Articles | Volume 24, issue 3
https://doi.org/10.5194/acp-24-1961-2024
https://doi.org/10.5194/acp-24-1961-2024
Research article
 | 
14 Feb 2024
Research article |  | 14 Feb 2024

Tethered balloon-borne observations of thermal-infrared irradiance and cooling rate profiles in the Arctic atmospheric boundary layer

Michael Lonardi, Elisa F. Akansu, André Ehrlich, Mauro Mazzola, Christian Pilz, Matthew D. Shupe, Holger Siebert, and Manfred Wendisch

Data sets

BELUGA TIR radiation profile measurements at MOSAiC and Ny-Alesund Michael Lonardi et al. https://doi.org/10.5281/zenodo.8079768

Atmospheric Surface Flux Station #50 measurements (Level 3 Final), Multidisciplinary Drifting Observatory for the Study of Arctic Climate (MOSAiC), central Arctic, October 2019-September 2020 Christopher Cox et al. https://doi.org/10.18739/A2XD0R00S

MOSAiC radiosonde data (level 3) Marion Maturilli et al. https://doi.org/10.1594/PANGAEA.943870

High resolution radiosonde measurements from station Ny-Ålesund (2017-04 et seq) Marion Maturilli https://doi.org/10.1594/PANGAEA.914973

Climate Change Tower Radiation Data Mauro Mazzola et al. https://data.iadc.cnr.it/erddap/tabledap/cct_radiation_d2.html

Custom collection of categorize, classification, droplet effective radius, ice effective radius, ice water content, and liquid water content data from Ny-Ålesund between 1 Sep 2021 and 30 May 2022 Kerstin Ebell et al. https://doi.org/10.60656/2498625552e84611

Custom collection of categorize, classification, ice water content, lidar, and liquid water content data from RV Polarstern between 28 Sep 2019 and 1 Oct 2020 R. Engelmann et al. https://hdl.handle.net/21.12132/2.241e5a2b37654e45

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Short summary
Profiles of thermal-infrared irradiance were measured at two Arctic sites. The presence or lack of clouds influences the vertical structure of these observations. In particular, the cloud top region is a source of radiative energy that can promote cooling and mixing in the cloud layer. Simulations are used to further characterize how the amount of water in the cloud modifies this forcing. A case study additionally showcases the evolution of the radiation profiles in a dynamic atmosphere.
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