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author Perez, José Angel Alvarez
Sant'Ana, Rodrigo
author_facet Perez, José Angel Alvarez
Sant'Ana, Rodrigo
collection Datos científicos de ciencias marinas y ambientales
contents The 'Mean Temperature of Catch (MTC)' was estimated for each year of the time series, as proposed by Cheung et al. (2013). This variable is expressed in degrees Celsius. 'Sea Bottom Temperature (SBT)' was derived from estimates provided by the high-resolution ocean general circulation INALT20 model (Schwarzkopf et al., 2019) for the study period (2000-2019) and was calculated by averaging the temperatures over 0.25° x 0.25° grid cells of the BMM and a water column up to 50 m above the seafloor. This variable is expressed is degrees Celsius. 'Annual volume transports of the Brazil-Malvinas confluence (BCt)' was extracted and compiled from Artana et al. (2019). This index was estimated for the period between 2000 and 2017. More detailed information about this index can be accessed in Artana et al. (2019). This variable expressed in Sverdrups (Sv). 'Simpson diversity index (Dm)' express the diversity of demersal fishing métiers (i.e. combination of target species, gear, and time of the year) operating each year of the time series, as determined by a process of classification of individual fishing trips. Catches of each métier operating during each year of time series summed and used to calculate Dm using the Simpson species diversity index formulation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_946391
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Environmental, oceanographic and fisheries strategy time series (2000-2019) for demersal species in the Brazilian Meridional Margin
Perez, José Angel Alvarez
Sant'Ana, Rodrigo
Bottom water temperature; Brazilian_Demersal_Fisheries_Time_Series; Catch composition; Climate change; DATE/TIME; Fishing port survey; iAtlantic; INHALT (General ocean circulation model), Schwarzkopf et al. 2019; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; Model; Simpson index of diversity; Simpson index of diversity, standard deviation; Southwest Atlantic; SW Atlantic; Temperature, water; Temperature anomaly; Transport, volumetric
The 'Mean Temperature of Catch (MTC)' was estimated for each year of the time series, as proposed by Cheung et al. (2013). This variable is expressed in degrees Celsius. 'Sea Bottom Temperature (SBT)' was derived from estimates provided by the high-resolution ocean general circulation INALT20 model (Schwarzkopf et al., 2019) for the study period (2000-2019) and was calculated by averaging the temperatures over 0.25° x 0.25° grid cells of the BMM and a water column up to 50 m above the seafloor. This variable is expressed is degrees Celsius. 'Annual volume transports of the Brazil-Malvinas confluence (BCt)' was extracted and compiled from Artana et al. (2019). This index was estimated for the period between 2000 and 2017. More detailed information about this index can be accessed in Artana et al. (2019). This variable expressed in Sverdrups (Sv). 'Simpson diversity index (Dm)' express the diversity of demersal fishing métiers (i.e. combination of target species, gear, and time of the year) operating each year of the time series, as determined by a process of classification of individual fishing trips. Catches of each métier operating during each year of time series summed and used to calculate Dm using the Simpson species diversity index formulation.
title Environmental, oceanographic and fisheries strategy time series (2000-2019) for demersal species in the Brazilian Meridional Margin
topic Bottom water temperature; Brazilian_Demersal_Fisheries_Time_Series; Catch composition; Climate change; DATE/TIME; Fishing port survey; iAtlantic; INHALT (General ocean circulation model), Schwarzkopf et al. 2019; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; Model; Simpson index of diversity; Simpson index of diversity, standard deviation; Southwest Atlantic; SW Atlantic; Temperature, water; Temperature anomaly; Transport, volumetric
url https://doi.org/10.1594/PANGAEA.946391