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South Pole

From left, graduate students Thomas Reilly and Hanxiao Wu with Weisen Shen. Wu and Shen are holding two of the 183 sensors they will place in the Antarctic. The team is shipping the sensors in the black container, which will travel through Port Hueneme, California and New Zealand before reaching the South Pole. Photo by Maeve McCarthy/ Angela Gruo

By Daniel Dunaief

While it’s easy to see and study materials in valleys or on the tops of bare mountains, it’s much more difficult to know what’s beneath 2.7 kilometers of ice. Turns out, that kind of question is much more than academic or hypothetical.

At the South Pole, glaciers sit on top of land that never sees the light of day, but that is relevant for the future of cities like Manhattan and Boston.

The solid land beneath glaciers has a strong effect on the movement of the ice sheet, which can impact the melting rate of the ice and sea level change.

Weisen Shen, Assistant Professor in the Department of Geosciences at Stony Brook University, recently received over $625,000 over the course of five years from the National Science Foundation to study the unexplored land beneath the East Antarctic Ice Sheet at the South Pole.

The subglacial water and hydrosystems, together with geology such as sediment or hard rocks, affect the dynamics and contribute to the movement speed of the ice sheet.

Once Shen provides a better understanding of the material beneath the ice, including glacial water, he can follow that up with other researchers to interpret the implications of ice sheet dynamics.

“We can predict better what’s the contribution of the Antarctic ice sheet to the sea level change” which will offer modelers a way to gauge the likely impact of global warming in future decades, he said.

Using seismic data

Starting this November, Shen and graduate students Siyuan Sui, Thomas Reilly and Hanxiao Wu will venture for two months to the South Pole with seismic monitors.

By placing 183 seismic nodes and installing an additional eight broad-band seismic stations, Shen and his team will quantify the seismic properties and, eventually, use them to infer the composition, density and temperature structure of the crust and the uppermost mantle.

The temperature when they place these monitors will be 10 to 30 degrees below 0 degrees Fahrenheit. They will need to do some digging as they deploy these sensors near the surface.

While the South Pole is believed to be geologically stable, signs of sub-glacial melting suggest the crust may bear a higher concentration of highly radioactive elements such as uranium, thorium and potassium.

Those natural elements “produce heat all the time,” said Shen. 

The process and analysis of seismic waves works in the same way it would for the study of a prism. Looking at the refraction of light that enters and leaves the prism from various angles can help researchers differentiate light with different frequencies, revealing clues about the structure and composition of the prism.

Earth materials, meanwhile will also cause a differentiation in the speed of surface waves according to their frequencies. The differentiation in speeds is called “dispersion,” which Shen and his team will use to quantify the seismic properties. The area has enough natural waves that Shen won’t need to generate any man-made energy waves.

“We are carefully monitoring how fast [the seismic energy] travels” to determine the temperature, density and rock type, Shen said.

The water beneath the glacier can act like a slip ’n slide, making it easier for the glacier to move.

Some large lakes in Antarctica, such as Lake Vostok, have been mapped. The depth and contours of sub glacier lakes near the South Pole, however, are still unclear.

“We have to utilize a lot of different methods to study that,” said Shen.

The Stony Brook researcher will collaborate with colleagues to combine his seismic results with other types of data, such as radar, to cross examine the sub ice structures.

The work will involve three years of gathering field data and two years of analysis.

Educational component

In addition to gathering and analyzing data, Shen has added a significant educational component to the study. For the first time, he is bringing along Brentwood High School science teacher Dr. Rebecca Grella, A PhD graduate from Stony Brook University’s Ecology and Evolutionary Biology program, Grella will provide lectures and classes remotely from the field.

In addition to bringing a high school teacher, Shen will fund graduate students at Stony Brook who can help Brentwood students prepare for the Earth Science regents exam.

Shen is working with Kamazima Lwiza, Associate Professor in the School of Marine and Atmospheric Sciences at Stony Brook, to bring Earth Science, including polar science, to schools in New York City and on Long Island with a bus equipped with mobile labs.

Lwiza, who is the Principal Investigator on the EarthBUS project, will work together with Shen to build a course module that includes a 45-minute lecture and exhibition.

Shen feels that the project will help him prepare to better educate students in graduate school, college, and K-12 in the community.

He feels a strong need to help K-12 students in particular with Earth Science.

As for students outside Brentwood, Shen said he has an open door policy in which the lab is receptive to high school and undergraduate students who would like to participate in his research all year long.

Once he collects the first batch of data from the upcoming trip to the South Pole, he will have to do considerable data processing, analysis and interpretation.

While Shen is looking forward to the upcoming field season, he knows he will miss time in his Stony Brook home with his wife Jiayi Xie, and his four-and-a-half year old son Luke and his 1.5 year old son Kai.

“It’s a huge burden for my wife,” Shen said, whose wife is working full time. When he returns, he “hopes to make it up to them.”

Shen believes, however, that the work he is doing is important in the bigger picture, including for his children.

Record high temperatures, which are occurring in the United States and elsewhere this summer, will “definitely have an impact on the dynamics of the ice sheet.” At the same time, the Antarctic ice sheet is at a record low.

“This is concerning and makes [it] more urgent to finish our work there,” he added.

The temperatures at the poles are heating up more rapidly than those at the equator. Pixabay photo

By Daniel Dunaief

On any given day, heat waves can bring record-breaking temperatures, while winter storms can include below average cold temperatures or snow.

Edmund Chang. Photo from SBU

Weather and climate experts don’t generally make too much of a single day or even a few days amid an otherwise normal trend. But, then, enough of these exceptional days over the course of years can skew models of the climate, which refers to average temperature and atmospheric conditions for a region.

If the climate is steady, “we should see approximately the same number of hot and cold records being broken,” said Edmund Chang, Professor at the School of Marine and Atmospheric Sciences at Stony Brook University. “Over the past few decades, we have seen many more hot records being broken than cold records, indicating the climate is getting hotter.”

Recent heat

Indeed, just last week, before a heatwave hit the northeastern United States, the United Kingdom reported the hottest day on record, with the temperature at Heathrow Airport reaching above 104 degrees.

Erinna Bowman, who grew up in Stony Brook and has lived in London since 2009, said the temperature felt “like a desert,” with hot, dry heat radiating up in the urban setting. Most homes in London don’t have air conditioning, although public spaces like supermarkets and retail stores do.

“I’m accustomed to the summer getting quite hot, so I was able to cope,” said Bowman. Indeed, London is usually considerably cooler during the summer, with average temperatures around 73 degrees.

Michael Jensen. Photo from BNL

News coverage of the two extraordinarily hot days in London “was very much framed in the context of a changing climate,” Bowman said. The discussion of a hotter temperature doesn’t typically use the words “climate change,” but, instead, describes the phenomenon as “global heating.”

For climate researchers in the area, the weather this summer has also presented unusual challenges.

Brookhaven National Laboratory meteorologist Michael Jensen spent four years planning for an extensive study of convective clouds in Houston, in a study called Tracking Aerosol Convection Interactions, or Tracer.

“Our expectation is that we would be overwhelmed” with data from storms produced in the city, he said. “That’s not what we’re experiencing.”

The weather, which has been “extremely hot and extremely dry,” has been more typical of late August or early September. “This makes us wonder what August is going to look like,” he said.

Jensen, however, is optimistic that his extensive preparation and numerous pieces of equipment to gather meteorological data will enable him to collect considerable information.

Warming at the poles

Broadly speaking, heat waves have extended for longer periods of time in part because the temperatures at the poles are heating up more rapidly than those at the equator. The temperature difference between the tropics and the poles causes a background flow from west to east that pushes storms along, Chang explained.

The North Pole, however, has been warming faster than the tropics. A paper by his research group showed that the lower temperature gradient led to a weakening of the storm track.

When summer Atlantic storms pass by, they provide relief from the heat and can induce more clouds that can lead to cooler temperatures. Weakening these storms can lead to fewer clouds and less cooler air to relieve the heat, Chang added.

Rising sea levels

Malcolm Bowman. Photo from SBU

Malcolm Bowman, who is Erinna Bowman’s father and is Distinguished Service Professor at the School of Marine and Atmospheric Sciences at Stony Brook University, believes the recent ice melting in Greenland, which has been about 10 degrees above normal, could lead to a rise in sea levels of about one inch this summer. “It will slowly return to near normal as the fresh water melt spreads slowly over all the world’s oceans,” he added.

Bowman, who has studied sea level rises and is working on mitigation plans for the New York area in the event of a future major storm, is concerned about the rest of the hurricane season after the level of warming in the oceans this summer. 

“Those hurricanes which follow a path over the ocean, especially following the Gulf Stream, will remain strong and may gather additional strength from the heat of the underlying water,” he explained in an email.

Bowman is the principal investigator on a project titled “Long Island South Shore Sea Gates Study.”

He is studying the potential benefit of six possible sea gates that would be located across inlets along Nassau and Suffolk County. He also suggests that south shore sand dunes would need to be built up to a height of 14 feet above normal high tide.

Meanwhile, the Army Corps of Engineers has come up with a tentatively selected plan for New York Harbor that it will release some time in the fall. Bowman anticipates the study will be controversial as the struggle between green and grey infrastructure — using natural processes to manage the water as opposed to sending it somewhere else — heats up.

As for the current heat waves, Bowman believes they are a consistent and validating extension of climate change.

Model simulations

In his lab, Chang has been looking at model simulations and is trying to understand what physical processes are involved. He is comparing these simulations with observations to determine the effectiveness of these projections.

To be sure, one of the many challenges of understanding the weather and climate is that numerous factors can influence specific conditions.

“Chaos in the atmosphere could give rise to large variations in weather” and to occasional extremes, Chang said. 

Before coming to any conclusions about longer term patterns or changes in climate, Chang said he and other climate modelers examine collections of models of the atmosphere to assess how likely specific conditions may occur due to chaos even without climate change.

“We have to rule out” climate variability to understand and appreciate the mechanisms involved in any short term changes in the weather, he added.

Still, Chang said he and other researchers are certain that high levels of summer heat will be a part of future climate patterns. 

“We are confident that the increase in temperature will result in more episodes of heat waves,” he said.

Penguins are among the few animals that live in the South Pole. Stock photo

By Elof Axel Carlson

Elof Axel Carlson

Life abounds from pole to pole and from the bottom of oceans to the peaks of Asian mountain tops. It does this by using the air, water and land to sustain life.

For most of the time on Earth life was confined to single-celled organisms, mostly bacteria. They take in water across a cell membrane. Most do not use oxygen from the air. Those that do came later, when some bacteria developed tools to use sunlight to combine carbon dioxide in the air with water to produce food (carbohydrates) and more abundant energy for the cell. They released oxygen and the atmosphere began to accumulate oxygen. 

Most forms of multicellular life use oxygen from the air to provide the energy to sustain their cellular life. Multicellularity permitted specialization of cells to form tissues, and the tissues then permitted organs to specialize in exchanging carbon dioxide (a waste product for animals) for oxygen.

The branching of limbs on trees is efficient to increase surfaced area for gaseous exchanges. So too are the branching of filaments in the gills of fish or the trachea of insects or the branching of the bronchi in our lungs.

When I see a tree, I see those organ systems reaching skyward with terminal leaves and an equally branched underground of roots, which are bringing in water and minerals from the land into which they are penetrated. The artist sees the beauty of the landscape. The mystic feels the awe of the complexity that seems beyond human comprehension. The scientist explores the structures and assigns functions as they emerge through the tools of science and experimentation.

It is as thrilling to me to see the cellular network of living tissues or organs under a microscope as it is to watch the changing scenery of life when driving from Indiana to New York, or taking walks in Amsterdam, Capetown, Samara, the Seychelles, the nature preserves in Kenya or the beaches of Baja Mexico.

I think of life through time as a fractal drawing with many repetitions creating new patterns. All of life requires a few basic activities. Life requires molecules to form membranes. It requires carbon-based compounds to produce the organelles that compose a cell.  All life (except viruses) is cellular. Life requires molecules that can store information to provide the molecules of life — proteins, nucleic acids, carbohydrates and lipids.

I think of the tools of the artist — a palette, brushes, tubes of oil paint, a canvas stretched on a frame, an easel to hold it. The artist can meticulously render a face, a still life or a landscape with the skills of many hundreds of hours of practice. 

Life also uses cellular tools to construct more complex membranes, organelles, chromosomes and vesicles to a symphony of functioning parts. Science enriches our understanding, opens new worlds of the very small and the very large that we do not normally see.  At most, a galaxy other than our own Milky Way is a mere dot in the sky, but close up it has 100 billion stars in it, most of them like our own sun. Our universe has billions of galaxies. 

As I type a page for an article or book, I am aware that I am coordinating the 37 trillion cells composing me. Human life mimics the universe in its immensity as our Earth now contains some 7 billion people. But this is humbled by the immensity of the astronomer’s universe or the biologist’s inventory of our own cells.    

Elof Axel Carlson is a distinguished teaching professor emeritus in the Department of Biochemistry and Cell Biology at Stony Brook University.