Reconstruction of sea level around the Korean Peninsula using cyclostationary empirical orthogonal functions

<p>Since the advent of the modern satellite altimeter era, the understanding of the sea level has increased dramatically. The satellite altimeter record, however, dates back only to the 1990s. The tide gauge record, on the other hand, extends through the 20th century but with poor spatial...

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Main Authors: S.-H. Cheon, B. D. Hamlington, K.-D. Suh
Format: Article
Language:English
Published: Copernicus Publications 2018-09-01
Series:Ocean Science
Online Access:https://www.ocean-sci.net/14/959/2018/os-14-959-2018.pdf
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spelling doaj-19da37ceef1a4ed393bb8f069a9f49572020-11-25T01:10:12ZengCopernicus PublicationsOcean Science1812-07841812-07922018-09-011495997010.5194/os-14-959-2018Reconstruction of sea level around the Korean Peninsula using cyclostationary empirical orthogonal functionsS.-H. Cheon0B. D. Hamlington1K.-D. Suh2Department of Ocean, Earth and Atmospheric Sciences, Old Dominion University, Norfolk, VA, USADepartment of Ocean, Earth and Atmospheric Sciences, Old Dominion University, Norfolk, VA, USAInstitute of Construction and Environmental Engineering, Seoul National University, Seoul, South Korea<p>Since the advent of the modern satellite altimeter era, the understanding of the sea level has increased dramatically. The satellite altimeter record, however, dates back only to the 1990s. The tide gauge record, on the other hand, extends through the 20th century but with poor spatial coverage when compared to the satellites. Many studies have been conducted to create a dataset with the spatial coverage of the satellite datasets and the temporal length of the tide gauge records by finding novel ways to combine the satellite data and tide gauge data in what is known as sea level reconstruction. However, most of the reconstructions of sea level were conducted on a global scale, leading to reduced accuracy on regional levels, especially when there are relatively few tide gauges. The seas around the Korean Peninsula are one such area with few tide gauges before 1960. In this study, new methods are proposed to reconstruct past sea level around the Korean Peninsula. Using spatial patterns obtained from a cyclostationary empirical orthogonal function decomposition of satellite data, we reconstruct sea level over the period from 1900 to 2014. Sea surface temperature data and altimeter data are used simultaneously in the reconstruction process, leading to an elimination of reliance on tide gauge data. Although we did not use the tide gauge data in the reconstruction process, the reconstructed sea level has a better agreement with the tide gauge observations in the region than previous studies that incorporated the tide gauge data. This study demonstrates a reconstruction technique that can potentially be used at regional levels, with particular emphasis on areas with poor tide gauge coverage.</p>https://www.ocean-sci.net/14/959/2018/os-14-959-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S.-H. Cheon
B. D. Hamlington
K.-D. Suh
spellingShingle S.-H. Cheon
B. D. Hamlington
K.-D. Suh
Reconstruction of sea level around the Korean Peninsula using cyclostationary empirical orthogonal functions
Ocean Science
author_facet S.-H. Cheon
B. D. Hamlington
K.-D. Suh
author_sort S.-H. Cheon
title Reconstruction of sea level around the Korean Peninsula using cyclostationary empirical orthogonal functions
title_short Reconstruction of sea level around the Korean Peninsula using cyclostationary empirical orthogonal functions
title_full Reconstruction of sea level around the Korean Peninsula using cyclostationary empirical orthogonal functions
title_fullStr Reconstruction of sea level around the Korean Peninsula using cyclostationary empirical orthogonal functions
title_full_unstemmed Reconstruction of sea level around the Korean Peninsula using cyclostationary empirical orthogonal functions
title_sort reconstruction of sea level around the korean peninsula using cyclostationary empirical orthogonal functions
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2018-09-01
description <p>Since the advent of the modern satellite altimeter era, the understanding of the sea level has increased dramatically. The satellite altimeter record, however, dates back only to the 1990s. The tide gauge record, on the other hand, extends through the 20th century but with poor spatial coverage when compared to the satellites. Many studies have been conducted to create a dataset with the spatial coverage of the satellite datasets and the temporal length of the tide gauge records by finding novel ways to combine the satellite data and tide gauge data in what is known as sea level reconstruction. However, most of the reconstructions of sea level were conducted on a global scale, leading to reduced accuracy on regional levels, especially when there are relatively few tide gauges. The seas around the Korean Peninsula are one such area with few tide gauges before 1960. In this study, new methods are proposed to reconstruct past sea level around the Korean Peninsula. Using spatial patterns obtained from a cyclostationary empirical orthogonal function decomposition of satellite data, we reconstruct sea level over the period from 1900 to 2014. Sea surface temperature data and altimeter data are used simultaneously in the reconstruction process, leading to an elimination of reliance on tide gauge data. Although we did not use the tide gauge data in the reconstruction process, the reconstructed sea level has a better agreement with the tide gauge observations in the region than previous studies that incorporated the tide gauge data. This study demonstrates a reconstruction technique that can potentially be used at regional levels, with particular emphasis on areas with poor tide gauge coverage.</p>
url https://www.ocean-sci.net/14/959/2018/os-14-959-2018.pdf
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