Estimating temperature in Fram Strait using DAMOCLES and ACOBAR acoustic tomography data by exploiting small-scale variability

The effects of the small-scale ocean variablity in Fram Strait on the acoustic propagation there are now well documented. In the process of working through the acoustic forward problem to understand the nature of the tomography data acquired there, a more accurate approach to computing inverses of t...

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Main Author: Dushaw, Brian
Format: Report
Language:English
Published: Zenodo 2017
Subjects:
Online Access:https://doi.org/10.5281/zenodo.7432202
id ftzenodo:oai:zenodo.org:7432202
record_format openpolar
spelling ftzenodo:oai:zenodo.org:7432202 2024-09-09T19:25:46+00:00 Estimating temperature in Fram Strait using DAMOCLES and ACOBAR acoustic tomography data by exploiting small-scale variability Dushaw, Brian 2017-12-13 https://doi.org/10.5281/zenodo.7432202 eng eng Zenodo https://zenodo.org/communities/nersc-research https://doi.org/10.5281/zenodo.7432201 https://doi.org/10.5281/zenodo.7432202 oai:zenodo.org:7432202 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Oceanography Arctic Fram Strait Acoustics Tomography Acoustic propagation Inverse model info:eu-repo/semantics/report 2017 ftzenodo https://doi.org/10.5281/zenodo.743220210.5281/zenodo.7432201 2024-07-27T06:26:26Z The effects of the small-scale ocean variablity in Fram Strait on the acoustic propagation there are now well documented. In the process of working through the acoustic forward problem to understand the nature of the tomography data acquired there, a more accurate approach to computing inverses of those data to obtain estimates for sound speed or temperature became apparent. This approach exploits the stochastic effects on the acoustic ray paths and travel times; inasmuch as it relies on the essential nature of the acoustic propagation it is an optimal approach to inverse estimates. Although the steps to computing the inverses for Fram Strait are documented by existing recent publications in the major oceanographic journals, the precise formulations for the components of the inverses presently employed are separated in several of those publications. This report therefore brings these pieces together into a single document, while showing some of the details of the inverse estimates and documenting some of the results for each of the acoustic paths for which data are available. NERSC Technical Report no. 378 Report Arctic Fram Strait Zenodo Arctic Damocles ENVELOPE(-69.350,-69.350,-69.650,-69.650)
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Oceanography
Arctic
Fram Strait
Acoustics
Tomography
Acoustic propagation
Inverse model
spellingShingle Oceanography
Arctic
Fram Strait
Acoustics
Tomography
Acoustic propagation
Inverse model
Dushaw, Brian
Estimating temperature in Fram Strait using DAMOCLES and ACOBAR acoustic tomography data by exploiting small-scale variability
topic_facet Oceanography
Arctic
Fram Strait
Acoustics
Tomography
Acoustic propagation
Inverse model
description The effects of the small-scale ocean variablity in Fram Strait on the acoustic propagation there are now well documented. In the process of working through the acoustic forward problem to understand the nature of the tomography data acquired there, a more accurate approach to computing inverses of those data to obtain estimates for sound speed or temperature became apparent. This approach exploits the stochastic effects on the acoustic ray paths and travel times; inasmuch as it relies on the essential nature of the acoustic propagation it is an optimal approach to inverse estimates. Although the steps to computing the inverses for Fram Strait are documented by existing recent publications in the major oceanographic journals, the precise formulations for the components of the inverses presently employed are separated in several of those publications. This report therefore brings these pieces together into a single document, while showing some of the details of the inverse estimates and documenting some of the results for each of the acoustic paths for which data are available. NERSC Technical Report no. 378
format Report
author Dushaw, Brian
author_facet Dushaw, Brian
author_sort Dushaw, Brian
title Estimating temperature in Fram Strait using DAMOCLES and ACOBAR acoustic tomography data by exploiting small-scale variability
title_short Estimating temperature in Fram Strait using DAMOCLES and ACOBAR acoustic tomography data by exploiting small-scale variability
title_full Estimating temperature in Fram Strait using DAMOCLES and ACOBAR acoustic tomography data by exploiting small-scale variability
title_fullStr Estimating temperature in Fram Strait using DAMOCLES and ACOBAR acoustic tomography data by exploiting small-scale variability
title_full_unstemmed Estimating temperature in Fram Strait using DAMOCLES and ACOBAR acoustic tomography data by exploiting small-scale variability
title_sort estimating temperature in fram strait using damocles and acobar acoustic tomography data by exploiting small-scale variability
publisher Zenodo
publishDate 2017
url https://doi.org/10.5281/zenodo.7432202
long_lat ENVELOPE(-69.350,-69.350,-69.650,-69.650)
geographic Arctic
Damocles
geographic_facet Arctic
Damocles
genre Arctic
Fram Strait
genre_facet Arctic
Fram Strait
op_relation https://zenodo.org/communities/nersc-research
https://doi.org/10.5281/zenodo.7432201
https://doi.org/10.5281/zenodo.7432202
oai:zenodo.org:7432202
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.743220210.5281/zenodo.7432201
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