Airborne observations of far-infrared upwelling radiance in the Arctic

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Libois, Quentin, Ivanescu, Liviu, Blanchet, Jean-Pierre, Schulz, Hannes, Bozem, Heiko, Leaitch, W. Richard, Burkart, Julia, Abbatt, Jonathan, Herber, Andreas, Aliabadi, Amir, Girard, Éric
• Other Authors: Centre ESCER, Université du Québec à Montréal = University of Québec in Montréal (UQAM), Alfred Wegener Institute for Polar and Marine Research (AWI), Institute for Atmospheric Physics Mainz (IPA), Johannes Gutenberg - Universität Mainz (JGU), Environment and Climate Change Canada, Department of Chemistry University of Toronto, University of Toronto, University of Guelph
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2016
• Subjects: [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]; Arctic
• Online Access: https://hal.archives-ouvertes.fr/hal-03187135; https://hal.archives-ouvertes.fr/hal-03187135/document; https://hal.archives-ouvertes.fr/hal-03187135/file/Libois2016_NETCARE.pdf; https://doi.org/10.5194/acp-16-15689-2016

International audience The first airborne measurements of the Far-InfraRed Radiometer (FIRR) were performed in April 2015 during the panarctic NETCARE campaign. Vertical profiles of spectral upwelling radiance in the range 8–50 µm were measured in clear and cloudy conditions from the surface up to 6 km. The clear sky profiles highlight the strong dependence of radiative fluxes to the temperature inversion typical of the Arctic. Measurements acquired for total column water vapour from 1.5 to 10.5 mm also underline the sensitivity of the far-infrared greenhouse effect to specific humidity. The cloudy cases show that optically thin ice clouds increase the cooling rate of the atmosphere, making them important pieces of the Arctic energy balance. One such cloud exhibited a very complex spatial structure, characterized by large horizontal heterogeneities at the kilometre scale. This emphasizes the difficulty of obtaining representative cloud observations with airborne measurements but also points out how challenging it is to model polar clouds radiative effects. These radiance measurements were successfully compared to simulations, suggesting that state-of-the-art radiative transfer models are suited to study the cold and dry Arctic atmosphere. Although FIRR in situ performances compare well to its laboratory performances, complementary simulations show that upgrading the FIRR radiometric resolution would greatly increase its sensitivity to atmospheric and cloud properties. Improved instrument temperature stability in flight and expected technological progress should help meet this objective. The campaign overall highlights the potential for airborne far-infrared radiometry and constitutes a relevant reference for future similar studies dedicated to the Arctic and for the development of spaceborne instruments.