Meteorological conditions during the MOSAiC expedition

• Published in: Elementa: Science of the Anthropocene
• Main Authors: Rinke, Annette, Cassano, John J., Cassano, Elizabeth N., Jaiser, Ralf, Handorf, Dörthe
• Format: Article in Journal/Newspaper
• Language: English
• Published: University of California Press 2021
• Subjects: Arctic; North Atlantic; Siberia
• Online Access: http://dx.doi.org/10.1525/elementa.2021.00023; http://online.ucpress.edu/elementa/article-pdf/doi/10.1525/elementa.2021.00023/474726/elementa.2021.00023.pdf

This article sets the near-surface meteorological conditions during the Multidisciplinary drifting Observatory for the Study of Arctic Climate expedition in the context of the interannual variability and extremes within the past 4 decades. Hourly ERA5 reanalysis data for the Polarstern trajectory for 1979–2020 are analyzed. The conditions were relatively normal given that they were mostly within the interquartile range of the preceding 4 decades. Nevertheless, some anomalous and even record-breaking conditions did occur, particularly during synoptic events. Extreme cases of warm, moist air transported from the northern North Atlantic or northwestern Siberia into the Arctic were identified from late fall until early spring. Daily temperature and total column water vapor were classified as being among the top-ranking warmest/wettest days or even record-breaking based on the full record. Associated with this, the longwave radiative fluxes at the surface were extremely anomalous for these winter cases. The winter and spring period was characterized by more frequent storm events and median cyclone intensity ranking in the top 25th percentile of the full record. During summer, near melting point conditions were more than a month longer than usual, and the July and August 2020 mean conditions were the all-time warmest and wettest. These record conditions near the Polarstern were embedded in large positive temperature and moisture anomalies over the whole central Arctic. In contrast, unusually cold conditions occurred during the beginning of November 2019 and in early March 2020, related to the Arctic Oscillation. In March, this was linked with anomalously strong and persistent northerly winds associated with frequent cyclone occurrence to the southeast of the Polarstern.