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Explora: Environment

                                                                                   and Resource



                                        ORIGINAL RESEARCH ARTICLE
                                        Mechanisms driving ocean stratification and

                                        mixed layer deepening



                                        Éric Zeltz*
                                        Independent Scholar, La Motte en Champsaur, Hautes-Alpes, France



                                        Abstract

                                        This article aims to better understand the links between climate change and the
                                        recently observed significant increases in ocean stratification and the deepening
                                        of the mixed layer. Using a time series of ocean stratification data, we investigate
                                        potential “signals” of interactions with other climatic phenomena. Our findings reveal
                                        that the observed temporal patterns in stratification are primarily influenced by the
                                        El Niño-Southern Oscillation. However, this influence alone does not account for
                                        the overall increase in stratification or the deepening of the mixed layer observed
                                        since the 1960s. Instead, we demonstrate that these two phenomena are largely
                                        driven by the warming of the upper oceanic stratum (UOS). To incorporate these
                                        findings, we adapted a climate model developed in 2023, enabling it to account for
                                        the identified drivers. The enhanced model generates projections for five key global
                                        climate parameters: atmospheric temperature at the ocean level, UOS temperature,
                                        ocean cloudiness, ocean stratification, and mixed layer deepening. Our mathematical
                                        analysis of the model indicates that the relationships underlying these variables
                                        impose a clear growth trend on each of the five parameters, which eventually stabilizes
                                        toward finite limits. This stabilization results in values that remain within reasonable
            *Corresponding author:      bounds, minimizing their impact on the planet and the global ecosystem. Under a
            Éric Zeltz
            (ericzeltz@wanadoo.fr)      comparable scenario, for example, the model predicts an increase of approximately
                                        1℃ in global atmospheric temperature by 2100 – significantly lower than the 2°C
            Citation: Zeltz É. Mechanisms
            driving ocean stratification and   increase projected by the Intergovernmental Panel on Climate Change (IPCC).
            mixed layer deepening. Explora
            Environ Resour. 2024;1(1):4578.
            doi: 10.36922/eer.4578      Keywords: Climate modeling; Ocean stratification; Mixed layer; El Niño-Southern
                                        Oscillation; Natural climate regulation
            Received: August 19, 2024
            Accepted: October 31, 2024
            Published Online: December 5,
            2024                        1. Introduction
            Copyright: © 2024 Author(s).   Recent studies indicate that ocean stratification and vertical stability have increased
            This is an Open-Access article                         1-3
            distributed under the terms of the   significantly over the past 50 years.  The main drivers of this phenomenon, as identified
            Creative Commons Attribution   in these studies, include:
            License, permitting distribution,   (i)  Surface warming due to global warming: The increase in heat at the ocean’s surface
            and reproduction in any medium,
            provided the original work is   intensifies density differences between successive water layers, thereby strengthening
            properly cited.                thermal barriers between the upper ocean layer and deeper waters. 1-3
            Publisher’s Note: AccScience   (ii)  Melting polar ice: Warming-induced ice melt releases substantial amounts of
            Publishing remains neutral with   freshwater, which is lighter than saltwater. This freshwater remains on the top water
            regard to jurisdictional claims in
            published maps and institutional   layer, further warming and reinforcing the thermal barrier with deeper layers of the
            affiliations.                  oceans. 2


            Volume 1 Issue 1 (2024)                         1                                doi: 10.36922/eer.4578
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