In-situ sea temperature (∘C) and salinity (psu) at 800 m depth in the Madeira and Canary Islands region for the year 1990, based on CORA v5.2.

The left panel shows temperature and the right panel shows salinity. Warmer temperatures and higher salinity are represented in red tones, while cooler and fresher values appear in blue. Grid smoothing was applied to reduce artifacts due to sparse data coverage, particularly near islands and contine...

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Detalles Bibliográficos
Autores: Vasconcelos, Joana, Martínez, Javier, Guerra-Marrero, Airam, Otero-Ferrer, José Luis, Jurado-Ruzafa, Alba, Sousa, Ricardo, Hernández-González, Carlos Luis, Freitas, Mafalda, Tuset, Víctor M.
Tipo de recurso: conjunto de datos
Estado:Versión publicada
Fecha de publicación:2025
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/397360
Acceso en línea:http://hdl.handle.net/10261/397360
Access Level:acceso abierto
Palabra clave:Provides valuable insights
Offshore areas may
Effective fisheries management
Economically important scabbardfish
Drifting longline fishery
Div >< p
Improves species discrimination
Clarifying species identity
Accurate species identification
Aphanopus intermedius </
Aphanopus carbo </
Aphanopus </
Intermedius </
Carbo </
Cryptic species
Study explores
Study demonstrates
Stock assessments
Spawning season
Similar morphologies
Progressive expansion
Population dynamics
Overlapping ranges
Otolith samples
Northeastern atlantic
New grounds
Likely influenced
Including variations
Higher presence
Habitat use
Generally dominating
Findings contribute
Environmental changes
Depths greater
Based method
Analyzed using
African coast
Descripción
Sumario:The left panel shows temperature and the right panel shows salinity. Warmer temperatures and higher salinity are represented in red tones, while cooler and fresher values appear in blue. Grid smoothing was applied to reduce artifacts due to sparse data coverage, particularly near islands and continental slopes. These maps provide an indicative overview of oceanographic conditions at the onset of the study period, but are not directly comparable to GLORYS12V1-based maps of potential temperature.

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