Enhancement of the southward return flow of the Atlantic Meridional Overturning Circulation by data assimilation and its influence in an assimilative ocean simulation forced by CORE-II atmospheric forcing

• Published in: Climate dynamics Vol. 49; no. 3; pp. 869 - 889
• Main Authors: Fujii, Yosuke, Tsujino, Hiroyuki, Toyoda, Takahiro, Nakano, Hideyuki
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.08.2017; Springer; Springer Nature B.V
• Subjects: Atlantic Meridional Overturning Circulation (AMOC); Atmospheric forcing; Circulation; Climatology; Coastal environments; Coastal waves; Computer simulation; Cores; Data; Data assimilation; Data collection; Deep layer; Deep water; Earth and Environmental Science; Earth Sciences; Geophysics/Geodesy; Integration; Methods; Observations; Ocean circulation; Ocean models; Ocean-atmosphere interaction; Oceanography; Oceans; Overflow; Reliability; Return flow; Simulation; Technology application; Temperature effects; Upper ocean; Variability; Water depth; Wave propagation; Weather forecasting; Southern Ocean; Ocean Reanalyses Intercomparison Project (ORA-IP); Coordinated Ocean-ice Reference Experiment II (CORE-II); Ocean general circulation model; Atlantic Meridional Overturning Circulation (AMOC); Data assimilation
• DOI: 10.1007/s00382-015-2780-1
• ISSN: 0930-7575

This paper examines the difference in the Atlantic Meridional Overturning Circulation (AMOC) mean state between free and assimilative simulations of a common ocean model using a common interannual atmospheric forcing. In the assimilative simulation, the reproduction of cold cores in the Nordic Seas, which is absent in the free simulation, enhances the overflow to the North Atlantic and improves AMOC with enhanced transport of the deeper part of the southward return flow. This improvement also induces an enhanced supply of North Atlantic Deep Water (NADW) and causes better representation of the Atlantic deep layer despite the fact that correction by the data assimilation is applied only to temperature and salinity above a depth of 1750 m. It also affects Circumpolar Deep Water in the Southern Ocean. Although the earliest influence of the improvement propagated by coastal waves reaches the Southern Ocean in 10–15 years, substantial influence associated with the arrival of the renewed NADW propagates across the Atlantic Basin in several decades. Although the result demonstrates that data assimilation is able to improve the deep ocean state even if there is no data there, it also indicates that long-term integration is required to reproduce variability in the deep ocean originating from variations in the upper ocean. This study thus provides insights on the reliability of AMOC and the ocean state in the Atlantic deep layer reproduced by data assimilation systems.