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...
Main Authors: | , |
---|---|
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 |
id |
doaj-ecb967390706447b8a6a0b3578c69c46 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT nkudryavtseva satellitealtimetryrevealsspatialpatternsofvariationsinthebalticseawaveclimate AT tsoomere satellitealtimetryrevealsspatialpatternsofvariationsinthebalticseawaveclimate AT tsoomere satellitealtimetryrevealsspatialpatternsofvariationsinthebalticseawaveclimate |
_version_ |
1725270948570988544 |