Strauss Benjamin H, Kulp Scott, Levermann Anders
Climate Central, Princeton, NJ 08542;
Potsdam Institute for Climate Impact Research, 14473 Potsdam, Germany; Physics Institute of Potsdam University, 14476 Potsdam, Germany.
Proc Natl Acad Sci U S A. 2015 Nov 3;112(44):13508-13. doi: 10.1073/pnas.1511186112. Epub 2015 Oct 12.
Anthropogenic carbon emissions lock in long-term sea-level rise that greatly exceeds projections for this century, posing profound challenges for coastal development and cultural legacies. Analysis based on previously published relationships linking emissions to warming and warming to rise indicates that unabated carbon emissions up to the year 2100 would commit an eventual global sea-level rise of 4.3-9.9 m. Based on detailed topographic and population data, local high tide lines, and regional long-term sea-level commitment for different carbon emissions and ice sheet stability scenarios, we compute the current population living on endangered land at municipal, state, and national levels within the United States. For unabated climate change, we find that land that is home to more than 20 million people is implicated and is widely distributed among different states and coasts. The total area includes 1,185-1,825 municipalities where land that is home to more than half of the current population would be affected, among them at least 21 cities exceeding 100,000 residents. Under aggressive carbon cuts, more than half of these municipalities would avoid this commitment if the West Antarctic Ice Sheet remains stable. Similarly, more than half of the US population-weighted area under threat could be spared. We provide lists of implicated cities and state populations for different emissions scenarios and with and without a certain collapse of the West Antarctic Ice Sheet. Although past anthropogenic emissions already have caused sea-level commitment that will force coastal cities to adapt, future emissions will determine which areas we can continue to occupy or may have to abandon.
人为碳排放导致长期海平面上升,其幅度大大超过本世纪的预测,给沿海发展和文化遗产带来了严峻挑战。基于先前发表的将排放与变暖以及变暖与海平面上升联系起来的关系进行分析表明,到2100年若碳排放仍不减少,最终将导致全球海平面上升4.3 - 9.9米。根据详细的地形和人口数据、当地高潮线以及不同碳排放和冰盖稳定性情景下的区域长期海平面上升趋势,我们计算了美国市级、州级和国家级生活在濒危土地上的当前人口数量。对于无节制的气候变化,我们发现有超过2000万人居住的土地受到影响,且广泛分布在不同的州和海岸。总面积包括1185 - 1825个市政区域,其中目前一半以上人口居住的土地将受到影响,其中至少有21个城市居民超过10万。在积极减排的情况下,如果西南极冰盖保持稳定,这些市政区域中一半以上将避免面临这种情况。同样,受威胁的美国人口加权面积中一半以上可以幸免。我们提供了不同排放情景下、有无西南极冰盖一定程度崩塌情况下受影响城市和州人口的清单。尽管过去的人为排放已经造成了海平面上升趋势,迫使沿海城市进行适应,但未来的排放将决定哪些地区我们可以继续占据,哪些地区可能不得不放弃。