A Brief Climatology of Dunkelflaute Events over and Surrounding the North and Baltic Sea Areas

In the coming decades, the European energy system is expected to become increasingly reliant on non-dispatchable generation such as wind and solar power. Under such a renewable energy scenario, a better characterization of the extreme weather condition ‘Dunkelflaute’, which can lead to a sustained r...

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Main Authors: Bowen Li, Sukanta Basu, Simon J. Watson, Herman W. J. Russchenberg
Format: Article
Language:English
Published: MDPI AG 2021-10-01
Series:Energies
Subjects:
Online Access:https://www.mdpi.com/1996-1073/14/20/6508
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author Bowen Li
Sukanta Basu
Simon J. Watson
Herman W. J. Russchenberg
author_facet Bowen Li
Sukanta Basu
Simon J. Watson
Herman W. J. Russchenberg
author_sort Bowen Li
collection DOAJ
description In the coming decades, the European energy system is expected to become increasingly reliant on non-dispatchable generation such as wind and solar power. Under such a renewable energy scenario, a better characterization of the extreme weather condition ‘Dunkelflaute’, which can lead to a sustained reduction of wind and solar power, is important. In this paper, we report findings from the very first climatological study of Dunkelflaute events occurring in eleven countries surrounding the North and Baltic Sea areas. By utilizing multi-year meteorological and power production datasets, we have quantified various statistics pertaining to these events and also identified their underlying meteorological drivers. It was found that almost all periods tagged as Dunkelflaute events (with a length of more than 24 h) are in November, December, and January for these countries. On average, there are 50–100 h of such events happening in each of these three months per year. The limited wind and solar power production during Dunkelflaute events is shown to be mainly driven by large-scale high-pressure systems and extensive low-cloud coverage. Even though the possibility of simultaneous Dunkelflaute events in neighboring countries can be as high as 30–40%, such events hardly occur simultaneously in all the eleven countries. Through an interconnected EU-11 power system, the mean frequency of Dunkelflaute drops from 3–9% for the individual countries to approximately 3.5% for the combined region, highlighting the importance of aggregating production over a wide area to better manage the integration of renewable energy generation.
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spelling doaj.art-f7a06838b5ef40c59546a30d2a70ace32023-11-22T18:04:14ZengMDPI AGEnergies1996-10732021-10-011420650810.3390/en14206508A Brief Climatology of Dunkelflaute Events over and Surrounding the North and Baltic Sea AreasBowen Li0Sukanta Basu1Simon J. Watson2Herman W. J. Russchenberg3Faculty of Civil Engineering and Geosciences, Delft University of Technology, 2628 CN Delft, The NetherlandsFaculty of Civil Engineering and Geosciences, Delft University of Technology, 2628 CN Delft, The NetherlandsFaculty of Aerospace Engineering, Delft University of Technology, 2629 HS Delft, The NetherlandsFaculty of Civil Engineering and Geosciences, Delft University of Technology, 2628 CN Delft, The NetherlandsIn the coming decades, the European energy system is expected to become increasingly reliant on non-dispatchable generation such as wind and solar power. Under such a renewable energy scenario, a better characterization of the extreme weather condition ‘Dunkelflaute’, which can lead to a sustained reduction of wind and solar power, is important. In this paper, we report findings from the very first climatological study of Dunkelflaute events occurring in eleven countries surrounding the North and Baltic Sea areas. By utilizing multi-year meteorological and power production datasets, we have quantified various statistics pertaining to these events and also identified their underlying meteorological drivers. It was found that almost all periods tagged as Dunkelflaute events (with a length of more than 24 h) are in November, December, and January for these countries. On average, there are 50–100 h of such events happening in each of these three months per year. The limited wind and solar power production during Dunkelflaute events is shown to be mainly driven by large-scale high-pressure systems and extensive low-cloud coverage. Even though the possibility of simultaneous Dunkelflaute events in neighboring countries can be as high as 30–40%, such events hardly occur simultaneously in all the eleven countries. Through an interconnected EU-11 power system, the mean frequency of Dunkelflaute drops from 3–9% for the individual countries to approximately 3.5% for the combined region, highlighting the importance of aggregating production over a wide area to better manage the integration of renewable energy generation.https://www.mdpi.com/1996-1073/14/20/6508climatological analysisgrid connectionpower reliabilitysolar energywind energy
spellingShingle Bowen Li
Sukanta Basu
Simon J. Watson
Herman W. J. Russchenberg
A Brief Climatology of Dunkelflaute Events over and Surrounding the North and Baltic Sea Areas
Energies
climatological analysis
grid connection
power reliability
solar energy
wind energy
title A Brief Climatology of Dunkelflaute Events over and Surrounding the North and Baltic Sea Areas
title_full A Brief Climatology of Dunkelflaute Events over and Surrounding the North and Baltic Sea Areas
title_fullStr A Brief Climatology of Dunkelflaute Events over and Surrounding the North and Baltic Sea Areas
title_full_unstemmed A Brief Climatology of Dunkelflaute Events over and Surrounding the North and Baltic Sea Areas
title_short A Brief Climatology of Dunkelflaute Events over and Surrounding the North and Baltic Sea Areas
title_sort brief climatology of dunkelflaute events over and surrounding the north and baltic sea areas
topic climatological analysis
grid connection
power reliability
solar energy
wind energy
url https://www.mdpi.com/1996-1073/14/20/6508
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