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首页> 外文期刊>Marine policy >Future marine ecosystem drivers, biodiversity, and fisheries maximum catch potential in Pacific Island countries and territories under climate change
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Future marine ecosystem drivers, biodiversity, and fisheries maximum catch potential in Pacific Island countries and territories under climate change

机译:气候变化下太平洋岛国和地区未来海洋生态系统驱动力,生物多样性和渔业的最大捕获潜力

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摘要

AbstractThe increase in anthropogenic CO2emissions over the last century has modified oceanic conditions, affecting marine ecosystems and the goods and services that they provide to society. Pacific Island countries and territories are highly vulnerable to these changes because of their strong dependence on ocean resources, high level of exposure to climate effects, and low adaptive capacity. Projections of mid-to-late 21st century changes in sea surface temperature (SST), dissolved oxygen, pH, and net primary productivity (NPP) were synthesized across the tropical Western Pacific under strong climate mitigation and business-as-usual scenarios. These projections were used to model impacts on marine biodiversity and potential fisheries catches. Results were consistent across three climate models, indicating that SST will rise by ≥ 3°C, surface dissolved oxygen will decline by ≥ 0.01mlL−1, pH will drop by ≥ 0.3, and NPP will decrease by 0.5gm−2d−1across much of the region by 2100 under the business-as-usual scenario. These changes were associated with rates of local species extinction of > 50% in many regions as fishes and invertebrates decreased in abundance or migrated to regions with conditions more suitable to their bio-climate envelope. Maximum potential catch (MCP) was projected to decrease by > 50% across many areas, with the largest impacts in the western Pacific warm pool. Climate change scenarios that included strong mitigation resulted in substantial reductions of MCP losses, with the area where MCP losses exceeded 50% reduced from 74.4% of the region under business-as-usual to 36.0% of the region under the strong mitigation scenario.HighlightsUnder the RCP 8.5 scenario, tropical Pacific temperature will rise by ≥ 3°C by 2100.This is accompanied by declines in dissolved oxygen, pH, and net primary production.This will lead to local extinctions of up to 80% of marine species in some regions.9 of 17 Pacific Island entities experience ≥ 50% declines in maximum catch potential.Impacts can be greatly reduced by mitigation measures under the RCP 2.6 scenario.
机译: 摘要 上世纪人类活动产生的CO 2 排放量的增加改变了海洋条件,影响了海洋生态系统以及它们向社会提供的商品和服务。太平洋岛国和地区由于对海洋资源的高度依赖,高度暴露于气候影响以及适应能力低,因此极易受到这些变化的影响。在强烈的气候减缓和一切照旧的情况下,整个热带西太平洋地区合成了21世纪中后期的海表温度(SST),溶解氧,pH和净初级生产力(NPP)变化的预测。这些预测被用来模拟对海洋生物多样性和潜在捕捞量的影响。三种气候模型的结果一致,表明SST升高≥3°C,表面溶解氧降低≥0.01mlL -1 ,pH降低减少≥0.3,NPP将减少0.5gm − 2 d − 1 照常营业情景下,到2100年该地区的经济增长。这些变化与许多区域的当地物种灭绝率> 50%有关,因为鱼类和无脊椎动物的数量大量减少或迁移到了更适合其生物气候环境的区域。预计许多地区的最大潜在捕捞量(MCP)将下降> 50%,其中对西太平洋暖池的影响最大。包括强有力的缓解措施的气候变化情景导致了MCP损失的大幅减少,MCP损失超过50%的区域从照常营业的区域的74.4%减少到强有力的缓解情景的36.0%。 / ce:simple-para> 突出显示 在RCP 8.5方案下,热带太平洋温度将升高≥ 2100年3°C。 这伴随着溶解氧,pH和净初级生产力的下降。 这将导致当地灭绝在某些地区多达80%的海洋物种。 < ce:para id =“ p0020” view =“ all”> 17个太平洋岛上的9个实体的最大捕获潜力下降了≥50%。 在RCP 2.6方案下,缓解措施可以大大减少影响。

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