Airborne observations of cloud properties during their evolution from organized streets to isotropic cloud structures along an Arctic cold air outbreak

None, None; None, None; None, None; None, None; None, None; None, None; None, None; None, None; None, None; None, None; None, None; None, None; None, None; None, None; None, None

Airborne observations of cloud properties during their evolution from organized streets to isotropic cloud structures along an Arctic cold air outbreak

Preprint (2025)

Author(s)

Marcus Klingebiel (University of Leipzig)

André Ehrlich (University of Leipzig)

Micha Gryschka (Leibniz Universität Hannover)

Nils Risse (Universität zu Köln)

Nina Maherndl (University of Leipzig)

Imke Schirmacher (Universität zu Köln)

Sophie Rosenburg (University of Leipzig)

Sabine Hörnig (University of Leipzig)

Manuel Moser (Deutsches Zentrum für Luft- und Raumfahrt (DLR), Johannes Gutenberg-University Mainz)

Evelyn Jäkel (University of Leipzig)

Michael Schäfer (University of Leipzig)

Hartwig Deneke (Leibniz-Institut für Troposphärenforschung)

Mario Mech (Universität zu Köln)

Christiane Voigt (Deutsches Zentrum für Luft- und Raumfahrt (DLR), Johannes Gutenberg-University Mainz)

Manfred Wendisch (University of Leipzig)

Affiliation

External organisation

DOI related publication

https://doi.org/10.5194/egusphere-2025-201 Final published version

To reference this document use

https://resolver.tudelft.nl/uuid:96ab513c-3141-4bde-a91d-9586d68d5d4c

More Info

expand_more

Publication Year

2025

Language

English

Affiliation

External organisation

Publisher

EGUsphere Preprint repository

Downloads counter

235

Abstract

This case study explores the evolution of clouds during an Arctic cold air outbreak in the Fram Strait region observed during the HALO-(𝒜𝒞)3 aircraft campaign. Our research provides information about the formation, structure, micro- and macrophysical properties, radiative effects and investigates the role of vertical wind shear and buoyancy forces in the transition from regular cloud streets to rather isotropic cloud patterns. Our findings show that lower horizontal boundary layer wind speeds (< 12 m s-1) disrupt the formation of cloud streets, leading to more isotropic cloud patterns, characterized by increasing cloud fraction (from 0.73 to 0.84), cloud top height (from 330 m to 390 m), and quantify the increase of liquid water path as well. In addition, we observe an increase of the number concentration of ice crystals in a size range between 100 µm and 1000 µm and notable riming processes within organized cloud streets. Concurrent radiation measurements in our case study reveal that isotropic cloud patterns can exhibit either low or high albedo as well as low or high Fnet,TIR, suggesting that these patterns represent different developing stages.