Following moist intrusions into the Arctic using SHEBA observations in a Lagrangian perspective

Ali, Syed Mubashshir; Pithan, Felix (2020). Following moist intrusions into the Arctic using SHEBA observations in a Lagrangian perspective. Quarterly Journal of the Royal Meteorological Society, 146(732), pp. 3522-3533. Royal Meteorological Society 10.1002/qj.3859

Preview

Text qj.3859.pdf - Accepted Version Available under License Publisher holds Copyright. Download (7MB) | Preview

Warm and moist air masses are transported into the Arctic from lower latitudes throughout the year. Especially in winter, such moist intrusions can trigger cloud formation and surface warming. While a typical cloudy state of the Arctic winter boundary layer has been linked to the advection of moist air masses, direct observations of the transformation from moist mid‐latitude to dry Arctic air are lacking. Here, we have used observations from the Surface Heat Budget of the Arctic Ocean(SHEBA) project to compile Eulerian observations along the trajectories of warm and cold air masses in a Lagrangian sense, showing the cooling and drying of air masses over sea ice and moistening over the open ocean. Air masses originating mostly over open water generate cloudy conditions over the observation site, whereas air masses originating over continents or sea ice generate radiatively clear conditions. We recommend using our case studies for modelling work and the method of linking expeditions to station soundings via back‐trajectories for future campaigns.

Interest & Impact

Downloads

106 since deposited on 25 Jun 2020
30 in the past 12 months

Citations

5 Citations in Web of Science ®
6 Citations in Scopus

Search

in Google Scholar™

Services

Actions (login required)

Edit item

Actions (login required)

Edit item