Articles | Volume 2, issue 1
https://doi.org/10.5194/wcd-2-281-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/wcd-2-281-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
29 Mar 2021
Research article | Highlight paper |
| 29 Mar 2021
| 29 Mar 2021
How Rossby wave breaking modulates the water cycle in the North Atlantic trade wind region
Franziska Aemisegger
CORRESPONDING AUTHOR
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich,
8092, Switzerland
Raphaela Vogel
LMD/IPSL, Sorbonne University, CNRS, Paris, France
Pascal Graf
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich,
8092, Switzerland
Fabienne Dahinden
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich,
8092, Switzerland
Leonie Villiger
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich,
8092, Switzerland
Friedhelm Jansen
Max Planck Institute for Meteorology, Hamburg, Germany
Sandrine Bony
LMD/IPSL, Sorbonne University, CNRS, Paris, France
Bjorn Stevens
Max Planck Institute for Meteorology, Hamburg, Germany
Heini Wernli
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich,
8092, Switzerland
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Cited
20 citations as recorded by crossref.
- Marine Boundary Layer Decoupling and the Stable Isotopic Composition of Water Vapor J. Galewsky et al. 10.1029/2021JD035470
- Mesoscale spatio-temporal variability of airborne lidar-derived aerosol properties in the Barbados region during EUREC4A P. Chazette et al. 10.5194/acp-22-1271-2022
- Cloud Botany: Shallow Cumulus Clouds in an Ensemble of Idealized Large‐Domain Large‐Eddy Simulations of the Trades F. Jansson et al. 10.1029/2023MS003796
- EUREC<sup>4</sup>A B. Stevens et al. 10.5194/essd-13-4067-2021
- Water isotopic characterisation of the cloud–circulation coupling in the North Atlantic trades – Part 1: A process-oriented evaluation of COSMOiso simulations with EUREC4A observations L. Villiger et al. 10.5194/acp-23-14643-2023
- On the daily cycle of mesoscale cloud organization in the winter trades J. Vial et al. 10.1002/qj.4103
- Retrieving H<sub>2</sub>O/HDO columns over cloudy and clear-sky scenes from the Tropospheric Monitoring Instrument (TROPOMI) A. Schneider et al. 10.5194/amt-15-2251-2022
- Sources of Uncertainty in Mid‐Tropospheric Tropical Humidity in Global Storm‐Resolving Simulations T. Lang et al. 10.1029/2022MS003443
- Unravelling the transport of moisture into the Saharan Air Layer using passive tracers and isotopes F. Dahinden et al. 10.1002/asl.1187
- Isotopic measurements in water vapor, precipitation, and seawater during EUREC4A A. Bailey et al. 10.5194/essd-15-465-2023
- Lagrangian formation pathways of moist anomalies in the trade-wind region during the dry season: two case studies from EUREC<sup>4</sup>A L. Villiger et al. 10.5194/wcd-3-59-2022
- The meteorological drivers of mass coral bleaching on the central Great Barrier Reef during the 2022 La Niña L. Richards et al. 10.1038/s41598-024-74181-2
- A climatology of trade-wind cumulus cold pools and their link to mesoscale cloud organization R. Vogel et al. 10.5194/acp-21-16609-2021
- Disentangling different moisture transport pathways over the eastern subtropical North Atlantic using multi-platform isotope observations and high-resolution numerical modelling F. Dahinden et al. 10.5194/acp-21-16319-2021
- Quantifying free tropospheric moisture sources over the western tropical Atlantic with numerical water tracers and isotopes S. Botsyun et al. 10.1002/asl.1274
- EUREC<sup>4</sup>A observations from the SAFIRE ATR42 aircraft S. Bony et al. 10.5194/essd-14-2021-2022
- A survey of radiative and physical properties of North Atlantic mesoscale cloud morphologies from multiple identification methodologies R. Eastman et al. 10.5194/acp-24-6613-2024
- Water isotopic characterisation of the cloud–circulation coupling in the North Atlantic trades – Part 2: The imprint of the atmospheric circulation at different scales L. Villiger & F. Aemisegger 10.5194/acp-24-957-2024
- Process‐oriented evaluation of the oversea AROME configuration: Focus on the representation of cloud organisation F. Beucher et al. 10.1002/qj.4354
- Characterizing water vapour concentration dependence of commercial cavity ring-down spectrometers for continuous on-site atmospheric water vapour isotope measurements in the tropics S. Komiya et al. 10.5194/amt-14-1439-2021
19 citations as recorded by crossref.
- Marine Boundary Layer Decoupling and the Stable Isotopic Composition of Water Vapor J. Galewsky et al. 10.1029/2021JD035470
- Mesoscale spatio-temporal variability of airborne lidar-derived aerosol properties in the Barbados region during EUREC4A P. Chazette et al. 10.5194/acp-22-1271-2022
- Cloud Botany: Shallow Cumulus Clouds in an Ensemble of Idealized Large‐Domain Large‐Eddy Simulations of the Trades F. Jansson et al. 10.1029/2023MS003796
- EUREC<sup>4</sup>A B. Stevens et al. 10.5194/essd-13-4067-2021
- Water isotopic characterisation of the cloud–circulation coupling in the North Atlantic trades – Part 1: A process-oriented evaluation of COSMOiso simulations with EUREC4A observations L. Villiger et al. 10.5194/acp-23-14643-2023
- On the daily cycle of mesoscale cloud organization in the winter trades J. Vial et al. 10.1002/qj.4103
- Retrieving H<sub>2</sub>O/HDO columns over cloudy and clear-sky scenes from the Tropospheric Monitoring Instrument (TROPOMI) A. Schneider et al. 10.5194/amt-15-2251-2022
- Sources of Uncertainty in Mid‐Tropospheric Tropical Humidity in Global Storm‐Resolving Simulations T. Lang et al. 10.1029/2022MS003443
- Unravelling the transport of moisture into the Saharan Air Layer using passive tracers and isotopes F. Dahinden et al. 10.1002/asl.1187
- Isotopic measurements in water vapor, precipitation, and seawater during EUREC4A A. Bailey et al. 10.5194/essd-15-465-2023
- Lagrangian formation pathways of moist anomalies in the trade-wind region during the dry season: two case studies from EUREC<sup>4</sup>A L. Villiger et al. 10.5194/wcd-3-59-2022
- The meteorological drivers of mass coral bleaching on the central Great Barrier Reef during the 2022 La Niña L. Richards et al. 10.1038/s41598-024-74181-2
- A climatology of trade-wind cumulus cold pools and their link to mesoscale cloud organization R. Vogel et al. 10.5194/acp-21-16609-2021
- Disentangling different moisture transport pathways over the eastern subtropical North Atlantic using multi-platform isotope observations and high-resolution numerical modelling F. Dahinden et al. 10.5194/acp-21-16319-2021
- Quantifying free tropospheric moisture sources over the western tropical Atlantic with numerical water tracers and isotopes S. Botsyun et al. 10.1002/asl.1274
- EUREC<sup>4</sup>A observations from the SAFIRE ATR42 aircraft S. Bony et al. 10.5194/essd-14-2021-2022
- A survey of radiative and physical properties of North Atlantic mesoscale cloud morphologies from multiple identification methodologies R. Eastman et al. 10.5194/acp-24-6613-2024
- Water isotopic characterisation of the cloud–circulation coupling in the North Atlantic trades – Part 2: The imprint of the atmospheric circulation at different scales L. Villiger & F. Aemisegger 10.5194/acp-24-957-2024
- Process‐oriented evaluation of the oversea AROME configuration: Focus on the representation of cloud organisation F. Beucher et al. 10.1002/qj.4354
Latest update: 13 Dec 2024
Short summary
The interaction of clouds in the trade wind region with the atmospheric flow is complex and at the heart of uncertainties associated with climate projections. In this study, a natural tracer of atmospheric circulation is used to establish a link between air originating from dry regions of the midlatitudes and the occurrence of specific cloud patterns. Two pathways involving transport within midlatitude weather systems are identified, by which air is brought into the trades within 5–10 d.
The interaction of clouds in the trade wind region with the atmospheric flow is complex and at...
