Decadal Strengthening of Interior Flow of North Atlantic Deep Water Observed by GRACE Satellites

• Main Authors: Koelling, Jannes, Send, Uwe, Lankhorst, Matthias
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2020
• Subjects: North Atlantic deep water; Grace Satellites; Gravity Recovery and Climate Experiment; ocean mass; Deep Western Boundary Current; Atlantic Meridional Overturning Circulation; North Atlantic Deep Water; North Atlantic
• Online Access: https://escholarship.org/uc/item/5pn168f2; https://escholarship.org/content/qt5pn168f2/qt5pn168f2.pdf

The Gravity Recovery and Climate Experiment (GRACE) satellite mission provides information on changes to the Earth’s gravity field, including ocean mass. Long-term trends in the GRACE data are often considered unreliable due to uncertainties in the corrections made to calculate ocean mass from the raw measurements. Here, we use an independent estimate of ocean mass from satellite altimetry and in situ density data from five mooring sites and repeat hydrography to validate trends in GRACE over the North Atlantic, finding substantial agreement between the methods. The root mean square difference between ocean mass changes calculated with this method from the mooring data and those measured by GRACE is 3.5 mm/decade, much lower than the mean signal of 15.6±1.8 mm/decade for GRACE and 17.8±5.2 mm/decade for the altimetry-mooring estimate. The GRACE ocean mass data are then used to study the change in the deep circulation of the North Atlantic between the 2002/04/01-2009/03/31 and 2010/04/01-2017/03/31 periods, revealing a large-scale anticyclonic circulation anomaly off the North American coast. The change is associated with an increase of 13.9 ± 3.3 Sv (1Sv = 106 m3 s −1) of southward North Atlantic Deep Water flow in the interior between 30◦N and 40◦N, largely balanced by a northward anomaly of 10.7±3.3 Sv for the boundary circulation. This implies an increased importance of interior pathways compared to the Deep Western Boundary Current for the spreading of North Atlantic Deep Water, which constitutes the lower limb of the Atlantic Meridional Overturning Circulation.