globalchange  > 气候减缓与适应
DOI: 10.1029/2018JC013959
Scopus记录号: 2-s2.0-85050802232
论文题名:
Can We Model the Effect of Observed Sea Level Rise on Tides?
作者: Schindelegger M.; Green J.A.M.; Wilmes S.-B.; Haigh I.D.
刊名: Journal of Geophysical Research: Oceans
ISSN: 21699275
出版年: 2018
卷: 123, 期:7
起始页码: 4593
结束页码: 4609
语种: 英语
英文关键词: barotropic modeling ; ocean tides ; sea level rise ; self-attraction and loading ; tidal variability
英文摘要: The link between secular changes in the lunar semidiurnal ocean tide (M2) and relative sea level rise is examined based on numerical tidal modeling and the analysis of long-term sea level records from Europe, Australia, and the North American Atlantic coasts. The study sets itself apart from previous work by using a 1/12° global tide model that incorporates the effects of self-attraction and loading through time-step-wise spherical harmonic transforms instead of iteration. This novel self-attraction and loading implementation incurs moderate computational overheads (some 50%) and facilitates the simulation of shelf sea tides with a global root mean square error of 14.6 cm in depths shallower than 1,000 m. To reproduce measured tidal changes in recent decades, the model is perturbed with realistic water depth changes, compiled from maps of altimetric sea level trends and postglacial crustal rebound. The M2 response to the adopted sea level rise scenarios exhibits peak sensitivities in the North Atlantic and many marginal seas, with relative magnitudes of 1–5% per century. Comparisons with a collection of 45 tide gauge records reveals that the model reproduces the sign of the observed amplitude trends in 80% of the cases and captures considerable fractions of the absolute M2 variability, specifically for stations in the Gulf of Mexico and the Chesapeake-Delaware Bay system. While measured-to-model disparities remain large in several key locations, such as the European Shelf, the study is deemed a major step toward credible predictions of secular changes in the main components of the ocean tide. ©2018. American Geophysical Union. All Rights Reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/113553
Appears in Collections:气候减缓与适应

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作者单位: Institute of Geodesy and Geoinformation, University of Bonn, Bonn, Germany; School of Ocean Sciences, Menai Bridge, United Kingdom; College of Earth, Ocean, and Atmosphere Sciences, Oregon State University, Corvallis, OR, United States; Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, United Kingdom

Recommended Citation:
Schindelegger M.,Green J.A.M.,Wilmes S.-B.,et al. Can We Model the Effect of Observed Sea Level Rise on Tides?[J]. Journal of Geophysical Research: Oceans,2018-01-01,123(7)
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