Environmental Internship Program - 2023 Booklet
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
- Page 41 and 42: Sriya Kotta ’26 CIVIL AND ENVIRON
- Page 43 and 44: Charlie Nuermberger ’25 COMPARATI
- Page 45 and 46: Jamie Rodriguez ’24 ENGLISH PROJE
- Page 47 and 48: Molly Taylor ’25 HISTORY Certific
- Page 49 and 50: Lily Weaver ’26 COMPUTER SCIENCE
- Page 51 and 52: Brooke Beers ’25 CIVIL AND ENVIRO
- Page 53 and 54: Sava Evangelista ’26 COMPUTER SCI
- Page 55 and 56: Alliyah Gregory ’25 ECOLOGY AND E
- Page 57 and 58: Noe Iwasaki ’26 UNDECLARED PROJEC
- Page 59 and 60: Chien Nguyen ’25 COMPUTER SCIENCE
- Page 61 and 62: Martina Qua ’25 CIVIL AND ENVIRON
- Page 63 and 64: Angelica She ’26 CIVIL AND ENVIRO
- Page 65 and 66: Sarina Wen ’26 CHEMICAL AND BIOLO
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- Page 71 and 72: Yagiz Devre ’26 COMPUTER SCIENCE
- Page 73 and 74: Helena Frudit ’25 MECHANICAL AND
- Page 75 and 76: John Kim ’25 PHYSICS Certificates
- Page 77 and 78: Nicholas Lim ’24 SCHOOL OF PUBLIC
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- Page 81 and 82: Chloe Park ’25 CHEMISTRY Certific
- Page 83 and 84: Azhar Razin ’26 CHEMICAL AND BIOL
- Page 85 and 86: Maya Avida ’26 PHYSICS Certificat
- Page 87 and 88: Rebecca Cho ’26 GEOSCIENCES OCEAN
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- Page 95 and 96: Tienne Yu ’26 MOLECULAR BIOLOGY O
- Page 97 and 98: Braeden Carroll ’26 CIVIL AND ENV
- Page 99 and 100: Ashley DeFrates ’25 CIVIL AND ENV
- Page 101 and 102: PROJECT TITLE Molecular Simulation
- Page 103 and 104: Wiley Kohler ’25 MATHEMATICS PROJ
- Page 105 and 106: Christopher Li ’26 CIVIL AND ENVI
- Page 107 and 108: Alyssa Ritchie ’25 CHEMISTRY Cert
- Page 109 and 110: Acknowledgments FUNDING FOR THE 202
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