Laboratoire Interuniversitaire des Systèmes Atmosphériques, Université Paris Est Créteil, Université de Paris, Institut Pierre-Simon Laplace, Créteil, France
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Catania, Italy
Nelson Bègue
Laboratoire de l'Atmosphère et des Cyclones (LACy), UMR 8105 CNRS, Université de La Réunion, Météo-France, Saint-Denis de la Réunion, 97400, France
Hassan Bencherif
Laboratoire de l'Atmosphère et des Cyclones (LACy), UMR 8105 CNRS, Université de La Réunion, Météo-France, Saint-Denis de la Réunion, 97400, France
Guillaume Payen
Observatoire des Sciences de l'Univers – Réunion (OSU-R), Saint-Denis, 97400, France
Nicolas Marquestaut
Observatoire des Sciences de l'Univers – Réunion (OSU-R), Saint-Denis, 97400, France
Valentin Duflot
Laboratoire de l'Atmosphère et des Cyclones (LACy), UMR 8105 CNRS, Université de La Réunion, Météo-France, Saint-Denis de la Réunion, 97400, France
now at: Department for Atmospheric and Climate Research, NILU, Kjeller, Norway
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Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 358 (including HTML, PDF, and XML)
Thereof 339 with geography defined
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Total article views: 66 (including HTML, PDF, and XML)
Thereof 66 with geography defined
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Total article views: 292 (including HTML, PDF, and XML)
Thereof 273 with geography defined
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This study quantifies the radiative impact over Réunion Island (21° S, 55° E) of the aerosols and water vapor injected into the stratosphere by the Hunga volcano in the South Pacific. The overall aerosol and water vapor impact on the Earth’s radiation budget for the whole period is negative (cooling, -0.82 ± 0.35 W m-2) and dominated by the aerosols. At the Earth’s surface, aerosols are the main drivers and produce a negative (cooling, -1.04 ± 0.36 W m-2) radiative impact.
This study quantifies the radiative impact over Réunion Island (21° S, 55° E) of the aerosols...