PUBLICATIONS

AWACA publications

January 2026

The erosion of surface snow by the wind is an important process for the Antarctic surface mass balance. This study presents the first development of a parameterisation of blowing snow for a global climate model. Simulations avec evaluated using measurements in Antarctica. Results show an overall decrease of the snow accumulation in the escarpment region of the ice sheet due to snow erosion and an increase at the coast due to blowing snow deposition and increase in precipitation.

November 2025

Katabatic winds are a key feature of the climate of Antarctica, but substantial biases remain in their representation in atmospheric models. This study investigates a katabatic wind event in an atmospheric circulation model using in-situ observations. The framework allows to disentangle which part of the bias is due to horizontal resolution, to parameter calibration and to structural deficiencies in the model. We underline in particular the need to refine the physics of the model snow cover.

October 2025

We present a novel 2.5-month record of the atmospheric water vapour isotopic composition during the austral summer 2023–2024 at Concordia Station on the Antarctic Plateau. We show that two independent laser spectrometers accurately record the diurnal variability of the atmospheric water vapour 𝛿18O, 𝛿D, and d-excess. We compare the measurements against outputs of the isotope-enabled general circulation model LMDZ6-iso to show how the data can be used to evaluate such models.

August 2025

As part of his research project at ENSTA, Maxime Coste assessed the representativeness of an AWACA “golden event” selected in February 2025 using 15 years of MRR (Micro Rain Radar) data from Dumont d’Urville, and explored, using artificial intelligence methods applied to ceilometer measurements, how to fill the MRR surface blind zone.

July 2025

In December 2018, an atmospheric river event from the Atlantic reached Dome C, East Antarctica, causing a +18 °C warming, tripled water vapour, and a strong isotopic anomaly in water vapour (+ 17 ‰ for δ18O) at the surface. During the peak of the event, we found 70 % of the water vapour came from local snow sublimation, and 30 % from the atmospheric river itself, highlighting both large-scale advection and local interactions at the surface.

March 2025

Water vapour isotopes are important tools to better understand processes governing the atmospheric hydrological cycle. In polar regions, their measurement helps to improve the interpretation of water isotopic records in ice cores. However, in situ water vapour isotopic monitoring is an important challenge, especially in dry places of East Antarctica. We present here an alternative laser spectroscopy technique adapted for such measurements, with a limit of detection down to 10 ppm humidity.

February 2025

The transport of water isotopes by the atmosphere plays a key role in interpreting Antarctic climate archives. This study evaluates the LMDZ6iso atmospheric model using snow, precipitation and vapour isotope measurements from both coastal and inland East Antarctica. The model is assessed at spatial, seasonal and diurnal scales, and the contribution of individual processes to boundary layer vapour isotopes is analysed. Results highlight the importance of isotopic exchanges during sublimation and condensation at low temperature, and suggest that including these processes would improve the representation of water isotopes in climate models.

October 2024

This study introduces a new fully tunable TKE-l parameterization for turbulent diffusion in planetary atmospheres. The scheme is designed with a minimal set of adjustable parameters and a mixing length formulation that accounts for both stability and wind shear, making it applicable to Earth and Mars. Emphasis is placed on ensuring numerical stability at large time steps, a key challenge in simulating stable boundary layers. After calibration on idealized 1D cases, the parameterization successfully reproduces Antarctic and Martian nocturnal boundary layers in 3D simulations, demonstrating its robustness and versatility.

figure CALIPSO
July 2024

As part of her Master’s internship (M2), Justine Charrel evaluated cloud cover over Antarctica in the latest version of the LMDZ6A climate model using observations from the CALIPSO satellite.

May 2024

Coastal surface winds in Antarctica are amongst the strongest winds on Earth. They are either driven by the cooling of the surface air mass by the ice sheet (katabatic) or by large-scale pressure systems. Here we compute the relative contribution of these drivers. We find that seasonal variations in the wind speed come from the katabatic acceleration, but, at a 3-hourly timescale, none of the large-scale or katabatic accelerations can be considered as the main driver.

Publications related to AWACA

  • Landais, A., Agosta, C., Vimeux, F., Magand, O., Solis, C., Cauquoin, A., Dutrievoz, N., Risi, C., Leroy-Dos Santos, C., FourrĂ©, E., Cattani, O., Jossoud, O., Minster, B., PriĂ©, F., Casado, M., Dommergue, A., Bertrand, Y., and Werner, M.: Abrupt excursions in water vapor isotopic variability at the Pointe Benedicte observatory on Amsterdam Island, Atmos. Chem. Phys., 24, 4611–4634, https://doi.org/10.5194/acp-24-4611-2024, 2024.