Water isotopic characterisation of the cloud-circulation coupling in the North Atlantic trades-Part 1

Autor(en)
Leonie Villiger, Marina Dütsch, Sandrine Bony, Marie Lothon, Stephan Pfahl, Heini Wernli, Pierre Etienne Brilouet, Patrick Chazette, Pierre Coutris, Julien Delanoë, Cyrille Flamant, Alfons Schwarzenboeck, Martin Werner, Franziska Aemisegger
Abstrakt

Naturally available, stable, and heavy water molecules such as HDO and H218O have a lower saturation vapour pressure than the most abundant light water molecule H216O; therefore, these heavy water molecules preferentially condense and rain out during cloud formation. Stable water isotope observations thus have the potential to provide information on cloud processes in the trade-wind region, in particular when combined with high-resolution model simulations. In order to evaluate this potential, nested COSMOiso (isotope-enabled Consortium for Small Scale Modelling; ) simulations with explicit convection and horizontal grid spacings of 10, 5, and 1ĝ€¯km were carried out in this study over the tropical Atlantic for the time period of the EUREC4A (Elucidating the role of clouds-circulation coupling in climate; ) field experiment. The comparison to airborne in situ and remote sensing observations shows that the three simulations are able to distinguish between different mesoscale cloud organisation patterns as well as between periods with comparatively high and low rain rates. Cloud fraction and liquid water content show a better agreement with aircraft observations with higher spatial resolution, because they show strong spatial variations on the scale of a few kilometres. A low-level cold-dry bias, including too depleted vapour in the subcloud and cloud layer and too enriched vapour in the free troposphere, is found in all three simulations. Furthermore, the simulated secondary isotope variable d-excess in vapour is overestimated compared to observations. Special attention is given to the cloud base level, which is the formation altitude of shallow cumulus clouds. The temporal variability of the simulated isotope variables at cloud base agrees reasonably well with observations, with correlations of the flight-To-flight data as high as 0.7 for I2H and d-excess. A close examination of isotopic characteristics under precipitating clouds, non-precipitating clouds, clear-sky and dry-warm patches at the altitude of cloud base shows that these different environments are represented faithfully in the model with similar frequencies of occurrence, isotope signals, and specific-humidity anomalies as found in the observations. Furthermore, it is shown that the 2H of cloud base vapour at the hourly timescale is mainly controlled by mesoscale transport and not by local microphysical processes, while the d-excess is mainly controlled by large-scale drivers. Overall, this evaluation of COSMOiso, including the isotopic characterisation of different cloud base environments, suggests that the simulations can be used for investigating the role of atmospheric circulations on different scales for controlling the formation of shallow cumulus clouds in the trade-wind region, as will be done in part 2 of this study.

Organisation(en)
Institut für Meteorologie und Geophysik
Externe Organisation(en)
Eidgenössische Technische Hochschule Zürich, Université Paris VI - Pierre-et-Marie-Curie, Université de Toulouse, Freie Universität Berlin (FU), Centre National De La Recherche Scientifique (CNRS), Université de Versailles-Saint-Quentin-en-Yvelines, Univeristé Clermont Auvergne, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung
Journal
Atmospheric Chemistry and Physics
Band
23
Seiten
14643-14672
Anzahl der Seiten
30
ISSN
1680-7316
DOI
https://doi.org/10.5194/acp-23-14643-2023
Publikationsdatum
11-2023
Peer-reviewed
Ja
ÖFOS 2012
105204 Klimatologie, 105206 Meteorologie
ASJC Scopus Sachgebiete
Atmospheric Science
Sustainable Development Goals
SDG 13 – Maßnahmen zum Klimaschutz
Link zum Portal
https://ucrisportal.univie.ac.at/de/publications/2c11b6c5-6c46-45b7-9fee-4b8ce8ad8b7b