OREGON STATE UNIVERSITY

college of earth

New study finds charred forests increase snowmelt rate

CORVALLIS, Ore. – When a major wildfire destroys a large forested area in the seasonal snow zone, snow tends to accumulate at a greater level in the burned area than in adjacent forests. But a new study found that the snowpack melts much quicker in these charred areas, potentially changing the seasonal runoff pattern of rivers and streams.

The study by Oregon State University researchers, which was funded by the National Science Foundation, documented a 40 percent reduction of albedo – or reflectivity – of snow in the burned forest during snowmelt, and a 60 percent increase in solar radiation reaching the snow surface.

The reason, the researchers say, is that fires burn away the forest canopy and later, the charred tree snags shed burned particles onto the snow, lowering its reflectivity and causing it to absorb more solar radiation.

Results of the study were published this week in the journal Geophysical Research Letters.

“As the snow accumulates in the winter, you don’t see much of a difference in albedo between a healthy, unburned forest and a charred forest,” said Kelly Gleason, an OSU doctoral student in geography and lead author on the study. “But when the snow begins to melt in the spring, large amounts of charred debris are left behind, darkening the snow to a surprising extent.”

In the study site, at an elevation of nearly 5,000 feet in the Oregon High Cascades near the headwaters of the McKenzie River, the researchers founded that the snowpack in the charred forest disappeared 23 days earlier and had twice the “ablation” or melting rate than an adjacent unburned forest in the same watershed.

Anne Nolin, who is Gleason’s major professor and a co-author on the study, said the researchers have not yet examined the hydrological effect of this earlier melting, but “logic suggests that it would contribute to what already is a problem under climate change – earlier seasonal runoff of winter snow.”

“The impact of these charred particles is significant,” said Nolin, a professor in OSU’s College of Earth, Ocean, and Atmospheric Sciences. “They are really dark – much darker than the needles, lichens and other naturally occurring materials that fall in a healthy, unburned forest.

“We know that the shedding of the charred particles lasts at least two years – and it might extend as long as eight to 10 years before the trees fall,” she added.  “It has a major impact on snowmelt that hasn’t fully been appreciated.”

The problem may be compounded in the future as climate change is expected to significantly increase the occurrence of wildfires in the western United States – and perhaps beyond.

“Most of the precipitation in the mountains of the western U.S. falls as snow and the accumulated snowpack acts as kind of a winter reservoir, holding back water until summer when the highest demand for it occurs,” Gleason pointed out. “Our findings could help resource managers better anticipate the availability of water in areas that have been affected by severe forest fires.”

Such areas are increasingly plentiful, according to Nolin. The OSU researchers conducted a spatial analysis of major forest fires from 2000 to 2012 and found that more than 80 percent of those fires in the western U.S. were in the seasonal snow zone, and were on average 4.4 times larger than fires outside the seasonal snow zone. Nearly half of those major fires were within the Columbia River basin, especially in Idaho and the northern Rockey Mountains.

Other areas are affected as well, including the southern Oregon/northern California mountain regions, and the high country of Arizona and New Mexico. The amount of burned area since 2000 that the OSU researchers examined in their spatial analysis of where forest fires occurred in the seasonal snow zone was roughly the size of Ohio.

“It’s a bit of a paradox,” Nolin said. “Other studies have shown that when you remove the dark forest canopy and expose the snow, the area gets brighter and acts as a negative forcing on atmospheric temperatures, slowing climate change. But hydrologically, the effect is the opposite – the increased solar radiation and decreased snow albedo causes much earlier snowmelt, potentially amplifying the effects of climate change.

“What does it mean for your water supply when headwater catchments burn, the snow melts faster and the spring runoff begins even earlier?” she added. “It is a provocative question for resource managers.”

Media Contact: 
Source: 

Kelly Gleason, gleasoke@science.oregonstate.edu

 

Anne Nolin, 541-737-8051 (cell phone: 541-740-6804); nolina@geo.oregonstate.edu

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The charred forest

 

Aftermath of fire

 

Burned debris

 

Charred bark

Researchers going public on quest to identify plankton species

NEWPORT, Ore. – Researchers using an innovative underwater imaging system have taken millions of photos of plankton ranging from tiny zooplankton to small jellyfish – and now they are seeking help from the public to identify the species.

The “Plankton Portal” project is a partnership between the University of Miami, Oregon State University and Zooniverse.org to engage volunteers in an online citizen science effort.

“One of the goals of the project is discovery,” said Robert Cowen, new director of OSU’s Hatfield Marine Science Center in Newport, Ore., who led the project to capture the images while at Miami’s Rosenstiel School of Marine and Atmospheric Sciences. “Computers can take pictures and even analyze images, but it takes humans to identify relationships to other organisms and recognize their behavior.

“Computers don’t really care about context – whether something is up or down in the water column and what else might be in the neighborhood,” he added. “People can do that. And we hope to have thousands of them look at the images.”

Interested persons may sign up for the project at www.planktonportal.org, which goes online this week (the official launch is Sept. 17).

Zooniverse.org is a popular citizen science website that engages millions of participants to study everything from far-away stars, to whale sounds, to cancer cells – and aid scientists with their observations. It works by training volunteers and validating their credibility by how often their observations are accurate.

“It is an increasingly popular pursuit for people interested in science and nature – from high school students to senior citizens,” said Jessica Luo, a University of Miami doctoral student working with Cowen.

“Each image is looked at by multiple users and identification is done by a weighting system,” said Luo, who is now working at OSU’s Hatfield center. “The system not only looks for consensus, but rapidity of conclusion. It works amazingly well and the data from this project will help us better begin to explore the thousands of species in the planktonic world.”

With funding from the National Science Foundation’s Directorate for Geosciences and the National Oceanic and Atmospheric Administration, Cowen developed the “In Situ Ichthyoplankton Imaging System,” or ISIIS, while at Miami – along with Cedric Guigand of UM and Charles Cousin of Bellamare, LLC.

ISIIS combines shadowgraph imaging with a high-resolution line-scan camera to record plankton at 17 images per second. Cowen and his colleagues have used the system to study larval fish, crustaceans and jellyfish in diverse marine systems, including the Gulf of Mexico, the mid-Atlantic Ocean, the California coast, and the Mediterranean Sea.

At the same time ISIIS is capturing images, he says, other instruments are recording oceanographic conditions, including temperature, salinity, dissolved oxygen and other measurements. These data, coupled with the images, are available to the public via Zooniverse.org.

“In three days, we can collect data that would take us more than three years to analyze,” Cowen said, “which is why we need the help of the public. With the volume ISIIS generates, it is impossible for a handful of scientists to classify every image by hand, which is why we are exploring different options for image analysis – from automatic image recognition software to crowd-sourcing to citizen scientists.”

Luo said the researchers hope to secure future funding to study plankton – which includes a variety of crustaceans and jellyfish in the water column – off the Pacific Northwest coast.

“Most images of plankton are taken in a laboratory, or collected from nets on a ship,” said Cowen, who is a professor in OSU’s College of Earth, Ocean, and Atmospheric Sciences. “ISIIS gives us the rare ability to see them in their natural environment, which is a unique perspective that will enable us to learn more about them and the critical role they play in the marine food web.”

Other researchers on the project include graduate student Adam Greer, and undergraduate students Dorothy Tang, Ben Grassian and Jenna Binstein – all at the University of Miami.

Media Contact: 
Source: 

Jessica Luo, 650-387-5700; Jessica.luo@rsmas@miami.edu;

 

Bob Cowen, 541-867-0211; Robert.Cowen@oregonstate.edu

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Plankton Portlal

plankton_crew

Plankton Portal

Corvallis Science Pub focuses on the future of the oceans

CORVALLIS, Ore. – Warming ocean temperatures, rising acidity and reduced biological productivity threaten the livelihoods of about 2 billion people who depend on marine ecosystems, according to a report by an international team of 29 scientists last fall.

At the May 12 Corvallis Science Pub, Andrew Thurber, a post-doctoral researcher at Oregon State University who helped to conceive the study, will discuss how the oceans are responding to a changing climate. The Science Pub presentation, which is free and open to the public, begins at 6 p.m. in the Majestic Theater located at 115 S.W. Second St. in Corvallis.

“What is really sobering about these findings is that they don’t even include other impacts to the world’s oceans such as sea level rise, pollution, over-fishing, and increasing storm intensity and frequency,” he said. “All of these could compound the problem significantly.”

Thurber’s research focuses on deep-sea ecosystems, particularly the role of invertebrates in recycling nutrients and sequestering carbon. He has conducted experiments under seasonal sea ice in Antarctica and explored communities that live around methane seeps near New Zealand and Costa Rica.

Thurber received his Ph.D. from the Scripps Institution of Oceanography, UC San Diego. His work has been supported by the National Science Foundation.

Sponsors of Science Pub include Terra magazine at OSU, the Downtown Corvallis Association and the Oregon Museum of Science and Industry.

Media Contact: 
Source: 

Andrew Thurber, 541-737-8251

Geochemist to present Condon Lecture

CORVALLIS, Ore. – Richard Carlson, a geologist, geochemist, and planetary scientist from the Carnegie Institution in Washington, D.C., will present the 2014 Thomas Condon Lecture at Oregon State University on Wednesday, March 5.

The free public lecture, "A History of Earth Formation," is designed for a non-specialist audience. It begins at 7:30 p.m. in Austin Auditorium of the LaSells Stewart Center on the OSU campus. The Condon Lecture, named after a pioneer of Oregon geology, helps to interpret significant scientific research for non-scientists.

Carlson is a staff scientist at the Department of Terrestrial Magnetism at the Carnegie Institution. He conducts research on the history and evolution of the crust and interior of Earth, Mars, the moon and different asteroids to understand the mechanisms of planet formation and the way in which planets develop habitable surfaces.

He uses isotope geochemistry to study element formation in stars and how those elements are delivered throughout the solar system. His studies have taken to southern Africa, Brazil, the Arctic coast of Hudson’s Bay, eastern Oregon, and most recently, central Mongolia.

The recipient of numerous awards, Carlson was elected to the National Academy of Sciences in 2012.

While at OSU, Carlson will also give a more technical presentation on a related topic. His George Moore Lecture, “Pacific Northwest Volcanism: The Connection of Mantle Dynamics and Continent Formation,”   will be held Thursday, March 6, beginning at 4 p.m. in Kelley Engineering Room 1003.

The presentations are sponsored by the OSU Research Office and the College of Earth, Ocean, and Atmospheric Sciences.

Media Contact: 
Source: 

John Dilles, 541-737-1245 or dillesj@geo.oregonstate.edu

Noted oceanographer to speak Nov. 12 at Hatfield

NEWPORT, Ore. – Don Walsh, a pioneering oceanographer famous for his 1960 dive to the deepest part of the ocean, will visit Newport on Tuesday, Nov. 12.

Walsh will give a free public lecture at Oregon State University’s Hatfield Marine Science Center. His presentation, “Lunch on Board the Titanic: Two Miles Deep in the Atlantic,” begins at 6:30 p.m. In his talk, Walsh will share his experience diving in a submersible down to the Titanic and other adventures from his career of more than 40 years.

A retired captain from the U.S. Navy, Walsh went on to enjoy a lengthy career as an oceanographer and ocean engineer who explored the deep oceans and polar regions. He has commanded submarines as a naval officer and deep-sea submersibles as a researcher.

In 1960, Walsh and Swiss oceanographer Jacques Piccard boarded the bathyscaphe Trieste and descended to the floor of the Mariana Trench in the northern Pacific Ocean – a depth of more than 35,000 feet, or nearly seven miles. It took five hours to reach the seafloor, and at 30,000 feet they heard a loud crack. Upon reaching the bottom, they discovered cracks in the window, and quickly began ascending.

The historic dive received worldwide attention. It also remained a world record dive for 52 years until James Cameron piloted his Deepsea Challenger to the same place in 2012.

Walsh, who has a courtesy appointment in OSU’s College of Earth, Ocean, and Atmospheric Sciences, will also visit schools in Newport during the week and give a seminar at the Hatfield Marine Science Center. That talk, intended for a research audience, is titled “Going the Last Seven Miles – Looking Backwards at the Future.” It begins at 3:30 p.m. on Nov. 12 in the Hennings Auditorium.

Media Contact: 
Source: 

Maryann Bozza, 541-867-0234; maryann.bozza@oregonstate.edu

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don_walsh
Don Walsh

OSU oceanography dean to speak at ARCS Foundation

PORTLAND, Ore. – Mark Abbott, dean of the College of Earth, Ocean, and Atmospheric Sciences at Oregon State University, will give the keynote speech at the Achievement Rewards for College Scientists (ARCS) Foundation scholars luncheon on Tuesday, Oct. 22, in Portland.

The event begins at 11 a.m. at the Portland Art Museum, where 52 ARCS scholars will be honored and present posters of their research. Ticket information is available online at: https://www.arcsfoundation.org/portland/news/portland-chapters-9th-annual-luncheon-celebrates-50-american-science-scholars

Abbott’s talk, “Our Oceans under Pressure,” will outline how human impacts on the world’s oceans are increasing, raising concern for such issues as declining fisheries, sea level rise, pollution, acidification, harmful algal blooms, and marine “dead zones.”

Abbott is president of the Oceanographic Society and a former member of the National Science Board. In 2011, he received the prestigious Jim Gray eScience Award in Stockholm, Sweden, from Microsoft Research for his leadership in blending science and computing technology. He joined the OSU faculty in 1988 and has served as dean of the college since 2001.

Julia Maxson of Oregon Health & Science University will be the featured ARCS Scholar Alumna speaker. Her talk is titled “Using Genetics to Find Better Cancer Treatments.”

Fifty-two scholars at OSU and OHSU will be honored at this ninth annual luncheon.

Media Contact: 
Source: 

Jean Josephson, ARCS president, jeanjosephson@gmail.com

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Mark Abbott
Mark Abbott

Ocean sound: The Oregon Coast rules when it comes to ambient noise

NEWPORT, Ore. – For more than a year, scientists at Oregon State University’s Hatfield Marine Science Center deployed a hydrophone in 50 meters of water just off the coast of Newport, Ore., so they could listen to the natural and human-induced sounds emanating from the Pacific Ocean environment.

Their recently published analysis has a simple conclusion: It’s really noisy out there.

There are ships, including container shipping traffic, commercial fishers and recreationalists. There are environmental sounds, from waves pounding the beach, to sounds generating by heavy winds. And there are biological sounds, especially the vocalizations of blue whales and fin whales. And not only is Oregon’s ocean sound budget varied, it is quite robust.

“We recorded noise generated from local vessels during 66 percent of all hours during the course of a year,” said Joe Haxel, an OSU doctoral student who is affiliated with both the Cooperative Institute for Marine Resources Studies (CIMRS) and NOAA’s Pacific Marine Environmental Laboratory acoustics program at the Hatfield center. “In fact, there is an acoustic spike during the opening of the commercial crabbing season related to the high number of boats working the shallow coastal waters at the same time.

“But, at times, the biggest contributor to the low-frequency sound budget is from the surf breaking on the beach a few kilometers away,” he added. “That’s where Oregon trumps most other places. There haven’t been a lot of studies targeting surf-generated sound and its effect on ambient noise levels in the coastal ocean, but the few that are out there show a lot less noise than we have. Our waves are off the charts.”

The year-long study of noise, which was published in the Journal of the Acoustical Society of America, was supported by the Department of Energy, the Oregon Wave Energy Trust, NOAA and OSU.

The study is about more than scientific curiosity, researchers say. The research was carried out in support of OSU’s Northwest National Marine Renewable Energy Center and will play an important role in determining whether testing of wave energy devices off the Oregon coast may have environmental impacts.

Scientists must know what naturally occurring sounds exist, and at what levels, so when new sounds are introduced, there is some context for evaluating their intensity and impact.

Documenting marine noises for an entire year isn’t easy, the researchers pointed out. First, the equipment must withstand the rugged Pacific Ocean, so the OSU researchers deployed the hydrophone near the seafloor in about 50 meters of water so violent winter storms wouldn’t destroy the instrumentation. They focused on low-frequency sounds, where the majority of noise emitted by wave energy converters is expected to occur.

After combing through an entire year of data, they determined that Oregon’s low-frequency noise budget is often dominated by the constant sounds of breaking surf. These weren’t necessarily the loudest noises, though.

“The strongest signal we got during the course of the year came from a boat that drove right over our mooring,” said Haxel, who is pursuing his doctorate through OSU’s College of Earth, Ocean, and Atmospheric Sciences. “The second loudest sound came from the vocalizations of a blue whale, which can be incredibly loud. We were told by colleagues at the Marine Mammal Institute that blue whales have been sighted close to shore in recent years and it was probably within several kilometers of the hydrophone.”

Haxel said the OSU researchers also recorded numerous vocalizations of fin whales and humpback whales, but a startling omission was that of gray whales, one of the most common West Coast whales.

“We didn’t document a single gray whale sound during the entire year, which was really surprising,” Haxel said. “Even during times when gray whales were visually sighted from shore within close proximity of the hydrophone, we never recorded any vocalizations. One theory is that they are trying to keep as quiet as possible so they don’t give away their location to orcas, which target their calves.”

Another unusual source of noise was the wind. Even at 50 meters below the surface, the hydrophone picked up sound from the wind – but not in the way one might think. It wasn’t the howling of the wind that was noticeable, Haxel said, but the ensuing waves, known as “whitecaps” or “wind chop,” and the clouds of bubbles that were injected into the water column.

Haxel compared his data on Oregon sounds to a handful of studies in the literature associated with high-energy environmental conditions to see how the region fared. All of the other studies were limited: a Monterey Bay, Calif., survey focused only on surf noises. A study off the Florida coast examined wind-generated sounds. And a study of the Scotia Shelf in Canada looked at wind and surf.

Oregon noise levels were similar to other regions for frequencies above 100 Hz, Haxel said, but rose sharply for frequencies affected by surf-generated noise – generally below 100 Hz.

“The bottom line is that the Pacific Ocean in the Northwest can be a remarkably loud environment and our wave climate in particular is amazing,” Haxel said. “That’s why wave energy is being targeted for this region in the first place. The study will provide some valuable information as the wave energy industry goes forward.

“We will be able to measure noise levels from the testing, or even the loading and unloading of equipment from the vessels, and compare those measurements with the range of background ambient sound levels already occurring in the area,” he added.

“It is a balancing act as some noise from the testing sites may serve as a warning signal for whales and other animals to avoid the area, helping to reduce the risk for collision or entanglement,” Haxel said. “But adding too much noise can be harmful, disrupting their communication or navigation.”

Media Contact: 
Source: 

Joe Haxel, 541-867-0282; joe.haxel@oregonstate.edu

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Tail of the whale
Blue whale vocalizations
are second loudest


 Coastal waves
Breaking surf tops
the charts for noise

 

Sound file of breaking surf:

http://oregonstate.edu/dept/ncs/media/wave-breaking.wav

 

Sound file of boat motors:

http://oregonstate.edu/dept/ncs/media/boat-noise.wav

Study documents early warming of West Antarctica at end of last ice age

CORVALLIS, Ore. – West Antarctica began emerging from the last ice age about 22,000 years ago – well before other regions of Antarctica and the rest of the world, according to a team of scientists who analyzed a two-mile-long ice core, one of the deepest ever drilled in Antarctica.

Scientists say that changes in the amount of solar energy triggered the warming of West Antarctica and the subsequent release of carbon dioxide (CO2) from the Southern Ocean amplified the effect and resulted in warming on a global scale, eventually ending the ice age.

Results of the study were published this week in the journal Nature. The authors are all members of the West Antarctic Ice Sheet Divide project, which was funded by the National Science Foundation.

The study is significant because it adds to the growing body of scientific understanding about how the Earth emerges from an ice age. Edward Brook, an Oregon State University paleoclimatologist and co-author on the Nature study, said the key to this new discovery about West Antarctica resulted from analysis of the 3,405-meter ice core.

“This ice core is special because it came from a place in West Antarctica where the snowfall is very high and left an average of 20 inches of ice or more per year to study,” said Brook, a professor in OSU’s College of Earth, Ocean, and Atmospheric Sciences. “Not only did it allow us to provide more accurate dating because we can count the layers, it gave us a ton more data – and those data clearly show an earlier warming of the region than was previously thought.”

Previous studies have pointed to changes in the Earth’s orbit around the sun as the initial trigger in deglaciation during the last ice age. An increase in the intensity of summer sunlight in the northern hemisphere melted ice sheets in Canada and Europe starting at about 20,000 years ago and is believed to have triggered warming elsewhere on the globe.

It previously was thought that Antarctica started its major warming a few thousand years later, at about 18,000 years before present. However, the new study shows that at least part of Antarctica started to warm 2,000 to 4,000 years before this. The authors hypothesize that changes in the total amount of sunlight in Antarctica and melt-back of sea ice caused early warming at this coastal site – warming that is not recorded by ice cores in the interior of the continent.

“The site of the core is near the coast and it conceivably feels the coastal influence much more so than the inland sites where most of the high-elevation East Antarctic cores have been drilled,” Brook said. “As the sunlight increased, it reduced the amount of sea ice in the Southern Ocean and warmed West Antarctica. The subsequent rise of CO2 then escalated the process on a global scale.”

“What is new here is our observation that West Antarctica did not wait for a cue from the Northern Hemisphere before it began warming,” Brook said, “What hasn’t changed is that the initial warming and melting of the ice sheets triggered the release of CO2 from the oceans, which accelerated the demise of the ice age.”

Brook said the recent increase in CO2 via human causes is also warming the planet, “but much more rapidly.”

Media Contact: 
Source: 

Ed Brook, 541-737-8197; brook@geo.oregonstate.edu

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ice core wintering

 

drilled ice core

 

HZBS400B

Study finds novel worm community affecting methane release in ocean

CORVALLIS, Ore. – Scientists have discovered a super-charged methane seep in the ocean off New Zealand that has created its own unique food web, resulting in much more methane escaping from the ocean floor into the water column.

Most of that methane, a greenhouse gas 23 times more potent than carbon dioxide at warming our atmosphere, is likely consumed by biological activity in the water, the scientists say. Thus it will not make it into the atmosphere, where it could exacerbate global warming. However, the discovery does highlight scientists’ limited understanding of the global methane cycle – and specifically the biological interactions that create the stability of the ocean system.

Results of the study, which was funded primarily by the National Oceanic and Atmospheric Administration and the Federal Ministry of Education and Research in Germany, have just been published online in the journal Limnology and Oceanography.

“We didn’t discover any major ‘burps’ of methane escaping into the atmosphere,” said Andrew R. Thurber, a post-doctoral researcher at Oregon State University and lead author on the study. “However, some of the methane seeps are releasing hundreds of times the amounts of methane we typically see in other locations, so the structure and interactions of this unique habitat certainly got our attention.

“What made this discovery most exciting was that it is one of the first and best examples of a direct link between a food web and the dynamics that control greenhouse gas emissions from the ocean,” Thurber added.

The scientists first discovered this new series of methane seeps in 600 to 1,200 meters of water off North Island of New Zealand in 2006 and 2007. The amount of methane emitted from the seeps was surprisingly high, fueling a unique habitat dominated by polychaetes, or worms, from the family Ampharetidae.

"They were so abundant that the sediment was black from their dense tubes,” Thurber pointed out.

Those tubes, or tunnels in the sediment, are critical, the researchers say. By burrowing into the sediment, the worms essentially created tens of thousands of new conduits for methane trapped below the surface to escape from the sediments. Bacteria consumes much of the methane, converting it to carbon dioxide, and the worms feast on the enriched bacteria – bolstering their healthy population and leading to more tunnels and subsequently, greater methane release.

The researchers say that there is one more critical element necessary for the creation of this unique habitat – oxygen-rich waters near the seafloor that the bacteria harness to consume the methane efficiently. The oxygen also enables the worms to breathe better and in turn consume the bacteria at a faster rate.

“In essence, the worms are eating so much microbial biomass that they are shifting the dynamics of the sediment microbial community to an oxygen- and methane-fueled habitat – and the worms’ movements and grazing are likely causing the microbial populations to eat methane faster,” said Thurber, who works in OSU’s College of Earth, Ocean, and Atmospheric Sciences. “That process, however, also leads to more worms that build more conduits in the sediments, and this can result in the release of additional methane.”

Methane seeps and worm communities are present in many other areas around the world, the researchers point out, including the Pacific Northwest. However, the deep water in many of these locations has low levels of oxygen, which the scientists think is a factor that constrains the growth of the worm populations. In contrast, the study sites off New Zealand are bathed in cold, oxygen-rich water from the Southern Ocean that fuels these unique habitats.

“The large amounts of methane consumed by bacteria have kept it from reaching the surface,” Thurber said. “Those bacteria essentially are putting the pin back in the methane grenade. But we don’t know if the worms ultimately may overgraze the bacteria and overtax the system. It’s something we haven’t really seen before.”

Also participating in the study were scientists from Scripps Institution of Oceanography, the National Institute of Water and Atmospheric Research in Wellington, New Zealand, and the Helmholtz Centre for Ocean Research in Germany.

Media Contact: 
Source: 

Andrew Thurber, 541-737-8251; athurber@coas.oregonstate.edu

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Poly_red Ampharetid_feeding

Worm feeding

 

Poly_red Ampharetid_pic3

Worm outside its tube

 

AmphBeds

Worm bed off coast

of New Zealand

Oregon State University students produce interactive iBook Atlas of the Columbia River Basin

Another version of this story is available on Terra magazine at Oregon State.

CORVALLIS, Ore. — The Columbia River Basin comes to life in a new digital atlas produced by Oregon State University cartography students. Starting with ArcMap, they created an iBook — accessible via Apple’s iPad — which combines the look and feel of a traditional paper book with the touch-screen features of a tablet computer.

Through colorful maps, animations, photos and video, the new atlas allows users to explore the basin’s geology, climate, social history and land use. It shows the location and extent of historical and current tribal lands — Kootenai, Nez Perce, Umatilla and others — the region’s population centers and a time-lapse display of dam construction from 1900 to the present. Maps also show the location of salmon runs, recreation sites and public lands. 

Under the guidance of Bernhard Jenny, cartographer and assistant professor in the College of Earth, Ocean, and Atmospheric Sciences, 17 graduate and undergraduate students published the Atlas of the Columbia River Basin. It can be downloaded free as a PDF or iBook from the cartography and visualization group at Oregon State. Jenny has submitted it to Apple’s iTunes library.

Creating the interactive and static maps required the use of three different software packages, says Jenny. Students used ArcMap to merge geospatial data from different sources and design the maps. They reprojected the maps to a local coordinate system that was optimized for the portrayal of the transboundary Columbia Basin. After exporting the maps from ArcMap into Adobe Illustrator, they fine-tuned symbolization, labeling and layout. The last step consisted of placing the maps in iBooks Author, the authoring software for creating eBooks for the iPad. The maps were combined with interactive features, text, diagrams and other elements and laid out in this authoring software.

Unlike most atlases that are restricted by national and state borders, this atlas crosses the boundary between Canada and the United States, says Kimberly Ogren, an Oregon State Ph.D. student. Ogren helped to develop the 33-page document as a student in Jenny’s course on computer-assisted cartography.

“If you apply cartography concepts in the right way,” she says, “you will create a map that draws people to the information and conveys it effectively. People will want to learn more. That’s our hope for this atlas.”

Not Just Another Digital Map

More than a useful resource about the Columbia basin, the new atlas is also a milestone in cartography. “Cartographers haven’t used these new formats with all their features,” says Jenny. He notes that the first digital map (The Electronic Atlas of Canada) was created in 1981, but it and its successors have been more useful for specialists than for the general public.

“Those atlases don’t have individual page layouts or elements like diagrams and pictures,” he says. “They’re more standardized in their appearance and functionality.” In essence, most digital atlases provide a visual interface for viewing and analyzing data rather than an educational resource for the public.

In contrast, the Atlas of the Columbia River Basin presents information in a format that is accessible. It includes a table of contents and chapters. It integrates digital data with other book-like features and touch-screen functions that are familiar to any smart phone or tablet computer user.

The advantage for mapmakers, says Jenny, lies in the ease with which such atlases can be created. The downside is that creativity in terms of interactivity is limited to what the authoring software allows. In addition, e-books cannot be exported to multiple brands of devices. Apple’s iBook authoring software, for example, creates e-books only for Apple devices.

The evolution of atlases to tablet computers follows the growth in sales of iPads, Amazon’s Kindle and other tablets in the last few years. In 2014, says Jenny, sales of tablet computers are expected to outpace sales of desktop and notebook PCs combined. E-books have grown in popularity as well and accounted for about 20 percent of publishers’ revenues in 2012. In 2011, sales of e-books outpaced sales of hardcover adult fiction.

Jenny plans to continue incorporating iBook publishing in his cartography classes. Both he and Ogren say that students in the cartography class benefited by creating a product that they could show to future employers as well as family and friends.

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Media Contact: 
Source: 

Bernhard Jenny, 541-737-1204