Yearly Archives: 2021

Results from a study of clouds and aerosols conducted in the Azores revealed that new particles can seed the formation of clouds in the marine boundary layer—the atmosphere up to about a kilometer above Earth's surface—even over the open ocean, where the concentration of precursor gases was expected to be low. Image courtesy of the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) user facility.

Understanding previously undocumented source of new particle formation will improve models of aerosols, clouds, and their impact on Earth’s climate

New results from an atmospheric study over the Eastern North Atlantic reveal that tiny aerosol particles that seed the formation of clouds can form out of next to nothingness over the open ocean. This “new particle formation” occurs when sunlight reacts with molecules of trace gases in the marine boundary layer, the atmosphere within about the first kilometer above Earth’s surface. The findings, published in the journal Nature Communications, will improve how aerosols and clouds are represented in models that describe Earth’s climate so scientists can understand how the particles—and the processes that control them—might have affected the planet’s past and present, and make better predictions about the future.

“When we say ‘new particle formation,’ we’re talking about individual gas molecules, sometimes just a few atoms in size, reacting with sunlight,” said study co-author Chongai Kuang, a member of the Environmental and Climate Sciences Department at the U.S. Department of Energy’s Brookhaven National Laboratory. “It’s interesting to think about how something of that scale can have such an impact on our climate—on how much energy gets reflected or trapped in our atmosphere,” he said.

Using an aircraft outfitted with 55 atmospheric instrument systems, scientists traversed horizontal tracks above and through clouds and spiraled down through atmospheric layers to provide detailed measurements of aerosols and cloud properties. The aircraft data were supplemented by measurements made by ground-based radars and other instruments. Image courtesy of the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) user facility.

But modeling the details of how aerosol particles form and grow, and how water molecules condense on them to become cloud droplets and clouds, while taking into consideration how different aerosol properties (e.g., their size, number, and spatial distribution) affect those processes is extremely complex—especially if you don’t know where all the aerosols are coming from. So a team of scientists from Brookhaven and collaborators in atmospheric research around the world set out to collect data in a relatively pristine ocean environment. In that setting, they expected the concentration of trace gases to be low and the formation of clouds to be particularly sensitive to aerosol properties—an ideal “laboratory” for disentangling the complex interactions.

“This was an experiment that really leveraged broad and collaborative expertise at Brookhaven in aerosol observations and cloud observations,” Kuang said. Three of the lead researchers—lead authors Guangjie Zheng and Yang Wang, and Jian Wang, principal investigator of the Aerosol and Cloud Experiments in the Eastern North Atlantic [https://www.arm.gov/publications/backgrounders/docs/doe-sc-arm-16-020.pdf] (ACE-ENA) campaign—began their involvement with the project while working at Brookhaven and have remained close collaborators with the Lab since moving to Washington University in St. Louis in 2018.

Land and sea

Brookhaven Lab atmospheric scientist Chongai Kuang (center) with Art Sedlacek (left) and Stephen Springston (right) aboard ARM’s Gulfstream-159 (G-1) aircraft during a 2010 atmospheric sampling mission that was not part of this study. Image courtesy of the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) user facility.

The study made use of a long-term ground-based sampling station on Graciosa Island in the Azores (an archipelago 850 miles west of continental Portugal) and a Gulfstream-1 aircraft outfitted with 55 atmospheric instrument systems to take measurements at different altitudes over the island and out at sea. Both the ground station and aircraft belong to the DOE Office of Science’s Atmospheric Radiation Measurement (ARM) user facility [https://www.arm.gov/], managed and operated by a consortium of nine DOE national laboratories.

The team flew the aircraft on “porpoise flights,” ascending and descending through the boundary layer to get vertical profiles of the particles and precursor gas molecules present at different altitudes. And they coordinated these flights with measurements taken from the ground station.

The scientists hadn’t expected new particle formation to be happening in the boundary layer in this environment because they expected the concentration of the critical precursor trace gases would be too low.

“But there were particles that we measured at the surface that were larger than newly formed particles, and we just didn’t know where they came from,” Kuang said.

The aircraft measurements gave them their answer.

Many of the choreographed flight paths for this study traversed the open ocean and also crossed within the ranges of the ground-based scanning radars at DOE’s Atmospheric Radiation Measurement (ARM) Climate Research Facility on Graciosa Island in the Azores. Image courtesy of the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) user facility.

“This aircraft had very specific flight patterns during the measurement campaign,” Kuang said. “They saw evidence that new particle formation was happening aloft—not at the surface but in the upper boundary layer.” The evidence included a combination of elevated concentrations of small particles, low concentrations of pre-existing aerosol surface area, and clear signs that reactive trace gases such as dimethyl sulfide were being transported vertically—along with atmospheric conditions favorable for those gases to react with sunlight.

“Then, once these aerosol particles form, they attract additional gas molecules, which condense and cause the particles to grow to around 80-90 nanometers in diameter. These larger particles then get transported downward—and that’s what we’re measuring at the surface,” Kuang said.

“The surface measurements plus the aircraft measurements give us a really good spatial sense of the aerosol processes that are happening,” he noted.

At a certain size, the particles grow large enough to attract water vapor, which condenses to form cloud droplets, and eventually clouds.

Both the individual aerosol particles suspended in the atmosphere and the clouds they ultimately form can reflect and/or absorb sunlight and affect Earth’s temperature, Kuang explained.

Study implications

Framed by a brilliant rainbow, ARM’s Gulfstream-159 (G-1) research aircraft sits on the tarmac on Terceira Island during the Aerosol and Cloud Experiments in the Eastern North Atlantic (ACE-ENA) winter 2018 intensive operation period in the Azores. Image courtesy of the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) user facility.

So now that the scientists know new aerosol particles are forming over the open ocean, what can they do with that information?

“We’ll take this knowledge of what is happening and make sure this process is captured in simulations of Earth’s climate system,” Kuang said.

Another important question: “If this is such a clean environment, then where are all these precursor gases coming from?” Kuang asked. “There are some important precursor gases generated by biological activity in the ocean (e.g., dimethyl sulfide) that may also lead to new particle formation. That can be a nice follow-on study to this one—exploring those sources.”

Understanding the fate of biogenic gases such as dimethyl sulfide, which is a very important source of sulfur in the atmosphere, is key to improving scientists’ ability to predict how changes in ocean productivity will affect aerosol formation and, by extension, climate.

The research was funded by the DOE Office of Science, DOE’s Atmospheric System Research, and by NASA. In addition to the researchers from Brookhaven Lab and Washington University, the collaboration included scientists from Pacific Northwest National Laboratory; Missouri University of Science and Technology; the University of Washington, Seattle; NASA Langley Research Center; Science Systems and Applications Inc. in Hampton, Virginia; the Max Planck Institute for Chemistry in Mainz, Germany; and the Scripps Institution of Oceanography, University of California, San Diego.

Brookhaven National Laboratory is supported by the Office of Science of the U.S. Department of Energy.  The Office of Science is the single largest supporter of basic research in the physical sciences in the United States, and is working to address some of the most pressing challenges of our time.  For more information, please visit science.energy.gov [https://www.energy.gov/science/office-science].

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This home is a magnificent 5 bedroom, 5 bath colonial with separate in-law suite.
The amazing master suite has a full bath and sitting area, and there are 2 additional bedrooms with a full bath. Additional features include a cathedral ceiling den with fireplace, an open floor plan, and a huge new kitchen with high end appliances. The dining area has sliding doors to the country club back yard, with pool and gazebo. The beautiful basement is half-finished,
with outside entrance. Too much to list, and a must-see. $814,777
 
For more information click here

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This beautifully maintained 3 bedroom, 2 bath ranch has an open floor plan, a master with en suite, and hardwood floors throughout. The large living room opens to the dining room, and the cozy family room/den has a vaulted ceiling and stone fireplace. The updated kitchen, and eating area with French doors opens to a spacious deck, leading to the backyard in-ground pool.

The home, at 18 Merlin Lane, has a full basement with crawl space and finished area, with utility room washer and dryer, as well as an attached garage with pull down ladder for attic space.

Three Village SD#1

$519,999

For more information click here

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From left to right; Edna Louise Spears Elementary School Students Clara Pearce, Kemp Garrett and Nina Gnatenko. Photo from PJSD

Fifth grade students in Port Jefferson’s Edna Louise Spear Elementary School have been learning the engineering design process. They have used their skills to construct pompom launchers with a set number of simple objects including straws, popsicle sticks, tape, string and plastic cups to see how far their experiments could go.

As engineers, they examined the materials they could use, came up with their designs and moved on to building, testing, modifying and testing again. 

The students in Kari Costanzo’s class conducted an informal contest to see who developed the simplest and cheapest one (Nina Gnatenko), the sturdiest one (Kemp Garrett) and the one that went the farthest (Clara Pearce). 

Photo by Pixabay

By Michael Christodoulou

Michael Christodoulou
Michael Christodoulou

During the COVID-19 pandemic, many of us have been forced to work from home. But once we’ve moved past the virus, many workers may continue working from home. More than one-third of companies with employees who started working from home now think that remote work will stay more common post-pandemic, according to a Harvard Business School study. This shift to at-home work can affect people’s lives in many ways – and it may end up providing workers with some long-term financial advantages.

If you’re one of those who will continue working remotely, either full time or at least a few days a week, how might you benefit? Here are a few possibilities:

  • Reduced transportation costs – Over time, you can spend a lot of money commuting to and from work. The average commuter spends $2,000 to $5,000 per year on transportation costs, including gas, car maintenance, public transportation and other expenses, depending on where they live, according to the U.S. Bureau of Economic Analysis and the U.S. Census Bureau. If you are going to work primarily from home, you should be able to greatly reduce these costs.
  • Potentially lower car insurance premiums – Your auto insurance premiums are partially based on how many miles you drive each year. So, if you were to significantly reduce these miles by working from home, you might qualify for lower rates.
  • Lower expenditures on lunches – If you typically eat lunch in restaurants or get takeout while at work, you could easily be spending $50 or more per week – even more if you regularly get coffee drinks to go. By these figures, you could end up spending around $3,000 a year. Think how much you could reduce this bill by eating lunch at home during your remote workday.
  • Lower clothing costs – Despite the rise in “casual dress” days, plenty of workers still need to maintain appropriate office attire. By working from home, you can “dress down,” reducing your clothing costs and dry-cleaning bills.

As you can see, it may be possible for you to save quite a bit of money by working from home. How can you use your savings to help meet your long-term financial goals, such as achieving a comfortable retirement?

For one thing, you could boost your investments. Let’s suppose that you can save $2,500 each year by working remotely. If you were to invest this amount in a tax-deferred account, such as an IRA or your 401(k) or similar employer-sponsored plan and earned a hypothetical 6% annual return for 20 years, you’d accumulate more than $97,000 – and if you kept going for an additional 10 years, you’d have nearly $210,000. You’d eventually pay taxes on the amount you withdrew from these accounts (and withdrawals prior to age 59½ may be subject to a 10% IRS penalty), but you’d still end up pretty far ahead of where you’d be otherwise.)

You also might use part of your savings generated by remote work to help build an emergency fund containing a few months’ worth of living expenses. Without this fund, you might be forced to dip into your retirement accounts to pay for something like a major home repair.

Becoming an at-home worker will no doubt require some adjustments on your part – but, in strictly financial terms, it could lead to some positive results.

This article was written by Edward Jones for use by Michael Christodoulou, ChFC®,AAMS®,CRPC®,CRPS® of the Stony Brook Edward Jones.

Edward Jones, Member SIPC

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Students in Michelle Landetta's class. Photo from PJSD

It’s no wonder Port Jefferson Middle School students have been treating one another with more empathy, compassion and acceptance.

Students in Michelle Landetta’s class read R. J. Palacio’s bestselling book “Wonder” together, discussed its theme and steps they can take to promote kindness to others. Students and staff decorated and wrote inspirational quotes, positive affirmations and words of hope on the popsicle sticks that were provided to them.

They then created a “PJMS – We Stick Together” bulletin board right in a hallway of the school for all to not only admire their creative work, but to share in their refreshing ideas and promote everyone’s appreciation for the simple and joyful act of friendship. 

Photo from PJSD

Accelerator physicist Chuyu Liu, the run coordinator for this year's experiments at the Relativistic Heavy Ion Collider (RHIC), in the Main Control Room of the collider-accelerator complex at Brookhaven National Laboratory.

Final stage of Beam Energy Scan II will collect low-energy collision data needed to understand the transition of ordinary nuclear matter into a soup of free quarks and gluons

Accelerator physicists are preparing the Relativistic Heavy Ion Collider (RHIC), a DOE Office of Science user facility for nuclear physics research at DOE’s Brookhaven National Laboratory, for its 21st year of experiments, set to begin on or about February 3. Instead of producing high-energy particle smashups, the goal for this run is to maximize collision rates at the lowest energy ever achieved at RHIC.

STAR co-spokesperson Lijuan Ruan noted that this year’s run is the third and final leg of Beam Energy Scan II, a systematic study of RHIC collisions at low energies.

“Run 21 is the final step of Beam Energy Scan II (BES-II), a three-year systematic study of what happens when gold ions—gold atoms stripped of their electrons—collide at various low energies,” said Brookhaven physicist Lijuan Ruan, co-spokesperson for RHIC’s STAR experiment collaboration.

Nuclear physicists will examine the BES-II data, along with data from RHIC’s high-energy collisions, to map out how these collisions transform ordinary protons and neutrons into an extraordinary soup of free quarks and gluons—a substance that mimics what the early universe was like some 14 billion years ago. By turning the collision energy down, RHIC physicists can change the temperature and other variables to study how these conditions affect the transition from ordinary matter to early-universe hot quark-and-gluon soup.

“Out of the five energies of BES-II—9.8, 7.3, 5.75, 4.6, and 3.85 billion electron volts, or GeV—this year’s run at 3.85 GeV is the most difficult one,” said Brookhaven Lab accelerator physicist Chuyu Liu, the run coordinator. That’s because “RHIC’s beams of gold ions are really difficult to hold together at the lowest energy,” he explained.

In Run 21, the accelerator team will use a variety of innovative components and schemes to maintain the lifetime and intensity of the colliding ion beams under challenging conditions. Read on to learn more about RHIC’s Run 21 science goals and the accelerator features that will make the science possible.

Scanning the transition

Mapping nuclear phase changes is like studying how water changes under different conditions of temperature and pressure (net baryon density for nuclear matter). RHIC’s collisions “melt” protons and neutrons to create quark-gluon plasma (QGP). STAR physicists are exploring collisions at different energies, turning the “knobs” of temperature and baryon density, to look for signs of a “critical point.” That’s a set of conditions where the type of transition between ordinary nuclear matter and QGP changes from a smooth crossover observed at RHIC’s highest energies (gradual melting) to an abrupt “first order” phase change that’s more like water boiling in a pot.

As Ruan explained, the quest to map out the phases of nuclear matter and the transitions between them is somewhat similar to studying how water molecules transform from solid ice to liquid water and gaseous steam at different temperatures and pressures. But nuclear matter is trickier to study.

“We need a powerful particle collider and sophisticated detector systems to create and study the most extreme forms of nuclear matter,” she said. “Thanks to the incredible versatility of RHIC, we can use the ‘knob’ of collision energy and the intricate particle-tracking capabilities of the STAR detector to conduct this systematic study.”

RHIC’s highest collision energies (up to 200 GeV) produce temperatures more than 250,000 times hotter than the center of the Sun. Those collisions “melt” the protons and neutrons that make up gold atoms’ nuclei, creating an exotic phase of nuclear matter called a quark-gluon plasma (QGP). In QGP, quarks and gluons are “free” from their ordinary confinement within protons and neutrons, and they flow with virtually no resistance—like a nearly perfect liquid.

But QGP lasts a mere fraction of a second before “freezing out” to form new particles. RHIC physicists piece together details of how the melting and refreezing happen by taking “snapshots” of the particles that stream out of these collisions.

By systematically lowering the collision energy, the physicists are looking for signs of a so-called “critical point.” This would be a set of conditions where the type of transition between ordinary nuclear matter and QGP changes from the smooth crossover observed at RHIC’s highest energies (picture butter melting gradually on a counter), to an abrupt “first order” phase change (think of how water boils suddenly at a certain temperature and holds that temperature until all the molecules evaporate).

As physicists turn RHIC’s collision energy down, they expect to see large event-by-event fluctuations in certain measurements—similar to the turbulence an airplane experiences when entering a bank of clouds—as conditions approach a “critical point” in the nuclear phase transition. This year’s run at the lowest collision energy will contribute to this search.

“Theorists have predicted that certain key measurements at RHIC will exhibit dramatic event-by-event fluctuations when we approach this critical point,” Ruan said.

Some RHIC physicists liken these fluctuations to the turbulence an airplane experiences when it moves from smooth air into a bank of clouds and then back out again. Measurements from phase I of RHIC’s Beam Energy Scan (BES-I, with data collected between 2010 and 2017) revealed tantalizing hints of such turbulence. But because collisions are hard to achieve at low energies, the data from BES-I aren’t strong enough to draw definitive conclusions.

Now, in BES-II, a host of accelerator improvements have been implemented to maximize low-energy collision rates.

Cooling the ions

One of the innovations that Chuyu Liu and the other Collider-Accelerator Department (C-AD) physicists managing RHIC operations will take advantage of in Run 21 is a first-of-its-kind beam-cooling system. This Low Energy RHIC electron Cooling  (LEReC) system operated at full capacity for the first time in last year’s RHIC run, making it the world’s first implementation of electron cooling in a collider. But it will be even more important for the lowest-of-low collision energies this year.

“The longer the beam stays at low energy, the more ‘intra-beam scattering’ and ‘space charge’ effects degrade the beam quality, reducing the number of circulating ions,” said Liu. Simplistic translation: The positively charged ions tend to repel one another. (Remember: The ions are atoms of gold stripped of their electrons, leaving a lot of net positive charge from the 79 protons in the nucleus.) The scattering and the repulsive space charge cause the ions to spread out, essentially heating up the beam as it makes its way around the 2.4-mile-circumference RHIC accelerator. And spread-out ions are less likely to collide.

A host of accelerator improvements have been implemented to maximize RHIC’s low-energy collision rates. These include a series of components that inject a stream of cool electron bunches into the ion beams in these cooling sections of the two RHIC rings. The cool electrons extract heat to counteract the tendency of RHIC’s ions to spread out, thereby maximizing the chances the ions will collide when the beams cross at the center of RHIC’s STAR detector.

“The LEReC system operates somewhat similar to the way the liquid running through your home refrigerator extracts heat to keep your food cool,” said Wolfram Fischer, Associate Chair for Accelerators in C-AD, “but the technology needed to achieve this beam cooling is quite a bit more complicated.”

A series of components (special lasers and a photocathode gun) produces bunches of relatively cool electrons, which are accelerated to match the bunching and near-light-speed pace of RHIC’s ions. Transfer lines inject the cool electrons into the stream of ion bunches—first in one RHIC ring, then, after making a 180-degree turn, into the other. As the particles mix, the electrons extract heat, effectively squeezing the spread-out ion bunches back together. The warmed-up electron bunches then get dumped and replaced with a new cool batch.

“To add more flexibility for cooling optimization during this year’s run at RHIC’s lowest energy, where the space-charge effects and beam lifetime degradation are concerns for both the electrons and the ions, we installed a new ‘second harmonic’ radiofrequency (RF) cavity in the electron accelerator,” said Alexei Fedotov, the accelerator physicist who led the LEReC project.

These cavities generate the radio waves that push the electrons along their path, with the higher (second harmonic) frequency helping to flatten out the longitudinal profile of the electron bunches. “This should help to reduce the space charge effect in the electron beams to achieve better cooling performance at low energy,” Fedotov said.

“We plan to commission the new electron beam transport line in late January and start cooling ions with the new electron beam setup in early February,” he added.

More accelerator advances

Similarly, third-harmonic RF cavities installed in the ion accelerator rings will help to flatten the longitudinal profile of the ion bunches, reducing their peak intensity and space charges, Liu explained. “With that, more bunch intensity can be injected into RHIC to produce higher luminosity—a measure closely tied to collision rates,” he said.

The accelerator team will also be commissioning a new bunch-by-bunch feedback system to help stabilize the beam for a better lifetime. “This system measures how each ion bunch deviates from the center of the beam pipe, and then applies a proportional correction signal through a component called a kicker to nudge each bunch back to where it should be,” Liu said.

All this cooling and nudging will counteract the ions’ tendency to spread, which maximizes chances of collisions happening when the two beams cross at the center of STAR.

“This run will bring together many of the advances we’ve been working on at RHIC to meet the challenging conditions of low-energy collisions,” said Fischer. “STAR would have preferred to test the lowest energy first, but we needed to learn everything possible (and develop the electron cooling system) before we could embark on operation at the most difficult energy.”

RHIC operations are funded by the DOE Office of Science.

Brookhaven National Laboratory is supported by the U.S. Department of Energy’s Office of Science. The Office of Science is the single largest supporter of basic research in the physical sciences in the United States and is working to address some of the most pressing challenges of our time. For more information, visit https://www.energy.gov/science/ [https://www.energy.gov/science/].

Ric Statler

All Souls Church Rectory, 5 Mill Pond Road, Stony Brook hosts a Native American Drumming Meditation on Jan. 28 from 7 to 8:45 p.m. Led by elder drummer, Ric Statler, drumming meditation seeks to integrate the physical, mental, emotional, and spiritual parts of the human self, creating a state of well-being. Free. Call 631-655-7798 for further information.

Centereach’s girls fencing team opened their season on the right foot with a 16-11 victory over the Huntington Blue Devils at home Jan. 23.

Huntington head coach Michelle O’Brien said her team was still shy two of her fencers lacking the mandatory six practices but hopes to be at full strength soon.

“These young women have done their best at their meets so far, and although they fell short today, their spirits are high, and I am impressed with their competitiveness,” O’Brien said, adding that junior Abby Simpson notched her first win of the season.

Huntington is back out on the strip Jan. 26 where they travel to Commack for a 4:30 p.m. start. Centereach is back in action at home Jan. 27 where they host Walt Whitman at 6:30 p.m.

Sharon Gatz-Philbrick, Christian Neubert and Erika Gronenthal are striving to help their neighbors in need. Photo by Ottilie Philbrick

By Courtney Rehfeldt

When three residents of Port Jefferson saw COVID-19 presenting a financial impact on community members, they decided to come together and form Hometown Hope Port Jefferson. 

Launched by Sharon Gatz-Philbrick, Erika Gronenthal and Christian Neubert, the trio works to assist those in need while bringing the community together during a difficult time.  

“At the peak of the pandemic, businesses and schools closed, leaving families struggling to make ends meet,” Gatz-Philbrick said. “Families faced much uncertainty as bills piled up, and paychecks didn’t come. There was a struggle to put food on the table, and grocery shelves were bare. The list of worries seemed endless and the need for support and hope became apparent.”

Remembering the kindness she personally experienced from Port Jefferson locals, Gatz-Philbrick wanted to return the favor. 

“In the midst of a challenging time, residents from the village did so many amazing things for my children and me,” she said. “I wanted to create an organization that continued these amazing acts of kindness. Alone we can do so little, and together we can do so much more.”

Besides providing a helping hand, Hometown Hope has connected local volunteers and businesses in a joint effort. 

“Port Jefferson village is a small town,” Neubert said. “In a place where everyone knows your name, we wanted to allow neighbors to help neighbors. One small act of kindness can lead to an entire town of encouraging acts of goodness and positive change.”

Hometown Hope provided Thanksgiving meal boxes and collected gift donations for the holidays, teaming up with Torte Jeff Pie Co. and other local businesses to fulfill their mission. Mather Hospital has provided donations, and the group has gotten support from Infant Jesus food kitchen and Rima Potter Designs.

“There comes a time in all our lives where we need assistance, it is a humbling moment, and we are hoping to pay it forward in our community,” Gatz-Philbrick said. “A little bit of kindness goes a long way. We don’t always see who is hurting or why, but we want to be there for them if they need extra help or assistance. We believe having a strong support structure is perhaps one of the most important steps to healing.”

In addition to collecting monetary or specific item donations, Hometown Hope Port Jefferson is also looking for volunteers to donate their time to help collect and distribute items as well as assist with future initiatives in the new year. 

People who live in the Port Jefferson Village who need to apply for help can be nominated through the organization’s website, or can contact the group through social media. The organization can be found on Facebook by searching Hometown Hope Port Jefferson. or online at hometownhopepj.org.