Global sea level trends in the presence of variable sea level velocities, and variable accelerations

This study investigates, using a new variable-acceleration model, the validity of the implicit assertion in previous studies regarding global constant sea level rise accelerations. Thirteen out of twenty seven globally distributed tide gauge stations, with records longer than 80 years, exhibit stati...

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Main Authors: Bâki Iz H., Ding X.L., Shum C.K.
Format: Article
Language:English
Published: Sciendo 2013-09-01
Series:Journal of Geodetic Science
Subjects:
Online Access:https://doi.org/10.2478/jogs-2013-0020
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spelling doaj-f3e0d076443440cb99ac6fe124eab4e32021-09-06T19:41:39ZengSciendoJournal of Geodetic Science2081-99432013-09-013212713510.2478/jogs-2013-0020Global sea level trends in the presence of variable sea level velocities, and variable accelerationsBâki Iz H.0Ding X.L.1Shum C.K.2Dept. of Land Surveying and Geo-Informatics The Hong Kong Polytechnic University, Hong Kong, ChinaDept. of Land Surveying and Geo-Informatics The Hong Kong Polytechnic University, Hong Kong, ChinaDivision of Geodetic Science School of Earth Sciences The Ohio State University USAThis study investigates, using a new variable-acceleration model, the validity of the implicit assertion in previous studies regarding global constant sea level rise accelerations. Thirteen out of twenty seven globally distributed tide gauge stations, with records longer than 80 years, exhibit statistically significant quartic coefficients (p < 0.05) revealing the presence of variable sea level accelerations though not as a global phenomenon. Most of these stations initially exhibit decreasing negative velocities until early 20th century and increasing positive velocities after 1970’s following a period of constant velocities. It is shown that, for those locations experiencing statistically significant variable sea level accelerations, the estimates based on the conventional linear representation of linear sea level trends are not appropriate, and are notably biased for a number of stations. All solutions account for serial correlations, which otherwise induce biases in solution statistics. It is also demonstrated that the omission of non-linearities in sea level changes will bias the sea level trends for short records, such as those from satellite altimetry, as large as 3 mm/yr.https://doi.org/10.2478/jogs-2013-0020climate changesea level risesatellite altimetrytide gaugevariable accelerationvariable velocity
collection DOAJ
language English
format Article
sources DOAJ
author Bâki Iz H.
Ding X.L.
Shum C.K.
spellingShingle Bâki Iz H.
Ding X.L.
Shum C.K.
Global sea level trends in the presence of variable sea level velocities, and variable accelerations
Journal of Geodetic Science
climate change
sea level rise
satellite altimetry
tide gauge
variable acceleration
variable velocity
author_facet Bâki Iz H.
Ding X.L.
Shum C.K.
author_sort Bâki Iz H.
title Global sea level trends in the presence of variable sea level velocities, and variable accelerations
title_short Global sea level trends in the presence of variable sea level velocities, and variable accelerations
title_full Global sea level trends in the presence of variable sea level velocities, and variable accelerations
title_fullStr Global sea level trends in the presence of variable sea level velocities, and variable accelerations
title_full_unstemmed Global sea level trends in the presence of variable sea level velocities, and variable accelerations
title_sort global sea level trends in the presence of variable sea level velocities, and variable accelerations
publisher Sciendo
series Journal of Geodetic Science
issn 2081-9943
publishDate 2013-09-01
description This study investigates, using a new variable-acceleration model, the validity of the implicit assertion in previous studies regarding global constant sea level rise accelerations. Thirteen out of twenty seven globally distributed tide gauge stations, with records longer than 80 years, exhibit statistically significant quartic coefficients (p < 0.05) revealing the presence of variable sea level accelerations though not as a global phenomenon. Most of these stations initially exhibit decreasing negative velocities until early 20th century and increasing positive velocities after 1970’s following a period of constant velocities. It is shown that, for those locations experiencing statistically significant variable sea level accelerations, the estimates based on the conventional linear representation of linear sea level trends are not appropriate, and are notably biased for a number of stations. All solutions account for serial correlations, which otherwise induce biases in solution statistics. It is also demonstrated that the omission of non-linearities in sea level changes will bias the sea level trends for short records, such as those from satellite altimetry, as large as 3 mm/yr.
topic climate change
sea level rise
satellite altimetry
tide gauge
variable acceleration
variable velocity
url https://doi.org/10.2478/jogs-2013-0020
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