Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise

Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise

Tide gauge observations of relative sea-level trends between 1993 and 2018 around the contiguous United States can largely be attributed to a combination of changes in ocean mass, sterodynamic effects and vertical land motion, according to a sea-level budgeting exercise.

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Detalles Bibliográficos
Autores principales: T. C. Harvey, B. D. Hamlington, T. Frederikse, R. S. Nerem, C. G. Piecuch, W. C. Hammond, G. Blewitt, P. R. Thompson, D. P. S. Bekaert, F. W. Landerer, J. T. Reager, R. E. Kopp, H. Chandanpurkar, I. Fenty, D. Trossman, J. S. Walker, C. Boening
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
Materias:
Geology
QE1-996.5
Environmental sciences
GE1-350
Acceso en línea:https://doaj.org/article/b1473b2bb02e41cda50bff9c624c2d6d
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Descripción
Sumario:Tide gauge observations of relative sea-level trends between 1993 and 2018 around the contiguous United States can largely be attributed to a combination of changes in ocean mass, sterodynamic effects and vertical land motion, according to a sea-level budgeting exercise.

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