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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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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spelling	oai:doaj.org-article:b1473b2bb02e41cda50bff9c624c2d6d2021-11-14T12:12:52ZOcean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise10.1038/s43247-021-00300-w2662-4435https://doaj.org/article/b1473b2bb02e41cda50bff9c624c2d6d2021-11-01T00:00:00Zhttps://doi.org/10.1038/s43247-021-00300-whttps://doaj.org/toc/2662-4435Tide 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.T. C. HarveyB. D. HamlingtonT. FrederikseR. S. NeremC. G. PiecuchW. C. HammondG. BlewittP. R. ThompsonD. P. S. BekaertF. W. LandererJ. T. ReagerR. E. KoppH. ChandanpurkarI. FentyD. TrossmanJ. S. WalkerC. BoeningNature PortfolioarticleGeologyQE1-996.5Environmental sciencesGE1-350ENCommunications Earth & Environment, Vol 2, Iss 1, Pp 1-10 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Geology QE1-996.5 Environmental sciences GE1-350
spellingShingle	Geology QE1-996.5 Environmental sciences GE1-350 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 Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise
description	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.
format	article
author	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
author_facet	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
author_sort	T. C. Harvey
title	Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise
title_short	Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise
title_full	Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise
title_fullStr	Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise
title_full_unstemmed	Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise
title_sort	ocean mass, sterodynamic effects, and vertical land motion largely explain us coast relative sea level rise
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/b1473b2bb02e41cda50bff9c624c2d6d
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Ocean mass, sterodynamic effects, and vertical land motion largely explain US coast relative sea level rise

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