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Future response of global coastal wetlands to sea-level rise

机译:全球沿海湿地对海平面上升的未来反应

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The response of coastal wetlands to sea-level rise during the twenty-first century remains uncertain. Global-scale projections suggest that between 20 and 90 per cent (for low and high sea-level rise scenarios, respectively) of the present-day coastal wetland area will be lost, which will in turn result in the loss of biodiversity and highly valued ecosystem services(1-3). These projections do not necessarily take into account all essential geomorphological(4-7) and socio-economic system feedbacks(8). Here we present an integrated global modelling approach that considers both the ability of coastal wetlands to build up vertically by sediment accretion, and the accommodation space, namely, the vertical and lateral space available for fine sediments to accumulate and be colonized by wetland vegetation. We use this approach to assess global-scale changes in coastal wetland area in response to global sea-level rise and anthropogenic coastal occupation during the twenty-first century. On the basis of our simulations, we find that, globally, rather than losses, wetland gains of up to 60 per cent of the current area are possible, if more than 37 per cent (our upper estimate for current accommodation space) of coastal wetlands have sufficient accommodation space, and sediment supply remains at present levels. In contrast to previous studies(1-3), we project that until 2100, the loss of global coastal wetland area will range between 0 and 30 per cent, assuming no further accommodation space in addition to current levels. Our simulations suggest that the resilience of global wetlands is primarily driven by the availability of accommodation space, which is strongly influenced by the building of anthropogenic infrastructure in the coastal zone and such infrastructure is expected to change over the twenty-first century. Rather than being an inevitable consequence of global sea-level rise, our findings indicate that large-scale loss of coastal wetlands might be avoidable, if sufficient additional accommodation space can be created through careful nature-based adaptation solutions to coastal management.
机译:在二十一世纪,沿海湿地对海平面上升的反应仍然不确定。全球范围内的预测表明,当今沿海湿地面积将损失20%至90%(分别针对低和高海平面上升情景),进而导致生物多样性丧失和高度重视生态系统服务(1-3)。这些预测未必考虑所有必要的地貌(4-7)和社会经济系统反馈(8)。在这里,我们提出一种综合的全球建模方法,该方法既考虑沿海湿地通过沉积物积聚垂直建立的能力,又考虑容纳空间,即可供细小沉积物累积并被湿地植被定殖的垂直和横向空间。我们使用这种方法来评估全球湿地面积的变化,以应对二十一世纪全球海平面上升和人为的沿海占领。根据我们的模拟,我们发现,如果超过37%(我们对当前住宿空间的最高估计数)的沿海湿地,在全球范围而不是在流失的情况下,最多可以增加当前面积的60%的湿地有足够的住宿空间,沉积物供应仍保持在目前水平。与先前的研究(1-3)相比,我们预计到2100年,假设除当前水平以外没有其他容纳空间,全球沿海湿地面积的损失将在0%到30%之间。我们的模拟表明,全球湿地的复原力主要由住宿空间的可用性驱动,而住宿空间的可用性受到沿海地区人为基础设施建设的强烈影响,并且预计这种基础设施将在二十一世纪发生变化。我们的发现并非不是全球海平面上升的必然结果,而是表明,如果可以通过谨慎的基于自然的沿海管理适应方案创造足够的额外住宿空间,则可以避免大规模的沿海湿地丧失。

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  • 来源
    《Nature》 |2018年第7722期|231-234|共4页
  • 作者单位

    Univ Lincoln, Sch Geog, Lincoln Ctr Water & Planetary Hlth, Lincoln, England;

    Univ Cambridge, Dept Geog, Cambridge Coastal Res Unit, Cambridge, England;

    Univ Antwerp, Ecosyst Management Res Grp, Antwerp, Belgium;

    Virginia Inst Marine Sci, Coll William & Mary, Gloucester Point, VA 23062 USA;

    Christian Albrechts Univ Kiel, Inst Geog, Kiel, Germany;

    Global Climate Forum, Berlin, Germany;

    UN Environm World Conservat Monitoring Ctr, Cambridge, England;

    Univ Southampton, Natl Oceanog Ctr, Ocean & Earth Sci, Southampton, Hants, England;

    Monash Univ, Sch Earth Atmosphere & Environm, Clayton, Vic, Australia;

    Christian Albrechts Univ Kiel, Inst Geog, Kiel, Germany;

    Global Climate Forum, Berlin, Germany;

    Univ Southampton, Fac Engn & Environm, Southampton, Hants, England;

    Univ Southampton, Fac Engn & Environm, Southampton, Hants, England;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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  • 入库时间 2022-08-18 02:51:36

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