2015
DOI: 10.1371/journal.pone.0141101
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Ocean Heat Content Reveals Secrets of Fish Migrations

Abstract: For centuries, the mechanisms surrounding spatially complex animal migrations have intrigued scientists and the public. We present a new methodology using ocean heat content (OHC), a habitat metric that is normally a fundamental part of hurricane intensity forecasting, to estimate movements and migration of satellite-tagged marine fishes. Previous satellite-tagging research of fishes using archival depth, temperature and light data for geolocations have been too coarse to resolve detailed ocean habitat utiliza… Show more

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Cited by 31 publications
(23 citation statements)
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“…Sea surface temperature corrected Kalman filter tracks were further refined with the fine‐scale geolocation method of Luo et al () which incorporated OHC estimated from Hybrid Coordinate Ocean Model (HYCOM) and a genetic algorithm (GA‐OHC). The concept of the OHC method, originally developed for use in hurricane intensity forecasts, integrates the thermal energy from the depths associated with the 26°C isotherm (D26) to the ocean surface following the equation of Palmen ().OHC=cnormalpρfalse∫D260Tz-26dz,where c p is the specific heat constant of water, ρ is seawater density, and T z is water temperature at depth z (Luo et al, ). In fisheries applications, the 26°C isotherm can be modified to any water temperature range, specifically by the lower bound of an animal's thermal range, such as the 20°C isotherm that we used in this study for tarpon since 99% of temperatures recorded by the tags were above this isotherm (Luo & Ault, ).…”
Section: Methodsmentioning
confidence: 99%
“…Sea surface temperature corrected Kalman filter tracks were further refined with the fine‐scale geolocation method of Luo et al () which incorporated OHC estimated from Hybrid Coordinate Ocean Model (HYCOM) and a genetic algorithm (GA‐OHC). The concept of the OHC method, originally developed for use in hurricane intensity forecasts, integrates the thermal energy from the depths associated with the 26°C isotherm (D26) to the ocean surface following the equation of Palmen ().OHC=cnormalpρfalse∫D260Tz-26dz,where c p is the specific heat constant of water, ρ is seawater density, and T z is water temperature at depth z (Luo et al, ). In fisheries applications, the 26°C isotherm can be modified to any water temperature range, specifically by the lower bound of an animal's thermal range, such as the 20°C isotherm that we used in this study for tarpon since 99% of temperatures recorded by the tags were above this isotherm (Luo & Ault, ).…”
Section: Methodsmentioning
confidence: 99%
“…Individual likelihood surfaces for each depth level were then multiplied together for an overall profile likelihood at that time point. (5) Ocean Heat Content (OHC) was obtained by integrating the heat content of the water column above the minimum daily temperature to the most shallow depth recorded by the tag for both the tag profiles and HYCOM fields (Luo et al, 2015). All observation-based likelihoods were formed using integrated likelihood calculations (Le Bris et al, 2013).…”
Section: Geolocation Methodsmentioning
confidence: 99%
“…The most probable track for the PSAT-tagged spearfish was constructed using the HMMoce package for R (Braun, Galuardi, & Thorrold, 2018). This approach leverages light levels, sea surface temperature (SST), depth-temperature profiles, and bathymetry Observation-based likelihoods were calculated at 12-hour resolution on a 9 km grid from remotely sensed SST, light-based longitude, and depth-temperature profile data collected by the tags, using three separate likelihood calculations: (a) An SST likelihood was generated for tag-based SST values compared to daily 1 km remotely sensed SST from Level-4 GHRSST products (Chao & Li, 2009);(b) light-based longitude likelihood was derived using estimates of longitude from GPE2 software (Wildlife Computers, Inc.); and (c) ocean heat content (OHC; Braun, Skomal, & Thorrold, 2018;Luo et al, 2015) was obtained by integrating the heat content of the water column above the 18°isotherm to the most shallow depth recorded by the tag. Tag-based OHC was compared to OHC calculations performed on daily reanalysis model depth-temperature products from the HYbrid Coordinate Ocean Model (HYCOM, 0.08°resolution; Bleck, 2002;Chassignet et al, 2007).…”
Section: Geolocation Methodsmentioning
confidence: 99%