@article {roberts_blueprint_2023,
	title = {A blueprint for integrating scientific approaches and international communities to assess basin-wide ocean ecosystem status},
	journal = {Communications Earth \& Environment},
	volume = {4},
	number = {1},
	year = {2023},
	note = {Number: 1 Publisher: Nature Publishing Group},
	month = {jan},
	abstract = {Ocean ecosystems are at the forefront of the climate and biodiversity crises, yet we lack a unified approach to assess their state and inform sustainable policies. This blueprint is designed around research capabilities and cross-sectoral partnerships. We highlight priorities including integrating basin-scale observation, modelling and genomic approaches to understand Atlantic oceanography and ecosystem connectivity; improving ecosystem mapping; identifying potential tipping points in deep and open ocean ecosystems; understanding compound impacts of multiple stressors including warming, acidification and deoxygenation; enhancing spatial and temporal management and protection. We argue that these goals are best achieved through partnerships with policy-makers and community stakeholders, and promoting research groups from the South Atlantic through investment and engagement. Given the high costs of such research ({\texteuro}800k to {\texteuro}1.7M per expedition and {\texteuro}30{\textendash}40M for a basin-scale programme), international cooperation and funding are integral to supporting science-led policies to conserve ocean ecosystems that transcend jurisdictional borders.},
	keywords = {Marine biology, physical oceanography},
	issn = {2662-4435},
	doi = {10.1038/s43247-022-00645-w},
	url = {https://www.nature.com/articles/s43247-022-00645-w},
	author = {Roberts, J. Murray and Devey, Colin W. and Biastoch, Arne and Carreiro-Silva, Marina and Dohna, Tina and Dorschel, Boris and Gunn, Vikki and Huvenne, Veerle A. I. and Johnson, David and Jollivet, Didier and Kenchington, Ellen and Larkin, Kate and Matabos, Marjolaine and Morato, Telmo and Naumann, Malik S. and Orejas, Covadonga and Perez, J. Angel A. and Ragnarsson, Stef{\'a}n {\'A} and Smit, Albertus J. and Sweetman, Andrew and Unger, Sebastian and Boteler, Benjamin and Henry, Lea-Anne}
}
@article {schiller-weiss_salinity_2023,
	title = {Do Salinity Variations Along the East Greenland Shelf Show Imprints of Increasing Meltwater Runoff?},
	journal = {Journal of Geophysical Research: Oceans},
	volume = {128},
	number = {10},
	year = {2023},
	note = {_eprint: https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023JC019890},
	pages = {e2023JC019890},
	abstract = {Accelerated melting of the Greenland Ice Sheet is considered a tipping element in the freshwater balance of the subpolar North Atlantic (SPNA). The East Greenland Current (EGC) and Coastal Current (EGCC) are the major conduits for transporting Arctic-sourced and Greenland glacial freshwater. Understanding freshwater changes in the EGC system and drivers thereof is crucial for connecting tipping elements in the SPNA. Using the eddy-rich model VIKING20X (1/20{\textdegree}) and Copernicus GLORYS12 (1/12{\textdegree}), we find that from 1993 to 2019 freshwater remains close to the shelf with interannual extremes in freshwater content (FWC) attributable to the imprint of Greenland melt only in years 2010 and 2012. Runoff increased significantly from 1995 to 2005 and Arctic freshwater export after 2005. Overall, regional wind patterns, sea ice melt and increasingly glacial ice and snow meltwater runoff along with the Arctic-sourced Polar Water set interannual FWC variations in the EGC system. We emphasize that these freshwater sources have different seasonal timing. South of 65{\textdegree}N sea ice melts year round and retreats to north of 65{\textdegree}N, where melt in summer prevails. Greenland runoff peaks in June{\textendash}August with only some locations of year round discharge. Alongshore winds intensify in fall and winter where reduced onshore Ekman transport allows for freshwater to spread laterally in the EGC. We show that sea ice melt, runoff and wind can cause interannual variations of comparable magnitude. All of which makes attributing ocean freshening events to Greenland meltwater inflow at current magnitudes a major challenge.},
	issn = {2169-9291},
	doi = {10.1029/2023JC019890},
	url = {https://onlinelibrary.wiley.com/doi/abs/10.1029/2023JC019890},
	author = {Schiller-Weiss, Ilana and Martin, Torge and Karstensen, Johannes and Biastoch, Arne}
}
@article {frohle_major_2022,
	title = {Major sources of North Atlantic Deep Water in the subpolar North Atlantic from Lagrangian analyses in an eddy-rich ocean model},
	journal = {Ocean Science},
	volume = {18},
	number = {5},
	year = {2022},
	note = {Publisher: Copernicus GmbH},
	pages = {1431{\textendash}1450},
	abstract = {The North Atlantic Deep Water (NADW) is a crucial component of the Atlantic meridional overturning circulation and is therefore an important factor of the climate system. In order to estimate the mean relative contributions, sources, and pathways of the NADW at the southern exit of the Labrador Sea, a Lagrangian particle experiment is performed. The particles were seeded according to the strength of the velocity field along the 53{\textopenbullet} N section and traced 40 years backward in time in the three dimensional velocity and hydrography field. The resulting transport pathways, their sources and corresponding transit timescales were inferred. Our experiment shows that, of the 30.1 Sv of NADW passing 53{\textopenbullet} N on average, the majority of this water is associated with a diapycnal mass flux without contact to the atmosphere, accounting for 14.3 Sv (48 \%), where 6.2 Sv originate from the Labrador Sea, compared to 4.7 Sv from the Irminger Sea. The second-largest contribution originates from the mixed layer with 7.2 Sv (24 \%), where the Labrador Sea contribution (5.9 Sv) dominates over the Irminger Sea contribution (1.0 Sv). Another 5.7 Sv (19 \%) of NADW crosses the Greenland{\textendash}Scotland Ridge within the NADW density class, where about two-thirds pass the Denmark Strait, while one-third crosses the Iceland{\textendash}Scotland Ridge. The NADW exported at 53{\textopenbullet} N is hence dominated by entrainment through the diapycnal mass flux and mixed-layer origin in the Labrador Sea.},
	issn = {1812-0784},
	doi = {10.5194/os-18-1431-2022},
	url = {https://os.copernicus.org/articles/18/1431/2022/},
	author = {Fr{\"o}hle, J{\"o}rg and Handmann, Patricia V. K. and Biastoch, Arne}
}
@article {RN269,
	title = {Perspectives on Marine Data Science as a Blueprint for Emerging Data Science Disciplines},
	journal = {Frontiers in Marine Science},
	volume = {8},
	year = {2021},
	pages = {678404},
	type = {Journal Article},
	doi = {10.3389/fmars.2021.678404},
	url = {https://app.dimensions.ai/details/publication/pub.1143539440 https://www.frontiersin.org/articles/10.3389/fmars.2021.678404/pdf},
	author = {Verwega, Maria-Theresia and Trahms, Carola and Antia, Avan N. and Dickhaus, Thorsten and Prigge, Enno and Prinzler, Martin H. U. and Renz, Matthias and Schartau, Markus and Slawig, Thomas and Somes, Christopher J. and Biastoch, Arne}
}
