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Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes

机译:南极冰板和发射场景控制在21世纪的极端海平面变化

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Uncertainties in Representative Concentration Pathway (RCP) scenarios and Antarctic Ice Sheet (AIS) melt propagate into uncertainties in projected mean sea-level (MSL) changes and extreme sea-level (ESL) events. Here we quantify the impact of RCP scenarios and AIS contributions on 21st-century ESL changes at tide-gauge sites across the globe using extreme-value statistics. We find that even under RCP2.6, almost half of the sites could be exposed annually to a present-day 100-year ESL event by 2050. Most tropical sites face large increases in ESL events earlier and for scenarios with smaller MSL changes than extratropical sites. Strong emission reductions lower the probability of large ESL changes but due to AIS uncertainties, cannot fully eliminate the probability that large increases in frequencies of ESL events will occur. Under RCP8.5 and rapid AIS mass loss, many tropical sites, including low-lying islands face a MSL rise by 2100 that exceeds the present-day 100-year event level.
机译:代表性浓度途径(RCP)情景和南极冰盖(AIS)的不确定性熔化在预计平均海平面(MSL)变化和极端海平面(ESL)事件中传播到不确定性中。在这里,我们使用极值统计量化全球潮汐仪表网站的潮流仪表的变化和AIS贡献的影响。我们发现即使在RCP2.6下,几乎一半的网站可以每年通过2050年到现在的100年ESL事件。大多数热带场所面临早期的ESL事件的大幅增加,而且对于较小的MSL变化的情景,比以外的MSL变化更大网站。强度减少较低的减少较大的ESL变化的概率,但由于AIS的不确定性,不能完全消除将发生ESL事件频率的大增加的概率。根据RCP8.5和快速的AIS大规模损失,许多热带场所,包括低洼岛屿面临的MSL上涨2100,超过当今100年的活动水平。

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