Environmental conditions in the North Atlantic sector of the Arctic during the HALO–(AC)³ campaign
The airborne field campaign HALO–(AC)³ took place from 07 March to 12 April 2022 and was designed to observe the transformation of air masses during their meridional transport in the North Atlantic sector of the Arctic. We evaluate the meteorological and sea ice conditions during the campai...
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ftcopernicus:oai:publications.copernicus.org:egusphere110685 2023-06-06T11:50:27+02:00 Environmental conditions in the North Atlantic sector of the Arctic during the HALO–(AC)³ campaign Walbröl, Andreas Michaelis, Janosch Becker, Sebastian Dorff, Henning Gorodetskaya, Irina Kirbus, Benjamin Lauer, Melanie Maherndl, Nina Maturilli, Marion Mayer, Johanna Müller, Hanno Neggers, Roel A. J. Paulus, Fiona M. Röttenbacher, Johannes Rückert, Janna E. Schirmacher, Imke Slättberg, Nils Ehrlich, André Wendisch, Manfred Crewell, Susanne 2023-04-13 application/pdf https://doi.org/10.5194/egusphere-2023-668 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-668/ eng eng doi:10.5194/egusphere-2023-668 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-668/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-668 2023-04-17T16:23:11Z The airborne field campaign HALO–(AC)³ took place from 07 March to 12 April 2022 and was designed to observe the transformation of air masses during their meridional transport in the North Atlantic sector of the Arctic. We evaluate the meteorological and sea ice conditions during the campaign based on the European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis v5 (ERA5), satellite data, and atmospheric soundings with respect to climatology and describe special synoptic events. HALO–(AC)³ started with a warm period (11–20 March) where strong southerly winds prevailed that caused moist and warm air intrusions (MWAIs). Two MWAIs were detected as Atmospheric Rivers (ARs). Compared to the ERA5 climatology (1979–2022), record breaking vertically integrated poleward heat and moisture fluxes averaged over 75.0–81.5° N were found. The related warm and moist air masses reached the central Arctic, causing the highest rainfall rates over the sea ice northwest of Svalbard recorded since the beginning of the ERA5 climatology. Subsequently, the cold period of HALO–(AC)³ started after the passage of a Shapiro–Keyser cyclone on 21 March when the wind regime turned to northerlies, advecting colder air into the Fram Strait. Until 08 April, marine cold air outbreaks (MCAOs) prevailed, including two strong MCAO events on 21–26 March and 01–02 April. In between, aged subpolar warm air was advected to the Fram Strait with northeasterly and easterly winds. On average, the campaign period was warmer than the climatology, especially due to the exceptionally strong ARs during the warm period. In the Fram Strait, the sea ice concentration (SIC) was within the 10–90 th percentiles of the climatology over the entire campaign duration. During the warm period, SIC was strongly reduced and an untypically large polynya for this season opened north of Svalbard. During the cold period, the polynya was closed again and above average SICs were found. We describe the environmental conditions of a Polar Low and ... Text Arctic Fram Strait North Atlantic Sea ice Svalbard Copernicus Publications: E-Journals Arctic Svalbard |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
The airborne field campaign HALO–(AC)³ took place from 07 March to 12 April 2022 and was designed to observe the transformation of air masses during their meridional transport in the North Atlantic sector of the Arctic. We evaluate the meteorological and sea ice conditions during the campaign based on the European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis v5 (ERA5), satellite data, and atmospheric soundings with respect to climatology and describe special synoptic events. HALO–(AC)³ started with a warm period (11–20 March) where strong southerly winds prevailed that caused moist and warm air intrusions (MWAIs). Two MWAIs were detected as Atmospheric Rivers (ARs). Compared to the ERA5 climatology (1979–2022), record breaking vertically integrated poleward heat and moisture fluxes averaged over 75.0–81.5° N were found. The related warm and moist air masses reached the central Arctic, causing the highest rainfall rates over the sea ice northwest of Svalbard recorded since the beginning of the ERA5 climatology. Subsequently, the cold period of HALO–(AC)³ started after the passage of a Shapiro–Keyser cyclone on 21 March when the wind regime turned to northerlies, advecting colder air into the Fram Strait. Until 08 April, marine cold air outbreaks (MCAOs) prevailed, including two strong MCAO events on 21–26 March and 01–02 April. In between, aged subpolar warm air was advected to the Fram Strait with northeasterly and easterly winds. On average, the campaign period was warmer than the climatology, especially due to the exceptionally strong ARs during the warm period. In the Fram Strait, the sea ice concentration (SIC) was within the 10–90 th percentiles of the climatology over the entire campaign duration. During the warm period, SIC was strongly reduced and an untypically large polynya for this season opened north of Svalbard. During the cold period, the polynya was closed again and above average SICs were found. We describe the environmental conditions of a Polar Low and ... |
format |
Text |
author |
Walbröl, Andreas Michaelis, Janosch Becker, Sebastian Dorff, Henning Gorodetskaya, Irina Kirbus, Benjamin Lauer, Melanie Maherndl, Nina Maturilli, Marion Mayer, Johanna Müller, Hanno Neggers, Roel A. J. Paulus, Fiona M. Röttenbacher, Johannes Rückert, Janna E. Schirmacher, Imke Slättberg, Nils Ehrlich, André Wendisch, Manfred Crewell, Susanne |
spellingShingle |
Walbröl, Andreas Michaelis, Janosch Becker, Sebastian Dorff, Henning Gorodetskaya, Irina Kirbus, Benjamin Lauer, Melanie Maherndl, Nina Maturilli, Marion Mayer, Johanna Müller, Hanno Neggers, Roel A. J. Paulus, Fiona M. Röttenbacher, Johannes Rückert, Janna E. Schirmacher, Imke Slättberg, Nils Ehrlich, André Wendisch, Manfred Crewell, Susanne Environmental conditions in the North Atlantic sector of the Arctic during the HALO–(AC)³ campaign |
author_facet |
Walbröl, Andreas Michaelis, Janosch Becker, Sebastian Dorff, Henning Gorodetskaya, Irina Kirbus, Benjamin Lauer, Melanie Maherndl, Nina Maturilli, Marion Mayer, Johanna Müller, Hanno Neggers, Roel A. J. Paulus, Fiona M. Röttenbacher, Johannes Rückert, Janna E. Schirmacher, Imke Slättberg, Nils Ehrlich, André Wendisch, Manfred Crewell, Susanne |
author_sort |
Walbröl, Andreas |
title |
Environmental conditions in the North Atlantic sector of the Arctic during the HALO–(AC)³ campaign |
title_short |
Environmental conditions in the North Atlantic sector of the Arctic during the HALO–(AC)³ campaign |
title_full |
Environmental conditions in the North Atlantic sector of the Arctic during the HALO–(AC)³ campaign |
title_fullStr |
Environmental conditions in the North Atlantic sector of the Arctic during the HALO–(AC)³ campaign |
title_full_unstemmed |
Environmental conditions in the North Atlantic sector of the Arctic during the HALO–(AC)³ campaign |
title_sort |
environmental conditions in the north atlantic sector of the arctic during the halo–(ac)³ campaign |
publishDate |
2023 |
url |
https://doi.org/10.5194/egusphere-2023-668 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-668/ |
geographic |
Arctic Svalbard |
geographic_facet |
Arctic Svalbard |
genre |
Arctic Fram Strait North Atlantic Sea ice Svalbard |
genre_facet |
Arctic Fram Strait North Atlantic Sea ice Svalbard |
op_source |
eISSN: |
op_relation |
doi:10.5194/egusphere-2023-668 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-668/ |
op_doi |
https://doi.org/10.5194/egusphere-2023-668 |
_version_ |
1767956203929862144 |