T. Spangehl et al.: Intercomparing the quality of recent reanalyses for offshore wind farm planning 125
Data availability. FINO data was downloaded from
http://fino.bsh.de (last access: 6 November 2023). Data was
made available by the FINO (Forschungsplattformen in Nord-
und Ostsee) initiative, which was funded by the German Federal
Ministry of Economic Affairs and Climate Action (BMWK)
on the basis of a decision by the German Bundestag, organised
by the Projekttraeger Juelich (PTJ) and coordinated by the
German Federal Maritime and Hydrographic Agency (BSH).
FINO data is now available via the new Insitu-Portal of BSH
https://www.bsh.de/EN/TOPICS/Monitoring_systems/MARNET_
monitoring_network/FINO/fino_node.html (Bundesamt für
Seeschifffahrt und Hydrographie, 2023b).
NEWA data is obtained from the New European Wind Atlas, a
free, web-based application developed, owned and operated by the
NEWA Consortium. For additional information see https://www.
neweuropeanwindatlas.eu/ (NEWA Consortium, 2023).
This study has been conducted using EU Copernicus Marine
Service Information. The WIND_GLO_PHY_L4_MY_012_006,
https://doi.org/10.48670/moi-00185 (EU Copernicus Marine Ser-
vice, 2023), product is used in the final version of the manuscript.
The ERA5 reanalysis data are publicly and freely available from
the producers at the Copernicus Climate Data Store (CDS; Hers-
bach et al., 2023, https://doi.org/10.24381/cds.adbb2d47), or via
ECMWF’s Meteorological Archival and Retrieval System (MARS).
The COSMO-REA6 reanalysis data are publicly available
at DWD’s Open Data Server (https://opendata.dwd.de/climate_
environment/REA/COSMO_REA6/, Deutscher Wetterdienst,
2023).
The Hamburg Ocean Atmosphere Parameters and Fluxes
from Satellite Data – HOAPS – 4.0 (Andersson et al., 2017,
https://doi.org/10.5676/EUM_SAF_CM/HOAPS/V002) are avail-
able from EUMETSAT Satellite Application Facility on Climate
Monitoring (CM SAF) via https://wui.cmsaf.eu, © (2023) (EU-
METSAT, 2023).
Selected parameters of HoKliSim-De are available via
https://doi.org/10.5676/DWD/HOKLISIM_V2022.01 (Brienen
et al., 2022).
Date from the Copernicus European Regional Re-
Analysis (CERRA) are publicly and freely available from
the producers at the Copernicus Climate Date Store (CDS;
https://doi.org/10.24381/cds.38b394e6, Schimanke et al., 2021a,
https://doi.org/10.24381/cds.622a565a, Schimanke et al., 2021b).
Author contributions. All authors contributed to the results and
evaluation presented here. TS wrote the first draft of the manuscript.
SSc contributed to integrating CERRA. SB contributed to integrat-
ing HoKliSim-De.
Competing interests. The contact author has declared that none
of the authors has any competing interests.
Disclaimer. Publisher’s note: Copernicus Publications remains
neutral with regard to jurisdictional claims made in the text, pub-
lished maps, institutional affiliations, or any other geographical rep-
resentation in this paper. While Copernicus Publications makes ev-
ery effort to include appropriate place names, the final responsibility
lies with the authors.
Special issue statement. This article is part of the special issue
“EMS Annual Meeting: European Conference for Applied Mete-
orology and Climatology 2022”. It is a result of the EMS Annual
Meeting: European Conference 2022. The corresponding presenta-
tion was part of session UP3.6: Global and regional reanalyses.
Acknowledgements. The authors thank Anja Niedorf (DWD)
and Marc Schröder (DWD) for the provision of data from EUMET-
SAT CM SAF (HOAPS v4 and its extension).
The authors thank Andrea Hahmann and one anonymous re-
viewer for their helpful comments.
Financial support. Part of this research has been supported by
the BMBF programme ClimXtreme (grant no. 01LP1904A).
Review statement. This paper was edited by Eric Bazile and re-
viewed by Andrea Hahmann and one anonymous referee.
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