Articles | Volume 18, issue 15
https://doi.org/10.5194/acp-18-11205-2018
© Author(s) 2018. 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-18-11205-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
13 Aug 2018
Research article |
| 13 Aug 2018
| 13 Aug 2018
An update on global atmospheric ice estimates from satellite observations and reanalyses
David Ian Duncan
CORRESPONDING AUTHOR
Department of Earth, Space, and Environment, Chalmers University of Technology, 41296, Gothenburg, Sweden
Patrick Eriksson
Department of Earth, Space, and Environment, Chalmers University of Technology, 41296, Gothenburg, Sweden
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- Sensing Horizontally Oriented Frozen Particles With Polarimetric Radio Occultations Aboard PAZ: Validation Using GMI Coincident Observations and Cloudsat a Priori Information R. Padulles et al. 10.1109/TGRS.2021.3065119
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- Synergistic radar and sub-millimeter radiometer retrievals of ice hydrometeors in mid-latitude frontal cloud systems S. Pfreundschuh et al. 10.5194/amt-15-677-2022
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- Introducing hydrometeor orientation into all-sky microwave and submillimeter assimilation V. Barlakas et al. 10.5194/amt-14-3427-2021
- Retrieval of ice water path from the Microwave Humidity Sounder (MWHS) aboard FengYun-3B (FY-3B) satellite polarimetric measurements based on a deep neural network W. Wang et al. 10.5194/amt-15-6489-2022
- Improved Representation of Clouds in the Atmospheric Component LMDZ6A of the IPSL‐CM6A Earth System Model J. Madeleine et al. 10.1029/2020MS002046
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- An Assessment of the Impacts of Cloud Vertical Heterogeneity on Global Ice Cloud Data Records From Passive Satellite Retrievals C. Wang et al. 10.1029/2018JD029681
Latest update: 21 Feb 2025
Short summary
Ice cloud mass is assessed on a global scale using the latest satellite and reanalysis datasets. While ice cloud variability driven by large-scale circulations is an area of relative consensus, models and observations disagree strongly on the overall magnitude and finer-scale variability of atmospheric ice mass. The results reflect limitations of the current Earth observing system and indicate ice microphysical assumptions as the likely culprit of disagreement.
Ice cloud mass is assessed on a global scale using the latest satellite and reanalysis datasets....
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