cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.13769354
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from 4DVARNET20 geostrophic velocities (1/24°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/20°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10912777) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.5281/zenodo.13769355
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from 4DVARNET20 geostrophic velocities (1/24°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/20°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10912777) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.15468/dl.2tdh85
title: Occurrence Download

description: A dataset containing 10 species occurrences available in GBIF matching the query:
{
 "and" : [
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil)"
 ]
 }
 },
 "Issue is one of (Continent derived from coordinates, Continent invalid, Coordinate reprojected, Coordinate rounded, Depth min max swapped, Country derived from coordinates, Depth non numeric, Depth not metric, Depth unlikely, Elevation min max swapped, Elevation non numeric, Elevation not metric, Elevation unlikely, Identified date invalid, Identified date unlikely, Modified date invalid, Modified date unlikely, Recorded date invalid, Recorded date mismatch, Recorded date unlikely, Occurrence status inferred from individual count, Georeferenced date unlikely, Georeferenced date invalid, ccurrence status inferred from basis of record)",
 "TaxonKey is Grewia cyclopetala Wawra & Peyr.",
 "Continent is Africa"
 ]
}

 The dataset includes 10 records from 6 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0028080-240906103802322/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.13769109
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from MIOST geostrophic velocities (1/72°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the MIOST algorithm (Ubelmann et al., 2019; https://doi.org/10.1029/2020JC016560) to altimetry L3-data (https://doi.org/10.5281/zenodo.10648981) at a resolution of 1/72° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/72º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.5281/zenodo.13769110
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from MIOST geostrophic velocities (1/72°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the MIOST algorithm (Ubelmann et al., 2019; https://doi.org/10.1029/2020JC016560) to altimetry L3-data (https://doi.org/10.5281/zenodo.10648981) at a resolution of 1/72° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/72º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.5281/zenodo.13753840
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from MIOST geostrophic velocities (1/24°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the MIOST algorithm (Ubelmann et al., 2019; https://doi.org/10.1029/2020JC016560) to altimetry L3-data (https://doi.org/10.5281/zenodo.10648981) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.5281/zenodo.13753841
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from MIOST geostrophic velocities (1/24°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the MIOST algorithm (Ubelmann et al., 2019; https://doi.org/10.1029/2020JC016560) to altimetry L3-data (https://doi.org/10.5281/zenodo.10648981) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.5281/zenodo.13752897
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/72°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/72° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/72º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.5281/zenodo.13752898
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/72°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/72° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/72º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.5281/zenodo.13746944
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/24°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.5281/zenodo.13746943
title: ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/24°)

description: This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)
DOI: 10.15468/dl.vmmazv
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "and" : [
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil)"
 ]
 }
 },
 "Issue is one of (Continent derived from coordinates, Continent invalid, Coordinate reprojected, Coordinate rounded, Depth min max swapped, Country derived from coordinates, Depth non numeric, Depth not metric, Depth unlikely, Elevation min max swapped, Elevation non numeric, Elevation not metric, Elevation unlikely, Identified date invalid, Identified date unlikely, Modified date invalid, Modified date unlikely, Recorded date invalid, Recorded date mismatch, Recorded date unlikely, Occurrence status inferred from individual count, Georeferenced date unlikely, Georeferenced date invalid, ccurrence status inferred from basis of record)",
 "TaxonKey is Grewia decemovulata Merxm.",
 "Continent is Africa"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0028081-240906103802322/datasets/export for details.
DOI: 10.5281/zenodo.13832990
title: SPARCS_WP4_Leipzig_City administration_amount of municipal strategies contributing to SPARCS

description: The amount of strategic documents from the city of Leipzig that the project has benefitted from or contributed to, assessed annually, covering the period from 2022 to 2024.
DOI: 10.5281/zenodo.13832991
title: SPARCS_WP4_Leipzig_City administration_amount of municipal strategies contributing to SPARCS

description: The amount of strategic documents from the city of Leipzig that the project has benefitted from or contributed to, assessed annually, covering the period from 2022 to 2024.
DOI: 10.5281/zenodo.11613001
title: ESA 4DMED-Sea - Finite-size Lyapunov Exponents in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/72°)

description: This product provides the Finite-size Lyapunov Exponents derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/72° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Size Lyapunov Exponents was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/72º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

fsle (2D)
DOI: 10.5281/zenodo.11613002
title: ESA 4DMED-Sea - Finite-size Lyapunov Exponents in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/72°)

description: This product provides the Finite-size Lyapunov Exponents derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/72° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Size Lyapunov Exponents was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/72º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

fsle (2D)
DOI: 10.5281/zenodo.13832953
title: The (digital) Wellbeing of German Smartphone Users_ Muench & Carolus
DOI: 10.5281/zenodo.13832954
title: The (digital) Wellbeing of German Smartphone Users_ Muench & Carolus
DOI: 10.5281/zenodo.11612963
title: ESA 4DMED-Sea - Finite-size Lyapunov Exponents in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/24°)

description: This product provides the Finite-size Lyapunov Exponents derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Size Lyapunov Exponents was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

fsle (2D)
DOI: 10.5281/zenodo.11612964
title: ESA 4DMED-Sea - Finite-size Lyapunov Exponents in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/24°)

description: This product provides the Finite-size Lyapunov Exponents derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Size Lyapunov Exponents was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

fsle (2D)
DOI: 10.5517/cc7n769
title: CCDC 227980: Experimental Crystal Structure Determination

description: Related Article: M.Nieger, J.Dzanis, H.Wamhoff|2004|CSD Communication|||
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5281/zenodo.11610886
title: ESA 4DMED-Sea - Finite-size Lyapunov Exponents in the Mediterranean Sea derived from 4DVARNET20 geostrophic velocities (1/72°)

description: This product provides the Finite-size Lyapunov Exponents derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/20°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10912777) at a resolution of 1/72° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Size Lyapunov Exponents was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/72º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

fsle (2D)
DOI: 10.5281/zenodo.11610889
title: ESA 4DMED-Sea - Finite-size Lyapunov Exponents in the Mediterranean Sea derived from 4DVARNET20 geostrophic velocities (1/72°)

description: This product provides the Finite-size Lyapunov Exponents derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/20°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10912777) at a resolution of 1/72° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Size Lyapunov Exponents was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

----------------------------------------------------------------------------------------

Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/72º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

-----------------------------------------------------------------------------------------

Variables:

lon (1D)

lat (1D)

time (1D)

fsle (2D)
DOI: 10.5517/ccwh8n8
title: CCDC 819040: Experimental Crystal Structure Determination

description: Related Article: A.J.Cruz-Cabeza, G.M.Day, W.Jones|2011|Phys.Chem.Chem.Phys.(PCCP)|13|12808|doi:10.1039/c1cp20927b
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.