Summertime increases in upper-ocean stratification and mixed-layer depth
|Author(s)||Sallee Jean-Baptiste1, Pellichero Violaine2, 3, Akhoudas Camille1, Pauthenet Etienne1, Vignes Lucie1, Schmidtko Sunke4, Garabato Alberto Naveira5, Sutherland Peter6, Kuusela Mikael7|
|Affiliation(s)||1 : orbonne Univ, CNRS IRD MNHN, LOCEAN, IPSL, Paris, France.
2 : Univ Tasmania, Inst Marine & Antarct Studies, Hobart, Tas, Australia.
3 : CSIRO Oceans & Atmosphere, Hobart, Tas, Australia.
4 : GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany.
5 : Univ Southampton, Natl Oceanog Ctr, Ocean & Earth Sci, Southampton, Hants, England.
6 : Univ Brest, Lab Oceanog Phys & Spatiale LOPS, Ifremer, CNRS,IRD,IUEM, Brest, France.
7 : Carnegie Mellon Univ, Dept Stat & Data Sci, Pittsburgh, PA 15213 USA.
|Source||Nature (0028-0836) (Nature Research), 2021-03 , Vol. 591 , N. 7851 , P. 592-598|
|WOS© Times Cited||8|
The surface mixed layer of the world ocean regulates global climate by controlling heat and carbon exchange between the atmosphere and the oceanic interior(1-3). The mixed layer also shapes marine ecosystems by hosting most of the ocean's primary production(4) and providing the conduit for oxygenation of deep oceanic layers. Despite these important climatic and life-supporting roles, possible changes in the mixed layer during an era of global climate change remain uncertain. Here we use oceanographic observations to show that from 1970 to 2018 the density contrast across the base of the mixed layer increased and that the mixed layer itself became deeper. Using a physically based definition of upper-ocean stability that follows different dynamical regimes across the global ocean, we find that the summertime density contrast increased by 8.9 +/- 2.7 per cent per decade (10(-6)-10(-5) per second squared per decade, depending on region), more than six times greater than previous estimates. Whereas prior work has suggested that a thinner mixed layer should accompany a more stratified upper ocean(5-7), we find instead that the summertime mixed layer deepened by 2.9 +/- 0.5 per cent per decade, or several metres per decade (typically 5-10 metres per decade, depending on region). A detailed mechanistic interpretation is challenging, but the concurrent stratification and deepening of the mixed layer are related to an increase in stability associated with surface warming and high-latitude surface freshening(8,9), accompanied by a wind-driven intensification of upper-ocean turbulence(10,11). Our findings are based on a complex dataset with incomplete coverage of a vast area. Although our results are robust within a wide range of sensitivity analyses, important uncertainties remain, such as those related to sparse coverage in the early years of the 1970-2018 period. Nonetheless, our work calls for reconsideration of the drivers of ongoing shifts in marine primary production, and reveals stark changes in the world's upper ocean over the past five decades.