Articles | Volume 25, issue 13
https://doi.org/10.5194/acp-25-7315-2025
https://doi.org/10.5194/acp-25-7315-2025
Research article
 | 
14 Jul 2025
Research article |  | 14 Jul 2025

Impact of weather systems on observed precipitation at Ny-Ålesund (Svalbard)

Kerstin Ebell, Christian Buhren, Rosa Gierens, Giovanni Chellini, Melanie Lauer, Andreas Walbröl, Sandro Dahlke, Pavel Krobot, and Mario Mech

Data sets

Parsivel disdrometer measurements at AWIPEV, Ny-Ålesund (2017-2021) Kerstin Ebell et al. https://doi.org/10.1594/PANGAEA.958395

Precipitation amount of Pluvio rain gauge at AWIPEV, Ny-Ålesund (2017-2021) Kerstin Ebell et al. https://doi.org/10.1594/PANGAEA.957612

Data set of detected atmospheric rivers, cyclones, and fronts within the region of 75◦N-82.5◦N, 0◦E-30◦E and at Ny-Ålesund (Svalbard) for 2017-2021 Melanie Lauer https://doi.org/10.5281/zenodo.13768032

Observed and corrected precipitation at Ny-Alesund H.-W. Jacobi and O. Champagne https://doi.org/10.57932/86e7a148-54cf-4d02-af11-39eb1ab417fe

Basic and other measurements of radiation at station Ny-Ålesund (2006-05 et seq) M. Maturilli https://doi.org/10.1594/PANGAEA.914927

RA5 hourly data on single levels from 1940 to present H. Hersbach et al. https://doi.org/10.24381/cds.adbb2d47

ERA5 hourly data on pressure levels from 1940 to present H. Hersbach et al. https://doi.org/10.24381/cds.bd0915c6

Global Atmospheric Rivers catalog for ERA5 reanalysis Melanie Lauer et al. https://doi.org/10.1594/PANGAEA.957161

Data set of detected atmospheric rivers, cyclones, and fronts within the region of 75°N – 82.5°N, 0°E – 30°E and at Ny-Ålesund (Svalbard) for 2017 – 2021 Melanie Lauer https://doi.org/10.5281/zenodo.13768032

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Short summary
Ground-based observations of precipitation are rare in the Arctic. Since 2017, additional temporally highly resolved precipitation measurements have been carried out by a precipitation gauge and an optical precipitation sensor at Ny-Ålesund, Svalbard. These new data facilitate the distinction between liquid and solid precipitation. Using reanalysis data, we also find that water vapor transport contributes strongly to precipitation and especially to extreme precipitation events.
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