4.7 Article

Climate regime shifts and biodiversity redistribution in the Bay of Biscay

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 803, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.149622

Keywords

Extreme events; Benthos; Basque coast; Climate change; GAMM; Geomorphology; Marine biodiversity; Anchovy

Funding

  1. Urban Klima 2050 from European Union's LIFE programme [LIFE 18 IPC 000001]
  2. European Union's Horizon 2020 research and innovation programme [869300]
  3. Basque Government
  4. Provincial Council of Gipuzkoa [2020-FELL-000007-01]

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The study identified four climate regime shifts in the Bay of Biscay, including sea warming, deepening of the winter mixed layer depth, sea-level rise, and increase of extreme wave height events. These changes may have impacted benthic communities and commercial species, with the climate conditions in the region not entirely matching the expected scenarios.
Global ocean warming, wave extreme events, and accelerating sea-level rise are challenges that coastal communities must address to anticipate damages in coming decades. The objective of this study is to undertake a timeseries analysis of climate change (CC) indicators within the Bay of Biscay, including the Basque coast. We used an integrated and flexible methodology, based on Generalized Additive Mixed Models, to detect trends on 19 indicators (including marine physics, chemistry, atmosphere, hydrology, geomorphology, biodiversity, and commercial species). The results of 87 long-term time series analysed (-512,000 observations), in the last four decades, indicate four groups of climate regime shifts: 1) A gradual shift associated with CC starting in the 1980s, with a warming of the sea surface down to 100 m depth in the bay (0.10-0.25 degrees C per decade), increase in air temperature and insolation. This warming may have impacted on benthic community redistribution in the Basque coast, favouring warm-water species relative to cold-water species. Weight at age for anchovy and sardine decreased in the last two decades. 2) Deepening of the winter mixed layer depth in the south-eastern bay that probably led to increases in nutrients, surface oxygen, and chlorophyll concentration. Current increases on chlorophyll and zooplankton (i.e., copepods) biomass are contrary to those expected under CC scenarios in the region. 3) Sea-level rise (1.5-3.5 cm per decade since 1990s), associated with CC. 4) Increase of extreme wave height events of 16.8 cm per decade in the south-eastern bay, probably related to stormy conditions in the last decade, with impacts on beach erosion. Estimating accurate rates of sea warming, sea-level rise, extreme events, and fore- seeing the future pathways of marine productivity, are key to define the best adaptation measures to minimize negative CC impacts in the region. (c) 2021 Elsevier B.V. All rights reserved.

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