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The Paris Climate Agreement and future sea-level rise from Antarctica

机译:巴黎气候协议和未来海平面从南极洲崛起

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An observationally calibrated ice sheet-shelf model suggests that global warming of 3 degrees C will trigger rapid Antarctic ice loss, contributing about 0.5 cm per year of sea-level rise by 2100.The Paris Agreement aims to limit global mean warming in the twenty-first century to less than 2 degrees Celsius above preindustrial levels, and to promote further efforts to limit warming to 1.5 degrees Celsius(1). The amount of greenhouse gas emissions in coming decades will be consequential for global mean sea level (GMSL) on century and longer timescales through a combination of ocean thermal expansion and loss of land ice(2). The Antarctic Ice Sheet (AIS) is Earth's largest land ice reservoir (equivalent to 57.9 metres of GMSL)(3), and its ice loss is accelerating(4). Extensive regions of the AIS are grounded below sea level and susceptible to dynamical instabilities(5-8) that are capable of producing very rapid retreat(8). Yet the potential for the implementation of the Paris Agreement temperature targets to slow or stop the onset of these instabilities has not been directly tested with physics-based models. Here we use an observationally calibrated ice sheet-shelf model to show that with global warming limited to 2 degrees Celsius or less, Antarctic ice loss will continue at a pace similar to today's throughout the twenty-first century. However, scenarios more consistent with current policies (allowing 3 degrees Celsius of warming) give an abrupt jump in the pace of Antarctic ice loss after around 2060, contributing about 0.5 centimetres GMSL rise per year by 2100-an order of magnitude faster than today(4). More fossil-fuel-intensive scenarios(9) result in even greater acceleration. Ice-sheet retreat initiated by the thinning and loss of buttressing ice shelves continues for centuries, regardless of bedrock and sea-level feedback mechanisms(10-12) or geoengineered carbon dioxide reduction. These results demonstrate the possibility that rapid and unstoppable sea-level rise from Antarctica will be triggered if Paris Agreement targets are exceeded.
机译:一个观察性校准冰盖现成模型表明3度,全球变暖C的温度将迅速触发南极冰盖的损失,由2100.The巴黎协定旨在促进每海平面上升的年约0.5厘米到限制全球平均变暖在21第一世纪至小于2摄氏度以上工业化前的水平,并促进进一步努力限制升温至1.5摄氏度(1)。温室气体排放在未来几十年内量将是必然的全球平均海平面(GMSL)上世纪和更长时间尺度通过海洋热膨胀和陆冰(2)损失的组合。南极冰盖(AIS)是地球上最大的陆地冰室(相当于57.9米GMSL的)(3),其冰层融化正在加速(4)。该AIS的广泛区域被接地海平面以下,易被能够产生非常迅速后退(8)的不稳定性的动态(5-8)。然而,对于巴黎协定温度指标的执行缓慢或停止这些不稳定性发作的潜力尚未得到直接与物理模型试验。这里我们使用的观测上校准冰盖现成的模型表明,全球变暖限制在2摄氏度以下,南极冰盖的损失将继续在整个二十一世纪类似于今天的一个步伐。然而,情景与当前的政策(允许摄氏度升温3度)更一致给2060左右后,在南极冰层融化的速度突然跳,按数量2100-订单比今天贡献约0.5厘米每年GMSL上升更快( 4)。更化石燃料密集的场景(9)导致甚至更大的加速度。通过拱托冰架的稀疏和脱发发起冰盖退缩持续几个世纪,无论基岩和海平面反馈机制(10-12)或geoengineered减少二氧化碳排放。这些结果表明,如果巴黎协定指标均超过南极洲快速和势不可挡的海平面上升将被触发的可能性。

著录项

  • 来源
    《Nature 》 |2021年第7857期| 83-89| 共7页
  • 作者单位

    Univ Massachusetts Amherst Dept Geosci Amherst MA 01003 USA;

    Penn State Univ Earth & Environm Syst Inst University Pk PA 16802 USA;

    Penn State Univ Earth & Environm Syst Inst University Pk PA 16802 USA|Penn State Univ Dept Geosci University Pk PA 16802 USA;

    Univ Calif Irvine Earth Syst Sci Irvine CA USA;

    Univ Bristol Sch Geog Sci Bristol Avon England;

    McGill Univ Dept Earth & Planetary Sci Montreal PQ Canada;

    Univ Massachusetts Amherst Dept Geosci Amherst MA 01003 USA;

    Woods Hole Oceanog Inst Dept Geol & Geophys Woods Hole MA 02543 USA;

    Rutgers State Univ Dept Earth & Planetary Sci Piscataway NJ USA;

    Rutgers State Univ Dept Earth & Planetary Sci Piscataway NJ USA;

    Rutgers State Univ Dept Earth & Planetary Sci Piscataway NJ USA;

    Univ Massachusetts Amherst Dept Geosci Amherst MA 01003 USA|Shanghai Jiao Tong Univ Sch Oceanog Shanghai Peoples R China;

    Univ Wisconsin Madison Dept Geosci Madison WI USA;

  • 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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