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      Sea level variability in Gulf of Guinea from satellite altimetry

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          Abstract

          Coastal zones with dense populations, low elevations and/or inadequate adaptive capacity are on the frontline of unprecedented impacts from climate change. The Gulf of Guinea (GoG), stretching from Liberia to Gabon, is in particular vulnerable to coastal flooding caused by local and/or climate-induced sea level rise. In this region, interannual to decadal coastal sea level changes remain poorly understood, mainly due to a lack of tide gauge stations. Here we use nearly three decades (1993–2021) of satellite altimetry data to study the link between the Equatorial Atlantic and coastal GoG sea level variability. The rate of mean sea level rise increased from 3.47 to 3.89 ± 0.10 mm/yr from the Equatorial oceanic domain to the GoG coastal area, with an acceleration of 0.094 ± 0.050 mm/yr 2. This corresponds to a mean sea level rise of about 8.9 cm over the entire altimetry period, 1993–2021. We focus on the (extreme) warm/cold events that occur in both the GoG during Atlantic Niños, and along the Angola-Namibia coast during Benguela Niños. Both events are driven by remote forcing via equatorial Kelvin waves and local forcing by local winds, freshwater fluxes and currents intensifications. Analysis of altimetry-based sea level, sea surface temperature anomalies, 20 °C isotherm based PIRATA moorings, and the Argo-based steric and thermometric sea level allows us to follow the coastal trapped waves (CTWs) along the GoG, and its link with major events observed along the strong Equatorial Atlantic warmings in 2010, 2012, 2019 and 2021. Both 2019 and 2021 warming have been identified as the warmest event ever reported in this region during the last 40 years. A lag of 1 month is observed between equatorial and West African coastal trapped wave propagation. This observation may help to better anticipate and manage the effects of extreme events on local ecosystems, fisheries, and socio-economic activities along the affected coastlines. In order to enable informed decision-making and guarantee the resilience of coastal communities in the face of climate change, it emphasises the significance of ongoing study in this field.

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          GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE

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            Three decades of high-resolution coastal sea surface temperatures reveal more than warming.

            Understanding and forecasting current and future consequences of coastal warming require a fine-scale assessment of the near-shore temperature changes. Here we show that despite the fact that 71% of the world's coastlines are significantly warming, rates of change have been highly heterogeneous both spatially and seasonally. We demonstrate that 46% of the coastlines have experienced a significant decrease in the frequency of extremely cold events, while extremely hot days are becoming more common in 38% of the area. Also, we show that the onset of the warm season is significantly advancing earlier in the year in 36% of the temperate coastal regions. More importantly, it is now possible to analyse local patterns within the global context, which is useful for a broad array of scientific fields, policy makers and general public.
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              Concepts and Terminology for Sea Level: Mean, Variability and Change, Both Local and Global

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                Author and article information

                Contributors
                franckeitel@gmail.com
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                27 February 2024
                27 February 2024
                2024
                : 14
                : 4759
                Affiliations
                [1 ]Department of Oceanography, University of Cape Town, ( https://ror.org/03p74gp79) Cape Town, South Africa
                [2 ]Geodesy Research Laboratory, National Institute of Cartography, P.O. Box 157, Yaoundé, Cameroon
                [3 ]Nansen-Tutu Center for Marine Environmental Research, University of Cape Town, ( https://ror.org/03p74gp79) Cape Town, South Africa
                [4 ]GRID grid.8689.f, ISNI 0000 0001 2228 9878, Nansen Environmental and Remote Sensing Center and Bjerknes Center for Climate Research, ; Bergen, Norway
                [5 ]Department of Forestry, Fisheries and the Environment, Oceans & Coasts Research, Cape Town, South Africa
                [6 ]7Analytics, Innovation District Solheimsviken 7c, 5054 Bergen, Norway
                [7 ]Laboratoire d’Etudes en Géophysique et Océanographie Spatiales (LEGOS), ( https://ror.org/02chvqy57) 18 Av. E. Belin, 31401 Toulouse Cedex 9, France
                [8 ]Nansen Scientific Society, Bergen, Norway
                Article
                55170
                10.1038/s41598-024-55170-x
                10899594
                38413702
                709ac439-b001-4c77-8e92-738963bacef1
                © The Author(s) 2024

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 16 August 2023
                : 21 February 2024
                Funding
                Funded by: Nansen Scientific Society through the Nansen-Tutu Centre Fellowship Scheme
                Funded by: Sea Level Predictions and Reconstructions (SeaPR) project funded by the Bjerknes Center for Climate Research (BCCR) initiative for strategic projects
                Funded by: European Space Agency’s DRAGON 5 project
                Categories
                Article
                Custom metadata
                © Springer Nature Limited 2024

                Uncategorized
                climate sciences,attribution,climate-change mitigation,physical oceanography,environmental impact

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