Unsupervised clustering identifies thermohaline staircases in the Canada Basin of the Arctic Ocean

Thermohaline staircases are a widespread stratification feature that impact the vertical transport of heat and nutrients and are consistently observed throughout the Canada Basin of the Arctic Ocean. Observations of staircases from the same time period and geographic region form clusters in temperat...

Full description

Bibliographic Details
Main Authors: Schee, Mikhail, Rosenblum, Erica, Lilly, Jonathan, Grisouard, Nicolas
Format: Other/Unknown Material
Language:unknown
Published: California Digital Library (CDL) 2024
Subjects:
Online Access:http://dx.doi.org/10.31223/x5v67w
id crescholarship:10.31223/x5v67w
record_format openpolar
spelling crescholarship:10.31223/x5v67w 2024-05-12T07:59:40+00:00 Unsupervised clustering identifies thermohaline staircases in the Canada Basin of the Arctic Ocean Schee, Mikhail Rosenblum, Erica Lilly, Jonathan Grisouard, Nicolas 2024 http://dx.doi.org/10.31223/x5v67w unknown California Digital Library (CDL) posted-content 2024 crescholarship https://doi.org/10.31223/x5v67w 2024-04-18T08:47:18Z Thermohaline staircases are a widespread stratification feature that impact the vertical transport of heat and nutrients and are consistently observed throughout the Canada Basin of the Arctic Ocean. Observations of staircases from the same time period and geographic region form clusters in temperature-salinity ($T$--$S$) space. Here, for the first time, we use an automated clustering algorithm called the Hierarchical Density-Based Spatial Clustering of Applications with Noise (HDBSCAN), to detect and connect individual well-mixed staircase layers across profiles from Ice-Tethered Profilers (ITPs). Our application only requires an estimate of the typical layer thickness and expected salinity range of staircases. We compare this method to two previous studies that used different approaches to detect layers, and reproduce several results including the mean lateral density ratio $R_L$ and that the difference in salinity between neighboring layers is a magnitude larger than the salinity variance within a layer. We find that we can accurately and automatically track individual layers in coherent staircases across time and space between different profiles. In evaluating the algorithm's performance, we find evidence of different physical features, namely splitting or merging layers and remnant intrusions. Further, we find a dependence of $R_L$ on pressure, whereas previous studies have reported constant $R_L$. Our results demonstrate that clustering algorithms are an effective and parsimonious method of identifying staircases in ocean profile data. Other/Unknown Material Arctic Arctic Ocean canada basin eScholarship Repository (University of California) Arctic Arctic Ocean Canada
institution Open Polar
collection eScholarship Repository (University of California)
op_collection_id crescholarship
language unknown
description Thermohaline staircases are a widespread stratification feature that impact the vertical transport of heat and nutrients and are consistently observed throughout the Canada Basin of the Arctic Ocean. Observations of staircases from the same time period and geographic region form clusters in temperature-salinity ($T$--$S$) space. Here, for the first time, we use an automated clustering algorithm called the Hierarchical Density-Based Spatial Clustering of Applications with Noise (HDBSCAN), to detect and connect individual well-mixed staircase layers across profiles from Ice-Tethered Profilers (ITPs). Our application only requires an estimate of the typical layer thickness and expected salinity range of staircases. We compare this method to two previous studies that used different approaches to detect layers, and reproduce several results including the mean lateral density ratio $R_L$ and that the difference in salinity between neighboring layers is a magnitude larger than the salinity variance within a layer. We find that we can accurately and automatically track individual layers in coherent staircases across time and space between different profiles. In evaluating the algorithm's performance, we find evidence of different physical features, namely splitting or merging layers and remnant intrusions. Further, we find a dependence of $R_L$ on pressure, whereas previous studies have reported constant $R_L$. Our results demonstrate that clustering algorithms are an effective and parsimonious method of identifying staircases in ocean profile data.
format Other/Unknown Material
author Schee, Mikhail
Rosenblum, Erica
Lilly, Jonathan
Grisouard, Nicolas
spellingShingle Schee, Mikhail
Rosenblum, Erica
Lilly, Jonathan
Grisouard, Nicolas
Unsupervised clustering identifies thermohaline staircases in the Canada Basin of the Arctic Ocean
author_facet Schee, Mikhail
Rosenblum, Erica
Lilly, Jonathan
Grisouard, Nicolas
author_sort Schee, Mikhail
title Unsupervised clustering identifies thermohaline staircases in the Canada Basin of the Arctic Ocean
title_short Unsupervised clustering identifies thermohaline staircases in the Canada Basin of the Arctic Ocean
title_full Unsupervised clustering identifies thermohaline staircases in the Canada Basin of the Arctic Ocean
title_fullStr Unsupervised clustering identifies thermohaline staircases in the Canada Basin of the Arctic Ocean
title_full_unstemmed Unsupervised clustering identifies thermohaline staircases in the Canada Basin of the Arctic Ocean
title_sort unsupervised clustering identifies thermohaline staircases in the canada basin of the arctic ocean
publisher California Digital Library (CDL)
publishDate 2024
url http://dx.doi.org/10.31223/x5v67w
geographic Arctic
Arctic Ocean
Canada
geographic_facet Arctic
Arctic Ocean
Canada
genre Arctic
Arctic Ocean
canada basin
genre_facet Arctic
Arctic Ocean
canada basin
op_doi https://doi.org/10.31223/x5v67w
_version_ 1798841252246978560