A comparison of coastal trapped wave model with velocity observations in Norske Trough, Northeast Greenland

Bottom-intensified flow of warm ocean water leads to basal melting of many Greenland glaciers. I here focus on Norske Trough, a topographic depression that transects the generally 150-m shallow continental shelf of Northeast Greenland where I analyze velocity, temperature, and salinity measured from...

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Main Author: Bae, Sohyun
Format: Thesis
Language:English
Published: University of Delaware 2021
Subjects:
Online Access:https://udspace.udel.edu/handle/19716/30066
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spelling ftunivdelaware:oai:udspace.udel.edu:19716/30066 2023-06-11T04:12:11+02:00 A comparison of coastal trapped wave model with velocity observations in Norske Trough, Northeast Greenland Bae, Sohyun 2021-09-30T19:13:17Z application/pdf https://udspace.udel.edu/handle/19716/30066 en eng University of Delaware https://login.udel.idm.oclc.org/login?url=https://www.proquest.com/dissertations-theses/comparison-coastal-trapped-wave-model-with/docview/2588066008/se-2?accountid=10457 1292743216 https://udspace.udel.edu/handle/19716/30066 Coastal trapped wave model Velocity observation Norske Trough Thesis 2021 ftunivdelaware 2023-05-01T12:57:08Z Bottom-intensified flow of warm ocean water leads to basal melting of many Greenland glaciers. I here focus on Norske Trough, a topographic depression that transects the generally 150-m shallow continental shelf of Northeast Greenland where I analyze velocity, temperature, and salinity measured from 2016 to 2017. A year-long mooring record indicates mean currents of about 6 cm/s towards the glaciers. Empirical Orthogonal Functions (EOF) reveal that about 80% of the variance is in the same direction as the mean flow. Currents thus move along the sloping bottom towards the glaciers and are modulated by temporal fluctuations. I identify monthly oscillations that are especially pronounced in winter. A more persistent oscillation at 24 days has an amplitude of about 1 cm/s that I diagnose for topographic Rossby wave dynamics. Horizontal motions at this frequency are almost uniform with depth, however, density stratification is not negligible. Observed Burger numbers B are Ο(1) with B={L_d}^2/L^2, L_d the internal Rossby radius, and L the width of the Norske Trough slope region. Ocean physics thus contain both barotropic and baroclinic elements of Rossby wave theory. Predicted and observed velocity profiles across the slope region agree well enough for a 16 km wide channel, however, the dispersion relation for such channels does not allow for baroclinic Rossby waves with the small vertical current shear I observe at monthly periods. I thus conclude that observations and theory are not entirely consistent and do not support the hypothesis that linear topographic Rossby waves explain velocity variations in Norske Trough unambiguously. Muenchow, Andreas M.S. University of Delaware, School of Marine Science and Policy Thesis Greenland The University of Delaware Library Institutional Repository Greenland Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008)
institution Open Polar
collection The University of Delaware Library Institutional Repository
op_collection_id ftunivdelaware
language English
topic Coastal trapped wave model
Velocity observation
Norske Trough
spellingShingle Coastal trapped wave model
Velocity observation
Norske Trough
Bae, Sohyun
A comparison of coastal trapped wave model with velocity observations in Norske Trough, Northeast Greenland
topic_facet Coastal trapped wave model
Velocity observation
Norske Trough
description Bottom-intensified flow of warm ocean water leads to basal melting of many Greenland glaciers. I here focus on Norske Trough, a topographic depression that transects the generally 150-m shallow continental shelf of Northeast Greenland where I analyze velocity, temperature, and salinity measured from 2016 to 2017. A year-long mooring record indicates mean currents of about 6 cm/s towards the glaciers. Empirical Orthogonal Functions (EOF) reveal that about 80% of the variance is in the same direction as the mean flow. Currents thus move along the sloping bottom towards the glaciers and are modulated by temporal fluctuations. I identify monthly oscillations that are especially pronounced in winter. A more persistent oscillation at 24 days has an amplitude of about 1 cm/s that I diagnose for topographic Rossby wave dynamics. Horizontal motions at this frequency are almost uniform with depth, however, density stratification is not negligible. Observed Burger numbers B are Ο(1) with B={L_d}^2/L^2, L_d the internal Rossby radius, and L the width of the Norske Trough slope region. Ocean physics thus contain both barotropic and baroclinic elements of Rossby wave theory. Predicted and observed velocity profiles across the slope region agree well enough for a 16 km wide channel, however, the dispersion relation for such channels does not allow for baroclinic Rossby waves with the small vertical current shear I observe at monthly periods. I thus conclude that observations and theory are not entirely consistent and do not support the hypothesis that linear topographic Rossby waves explain velocity variations in Norske Trough unambiguously. Muenchow, Andreas M.S. University of Delaware, School of Marine Science and Policy
format Thesis
author Bae, Sohyun
author_facet Bae, Sohyun
author_sort Bae, Sohyun
title A comparison of coastal trapped wave model with velocity observations in Norske Trough, Northeast Greenland
title_short A comparison of coastal trapped wave model with velocity observations in Norske Trough, Northeast Greenland
title_full A comparison of coastal trapped wave model with velocity observations in Norske Trough, Northeast Greenland
title_fullStr A comparison of coastal trapped wave model with velocity observations in Norske Trough, Northeast Greenland
title_full_unstemmed A comparison of coastal trapped wave model with velocity observations in Norske Trough, Northeast Greenland
title_sort comparison of coastal trapped wave model with velocity observations in norske trough, northeast greenland
publisher University of Delaware
publishDate 2021
url https://udspace.udel.edu/handle/19716/30066
long_lat ENVELOPE(-60.729,-60.729,-64.008,-64.008)
geographic Greenland
Andreas
geographic_facet Greenland
Andreas
genre Greenland
genre_facet Greenland
op_relation https://login.udel.idm.oclc.org/login?url=https://www.proquest.com/dissertations-theses/comparison-coastal-trapped-wave-model-with/docview/2588066008/se-2?accountid=10457
1292743216
https://udspace.udel.edu/handle/19716/30066
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