Satellite altimetry reveals spatial patterns of variations in the Baltic Sea wave climate

The main properties of the climate of waves in the seasonally ice-covered Baltic Sea and its decadal changes since 1990 are estimated from satellite altimetry data. The data set of significant wave heights (SWHs) from all existing nine satellites, cleaned and cross-validated against in situ meas...

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Main Authors: N. Kudryavtseva, T. Soomere
Format: Article
Language:English
Published: Copernicus Publications 2017-08-01
Series:Earth System Dynamics
Online Access:https://www.earth-syst-dynam.net/8/697/2017/esd-8-697-2017.pdf
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spelling doaj-ecb967390706447b8a6a0b3578c69c462020-11-25T00:45:18ZengCopernicus PublicationsEarth System Dynamics2190-49792190-49872017-08-01869770610.5194/esd-8-697-2017Satellite altimetry reveals spatial patterns of variations in the Baltic Sea wave climateN. Kudryavtseva0T. Soomere1T. Soomere2Wave Engineering Laboratory, Department of Cybernetics, School of Science, Tallinn University of Technology, Akadeemia tee 21, Tallinn, 12 618, EstoniaWave Engineering Laboratory, Department of Cybernetics, School of Science, Tallinn University of Technology, Akadeemia tee 21, Tallinn, 12 618, EstoniaEstonian Academy of Sciences, Kohtu 6, Tallinn, 10 130, EstoniaThe main properties of the climate of waves in the seasonally ice-covered Baltic Sea and its decadal changes since 1990 are estimated from satellite altimetry data. The data set of significant wave heights (SWHs) from all existing nine satellites, cleaned and cross-validated against in situ measurements, shows overall a very consistent picture. A comparison with visual observations shows a good correspondence with correlation coefficients of 0.6–0.8. The annual mean SWH reveals a tentative increase of 0.005 m yr<sup>−1</sup>, but higher quantiles behave in a cyclic manner with a timescale of 10–15 years. Changes in the basin-wide average SWH have a strong meridional pattern: an increase in the central and western parts of the sea and a decrease in the east. This pattern is likely caused by a rotation of wind directions rather than by an increase in the wind speed.https://www.earth-syst-dynam.net/8/697/2017/esd-8-697-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. Kudryavtseva
T. Soomere
T. Soomere
spellingShingle N. Kudryavtseva
T. Soomere
T. Soomere
Satellite altimetry reveals spatial patterns of variations in the Baltic Sea wave climate
Earth System Dynamics
author_facet N. Kudryavtseva
T. Soomere
T. Soomere
author_sort N. Kudryavtseva
title Satellite altimetry reveals spatial patterns of variations in the Baltic Sea wave climate
title_short Satellite altimetry reveals spatial patterns of variations in the Baltic Sea wave climate
title_full Satellite altimetry reveals spatial patterns of variations in the Baltic Sea wave climate
title_fullStr Satellite altimetry reveals spatial patterns of variations in the Baltic Sea wave climate
title_full_unstemmed Satellite altimetry reveals spatial patterns of variations in the Baltic Sea wave climate
title_sort satellite altimetry reveals spatial patterns of variations in the baltic sea wave climate
publisher Copernicus Publications
series Earth System Dynamics
issn 2190-4979
2190-4987
publishDate 2017-08-01
description The main properties of the climate of waves in the seasonally ice-covered Baltic Sea and its decadal changes since 1990 are estimated from satellite altimetry data. The data set of significant wave heights (SWHs) from all existing nine satellites, cleaned and cross-validated against in situ measurements, shows overall a very consistent picture. A comparison with visual observations shows a good correspondence with correlation coefficients of 0.6–0.8. The annual mean SWH reveals a tentative increase of 0.005 m yr<sup>−1</sup>, but higher quantiles behave in a cyclic manner with a timescale of 10–15 years. Changes in the basin-wide average SWH have a strong meridional pattern: an increase in the central and western parts of the sea and a decrease in the east. This pattern is likely caused by a rotation of wind directions rather than by an increase in the wind speed.
url https://www.earth-syst-dynam.net/8/697/2017/esd-8-697-2017.pdf
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