Probability that the seafloor is below the halocline in the Baltic - Original point dataset ÔÇô Version 2022
Based on DHI operational Hydrodynamic 3D Model DKBS2hd model run results, a point dataset describing for each year the probability of a certain seabed location in the Baltic Sea being located below the deep halocline has been created. The spatial coverage is the Baltic Sea. The spatial resolution is 5km. The temporal coverage is 20 years (2001-2020). The dataset is a point shapefile, the attribute table of which contains the following columns
- 20 columns whose name is in the form p[yyyy] (e.g; p2001), where yyyy is the year: for the year yyyy, probability of the point location being located below the deep halocline
- column ÔÇÿmeanÔÇÖ: probability average (i.e. average of the 20 yearly probabilities)
- column ÔÇÿstdÔÇÖ: probability standard deviation across the 20 years
The development of the original point dataset was funded by the EMODnet lot ÔÇÿSeabed HabitatsÔÇÖ for use in the development of the EUSeaMap product, more specifically in modeling the spatial distribution of the biological zones ÔÇÿcircalittoralÔÇÖ and ÔÇÿoffshore circalittoralÔÇÖ. According to the EUNIS habitat classification, in the Baltic Sea the circalittoral is above the halocline/pycnocline, while the offshore circalittoral is below.
Identificatie
Alternatieve titel | PH_BAL_000l_AVG_HALOCLINE_PT |
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Versiedatum | 2022-09-15T12:00:00 |
Type versiedatum | Publicatie: Uitgavedatum van de dataset. |
Dataset identificator | Probability that the seafloor is below the halocline in the Baltic - Original point dataset ÔÇô Version 2022 |
Inhoud
Krediet | EMODnet broad-scale seabed habitat map for Europe (2022), funded by the European Commission |
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Krediet | DHI, DKBS2, Hydrodynamic Model Setup and Validation, Technical note, DHI, August 2018. Available upon request to the author (see section 'author' in the current metadata) |
Status | compleet: Productie van de data is compleet / afgerond. |
Contactgegevens dataset(serie)
Naam Contactpersoon | Poul Hammer |
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Organisatie | DHI |
ph@dhigroup.com | |
Rol | Auteur: Partij die auteur is van de data. |
Contactgegevens dataset(serie)
Naam Contactpersoon | Mickaël Vasquez |
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Organisatie | Ifremer |
Mickael.Vasquez@ifremer.fr | |
Rol | Producent: Partij die de data heeft aangemaakt. |
Contactgegevens dataset(serie)
Naam Contactpersoon | Zyad Al-Hamdani |
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Organisatie | GEUS |
azk@geus.dk | |
Rol | Producent: Partij die de data heeft aangemaakt. |
Contactgegevens dataset(serie)
Naam Contactpersoon | Verner Brandbyge Ernstsen |
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Organisatie | GEUS |
vbe@geus.dk | |
Rol | Producent: Partij die de data heeft aangemaakt. |
Trefwoorden
GEMET - INSPIRE themes, version 1.0 | Oceanographic geographical features |
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GDI-Vlaanderen Trefwoorden | Metadata GDI-Vl-conform |
Overige trefwoorden |
Halocline
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Overige trefwoorden | Baltic Sea |
Ruimtelijk schema dataset(serie) | vector: Vector data wordt gebruikt om geografische data te representeren. |
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Ruimtelijke resolutie dataset(serie)
Noemer | 5 |
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Taal | Engels |
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Karakterset | UTF-8: 8-bit variabele grootte universele karakterset, gebaseerd op ISO/IEC 10646 |
Categorie(ën) |
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Begrenzing
Omschrijving geografische begrenzing | |||||||||
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Omschrijvende rechthoek
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Identificator geografische begrenzing |
Referentiesysteem
Horizontaal en/of verticaal referentiesysteem
Unieke code | 32633 |
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Codespace | EPSG |
Kwaliteit
Niveau kwaliteitsinformatie | Dataset: Informatie heeft betrekking op de dataset. |
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Bewerkingen
Algemene beschrijving herkomst | The model was run by DHI in August 2022. Based on the model results, the final dataset was produced using the following procedure: Firstly the Brunt-Vaisala frequency squared (N2 = -g/¤ü┬Àd¤ü/dz, where g is the acceleration due to gravity, ¤ü is local water density as calculated by the hydrodynamic model and z is the vertical distance) was calculated in every model grid point horizontally and vertically for every time step. The Brunt-Vaisala frequency squared represents the strength of the stratification of the water column at a certain location. Secondly for every time step and for every horizontal grid point, the depth of the vertical maximum Brunt-Vaisala frequency squared was determined ÔÇô this depth is assumed to represent the location of the deep halocline. In order to exclude any transient haloclines in the upper water column, a limit on the halocline depth of 25m was introduced such that only the water column below 25m was considered. Another limitation introduced in the analysis is that N^2 has to be above 0.0005s^-2 before it is accepted. This means that if N^2 at a certain time in a certain horizontal location is below this limit in the whole water column, then no halocline is identified. This lower limit on N^2 was introduced after some trial-and-error, in order to avoid identifying ÔÇÿfalseÔÇÖ haloclines. Notice that this limit is influenced by both physical and model resolution considerations. Thirdly the annual probability of a certain seabed location being located under the deep halocline was calculated as the amount of time steps where a deep halocline was identified divided by the total number of time steps. The above procedure has been performed for the years delivered from 2001 to 2020 (incl.). |
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Conformiteit
Domeinconsistentie
Resultaat
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Domeinconsistentie
Resultaat
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Toegangs- en gebruiksbeperkingen
Legale en veiligheidsbeperkingen
Beperkingen van de dataset(serie)
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Beperkingen van de dataset(serie)
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Beperkingen van de dataset(serie)
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Distributie
Distributieformaat | ESRI Shapefile (Version: 1.0) | ||||||||
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Overdracht
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Meta-metadata
Metadata identificator (fileIdentifier) | 9e4edb30-aefb-4551-9c6f-7cf324b4edb3 | ||||||||
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Taal metadatarecord | Engels | ||||||||
Karakterset metadatarecord | UTF-8: 8-bit variabele grootte universele karakterset, gebaseerd op ISO/IEC 10646 | ||||||||
Hiërarchisch niveau | Dataset: Informatie heeft betrekking op de dataset. | ||||||||
Metadata wijzigingsdatum | 2022-09-12T14:56:09.194Z | ||||||||
Naam metadatastandaard | ISO 19115:2003/19139 | ||||||||
Versie metadatastandaard | 1.0 | ||||||||
Metadata-auteur
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