Environmental Internship Program - 2023 Booklet

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05.12.2023 Views

OCEANS AND ATMOSPHERE Hugh Shields ’24 GEOSCIENCES Certificates: Applied and Computational Mathematics, Statistics and Machine Learning PROJECT TITLE SubZero: Discrete Element Sea Ice Modeling ORGANIZATION(S) School of Oceanography, University of Washington LOCATION(S) Seattle, Washington MENTOR(S) Georgy Manucharyan, Assistant Professor, School of Oceanography, University of Washington; Brandon Montemuro, Postdoctoral Scholar, School of Oceanography, University of Washington My research focused on pancake ice, a type of sea ice composed of rounded floes. Pancake ice is found in the Southern Ocean and has begun appearing more frequently in the Arctic due to climate change. The scale of pancake ice formation is too small to be resolved in today’s global climate models, and the processes that drive pancake ice formation are poorly understood. As pancake ice becomes more common, understanding its formation will be useful for naval navigation of an increasingly ice-free Arctic and will also help resolve oceanatmosphere couplings in climate models. I worked to reproduce pancake ice in SubZero, a sea ice model that represents chunks of ice as an interacting set of polygons constrained by physical laws, that can fracture, weld together and interact with topography. Specifically, I developed code to represent wavefields in the model, improving corner fracturing of floes at a small scale, and building in the capability for wave curvature-induced fractures, which are necessary processes for pancake ice formation. Working with SubZero gave me insight into the computational challenges of working with a complex discrete element model and the difficulties of modeling processes that are hard to observe. 92

Sophia Villacorta ’24 GEOSCIENCES OCEANS AND ATMOSPHERE PROJECT TITLE A Revised Pleistocene View of the Effect of Climate on North Pacific Oxygenation From Foraminifera-bound Nitrogen Isotopes ORGANIZATION(S) Sigman Research Laboratory, Department of Geosciences, Princeton University LOCATION(S) Princeton, New Jersey MENTOR(S) Daniel Sigman, Dusenbury Professor of Geological and Geophysical Sciences, Professor of Geosciences; Matthew Lacerra, Ph.D. candidate, Geosciences I utilized the foraminifera-bound nitrogen isotope as a climate proxy to reconstruct past changes in water-column denitrification strength in the Eastern Tropical North Pacific (ETNP). I focused on the region’s oxygen deficient zone, which is formed through a combination of slow ventilation and high biological productivity. Reconstructing this zone’s history is important for understanding climate controls on various ocean processes, including oxygen content, circulation and nutrient cycling. Under low oxygen conditions, organisms rely on nitrate for respiration, which increases the ratio of nitrogen-15 to nitrogen-14 ( 15 N/ 14 N) in the remaining nitrate. This nitrate is eventually consumed by organisms such as foraminifera in the surface ocean. When the resulting organic matter is buried on the seafloor, it preserves the signal of water column denitrification strength through time. I processed samples by sieving sediment material under a microscope to isolate specimens of two species of foraminifera, Neogloboquadrina dutertrei and Globorotalia menardii. I also assisted in chemically cleaning the specimens to prepare them for nitrogen isotope measurements using a mass spectrometer. I now have a solid grasp of this ocean system and how nitrogen isotopes can be used as a proxy for paleoclimate, which I hope to examine further in my senior independent research. 93

OCEANS AND<br />

ATMOSPHERE<br />

Hugh Shields ’24<br />

GEOSCIENCES<br />

Certificates: Applied and Computational<br />

Mathematics, Statistics and Machine Learning<br />

PROJECT TITLE<br />

SubZero: Discrete Element<br />

Sea Ice Modeling<br />

ORGANIZATION(S)<br />

School of Oceanography,<br />

University of Washington<br />

LOCATION(S)<br />

Seattle, Washington<br />

MENTOR(S)<br />

Georgy Manucharyan,<br />

Assistant Professor,<br />

School of Oceanography,<br />

University of Washington;<br />

Brandon Montemuro,<br />

Postdoctoral Scholar,<br />

School of Oceanography,<br />

University of Washington<br />

My research focused on pancake ice, a type of<br />

sea ice composed of rounded floes. Pancake ice<br />

is found in the Southern Ocean and has begun<br />

appearing more frequently in the Arctic due<br />

to climate change. The scale of pancake ice<br />

formation is too small to be resolved in today’s<br />

global climate models, and the processes<br />

that drive pancake ice formation are poorly<br />

understood. As pancake ice becomes more<br />

common, understanding its formation will be<br />

useful for naval navigation of an increasingly<br />

ice-free Arctic and will also help resolve oceanatmosphere<br />

couplings in climate models. I<br />

worked to reproduce pancake ice in SubZero, a<br />

sea ice model that represents chunks of ice as<br />

an interacting set of polygons constrained by<br />

physical laws, that can fracture, weld together<br />

and interact with topography. Specifically, I<br />

developed code to represent wavefields in the<br />

model, improving corner fracturing of floes at<br />

a small scale, and building in the capability for<br />

wave curvature-induced fractures, which are<br />

necessary processes for pancake ice formation.<br />

Working with SubZero gave me insight into<br />

the computational challenges of working with<br />

a complex discrete element model and the<br />

difficulties of modeling processes that are hard to<br />

observe.<br />

92

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