Marine Boundary Layer Heights in the Tropical and Subtropical Oceans Derived from COSMIC-2 Radio Occultation Data
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
https://link.springer.com/content/pdf/10.1007/s00376-022-2052-z.pdf
Reference38 articles.
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2. Anthes, R. A., and Coauthors, 2008: The COSMIC/FORMOSAT-3 mission: Early results. Bull. Amer. Meteor. Soc., 89, 313–334, https://doi.org/10.1175/BAMS-89-3-313.
3. Ao, C. O., D. E. Waliser, S. K. Chan, J.-L. Li, B. J. Tian, F. Q. Xie, and A. J. Mannucci, 2012: Planetary boundary layer heights from GPS radio occultation refractivity and humidity profiles. J. Geophys. Res., 117, D16117, https://doi.org/10.1029/2012JD017598.
4. Baars, H., A. Ansmann, R. Engelmann, and D. Althausen, 2008: Continuous monitoring of the boundary-layer top with lidar. Atmospheric Chemistry and Physics, 8, 7281–7296, https://doi.org/10.5194/acp-8-7281-2008.
5. Banta, R. M., and A. B. White, 2003: Mixing-height differences between land use types: Dependence on wind speed. J. Geophys. Res., 108, 4321, https://doi.org/10.1029/2002JD002748.
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1. A Comparison of Atmospheric Boundary Layer Height Determination Methods Using GNSS Radio Occultation Data;Atmosphere;2023-11-04
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