Articles | Volume 20, issue 14
https://doi.org/10.5194/acp-20-8989-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-20-8989-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
29 Jul 2020
Research article |
| 29 Jul 2020
| 29 Jul 2020
Differences in tropical high clouds among reanalyses: origins and radiative impacts
Jonathon S. Wright
CORRESPONDING AUTHOR
Ministry of Education Key Laboratory for Earth System Modeling, Department of Earth System Science, Tsinghua University, Beijing, China
Xiaoyi Sun
Ministry of Education Key Laboratory for Earth System Modeling, Department of Earth System Science, Tsinghua University, Beijing, China
Paul Konopka
Forschungszentrum Jülich (IEK-7: Stratosphere), Jülich, Germany
Kirstin Krüger
Department of Geosciences, University of Oslo, Oslo, Norway
Bernard Legras
Laboratoire de Météorologie Dynamique, UMR CNRS 8539, IPSL, PSL-ENS/Sorbonne Université/École Polytechnique, Paris, France
Andrea M. Molod
Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Susann Tegtmeier
Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, Canada
Guang J. Zhang
Scripps Institution of Oceanography, La Jolla, California, USA
Department of Atmospheric Sciences, Texas A & M University, College Station, Texas, USA
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- The role of tropical upwelling in explaining discrepancies between recent modeled and observed lower-stratospheric ozone trends S. Davis et al. 10.5194/acp-23-3347-2023
- Atmospheric tropical modes are important drivers of Sahelian springtime heatwaves K. Guigma et al. 10.1007/s00382-020-05569-9
- Impacts of tropical cyclones on the thermodynamic conditions in the tropical tropopause layer observed by A-Train satellites J. Feng & Y. Huang 10.5194/acp-21-15493-2021
- A Lagrangian View of Seasonal Stratosphere‐Troposphere Exchange M. Schoeberl et al. 10.1029/2022JD036772
- Clear-sky control of anvils in response to increased CO2 or surface warming or volcanic eruptions M. Saint-Lu et al. 10.1038/s41612-022-00304-z
- Specific Features of the Land-Sea Contrast of Cloud Liquid Water Path in Northern Europe as Obtained from the Observations by the SEVIRI Instrument: Artefacts or Reality? V. Kostsov & D. Ionov 10.3390/meteorology2040027
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- Spatio-Temporal Variation of Critical Relative Humidity Based on Multiple Datasets W. Zhang et al. 10.3390/rs15174187
- Arctic cloud properties and associated radiative effects in the three newer reanalysis datasets (ERA5, MERRA-2, JRA-55): Discrepancies and possible causes H. Yeo et al. 10.1016/j.atmosres.2022.106080
- Revisiting mechanisms of the Mesoamerican Midsummer drought J. García-Franco et al. 10.1007/s00382-022-06338-6
- Diffuse Radiation Forcing Constraints on Gross Primary Productivity and Global Terrestrial Evapotranspiration T. Chakraborty et al. 10.1029/2022EF002805
- CMIP6 captures the satellite-era jet slowdown and Arctic amplification, yet projects future jet speedup and tropical amplification R. Robinson et al. 10.1007/s00382-023-06839-y
- Environmental Response in Coupled Energy and Water Cloud Impact Parameters Derived from A-Train Satellites, ERA-Interim, and MERRA-2 L. Sun et al. 10.1175/JAMC-D-21-0078.1
- cloudbandPy 1.0: an automated algorithm for the detection of tropical–extratropical cloud bands R. Pilon & D. Domeisen 10.5194/gmd-17-2247-2024
- Changes in the global mean air temperature over land since 1980 I. Nita et al. 10.1016/j.atmosres.2022.106392
- The stratospheric Brewer–Dobson circulation inferred from age of air in the ERA5 reanalysis F. Ploeger et al. 10.5194/acp-21-8393-2021
Latest update: 19 Apr 2024
Short summary
High clouds are influential in tropical climate. Although reanalysis cloud fields are essentially model products, they are indirectly constrained by observations and offer global coverage with direct links to advanced water and energy cycle metrics, giving them many useful applications. We describe how high cloud fields are generated in reanalyses, assess their realism and reliability in the tropics, and evaluate how differences in these fields affect other aspects of the reanalysis state.
High clouds are influential in tropical climate. Although reanalysis cloud fields are...
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