Analysis of the Variability of Wave Energy Due to Climate Changes on the Example of the Black Sea

An analysis of the variability of wave climate and energy within the Black Sea for the period 1960–2011 was made using field data from the Voluntary Observing Ship Program. Methods using wavelet analysis were applied. It was determined that the power flux of wave energy in the Black Sea fl...

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Main Authors: Yana Saprykina, Sergey Kuznetsov
Format: Article
Language:English
Published: MDPI AG 2018-08-01
Series:Energies
Subjects:
Online Access:http://www.mdpi.com/1996-1073/11/8/2020
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spelling doaj-f4bfa0e8a7054d2fb1aa2f1ee4b954fc2020-11-24T21:17:19ZengMDPI AGEnergies1996-10732018-08-01118202010.3390/en11082020en11082020Analysis of the Variability of Wave Energy Due to Climate Changes on the Example of the Black SeaYana Saprykina0Sergey Kuznetsov1Shirshov Institute of Oceanology of Russian Academy of Sciences, Moscow 117997, RussiaShirshov Institute of Oceanology of Russian Academy of Sciences, Moscow 117997, RussiaAn analysis of the variability of wave climate and energy within the Black Sea for the period 1960–2011 was made using field data from the Voluntary Observing Ship Program. Methods using wavelet analysis were applied. It was determined that the power flux of wave energy in the Black Sea fluctuates: the highest value is 4.2 kW/m, the lowest is 1.4 kW/m. Results indicate significant correlations among the fluctuations of the average annual wave heights, periods, the power flux of wave energy, and teleconnection patterns of the North Atlantic Oscillation (NAO), the Atlantic Multi-decadal Oscillation (AMO), the Pacific Decadal Oscillation (PDO) and the East Atlantic/West Russia (EA/WR). It was revealed that, in positive phases of long-term periods of AMO (50–60 years) as well as PDO, NAO, and AO (40 years), a decrease of wave energy was observed; however, an increase in wave energy was observed in the positive phase of a 15-year period of NAO and AO. The positive phase of changes of EA/WR for periods 50–60, 20–25, and 13 years led to an increase of wave energy. The approximation functions of the oscillations of the average annual wave heights, periods, and the power flux of wave energy for the Black Sea are proposed.http://www.mdpi.com/1996-1073/11/8/2020wave energywave climate variabilitywavelet analysisteleconnection patterns
collection DOAJ
language English
format Article
sources DOAJ
author Yana Saprykina
Sergey Kuznetsov
spellingShingle Yana Saprykina
Sergey Kuznetsov
Analysis of the Variability of Wave Energy Due to Climate Changes on the Example of the Black Sea
Energies
wave energy
wave climate variability
wavelet analysis
teleconnection patterns
author_facet Yana Saprykina
Sergey Kuznetsov
author_sort Yana Saprykina
title Analysis of the Variability of Wave Energy Due to Climate Changes on the Example of the Black Sea
title_short Analysis of the Variability of Wave Energy Due to Climate Changes on the Example of the Black Sea
title_full Analysis of the Variability of Wave Energy Due to Climate Changes on the Example of the Black Sea
title_fullStr Analysis of the Variability of Wave Energy Due to Climate Changes on the Example of the Black Sea
title_full_unstemmed Analysis of the Variability of Wave Energy Due to Climate Changes on the Example of the Black Sea
title_sort analysis of the variability of wave energy due to climate changes on the example of the black sea
publisher MDPI AG
series Energies
issn 1996-1073
publishDate 2018-08-01
description An analysis of the variability of wave climate and energy within the Black Sea for the period 1960–2011 was made using field data from the Voluntary Observing Ship Program. Methods using wavelet analysis were applied. It was determined that the power flux of wave energy in the Black Sea fluctuates: the highest value is 4.2 kW/m, the lowest is 1.4 kW/m. Results indicate significant correlations among the fluctuations of the average annual wave heights, periods, the power flux of wave energy, and teleconnection patterns of the North Atlantic Oscillation (NAO), the Atlantic Multi-decadal Oscillation (AMO), the Pacific Decadal Oscillation (PDO) and the East Atlantic/West Russia (EA/WR). It was revealed that, in positive phases of long-term periods of AMO (50–60 years) as well as PDO, NAO, and AO (40 years), a decrease of wave energy was observed; however, an increase in wave energy was observed in the positive phase of a 15-year period of NAO and AO. The positive phase of changes of EA/WR for periods 50–60, 20–25, and 13 years led to an increase of wave energy. The approximation functions of the oscillations of the average annual wave heights, periods, and the power flux of wave energy for the Black Sea are proposed.
topic wave energy
wave climate variability
wavelet analysis
teleconnection patterns
url http://www.mdpi.com/1996-1073/11/8/2020
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