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Twenty-first-century climate change impacts on marine animal biomass and ecosystem structure across ocean basins

机译:二十一世纪的气候变化对海洋盆地海洋动物生物量和生态系统结构的影响

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Climate change effects on marine ecosystems include impacts on primary production, ocean temperature, species distributions, and abundance at local to global scales. These changes will significantly alter marine ecosystem structure and function with associated socio-economic impacts on ecosystem services, marine fisheries, and fishery-dependent societies. Yet how these changes may play out among ocean basins over the 21st century remains unclear, with most projections coming from single ecosystem models that do not adequately capture the range of model uncertainty. We address this by using six marine ecosystem models within the Fisheries and Marine Ecosystem Model Intercomparison Project (Fish-MIP) to analyze responses of marine animal biomass in all major ocean basins to contrasting climate change scenarios. Under a high emissions scenario (RCP8.5), total marine animal biomass declined by an ensemble mean of 15%-30% (+/- 12%-17%) in the North and South Atlantic and Pacific, and the Indian Ocean by 2100, whereas polar ocean basins experienced a 20%-80% (+/- 35%-200%) increase. Uncertainty and model disagreement were greatest in the Arctic and smallest in the South Pacific Ocean. Projected changes were reduced under a low (RCP2.6) emissions scenario. Under RCP2.6 and RCP8.5, biomass projections were highly correlated with changes in net primary production and negatively correlated with projected sea surface temperature increases across all ocean basins except the polar oceans. Ecosystem structure was projected to shift as animal biomass concentrated in different size-classes across ocean basins and emissions scenarios. We highlight that climate change mitigation measures could moderate the impacts on marine animal biomass by reducing biomass declines in the Pacific, Atlantic, and Indian Ocean basins. The range of individual model projections emphasizes the importance of using an ensemble approach in assessing uncertainty of future change.
机译:海洋生态系统的气候变化效应包括对全球范围内的主要生产,海洋温度,物种分布和丰富的影响。这些变化将显着改变海洋生态系统结构和函数与生态系统服务,海洋渔业和渔业依赖社会相关的社会经济影响。然而,在21世纪的海洋盆地中,这些变化如何尚不清楚,大多数预测来自单一生态系统模型,不会充分捕获模型不确定性范围。我们通过在渔业和海洋生态系统模型内联(FISH-MIP)内使用六个海洋生态系统模型来解决这一目标,以分析所有主要海洋盆地的海洋动物生物量对造影气候变化情景的反应。在高排放情景(RCP8.5)下,北部和南部大西洋和太平洋地区的合并平均值为15%-30%(+/- 12%-17%)下降的总海洋动物生物量下降2100,而极地海洋盆地经历了20%-80%(+/- 35%-200%)增加。在南太平洋的北极和最小的北极和最小的不确定性和模型分歧。在低(RCP2.6)排放情景下,预计变化减少。在RCP2.6和RCP8.5下,生物质投影与净初级生产的变化高度相关,并且与北极海外的所有海洋盆地的投影海面温度呈负相关。将生态系统结构预计将在海洋盆地和排放情景中集中在不同大小的课程中的动物生物量转变。我们强调,气候变化缓解措施可以通过降低太平洋,大西洋和印度洋盆地的生物量下降来缓解海洋动物生物量的影响。各种模型投影的范围强调了使用集合方法评估未来变革的不确定性的重要性。

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