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115 Research products

  • European Marine Science
  • 2019-2023
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  • European Marine Science

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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Reese, Lloyd; Gräwe, Ulf; Klingbeil, Knut; Li, Xiangyu; +2 Authors

    Supporting Python scripts used for data processing for Reese et al. (2023): "Local Mixing Determines Spatial Structure of Diahaline Exchange Flow in a Mesotidal Estuary: A Study of Extreme Runoff Conditions" [1]. River discharge information and topography as used for the numerical tidal Elbe setup applied in the same study. Contains: riverinfo.dat -- river and tributary freshwater input grid locations as grid cell indices rivers.nc -- freshwater forcing used in setup, contains sources from all included tributaries and Geesthacht. Data retrieved from [2,3,4] in combination with personal communication via the Bundesanstalt für Wasserbau (BAW). topo_smoothed_v20_z0.nc -- setup topography and curvilinear grid. Topography created from datasets [5,6], for the latter see also [7]. Python scripts used for the creation of the figures, namely: fig2: Figure 2 fig3: Figure 3 fig4: Figure 4 and Table 1 data fig5: Figure 5 and Table 2 salt data fig6: Figure 6 fig7-8: Figures 7,8 fig9: Figure 9 fig10: Figure 10 fig11: Figure 11 plot_salt_tidally-resolved: Tidally resolved stratification, not shown in paper plot_temperature_correlation_section2e: Correlation of observed and simulated temperature at same stations as Figure 5 (not shown) and Table 2 temperature data The model data used for the figures and loaded within the Python scripts is available from the corresponding author of the study [1]. Note that *paper_plot_forcing_validation.py, *paper_plot_tidal_analysis.py, and *paper_plot_salinity_correlation.py require observational data that is freely available via portal-tideelbe.de; for in-depth documentation see [1]. *paper_plot_forcing_validation.py additionally requires meteorological forcing data for the first figure panel, which cannot be made public due to its proprietary nature. The use of shapefiles to colour landmasses and plot the coastline in Figures 2, 6, and 11 has to be commented out in the respective Python scripts due to unclear copyright regarding the underlying data. However, omission of these shapefiles does not change the interpretation of the model results. ---- [1] L. Reese, U. Graewe, K. Klingbeil, X. Li, M. Lorenz, H. Burchard, 2023: Local mixing determines spatial structure of diahaline exchange flow in a mesotidal estuary – a study of extreme runoff conditions. J. Phys. Oceanogr., submitted. [2] Wasserstraßen- und Schifffahrtsamt Magdeburg, 2021: Abflussstation Neu Darchau. Wasserstraßen- und Schifffahrtsverwaltung des Bundes, accessed 10 March 2021, http://www.portal-tideelbe.de. [3] Landesamt für Landwirtschaft, Umwelt und ländliche Räume Schleswig-Holstein, 2022: Daily averaged freshwater runoff at Kellinghusen-Parkplatz and Kölln-Reisiek A23, 2012–2014. Hochwasser- und Sturmflutinformation Schleswig-Holstein, accessed 2 February 2022, https://www.umweltdaten.landsh.de/pegel/jsp/pegel.jsp?gui=ganglinie&thema=q&mstnr=114377;https://www.umweltdaten.landsh.de/pegel/jsp/pegel.jsp?mstnr=114527&wsize=free. [4] Niedersächsicher Landesbetrieb für Wasserwirtschaft, Küsten- und Naturschutz, 2022: Daily averaged freshwater runoff at gauges no. 5963101 (Oersdorf), 5945125 (Bienenbüttel), 5983110 (Rockstedt), and 5972105 (Schwinge), 2012–2014. Niedersächsische Landesdatenbank für wasserwirtschaftliche Daten, accessed 27 April 2022, http://www.wasserdaten.niedersachsen.de/cadenza/pages/home/welcome.xhtml. [5] Wasserstraßen- und Schifffahrtsamt Hamburg, 2011: DGM-W 2010 Unter- und Außenelbe (Digitales Geländemodell des Wasserlaufes - Multifunktionsmodell). Wasserstraßen- und Schifffahrtsverwaltung des Bundes, accessed 12 January 2021, https://www.kuestendaten.de/Tideelbe/DE/Service/Kartenthemen/Kartenthemen_node.html [6] Bundesamt für Seeschifffahrt und Hydrographie, 2019: AufMod Bathymetries German Bight 1982-2012 - WMS. Wasserstraßen- und Schifffahrtsverwaltung des Bundes, accessed 28 May 2013, https://gdk.gdi-de.org/geonetwork/srv/api/records/3543c490-d251-4948-830c-1da723a1a8eb. [7] Heyer, H., and K. Schrottke, 2015: Einführung, Aufgabenstellung und Bearbeitungsstruktur im KFKI-Projekt AufMod. Die Küste, 83, 1–18, ISBN: 978-3-939230-40-3.

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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Fritzsch, Bernadette;

    Software has played an increasingly important role in science over the years. However, software development has long led to a shadowy existence. However, as programs have become more complex and they have often been passed on as a legacy from one development team (often made up of temporary Ph.D. students) Research software as a foundation of scientific work has been increasingly pushed to the fore. In the meantime, job titles such as “research software engineer” have become established in various places. This talk examines the importance of research software in various contexts and how this affects developers of research software.

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    Authors: Bohaty, SM; Uenzelmann-Neben, G; Childress, LB; Archontikis, OA; +27 Authors
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    Oxford University Research Archive
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      Oxford University Research Archive
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    Authors: Bohaty, SM; Uenzelmann-Neben, G; Childress, LB; Archontikis, OA; +27 Authors
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    Oxford University Research Archive
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      Oxford University Research Archive
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    Authors: Bohaty, SM; Uenzelmann-Neben, G; Childress, LB; Archontikis, OA; +27 Authors
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Oxford University Re...arrow_drop_down
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    Oxford University Research Archive
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    Authors: Bohaty, SM; Uenzelmann-Neben, G; Childress, LB; Archontikis, OA; +27 Authors
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    Authors: Uenzelmann-Neben, G; Bohaty, SM; Childress, LB; Archontikis, OA; +27 Authors
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      Oxford University Research Archive
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    Authors: Uenzelmann-Neben, G; Bohaty, SM; Chirdress, LB; Archontikis, OA; +27 Authors

    During International Ocean Discovery Program Expedition 392, three sites were drilled on the Agulhas Plateau and one site was drilled in the Transkei Basin in the Southwest Indian Ocean. This region was positioned at paleolatitudes of ~53°–61°S during the Late Cretaceous (van Hinsbergen et al., 2015) (100–66 Ma) and within the new and evolving gateway between the South Atlantic, Southern Ocean, and southern Indian Ocean basins. Recovery of basement rocks and sedimentary sequences from the Agulhas Plateau sites and a thick sedimentary sequence in the Transkei Basin provides a wealth of new data to (1) determine the nature, origin, and bathymetric evolution of the Agulhas Plateau; (2) significantly advance the understanding of how Cretaceous temperatures, ocean circulation, and sedimentation patterns evolved as CO2 levels rose and fell and the breakup of Gondwana progressed; (3) document long- and short-term paleoceanographic variability through the Late Cretaceous and Paleogene; and (4) investigate geochemical interactions between igneous rocks, sediments, and pore waters through the life cycle of a large igneous province (LIP). Importantly, postcruise analysis of Expedition 392 drill cores will allow testing of competing hypotheses concerning Agulhas Plateau LIP formation and the role of deep ocean circulation changes through southern gateways in influencing Late Cretaceous–early Paleogene climate evolution.

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    Authors: Dransch, Doris; Rath, Willi;

    The Workshop is part of a yearly series within the AI/ML-Cluster in Subtopic 2.4 of the research program PoF IV: Changing Earth - Sustaining our Future.

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    Authors: Krumpen, Thomas; Jutila, Arttu; Sans Coll, Cristina; Horvath, Esther;

    IceBird Winter 2023 is part of a long-term sea ice observation program within the IceBird aircraft campaign series. IceBird was initiated in 2018 with the objective to ensure the long-term availability of a unique data record of direct sea-ice thickness observations to understand the role of the sea ice component for the causes and consequences of Arctic change, but is built on the heritage of airborne sea-ice thickness observations that date back to 2004. Compared to earlier airborne programs, IceBird has been enhanced with an improved sensor setup that also allows measuring snow depth on sea ice, fully collocated with sea-ice thickness and surface roughness at high resolution. The objectives of IceBird Winter 2023 include the continued quantification of trends, the separation of variability and extreme events of sea ice thickness and its snow cover in the Western Seas of the Arctic Ocean. The continuation of airborne sea-ice observation programs fulfils the requirement of consistent and long-term observations of key climate parameters. The data will be used to improve understanding of the response of sea ice and its snow cover to the ongoing warming of the Arctic and to improve snow models. Airborne data of snow and sea-ice thickness are also critically needed for the evaluation of sea-ice remote sensing products as well as for the evolution of algorithms for current and future satellite missions. Surveys from IceBird Winter 2023 will target the validation of sea-ice freeboard and snow depth estimates from CryoSat-2, ICESat-2, Sentinel-3A/B and AltiKa altimeters.

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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Reese, Lloyd; Gräwe, Ulf; Klingbeil, Knut; Li, Xiangyu; +2 Authors

    Supporting Python scripts used for data processing for Reese et al. (2023): "Local Mixing Determines Spatial Structure of Diahaline Exchange Flow in a Mesotidal Estuary: A Study of Extreme Runoff Conditions" [1]. River discharge information and topography as used for the numerical tidal Elbe setup applied in the same study. Contains: riverinfo.dat -- river and tributary freshwater input grid locations as grid cell indices rivers.nc -- freshwater forcing used in setup, contains sources from all included tributaries and Geesthacht. Data retrieved from [2,3,4] in combination with personal communication via the Bundesanstalt für Wasserbau (BAW). topo_smoothed_v20_z0.nc -- setup topography and curvilinear grid. Topography created from datasets [5,6], for the latter see also [7]. Python scripts used for the creation of the figures, namely: fig2: Figure 2 fig3: Figure 3 fig4: Figure 4 and Table 1 data fig5: Figure 5 and Table 2 salt data fig6: Figure 6 fig7-8: Figures 7,8 fig9: Figure 9 fig10: Figure 10 fig11: Figure 11 plot_salt_tidally-resolved: Tidally resolved stratification, not shown in paper plot_temperature_correlation_section2e: Correlation of observed and simulated temperature at same stations as Figure 5 (not shown) and Table 2 temperature data The model data used for the figures and loaded within the Python scripts is available from the corresponding author of the study [1]. Note that *paper_plot_forcing_validation.py, *paper_plot_tidal_analysis.py, and *paper_plot_salinity_correlation.py require observational data that is freely available via portal-tideelbe.de; for in-depth documentation see [1]. *paper_plot_forcing_validation.py additionally requires meteorological forcing data for the first figure panel, which cannot be made public due to its proprietary nature. The use of shapefiles to colour landmasses and plot the coastline in Figures 2, 6, and 11 has to be commented out in the respective Python scripts due to unclear copyright regarding the underlying data. However, omission of these shapefiles does not change the interpretation of the model results. ---- [1] L. Reese, U. Graewe, K. Klingbeil, X. Li, M. Lorenz, H. Burchard, 2023: Local mixing determines spatial structure of diahaline exchange flow in a mesotidal estuary – a study of extreme runoff conditions. J. Phys. Oceanogr., submitted. [2] Wasserstraßen- und Schifffahrtsamt Magdeburg, 2021: Abflussstation Neu Darchau. Wasserstraßen- und Schifffahrtsverwaltung des Bundes, accessed 10 March 2021, http://www.portal-tideelbe.de. [3] Landesamt für Landwirtschaft, Umwelt und ländliche Räume Schleswig-Holstein, 2022: Daily averaged freshwater runoff at Kellinghusen-Parkplatz and Kölln-Reisiek A23, 2012–2014. Hochwasser- und Sturmflutinformation Schleswig-Holstein, accessed 2 February 2022, https://www.umweltdaten.landsh.de/pegel/jsp/pegel.jsp?gui=ganglinie&thema=q&mstnr=114377;https://www.umweltdaten.landsh.de/pegel/jsp/pegel.jsp?mstnr=114527&wsize=free. [4] Niedersächsicher Landesbetrieb für Wasserwirtschaft, Küsten- und Naturschutz, 2022: Daily averaged freshwater runoff at gauges no. 5963101 (Oersdorf), 5945125 (Bienenbüttel), 5983110 (Rockstedt), and 5972105 (Schwinge), 2012–2014. Niedersächsische Landesdatenbank für wasserwirtschaftliche Daten, accessed 27 April 2022, http://www.wasserdaten.niedersachsen.de/cadenza/pages/home/welcome.xhtml. [5] Wasserstraßen- und Schifffahrtsamt Hamburg, 2011: DGM-W 2010 Unter- und Außenelbe (Digitales Geländemodell des Wasserlaufes - Multifunktionsmodell). Wasserstraßen- und Schifffahrtsverwaltung des Bundes, accessed 12 January 2021, https://www.kuestendaten.de/Tideelbe/DE/Service/Kartenthemen/Kartenthemen_node.html [6] Bundesamt für Seeschifffahrt und Hydrographie, 2019: AufMod Bathymetries German Bight 1982-2012 - WMS. Wasserstraßen- und Schifffahrtsverwaltung des Bundes, accessed 28 May 2013, https://gdk.gdi-de.org/geonetwork/srv/api/records/3543c490-d251-4948-830c-1da723a1a8eb. [7] Heyer, H., and K. Schrottke, 2015: Einführung, Aufgabenstellung und Bearbeitungsstruktur im KFKI-Projekt AufMod. Die Küste, 83, 1–18, ISBN: 978-3-939230-40-3.

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    Authors: Fritzsch, Bernadette;

    Software has played an increasingly important role in science over the years. However, software development has long led to a shadowy existence. However, as programs have become more complex and they have often been passed on as a legacy from one development team (often made up of temporary Ph.D. students) Research software as a foundation of scientific work has been increasingly pushed to the fore. In the meantime, job titles such as “research software engineer” have become established in various places. This talk examines the importance of research software in various contexts and how this affects developers of research software.

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    Authors: Bohaty, SM; Uenzelmann-Neben, G; Childress, LB; Archontikis, OA; +27 Authors
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    Authors: Bohaty, SM; Uenzelmann-Neben, G; Childress, LB; Archontikis, OA; +27 Authors
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    Authors: Bohaty, SM; Uenzelmann-Neben, G; Childress, LB; Archontikis, OA; +27 Authors
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    Authors: Bohaty, SM; Uenzelmann-Neben, G; Childress, LB; Archontikis, OA; +27 Authors
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    Authors: Uenzelmann-Neben, G; Bohaty, SM; Childress, LB; Archontikis, OA; +27 Authors
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    Authors: Uenzelmann-Neben, G; Bohaty, SM; Chirdress, LB; Archontikis, OA; +27 Authors

    During International Ocean Discovery Program Expedition 392, three sites were drilled on the Agulhas Plateau and one site was drilled in the Transkei Basin in the Southwest Indian Ocean. This region was positioned at paleolatitudes of ~53°–61°S during the Late Cretaceous (van Hinsbergen et al., 2015) (100–66 Ma) and within the new and evolving gateway between the South Atlantic, Southern Ocean, and southern Indian Ocean basins. Recovery of basement rocks and sedimentary sequences from the Agulhas Plateau sites and a thick sedimentary sequence in the Transkei Basin provides a wealth of new data to (1) determine the nature, origin, and bathymetric evolution of the Agulhas Plateau; (2) significantly advance the understanding of how Cretaceous temperatures, ocean circulation, and sedimentation patterns evolved as CO2 levels rose and fell and the breakup of Gondwana progressed; (3) document long- and short-term paleoceanographic variability through the Late Cretaceous and Paleogene; and (4) investigate geochemical interactions between igneous rocks, sediments, and pore waters through the life cycle of a large igneous province (LIP). Importantly, postcruise analysis of Expedition 392 drill cores will allow testing of competing hypotheses concerning Agulhas Plateau LIP formation and the role of deep ocean circulation changes through southern gateways in influencing Late Cretaceous–early Paleogene climate evolution.

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