Articles | Volume 16, issue 9
https://doi.org/10.5194/acp-16-5891-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-5891-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
13 May 2016
Research article |
| 13 May 2016
Marine boundary layer structure as observed by A-train satellites
University of Wyoming, Dept. Atmospheric Science, Laramie, WY, USA
University of Wyoming, Dept. Atmospheric Science, Laramie, WY, USA
Damao Zhang
University of Wyoming, Dept. Atmospheric Science, Laramie, WY, USA
Bing Chen
University of Wyoming, Dept. Atmospheric Science, Laramie, WY, USA
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- Estimating the Decoupling Degree of Subtropical Marine Stratocumulus Decks From Satellite Y. Zheng et al. 10.1029/2018GL078382
- The Subtropical Stratocumulus-Topped Planetary Boundary Layer: A Climatology and the Lagrangian Evolution R. Eastman et al. 10.1175/JAS-D-16-0336.1
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Latest update: 13 Nov 2024
Short summary
With a new 4-year satellite-based data set, the cloud-free marine boundary layer (MBL) structure characteristics over the eastern Pacific region were presented and analyzed together with the stratiform cloud top as the cloudy MBL top. Results showed that the behavior of MBL decouple structure and drizzling and non-drizzling stratiform cloud tops was mainly controlled by the inversion near the MBL top. Results in this paper will be valuable to evaluate and improve model simulation.
With a new 4-year satellite-based data set, the cloud-free marine boundary layer (MBL) structure...
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