Relative Particle Density (RPD) calculations using High Frequency Radar (HFR) observed surface currents around Palmer Deep Canyon from January to March of 2020

dc.contributor.author Veatch, Jacquelyn
dc.contributor.author Klinck, John M.
dc.contributor.author Oliver, Matthew
dc.contributor.author Kohut, Joshua
dc.contributor.author Statscewich, Hank
dc.coverage.spatial West Antarctic Peninsula
dc.coverage.spatial westlimit: -64.6; southlimit: -65; eastlimit: -63.8; northlimit: -64.7
dc.coverage.temporal 20200109 - 20200331 (UTC)
dc.date.accessioned 2024-01-23T16:04:23Z
dc.date.available 2024-01-23T16:04:23Z
dc.date.created 2024-01-08
dc.date.issued 2024-01-23
dc.description Dataset: Relative Particle Density
dc.description.abstract Relative Particle Density (RPD) reports the position of drifters at a single timestamp by normalizing the density of drifters within a gridded bin system in the study field. Relative Particle Density calculations begin with releasing virtual particles over a regular grid and tracking them through a velocity field (High Frequency Radar observed surface currents). RPD is then quantified by summing the number of drifters in each grid box, and normalizing by the median number of drifters in all grid boxes. New particles were released in a regular grid across the 80 % coverage of the HFR footprint every three hours. Particles were not counted until they had been advected in the velocity field for 6 hours (when the autocorrelation of the HFR velocities cross the e-fold), and were no longer counted when they were advected out of the HFR domain, or after they became three days old. Given the average residence time of 2 days (Kohut et al., 2018), the three-day threshold was 245 chosen to coordinate with the time phytoplankton will spend in the surface layer of the study domain. This methodology follows that used by (Oliver et al., 2019; Veatch et al., 2022, preprint: not peer reviewed). RPD reports the normalized number of drifters present in each gridded bin at each timestamp (Veatch et al., 2024 Figure 2C). Two dimensional HFR data is used to calculate RPD, creating the assumption that the integrated surface divergence is zero, and no particles are lost from the surface due to vertical velocities. Therefore, RPD will map the instantaneous concentration of surface associated particles across the entire domain given the evolving surface current fields provided by the HFR. For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/917926
dc.description.sponsorship NSF Office of Polar Programs (formerly NSF PLR) (NSF OPP) OPP-1745009, NSF Office of Polar Programs (formerly NSF PLR) (NSF OPP) OPP-1744884, NSF Office of Polar Programs (formerly NSF PLR) (NSF OPP) OPP-1745011
dc.identifier.citation Veatch, J., Klinck, J. M., Oliver, M., Kohut, J., & Statscewich, H. (2024). Relative Particle Density (RPD) calculations using High Frequency Radar (HFR) observed surface currents around Palmer Deep Canyon from January to March of 2020 (Version 1) [Data set]. Biological and Chemical Oceanography Data Management Office (BCO-DMO). https://doi.org/10.26008/1912/BCO-DMO.917926.1
dc.identifier.doi 10.26008/1912/bco-dmo.917926.1
dc.identifier.uri https://hdl.handle.net/1912/67497
dc.language.iso en_US
dc.publisher Biological and Chemical Oceanography Data Management Office (BCO-DMO). Contact: bco-dmo-data@whoi.edu
dc.relation.uri http://lod.bco-dmo.org/id/dataset/917926
dc.relation.uri https://doi.org/10.26008/1912/bco-dmo.917926.1
dc.rights Creative Commons Attribution 4.0
dc.rights.uri https://creativecommons.org/licenses/by/4.0/
dc.subject Lagrangian Coherent Structures
dc.subject Relative Particle Density
dc.subject High Frequency Radar
dc.title Relative Particle Density (RPD) calculations using High Frequency Radar (HFR) observed surface currents around Palmer Deep Canyon from January to March of 2020
dc.type Dataset
dspace.entity.type Publication
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