data needed for the algorithm to come up with an accurate measurement. The next step for the team, Landy said, is to find ways to cut down on that lead time.

There’s also the issue of CryoSat-2 itself. The mission is already on borrowed time, and operating about eight years past its nominal lifetime. The ESA mission is currently the only satellite equipped with both the radar and altimeter instruments needed for the program to work. Other satellites tend to use one or the other. A follow-on mission, ESA’s CRISTAL—short for Copernicus Polar Ice and Snow Topography Altimeter—is scheduled to launch in 2027.

Keep on chugging, CryoSat-2!

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Other News from the Cosmos

• Unistellar and the SETI institute launched a citizen science program for identifying exoplanets (i.e., planets orbiting stars outside our solar system).

• DART, or the Double Asteroid Redirection Test, is scheduled to slam into the asteroid Dimorphos on Monday at 7:14pm ET. And yes, NASA will be livestreaming the climax of the Earth defense mission.

• MIRI, the instrument aboard JWST that surveys the mid-infrared, has an issue with its medium-resolution spectroscopy (MRS) mode. Teams have paused MRS observations and the instrument’s other three modes are working fine.

• Earth’s crust has built up in fits and starts over billions of years. A new study suggests that the crust has grown faster each time Earth has passed through one of the spiral arms of the Milky Way.

• Astronomers identified the closest black hole we’ve found yet, 1,570 light years away, by observing a Sun-like star that appeared to be orbiting nothing.

• The Navy denied a two-year-old FOIA request for videos of UAP + UFOs, on the grounds that releasing them into the wild would “harm national security.”

• Mars InSight detected sound and seismic vibrations from four meteoroid strikes on the Red Planet for the first time.

The View from Space

I audibly gasped at this JWST image of Neptune when it was released yesterday. Here, you can clearly see the planet’s elusive rings. And that bluish flare above the planet isn’t a star—it’s the moon Triton, which reflects 70% of the light that hits it.