Category Archives: College of Earth Oceanic and Atmospheric Sciences

Small Differences Have Big Consequences to Keep the Oceans Happy

Swimming away from the rocky shores out to sea Grace Klinges, a 2^nd year PhD student in the Vega-Thurber Lab, is surrounded by short green sea grasses swaying in the waves, multi-colored brown sand and occasional dull grayish-brown corals dot the floor as she continues her research dive. However, the most interesting thing about this little island reef off the coast of Normanby Island, Papua New Guinea, is the forest of bubbles that envelopes Grace as she swims. Bubbles curiously squeak out everywhere along seafloor between sand grains and even eating their way through the corals themselves. It reminds one of how thick the fog can be in the Oregon hills, and like a passing cloud, the bubbles begin to dissipate the further away you swim from the shore, revealing an increasingly complex web of life wholly dependent on the corals that look more like color-shifting chameleons than their dull-colored cousins closer to the shore.

Grace took ~2,000 photos for each of 6 transects moving away from the carbon dioxide seeps. She is rendering these photos using a program called PhotoScan, which identifies areas of overlap between each photo to align them, and then generates a 3D model by calculating the depth of field of each image.

These bubbles emanating from the seafloor is part of a naturally occurring CO₂ seep found in rare parts of the world. While seemingly harmless as they dance up the water column, they are changing ocean chemistry by decreasing pH or making the water more acidic. The balance of life in our oceans is so delicate – the entire reef ecosystem is changing in such a way that provides a grim time machine into the future of Earth’s oceans if humans continue emitting greenhouse gasses at our current rate.

Corals are the foundation of these ocean ecosystems that fish and indigenous island communities rely on for survival. In order for corals to survive they depend on a partnership with symbiotic algae; through photosynthesis, the algae provide amino acids and sugars to the corals, and in return, the coral provides a sheltered environment for the algae and the precursor molecules of photosynthesis. Algae lend corals their magnificent colors, but algae are less like colorful chameleons and more like generous Goldilocks that need specific water temperatures and a narrow range of acidity to survive. Recall those bubbles of CO₂ rising from the seafloor? As the bubbles of CO₂ move upward they react with water and make it slightly more acidic, too acidic in fact for the algae to survive. In an unfortunate cascade of effects, a small 0.5 pH unit change out of a 14 unit scale of pH, algae cannot help corals survive, fish lose their essential coral habitat and move elsewhere leaving these indigenous island inhabitants blaming bubbles for empty nets. On the grander scale, it’s humans to blame for our continuous emissions rapidly increasing global ocean temperatures and lowering ocean pH. The only real question is when we’ll realize the same thing the local fishermen see now, how can we limit the damage to come?

The lovely Tara Vessel anchored in Gizo, Solomon Islands.

Grace Klinges is a 2^nd year Ph.D. student in the Microbiology Department who is using these natural CO₂ seeps as a proxy for what oceans could look like in the future, and she’s on the hunt for solutions. Her research area is highly publicized and is part of an international collaboration called Tara Expeditions as a representative of the Rebecca Vega Thurber Lab here at Oregon State, known for diving across the world seeking to better understand marine microbial ecology in this rapidly changing climate. Grace’s project is studying the areas directly affected by these water-acidifying CO₂ seeps and the surrounding reefs that return to normal ocean pH levels and water temperatures. By focusing her observations in this localized area, about a 60-meter distance moving away from shore, Grace is able to see a gradient of reef health that directly correlates with changing water chemistry. Through a variety of techniques (GoPro camera footage, temperature sensors, pH, and samples from coral and their native microbial communities) Grace hopes to produce a 3D model of the physical reef structures at this site to relate changing chemistry with changes in community complexity.

Tara scientists spend much of the sailing time between sites labeling tubes for sampling. Each coral sample taken will be split into multiple pieces, labeled with a unique barcode, and sent to various labs across the world, who will study everything from coral taxonomy and algal symbiont diversity to coral telomere length and reproduction rates. Photo © Tara Expeditions Foundation

One of the main ideas is that as you move further away from the CO₂ seeps the number of coral species, or coral diversity, increases which often is expressed in a huge variety of physical structures and colors. As the coral diversity increases so should the diversity of their microbiomes. Using genetic and molecular biology techniques, Grace and the Vega Thurber lab will seek to better understand which corals are the most robust at lower pH levels. However, this story gets even more complicated, because it’s not just the coral and algae that depend on each other, but ocean viruses, bacterial players, and a whole host of other microorganisms that interact to keep this ecological niche functioning. This network of complicated interactions between a variety of organisms in reef systems requires balance for the system to function. Affectionately named the “coral holobiont“, similar to a human’s microbiome, we are still far from understanding the relative importance of each player which is why Grace and her labmates have written a series of bioanalytic computer scripts to efficiently analyze the massive amounts of genetic information that is becoming more available in the field.

Grace was overjoyed after taking a break from sampling to swim with some dolphins who were very curious about the boat. Photo © Tara Expeditions Foundation

With the combination of Grace’s field work taking direct observations of our changing oceans, and her computer programming that will help researchers around the world classify organisms of unknown ecosystem function, our knowledge of the oceans will get a little less murky. Be sure to listen to the interview Sunday January 14^th at 7PM. You can learn more about the Vega Thurber lab here.

You can also download Grace’s iTunes Podcast Episode!

Ocean basins are like trumpets– no, really.

We’re all familiar with waves when we go to the coast and see them wash onto the beach. But since ocean waters are usually stratified by density, with warmer fresher waters on top of colder, saltier ones, waves can occur between water layers of different densities at depths up to hundreds of meters. These are called internal waves. They often have frequencies that are synched with the tides and can be pretty big–up to 200 meters in amplitude! Because of their immense size, these waves help transfer heat and nutrients from deep waters, meaning they have an impact on ocean current circulation and the growth of phytoplankton.

The line of foam on the surface of the ocean indicates the presence of an internal wave.

We still don’t understand a lot about how these waves work. Jenny Thomas is a PhD student working with Jim Lerczak in Physical Oceanography in CEOAS (OSU’s College of Earth, Ocean, and Atmospheric Sciences). Jenny studies the behavior of internal waves whose frequencies correspond with the tides (called internal tides) in ocean basins. This requires a bit of mathematical theory about how waves work, and some modeling of the dimensions of the basin and how it could affect the height of tides onshore.

Picture a bathtub with water in it. Say you push it back and forth at a certain rate until all the water sloshes up on one side while the water is low on the other side. In physics terms, you have pushed the water in the bathtub at one of its resonant frequencies to make all of it behave as a single wave. This is called being in a normal mode of motion. Jenny’s work on the normal modes of ocean basins suggests that the length-to-width ratio and the bathymetry of an ocean basin influence the structure of internal tides along the coast. Basically, if the tidal forcing and the shape of the basin coincide just right, they can excite a normal mode. The internal wave can then act like water in a bathtub sloshing up the side, pushing up on the lower-density water above it.

It turns out that water isn’t the only thing that can have normal modes. The air column in a wind instrument is another example. Jenny grew up a child of two musicians and earned a degree in trumpet performance from the University of Iowa, and she occasionally uses her trumpet to demonstrate the concept of normal modes. She can change pitches by buzzing her lips at different resonant frequencies of the trumpet–the pitch is not just controlled by the valves.

Jenny uses her trumpet to explain normal modes.

Near the end of her undergraduate degree at the University of Iowa, Jenny discovered that she had a condition called fibrous dysplasia that could potentially cause her mouth to become paralyzed. Deciding a career as a musician would be too risky, and realizing her aptitude for math and physics, she went back to school and earned a second undergraduate degree in physical oceanography at Old Dominion University. After a summer internship at Woods Hole Oceanographic Institution conducting fieldwork for the US Geological Survey, she decided to pursue a graduate degree at OSU to further examine the behavior of internal waves.

Tune in to 88.7 KBVR Corvallis to hear more about Jenny’s research and background (with a trumpet demo!) or stream the show live right here.

You can also download Jenny’s iTunes Podcast Episode!

Jenny helps prepare an instrument that will be lowered into the water to determine the density of ocean layers.

Jenny isn’t fishing. The instrument she is deploying is called a CTD for Conductivity, Temperature, and Depth–the three things it measures when in the water.

The Breathing Seafloor

In the cold, dark depths of the seafloor across the world, microbes living in sediments and on rocks are quietly breaking down organic material and sucking dissolved oxygen out of the seawater. The continental shelf off of Oregon’s coasts, home to a fishing industry that brings in over a hundred million dollars of revenue per year, is no exception. Does oxygen consumption, and therefore carbon cycling, vary by location, or across seasons? Setting a baseline to investigate these patterns of oxygen drawdown is crucial to understanding habitats and distributions of fish stocks, but will also establish what “normal” oxygen consumption looks like off our shores. Measurements like these are also used by the Intergovernmental Panel on Climate Change (IPCC) to estimate global patterns of carbon burial. If any forces were to shift these patterns in the future, we’d at least have a baseline to allow us to diagnose any “abnormal” conditions.

Peter Chace is a third-year PhD student of Ocean Ecology and Biogeochemistry in the College of Earth, Ocean, and Atmospheric Sciences (CEOAS). Peter’s research focuses on developing a technique of measuring fluxes of oxygen across the seafloor called Eddy covariance. This technique takes high-resolution time measurements of three-dimensional velocities of water moving in turbulent whorls, or random circular patterns, within the boundary layer of a fluid like air or water. Eddy covariance has been employed to measure fluxes across air layers on land for decades, but has only recently been applied in marine systems. A point-source oxygen measurement within this turbulent layer is measured with a microelectrode and combined with the velocity data to develop a flux. Why go through all this trouble? Other ways to measure oxygen fluxes, like putting chambers over an area of seafloor and waiting to measure an oxygen drawdown, require a lot of work and give little temporal resolution.

Workers on the RV Oceanus, Oregon State’s largest research vessel, deploy a benthic (seafloor) oxygen sensor.

Peter can calibrate his microelectrodes to measure other chemicals and obtain their fluxes across the seabed, but he is mainly focused on oxygen. To measure fluxes off the Oregon coast, Pete and his advisor, Dr. Clare Reimers, will head to sea on the RV Oceanus several times this fall and winter to deploy their sensor on the seafloor for days at a time. The desk-sized seafloor lander and the microelectrode attached to it are fragile, and the rough seas offshore Oregon in fall and winter will make it a challenging endeavor. We hope they pack enough seasickness medication and barf bags!

You get right up close and personal with the ocean when you send down these instruments… and this is on a clear day with calm seas!

Since growing up as a child in New Jersey, Peter has always wanted to learn about the ocean. While studying chemistry and marine biology at Monmouth University (in New Jersey) as an undergraduate, he completed a summer REU (Research Experience as an Undergraduate) with his current advisor, Clare Reimers, here at Oregon State University. He also interned for NOAA (the National Oceanic and Atmospheric Association), analyzing the chemistry of hydrothermal vent fluids with Dr. David Butterfield. Pete revisited a hydrothermal system on a cruise to the East Pacific Rise off of Central America where he got a remarkable opportunity to dive in Alvin, the submersible that discovered the wreckage of the Titanic.

Here’s Pete in the submersible Alvin just before the dive, checking his microelectrodes.

To hear more about Peter’s research on sensor development and his seafaring expeditions, tune in to Inspiration Dissemination on Sunday, October 15^th at 7pm on 88.7 KBVR Corvallis. Or stream it online here!

Breaking the Arctic ice

Thermal AVHRR image with land masked in black. Can see the lead coming off of Barrow Alaska very bright. The arrows are sea ice drift vectors.

Cascade over mossy rocks near Sol Duc Falls, Olympic National Park, WA.

When you hear about fractures in sea ice, you might visualize the enormous fissures that rupture ice shelves, which release massive icebergs to the sea. This is what happened back in July 2017 when a Delaware-sized iceberg broke off from the Larsen C ice shelf in Antarctica. However, there are other types of fractures occurring in sea ice that may be impacted by atmospheric conditions. Our guest this week, CEOAS Masters student Ben Lewis investigates how interactions between the atmosphere and sea ice in the Beaufort Sea (north of Alaska in the Canadian Archipelago) impact the formation of fractures. His research involves mapping atmospheric features, such as wind and pressure, at the point in time when the fractures occurred and provides insight into the effect of the atmosphere on the formation and propagation of fractures. Utilizing satellite imagery compiled by the Geographical Information Network of Alaska from 1993 to 2013, Ben has conducted a qualitative analysis to determine the location and time when these ice fractures occurred and what type of physical characteristics they possess.

Southern Alps from the summit of Avalanche Peak, New Zealand.

While fractures appear small on the satellite image, the smallest fractures that Ben can observe by are actually 250 meters wide. Fractures can span hundreds of kilometers, and the propagate very quickly; Ben cites one example of a fracture near Barrow, Alaska that grew to 500 kilometers within 6 hours!

Fractures are potentially deadly for people and animals hunting in the Arctic. As weather flux in the fragile Arctic ecosystem has become more erratic with climate change, it has been difficult for people to predict when it was safe to hunt on the ice based on patterns observed in prior seasons. Additionally, it has been problematic to track weather in the Arctic because of its harsh conditions and sparse population. A well-catalogued record of weather is not available for all locations. Modeling atmospheric conditions, such as pressure and wind, based on what has been captured by satelliteimagery, will facilitate better prediction of future fracture events.

Sunset over Sandfly Beach, New Zealand.

While pursuing an undergraduate degree in physics at the University of Arkansas, Ben was able to study abroad James Cook University in Australia, where he gravitated towards environmental physics, while taking advantage of incredible opportunities for nature photography. He also did a semester abroad in New Zealand, where he studied geophysical fluid dynamics and partial differential equations. Ben came to OSU as a post-baccalaureate student in climate science, and while at OSU, he became acquainted with his future PI, Jennifer Hutchings, and his interest in Arctic research grew. He cites learning about snowball earth, glaciology, and the cryosphere, as providing the basis for his desire to pursue Arctic climate research. Eventually, Ben would like to pursue a PhD, but in the immediate future, he plans to keep his options open for teaching and research opportunities.

Characterizing off-channel habitats in the Willamette River: Fish need to cool off too!

During the summer, when the mercury clears triple digits on the Fahrenheit scale, people seek out cooler spaces. Shaded parks, air conditioned ice cream parlors, and community pools are often top places to beat the heat. If you’re a resident of Corvallis, Oregon, you may head downtown to dip your toes in the Willamette River. Yet while the river offers a break from the hot temperatures for us, it is much too warm for the cold water fishes that call it home.

Where do fish go to cool off?

As a master’s student in the Water Resources Graduate Program at Oregon State University, Carolyn Gombert is working to understand where cold water habitat is located along the Willamette River. More importantly, she is seeking to understand the riverine and geomorphic processes responsible for creating the fishes’ version of our air conditioned ice cream parlors. By placing waterproof temperature loggers along sites in the upper Willamette, she hopes to shed light both on the temporal and spatial distribution of cold water patches, as well as the creation mechanisms behind such habitats.

The cart before the horse: seeking to reconcile science and policy

Because the Willamette Basin is home to Cutthroat trout and Chinook salmon, the river is subject to the temperature standard adopted by the state of Oregon in 2003. Between May through October, Cutthroat and Chinook require water cooler than 18 degrees Celsius (64.4 degrees Fahrenheit). Currently, the main channel of the Willamette regularly exceeds this threshold. The coolest water during this time is found in side channels or alcoves off the main stem. While Oregon law recognizes the benefits these “cold water refuges” can provide, our scientific understanding of how these features change over time is still in its early stages.

Emerging stories

Data collection for Carolyn’s project is slated to wrap up during September of 2017. However, preliminary results from temperature monitoring efforts suggest the subsurface flow of river water through gravel and sediment plays a critical role in determining water temperature. By pairing results from summer field work with historical data such as air photos and laser-based mapping techniques (LiDAR) like in the image below, it will be possible to link geomorphic change on the Willamette to its current temperature distributions.

Between 1994 and 2000, the Willamette River near Harrisburg, Oregon shifted from a path along the left bank to one along the right bank. This avulsion would have happened during a high flow event, likely the 1996 flood.

No stranger to narratives

Prior to beginning her work in hydrology at OSU, Carolyn earned a bachelor’s in English and taught reading at the middle school level. Her undergraduate work in creative writing neither taught her how to convert temperature units from Fahrenheit to Celsius nor how to maneuver in a canoe. But the time she spent crafting stories did show her that characters are not to be forced into a plot, much like data is not to be forced into a pre-meditated conclusion. Being fortunate enough to work with Stephen Lancaster as a primary advisor, Carolyn looks forward to exploring the subtleties that surface from the summer’s data.

If you’d like to hear more about the results from Carolyn’s work, she will be at the OSU Hydrophiles’ Pacific Northwest Water Research Symposium, April 23-24, 2018. Feel free to check out past Symposiums here. Additionally, to hear more about Carolyn’s journey through graduate school, you can listen to her interview on the Happie Heads podcast.

Carolyn conducting field work on the Willamette.

Carolyn Gombert wrote the bulk of this post, with a few edits contributed by ID hosts.

Project CHOMPIN: Parrotfish, nutrients, and the coral microbiome

CHOMPIN comic.

Ecology is the study of the relationships among organisms and the relationships of organisms to their physical surroundings. The interactions of organisms can be described as a complex web with many junctions or relationships, and a single ecologist may focus on one or many relationships in a community or ecosystem. Our guest this week, Rebecca (Becca) Maher PhD student in the Department of Microbiology, is interested in the effect of environmental stressors on the coral microbiome. Let’s break this down by interaction:

Beneficial algae, bacteria, and viruses interact with coral by living in coral tissue and forming the coral microbiome
Corals interact with other organisms in the coral reef ecosystem, such as parrot fish
Corals are affected by their surrounding environment: water temperature, water nutrients, and pollution

Becca at the Newport aquarium for Scientific Diver Training through Oregon State University.

You may be familiar with coral bleaching and coral reef decline from our past episodes. Corals form a mutualistic relationship (both organisms benefit) with algae, where algae take shelter within coral tissue and provide the coral with food from photosynthesis. It is well known that high temperatures lead to coral bleaching, or a shift in the coral microbiome resulting from the loss of beneficial algae that live within the coral. Coral bleaching is often fatal.

Becca is interested in other aspects of the coral microbiome, such as differences in the symbiotic bacterial communities brought about by nutrient enrichment from agricultural run-off and overfishing. Do corals in nutrient rich water have a different microbiome than corals in nutrient poor water? Do corals in highly fished areas have a different microbiome than corals in fish-rich areas? In overfished areas, predatory fish (e.g. parrotfish) may bite coral (hence Project CHOMPIN), and so how does the coral microbiome respond after wounding by parrotfish?

Becca diving at the Flower Garden Banks National Marine Sanctuary in the Northwest Gulf of Mexico for her undergraduate thesis at Rice University.

These questions are relevant for our knowledge of environmental factors that threaten coral reef ecosystems. Corals are in decline globally and with them are the high diversity of marine species that gain shelter and substrate from the coral reef. The information gained from Becca’s research may be informative for policy makers concerned with agricultural practices near marine areas and fishing regulations. Rebecca is traveling to Morrea, French Polynesia this August to set up her field and laboratory experiments at the Gump Biological Research Station.

This upcoming trip is highly anticipated for Becca, who has been pursuing research in marine ecosystems since her time at Rice University. After working with her undergraduate mentor Adrienne Correa at Rice, Becca’s general focus on Ecology shifted to a focus on Marine Ecology. For Becca, her project at Oregon State in the Vega Thurber Lab is a harmonious mix of field work, high-level experimental design, bioinformatics, and statistics—a nice capstone for a Marine Ecologist with aspirations for future research.

Hear more about Becca’s work with corals the Sunday at 7 PM on KBVR Corvallis 88.7FM. Not a local listener? Stream our broadcast live.

Using sediment cores to model climate conditions

In the lab of Andreas Schmittner in the College of Earth, Ocean, and Atmospheric Sciences, recently-graduated PhD student Juan Muglia has been developing a climate model to understand ocean current circulation, carbon cycling, and ocean biogeochemistry during the last ice age, focusing on the Southern Ocean surrounding Antarctica.

Juan has developed a climate model using data gathered from sediment cores, which are samples from the ocean floor that provide researchers with a glimpse into the elemental and organic composition of the ocean at different points in time. Scientists can acquire insight into the characteristics of the Earth’s past climate by analyzing the geologic record spanning thousands of years. Modeling the conditions of the last ice age, which occurred 20,000 years ago, allows researchers to better understand how the Earth responds to glacial and interglacial cycles, prompting the transition between cold and warm phases (we are currently in a warm interglacial period).

The process of generating an accurate climate model consists of tuning parameters embedded in the physics equations and fortran code of the model, to reproduce characteristics directly observable in modern times. If researchers can validate their model by reproducing directly observable characteristics, the model can then be used to investigate the climate at points in time beyond our direct observational capacity.

Since it’s not possible to directly measure temperature or nutrient composition of the ocean during the last ice age, Juan uses an indirect signature that serves as a proxy for direct measurement. Three isotopic sediment tracers, including 15Nitrogen, 14Carbon, and 13Carbon, are incorporated into Juan’s climate model as proxies for biological productivity and current circulation in the ocean. Investigating changes in the elemental composition of the ocean, also known as biogeochemistry, is important for understanding how climate and biology have transformed over thousands of years. The ocean serves as an enormous reservoir of carbon, and much more carbon is sequestered in the ocean than in the atmosphere. The exchange of carbon dioxide at the interface of the ocean and atmosphere is important for understanding how carbon dioxide has and will continue to impact pH, ocean currents, and biological productivity of the ocean.

Even as a kid, Juan dreamed of becoming an oceanographer. He grew up near the ocean in Argentina, surrounded by scientists; his mom was a marine botanist and his dad is a geologist. During his undergraduate studies, he majored in physics with the goal of eventually becoming a physical oceanographer, and his undergraduate thesis consisted of building fortran code for a statistical physics project. After finishing his post-doctoral studies at OSU, Juan plans to return to his hometown in Argentina, where he hopes to develop a model specific to the Argentinian climate.

Heavy Digging

Mine Algae!!!

When I think of mining, the first thing that comes to mind is the classic gold rush miners from the mid-1800s. Someone that looks a lot like Stinky Pete from Toy Story 2. I don’t mean to imply that this is, or isn’t, what a miner looks like. However, this does say something about the general lack of thought about mining practices. The EPA certainly isn’t as ignorant about mines as I am; in fact, as of 2014, they had designated over 1,300 sites around the country as superfund sites requiring extensive cleanup efforts. Tullia Upton is also thinking about mines much more deeply than the average person, and she is uncovering some alarming information.

During a road trip through southern Oregon, Tullia was bummed when she was told it was unsafe to swim in a local river, so she decided to dive a bit deeper, figuratively of course. She learned that this area has become dangerously polluted due to waste products of the Formosa mine.

The Formosa mine near Riddle, OR

Mining practices involve extensive digging and extracting of heavy metals which are normally buried in a reducing environment deep down within the earth’s sediment. The process of digging up these heavy metals leaves behind a staggering amount of unused material, known as tailings. Mining also exposes the metals to oxygen and allows them to leach into soils and the watershed. Due to runoff from the tailings and other waste at the Formosa mine, there is now an estimated 18 mile dead zone where no organism can live. The full extent of the damage being done to the local watershed has not been thoroughly mapped though.

Tullia analyzing samples in the lab

As she learned more about the dangerous metals coming from the mine, Tullia immediately got involved as a volunteer and secured research funding to study the pollution occurring at the Formosa mine. Tullia hopes to map the full extent of runoff from the Formosa mine and provide a better picture of the mess for the EPA, and other scientists, working on the cleanup process. When she finishes her Ph.D. here in Environmental Sciences, Tullia hopes to move on to a post-doc and eventually run her own research lab.

Tune in this Sunday, October 9th at 7pm PST to hear more about mine pollution and Tullia’s unique journey to grad school at OSU.

Heat and oxygen exchange at the interface of ocean and atmosphere.

Jenessa aboard OSU’s vessel the R/V Oceanus during a cruise for a field work course. She is deploying a vertical microstructure profile attached to a large winch: fishing for the big one!

As a physical oceanographer in the College of Earth, Ocean, and Atmospheric Sciences, Masters candidate Jenessa Duncombe is investigating how the movement of water impacts heat and oxygen exchange at the interface of the ocean and atmosphere. Combining analytical and modeling approaches in the labs of Roger Samelson and Eric Skyllingstad, Jenessa uses linear stability analysis to predict the circulation of water in the upper 300 feet of the ocean. Jenessa focuses on regions in the ocean with high rates of ocean and atmosphere exchange; those areas are common throughout the ocean, typically occurring near river mouths, along upwelling regions, or along strong surface currents, like the Gulf Stream. These regions can be thought of as the lungs of the ocean, responsible for the majority of oxygen and carbon dioxide uptake into the ocean. Jenessa’s goal for her research is to improve how surface ocean circulation is accounted for in global climate change models, hopefully making model predictions more accurate.

Satellite sea surface temperature image of the Gulf Stream. The red colors show the warm Gulf Stream waters traveling from the Gulf of Mexico, along the east coast, then traveling out into the Atlantic. Whirlpools of warm and cold water, called eddies, pinch off as the Gulf Stream becomes unstable heading into the Atlantic Ocean. Ocean eddies are (in Jenessa’s opinion) the coolest type of ocean circulation! For a dynamic look at ocean surface currents, check out this video from NASA called Perpetual Ocean. You can see the Gulf Stream and other strong currents, as well as whirlpools of warm and cold water spinning up in the ocean!

Jenessa’s interest in earth science began during middle school with encouragement from an inspirational teacher. During her undergraduate studies at Wesleyan University in Connecticut, Jenessa decided to major in earth science after becoming acquainted with other earth science majors who shared her interest in hiking. Structural geology and a physics course on the topic of waves and oscillations were among her favorite courses. In particular, waves and oscillations provided insight and clarity into her realization that visual patterns can be described by a mathematical equation. Jenessa cites a summer REU (Research Experiences for Undergraduates) at the University of Maryland through the NSF as a critical introduction to research. During the summer after finishing her undergraduate studies, Jenessa worked at Sandia National Laboratories in New Mexico, acquiring experience in research related to harnessing power generated from wave energy. After finishing her Masters degree, Jenessa plans to pursue a career in science writing.

Tune in on September 25th 2016 at 7PM to hear more from Jenessa about her research related to the movement of water in the ocean and the role it may play in climate change. You can listen on the radio at 88.7FM KBVR Corvallis or by streaming live.

Hungry, Hungry Microbes!

Today ocean acidification is one of the most significant threats to marine biodiversity in recorded human history. Caused primarily by excess carbon dioxide in the atmosphere, the decreasing pH of the world’s oceans is projected to reach a level at which a majority of coral reefs will die off by 2050. This would have global impacts on marine life; when it comes to maintaining total worldwide biodiversity, coral reefs are the most diverse and valuable ecosystems on the planet.

Unfortunately, there is reason to believe that ocean acidification might proceed at levels even faster than those predicted. Large resevoirs methane hydrates locked away in deep sea ice deposits under the ocean floor appear to be melting and releasing methane into the ocean and surrounding sediments due to the increasing temperature of the world’s oceans. If this process accelerates as waters continue to warm, then the gas escaping into the ocean and air might accelerate ocean acidification and other aspects of global climate change. That is, unless something– or someone– can stop it.

The area of the seafloor Scott studies lies several hundred to a few thousand meters below the surface–much too deep (and cold!) to dive down. Scott gets on a ship and works with a team of experienced technicians who use a crane to lift a device called a gravity corer off the ship deck and into the water, lowering it until it reaches the bottom, capturing and retrieving sediment.

This is where methanotrophs and Scott Klasek come in. A 3rd year PhD student in Microbiology at Oregon State University, Scott works with his advisor in CEOAS Rick Colwell and with Marta Torres to study the single celled creatures that live in the deep sea floor and consume excess methane. Because of their importance in the carbon cycle, and their potential value in mitigating the negative effects of deep sea methane hydrate melting, these methanotrophs have become a valuable subject of study in the fight to manage the changes in our environment occurring that have been associated with anthropogenic climate change.

Here Scott is opening a pressure reactor to sample the sediment inside. Sediment cores retrieved form the ocean floor can be used for microbial DNA extraction and other geochemical measurements. Scott places sediment samples in these reactors and incubates them at the pressure and temperature they were collected at, adding different amounts of methane to them to see how the microbial communities and methane consumption change over weeks and months.

Most people don’t wake up one morning as a kid and say to themselves, “You know what I want to be when I grow up? Someone who studies methanotrophs and the threat of warming arctic waters.” Scott Klasek is no exception, in fact, he went into his undergraduate career at University of Wisconsin, Madison expecting to pursue an academic career path in pre med. To learn all about Scott’s research, and the twists and turns that led him to it, tune in this Sunday, April 10th, at 7pm to 88.7 KBVR FM or stream the show live!