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{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,1,18]],"date-time":"2024-01-18T23:50:01Z","timestamp":1705621801145},"reference-count":94,"publisher":"Frontiers Media SA","license":[{"start":{"date-parts":[[2023,4,11]],"date-time":"2023-04-11T00:00:00Z","timestamp":1681171200000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"content-domain":{"domain":["frontiersin.org"],"crossmark-restriction":true},"short-container-title":["Front. Earth Sci."],"abstract":"<jats:p>Distinct events of warm and moist air intrusions (WAIs) from mid-latitudes have pronounced impacts on the Arctic climate system. We present a detailed analysis of a record-breaking WAI observed during the MOSAiC expedition in mid-April 2020. By combining Eulerian with Lagrangian frameworks and using simulations across different scales, we investigate aspects of air mass transformations <jats:italic>via<\/jats:italic> cloud processes and quantify related surface impacts. The WAI is characterized by two distinct pathways, Siberian and Atlantic. A moist static energy transport across the Arctic Circle above the climatological 90th percentile is found. Observations at research vessel Polarstern show a transition from radiatively clear to cloudy state with significant precipitation and a positive surface energy balance (SEB), i.e., surface warming. WAI air parcels reach Polarstern first near the tropopause, and only 1\u20132\u00a0days later at lower altitudes. In the 5\u00a0days prior to the event, latent heat release during cloud formation triggers maximum diabatic heating rates in excess of 20\u00a0K\u00a0d<jats:sup>-1<\/jats:sup>. For some poleward drifting air parcels, this facilitates strong ascent by up to 9\u00a0km. Based on model experiments, we explore the role of two key cloud-determining factors. First, we test the role moisture availability by reducing lateral moisture inflow during the WAI by 30%. This does not significantly affect the liquid water path, and therefore the SEB, in the central Arctic. The cause are counteracting mechanisms of cloud formation and precipitation along the trajectory. Second, we test the impact of increasing Cloud Condensation Nuclei concentrations from 10 to 1,000\u00a0cm<jats:sup>-3<\/jats:sup> (pristine Arctic to highly polluted), which enhances cloud water content. Resulting stronger longwave cooling at cloud top makes entrainment more efficient and deepens the atmospheric boundary layer. Finally, we show the strongly positive effect of the WAI on the SEB. This is mainly driven by turbulent heat fluxes over the ocean, but radiation over sea ice. The WAI also contributes a large fraction to precipitation in the Arctic, reaching 30% of total precipitation in a 9-day period at the MOSAiC site. However, measured precipitation varies substantially between different platforms. Therefore, estimates of total precipitation are subject to considerable observational uncertainty.<\/jats:p>","DOI":"10.3389\/feart.2023.1147848","type":"journal-article","created":{"date-parts":[[2023,4,11]],"date-time":"2023-04-11T05:58:07Z","timestamp":1681192687000},"update-policy":"http:\/\/dx.doi.org\/10.3389\/crossmark-policy","source":"Crossref","is-referenced-by-count":2,"title":["Surface impacts and associated mechanisms of a moisture intrusion into the Arctic observed in mid-April 2020 during MOSAiC"],"prefix":"10.3389","volume":"11","author":[{"given":"Benjamin","family":"Kirbus","sequence":"first","affiliation":[]},{"given":"Sofie","family":"Tiedeck","sequence":"additional","affiliation":[]},{"given":"Andrea","family":"Camplani","sequence":"additional","affiliation":[]},{"given":"Jan","family":"Chylik","sequence":"additional","affiliation":[]},{"given":"Susanne","family":"Crewell","sequence":"additional","affiliation":[]},{"given":"Sandro","family":"Dahlke","sequence":"additional","affiliation":[]},{"given":"Kerstin","family":"Ebell","sequence":"additional","affiliation":[]},{"given":"Irina","family":"Gorodetskaya","sequence":"additional","affiliation":[]},{"given":"Hannes","family":"Griesche","sequence":"additional","affiliation":[]},{"given":"D\u00f6rthe","family":"Handorf","sequence":"additional","affiliation":[]},{"given":"Ines","family":"H\u00f6schel","sequence":"additional","affiliation":[]},{"given":"Melanie","family":"Lauer","sequence":"additional","affiliation":[]},{"given":"Roel","family":"Neggers","sequence":"additional","affiliation":[]},{"given":"Janna","family":"R\u00fcckert","sequence":"additional","affiliation":[]},{"given":"Matthew D.","family":"Shupe","sequence":"additional","affiliation":[]},{"given":"Gunnar","family":"Spreen","sequence":"additional","affiliation":[]},{"given":"Andreas","family":"Walbr\u00f6l","sequence":"additional","affiliation":[]},{"given":"Manfred","family":"Wendisch","sequence":"additional","affiliation":[]},{"given":"Annette","family":"Rinke","sequence":"additional","affiliation":[]}],"member":"1965","published-online":{"date-parts":[[2023,4,11]]},"reference":[{"key":"B1","doi-asserted-by":"publisher","first-page":"3522","DOI":"10.1002\/qj.3859","article-title":"Following moist intrusions into the Arctic using SHEBA observations in a Lagrangian perspective","volume":"146","author":"Ali","year":"2020","journal-title":"Q. 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