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Americans Moving From Colder Climes Face New Weather Extremes: 100 Degree Temps and Drought – The Wall Street Journal

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SU(N) matter is about 3 billion times colder than deep space

An artist’s conception of the complex magnetic correlations physicists have observed with a groundbreaking quantum simulator at Kyoto University that uses ytterbium atoms about 3 billion times colder than deep space. Different colors represent the six possible spin states of each atom. The simulator uses up to 300,000 atoms, allowing physicists to directly observe how particles interact in quantum magnets whose complexity is beyond the reach of even the most powerful supercomputer. Credit: Ella Maru Studio/ K. Hazzard/Rice University

Japanese and U.S. physicists have used atoms about 3 billion times colder than interstellar space to open a portal to an unexplored realm of quantum magnetism.

“Unless an alien civilization is doing experiments like these right now, anytime this experiment is running at Kyoto University it is making the coldest fermions in the universe,” said Rice University’s Kaden Hazzard, corresponding theory author of a study published today in Nature Physics. “Fermions are not rare particles. They include things like electrons and are one of two types of particles that all matter is made of.”

A Kyoto team led by study author Yoshiro Takahashi used lasers to cool its fermions, atoms of ytterbium, within about one-billionth of a degree of absolute zero, the unattainable temperature where all motion stops. That’s about 3 billion times colder than interstellar space, which is still warmed by the afterglow from the Big Bang.

“The payoff of getting this cold is that the physics really changes,” Hazzard said. “The physics starts to become more quantum mechanical, and it lets you see new phenomena.”

Atoms are subject to the laws of quantum dynamics just like electrons and photons, but their quantum behaviors only become evident when they are cooled within a fraction of a degree of absolute zero. Physicists have used laser cooling to study the quantum properties of ultracold atoms for more than a quarter century. Lasers are used to both cool the atoms and restrict their movements to optical lattices, 1D, 2D or 3D channels of light that can serve as quantum simulators capable of solving complex problems beyond the reach of conventional computers.

Takahashi’s lab used optical lattices to simulate a Hubbard model, an oft-used quantum model created in 1963 by theoretical physicist John Hubbard. Physicists use Hubbard models to investigate the magnetic and superconducting behavior of materials, especially those where interactions between electrons produce collective behavior, somewhat like the collective interactions of cheering sports fans who perform “the wave” in crowded stadiums.

“The thermometer they use in Kyoto is one of the important things provided by our theory,” said Hazzard, associate professor of physics and astronomy and a member of the Rice Quantum Initiative. “Comparing their measurements to our calculations, we can determine the temperature. The record-setting temperature is achieved thanks to fun new physics that has to do with the very high symmetry of the system.”

An artist’s conception of the complex magnetic correlations physicists have observed with a groundbreaking quantum simulator at Kyoto University that uses ytterbium atoms about 3 billion times colder than deep space. Different colors represent the six possible spin states of each atom. The simulator uses up to 300,000 atoms, allowing physicists to directly observe how particles interact in quantum magnets whose complexity is beyond the reach of even the most powerful supercomputer. Credit: Ella Maru Studio/ K. Hazzard/Rice University

The Hubbard model simulated in Kyoto has special symmetry known as SU(N), where SU stands for special unitary group—a mathematical way of describing the symmetry—and N denotes the possible spin states of particles in the model. The greater the value of N, the greater the model’s symmetry and the complexity of magnetic behaviors it describes. Ytterbium atoms have six possible spin states, and the Kyoto simulator is the first to reveal magnetic correlations in an SU(6) Hubbard model, which are impossible to calculate on a computer.

“That’s the real reason to do this experiment,” Hazzard said. “Because we’re dying to know the physics of this SU(N) Hubbard model.”

Study co-author Eduardo Ibarra-García-Padilla, a graduate student in Hazzard’s research group, said the Hubbard model aims to capture the minimal ingredients to understand why solid materials become metals, insulators, magnets or superconductors.

“One of the fascinating questions that experiments can explore is the role of symmetry,” Ibarra-García-Padilla said. “To have the capability to engineer it in a laboratory is extraordinary. If we can understand this, it may guide us to making real materials with new, desired properties.”

Takahashi’s team showed it could trap up to 300,000 atoms in its 3D lattice. Hazzard said accurately calculating the behavior of even a dozen particles in an SU(6) Hubbard model is beyond the reach of the most powerful supercomputers. The Kyoto experiments offer physicists a chance to learn how these complex quantum systems operate by watching them in action.

The results are a major step in this direction, and include the first observations of particle coordination in an SU(6) Hubbard model, Hazzard said.

“Right now this coordination is short-ranged, but as the particles are cooled even further, subtler and more exotic phases of matter can appear,” he said. “One of the interesting things about some of these exotic phases is that they are not ordered in an obvious pattern, and they are also not random. There are correlations, but if you look at two atoms and ask, ‘Are they correlated?’ you won’t see them. They are much more subtle. You can’t look at two or three or even 100 atoms. You kind of have to look at the whole system.”

Physicists don’t yet have tools capable of measuring such behavior in the Kyoto experiment. But Hazzard said work is already underway to create the tools, and the Kyoto team’s success will spur those efforts.

“These systems are pretty exotic and special, but the hope is that by studying and understanding them, we can identify the key ingredients that need to be there in real materials,” he said.


Physicists harness electrons to make ‘synthetic dimensions’


More information:
Shintaro Taie, Observation of antiferromagnetic correlations in an ultracold SU(N) Hubbard model, Nature Physics (2022). DOI: 10.1038/s41567-022-01725-6. www.nature.com/articles/s41567-022-01725-6
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Which is colder: The North or South Pole?

The North Pole and South Pole are the coldest places on Earth. However, as similar as these areas might seem, one is far icier than the other.

So, which pole is colder?

Both the North Pole and South Pole are cold because their positions at the top and bottom of the planet mean they do not get any direct light (opens in new tab) from the sun. At both places, the sun always rests low on the horizon, even in the middle of their summers. During their winters, the sun lies so far below the horizon, it does not come up for months at a time.

In addition, the white surfaces of the ice and snow at the poles are highly reflective. This means that most of the energy from the sunlight that reaches them bounces back into space, keeping the air above those surfaces relatively cool.

Related: Why aren’t there polar bears in Antarctica?

Although these factors make both poles downright chilly, the South Pole remains significantly colder than the North Pole, according to the Woods Hole Oceanographic Institution (opens in new tab). The annual average temperature at the North Pole is minus 40 degrees Fahrenheit (minus 40 degrees Celsius) in winter and 32 F (0 C) in summer. In contrast, the South Pole’s averages are far frostier, with an annual average temperature of minus 76 F (minus 60 C) in winter and minus 18 F (minus 28.2 C) in summer.

Arctic vs. Antarctic

The main reason the South Pole is colder than the North Pole lies in the key difference between them. “The North Pole is an ocean and the South Pole is a continent,” Robin Bell, a polar scientist at Columbia University’s Lamont-Doherty Earth Observatory in New York, told Live Science.

The Arctic is an ocean surrounded by land. The Antarctic is land surrounded by ocean. Water cools and warms more slowly than land, resulting in fewer extremes of temperature. Even when the Arctic Ocean is covered with ice, the relatively warm temperature of its waters has a moderating effect on the climate there, helping the Arctic stay warmer than the Antarctic.

In addition, whereas the Arctic lies at sea level, Antarctica is the highest continent, with an average elevation of about 7,500 feet (2,300 meters). The higher one goes, the colder it gets.

Which pole has more ice?

Notice how the South Pole is on a continent, while the North Pole is located in an ocean. (Image credit: dikobraziy via Getty Images)

At both the North and South Poles, the ice cover varies over the course of the year, growing in the long, dark winters and melting in the bright, increasingly hot summers. 

Most of this variation in ice cover at both the North and South Poles is due to sea ice that floats, grows and melts over the ocean. Since the Arctic is almost completely surrounded by land, the sea ice that forms there is not as mobile as the sea ice in the Antarctic. As such, Arctic sea ice floes are more likely to converge, typically making Arctic sea ice thicker at about 6 to 9 feet (2 to 3 m) thick compared with Antarctic sea ice, which is about 3 to 6 feet (1 to 2 m) thick, according to the National Snow & Ice Data Center (opens in new tab) (NSIDC).

On average, Arctic sea ice reaches a minimum extent of about 2.5 million square miles (6.5 million square km) and a maximum extent of 6 million square miles (15.6 million square km), the NSIDC (opens in new tab) said. In comparison, on average, Antarctic sea ice has a smaller minimum extent of 1.2 million square miles (3.1 million square km) and a larger maximum extent of 7.2 million square miles (18.8 million square km).

Related: What is the coldest city in the world?

Still, on average, there is no doubt the South Pole possesses more total ice than the North Pole. This is because the South Pole is home to land ice in addition to its sea ice — the ice sheet on Antarctica is up to 3 miles (4.8 km) thick and covers about 5.3 million square miles (13.7 million square km), about the area of the contiguous United States and Mexico (opens in new tab) combined, according to the National Science Foundation (opens in new tab). All in all, Antarctica holds about 90% of all the world’s ice.

“The volume and mass of ice on the land changes little in the summer as a fraction of the amount in winter because the volume and mass are so large,” said Cecilia Bitz, a polar climate scientist at the University of Washington in Seattle.

Investigations into the amount of ice at the poles have revealed that both the thickness and extent of Arctic summer sea ice have dramatically declined over the past 30 years (opens in new tab). This is consistent with observations of a warming Arctic.

“Arctic and Greenland ice is decreasing rapidly primarily because of global warming,” Bitz told Live Science “And decreasing Arctic sea ice area tends to cause even more warming, amplifying the warming that starts the ice loss.” 

In contrast, “sea ice loss around Antarctica and glacial land ice loss on Antarctica have had mixed changes, ups and downs, over the last 40 years when we’ve had reasonably good records,” Bitz noted. “Antarctic climate dynamics are more complicated because air and ocean circulation are very important factors there.”

Originally published on Live Science.

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Updated D.C.-area forecast: Winter weather advisory tonight for colder areas north and west

The precipitation is likely to come in the form of rain but in colder areas of Montgomery (northern and western) and Loudoun counties and to the north and west, temperatures may settle around freezing allowing for a light glaze of ice. Untreated roads and walkways could become slick.

By sunrise Friday, the precipitation will have moved off and temperatures should quickly rise above freezing.

A somewhat subjective rating of the day’s weather, on a scale of 0 to 10.

2/10: Our fling with spring is now ending. Nearing freezing but no snow accumulating adds a sting.

  • Today: Light rain and sleet develop. Highs: 36-40
  • Tonight: Light rain, except freezing rain in our colder areas. Lows: 32-38
  • Tomorrow: Light rain ends midday, winds become gusty. Highs: 51-55

This is weather whiplash! After a day in the 70s, the 30s today are a painful reminder it is still February. Moisture is meager but should produce light rain today into tomorrow morning with some sleet and freezing rain in the mix, especially in our colder areas. The weekend is dry but cool.

Today (Thursday): Clouds quickly increase with rain developing during the morning. Some areas, especially north and northwest of the District, could see sleet in the mix at times, and even some snowflakes toward northern Maryland. Temperatures are parked in the mid-to-upper 30s all day amid light winds from the north. Precipitation may pause at times during the afternoon and amounts are generally light. Confidence: Medium-High

Tonight: Light rain showers pick back up again mid-evening and continue through the night with mainly calm winds. In our colder areas north and northwest of the Beltway, a little freezing rain can’t be ruled out which could lightly glaze untreated surfaces. Lows are in the mid-30s except near freezing in a few of those colder spots. Confidence: High

Follow us on Facebook, Twitter, and Instagram for the latest weather updates. Keep reading for the forecast through the weekend…

Tomorrow (Friday): Light rain showers linger through much of the morning with most areas to end up with around 0.5 inches of rain from the system. Skies clear in the afternoon as west winds gust up to 30 mph. As the rain lifts north, milder air sneaks in for the afternoon with highs in the low-to-mid 50s. Confidence: Medium-High

Tomorrow night: Gusty northwest winds linger well into the night with temperatures dropping rapidly. Overnight lows fall to mid-to-upper 20s under starry skies. Confidence: High

Saturday is partly sunny and chilly as a shower system passes far to our south. Highs only manage to reach low-to-mid 40s. Lows again fall to the mid-to-upper 20s thanks to clear skies and calm winds. Confidence: High

Predawn risers Sunday look to the east horizon for a Venus/Mars/crescent moon trio. Sunshine dominates and a band of snow passing through New England actually helps to pull a little warmer air into our area. Highs are mainly in the lower 50s. Overnight is still chilly with lows yet again in the mid-to-upper 20s. Confidence: Medium-High

Canadian air sneaks back in on Monday holding highs in the upper 30s to lower 40s. At least the sun shines brightly. Confidence: Medium-High

A daily assessment of the potential for at least 1 inch of snow in the next week, on a 0-10 scale.

1/10 (→): A few snowflakes could be in wintry mix in our northern areas Thursday but even a coating is unlikely. Then, after Friday, moisture is lacking.



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