13 citations as recorded by crossref.

1. Radiative closure and cloud effects on the radiation budget based on satellite and shipborne observations during the Arctic summer research cruise, PS106 C. Barrientos-Velasco et al. 10.5194/acp-22-9313-2022
2. Extending the Center for Western Weather and Water Extremes (CW3E) atmospheric river scale to the polar regions Z. Zhang et al. 10.5194/tc-18-5239-2024
3. Unraveling the contributions of atmospheric rivers on Antarctica crustal deformation and its spatiotemporal distribution during the past decade J. Li et al. 10.1093/gji/ggad306
4. Case studies of different types of precipitation at Ny-Ålesund, Arctic L. Saini et al. 10.1038/s41598-025-85833-2
5. Surface impacts and associated mechanisms of a moisture intrusion into the Arctic observed in mid-April 2020 during MOSAiC B. Kirbus et al. 10.3389/feart.2023.1147848
6. Using variable-resolution grids to model precipitation from atmospheric rivers around the Greenland ice sheet A. Waling et al. 10.5194/wcd-5-1117-2024
7. Influence of atmospheric rivers and associated weather systems on precipitation in the Arctic M. Lauer et al. 10.5194/acp-23-8705-2023
8. Observability of moisture transport divergence in Arctic atmospheric rivers by dropsondes H. Dorff et al. 10.5194/acp-24-8771-2024
9. Arctic cyclones have become more intense and longer-lived over the past seven decades X. Zhang et al. 10.1038/s43247-023-01003-0
10. Contrasting extremely warm and long-lasting cold air anomalies in the North Atlantic sector of the Arctic during the HALO-(𝒜 𝒞)3 campaign A. Walbröl et al. 10.5194/acp-24-8007-2024
11. Impact of atmospheric river evolutions on Greenland ice sheet mass changes over the last two decades, 2000–2019 J. Li et al. 10.1016/j.polar.2024.101158
12. Case study of a moisture intrusion over the Arctic with the ICOsahedral Non-hydrostatic (ICON) model: resolution dependence of its representation H. Bresson et al. 10.5194/acp-22-173-2022
13. How changes in the circulation patterns specific to the solid precipitations can affect these meteorological events in the Alpine stations of the Mediterranean region? Use of the ERA5 reanalyses G. Guerin & N. Viaux 10.1007/s00704-023-04733-5