ALBATROSS – ALtimetry for BAthymetry and TideRetrievals for the Southern Ocean, Sea ice and ice Shelves

The ALBATROSS Project (ALtimetry for BAthymetry and Tide Retrievals for the Southern Ocean, Sea ice and ice Shelves) , led by NOVELTIS in collaboration with DTU, NPI and UCL, is one of the activities funded by ESA in the frame of the Polar Science Cluster, with the objective to foster collaborative research and interdisciplinary networking actions.

In this framework, the ALBATROSS ESA Project aims to improve knowledge about bathymetry and ocean tides in the Southern Ocean.The knowledge about ocean tides is at the crossroads of many scientific fields, especially in the Polar regions, as it has significant impact on ocean circulation modelling and the understanding of the coupled dynamical response of the ocean, sea ice and ice shelves system, the quality and accuracy of sea surface height and sea ice parameter estimates from satellite altimetry, or the understanding of ice-shelf dynamics, for example.Today, this knowledge is still limited by several aspects, such as the quality of bathymetry information, hydrodynamic model resolution and in situ and satellite observations availability for data assimilation and model validation.

The objectives of the project are the following:

• Improve the knowledge on bathymetry around Antarctica, considering decade-long most recently reprocessed CryoSat datasets, innovative information on bathymetry gradient location through the analysis of sea ice surface roughness characteristics, and the compilation of the best available datasets in ice-shelf regions.
• Improve the knowledge on ocean tides in the Southern Ocean through the implementation of a high-resolution hydrodynamic model based on the most advanced developments in terms of ocean tide modelling, and data assimilation of observations, including satellite-altimetry derived tidal retrievals from the most recent and relevant satellite altimetry products.
• Improve satellite altimetry retrievals of sea surface heights and sea ice information thanks to the new tidal model solution.
• Improve the retrievals of ice shelves parameters thanks to the new tidal model solution.
• Share information and knowledge with other Polar science initiatives and projects.

The ALBATROSS Project was launched in May 2021 and will span over two years.

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Presentation at the Living Planet Symposium (LPS22):

ALBATROSS: Improving the bathymetry and ocean tide knowledge in theSouthern Ocean with satellite observations, M. Cancet, O. Andersen,M. Tsamados, G. Moholdt, F. Lyard, M. Restano, J. Benveniste

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PROJECT DOCUMENTS

• ALBATROSS ‐ Progress Report for First Quarterly Review

PUBLICATIONS & COMMUNICATIONS

• Cancet M., Lyard F., Andersen O., Tsamados M., Moholdt G., Benveniste J., ALBATROSS, ALtimetry for BAthymetry and Tide Retrievals for the Southern Ocean, Sea ice and ice Shelves, presentation at the ESA Polar Science Cluster Collocation virtual Meeting, 15-17 September 2021
• Cancet M., Fouchet E., Sahuc E., Lyard F., Andersen O., Dibarboure G., Picot N., Benveniste J., Improvement of the Bathymetry and Regional Tidal Modelling in the Arctic Ocean, presentation at the CryoSat 10th Anniversary Conference virtual event, 14-17 June 2021 (Announcement of the launch of the ALBATROSS project)

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The ALBATROSS Mid-Term Review meeting was held on the 23rd of June2022. The work on the bathymetry, coastline and grounding linedatasets that will feed the hydrodynamic tidal model is almostcompleted. Hydrodynamic tidal simulations have been performed inorder to assess the accuracy of the new bathymetry datasets andprovide feedback about improved areas and regions where furtherimprovements may be needed. The exploratory work on the linkagesbetween sea ice surface roughness computed from MISR data,bathymetry features and vertical tidal excursions shows promisingresults and could be used as a complementary tool to assess therealism of some features in the bathymetry models. Finally, thetidal harmonic constituents retrieved from 10 years of CryoSat-2observations in the Southern Ocean provide an invaluable validationdatabase for the tidal model, bridging the gap between the scarcecoastal in-situ observations and the Topex/Jason conventionalaltimetry observations that are limited to 66°S and stronglyaffected by the presence of sea ice. The implementation of the newhigh-resolution tidal atlas will continue in the coming months andwill be followed by an assessment phase