Articles | Volume 23, issue 13
https://doi.org/10.5194/acp-23-7699-2023
https://doi.org/10.5194/acp-23-7699-2023
Research article
 | 
13 Jul 2023
Research article |  | 13 Jul 2023

Trajectory enhancement of low-earth orbiter thermodynamic retrievals to predict convection: a simulation experiment

Mark T. Richardson, Brian H. Kahn, and Peter Kalmus

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Preprint under review for ESSD
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New sampling strategy mitigates a solar-geometry-induced bias in sub-kilometre vapour scaling statistics derived from imaging spectroscopy
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Boundary layer water vapour statistics from high-spatial-resolution spaceborne imaging spectroscopy
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Spectroscopic imaging of sub-kilometer spatial structure in lower-tropospheric water vapor
David R. Thompson, Brian H. Kahn, Philip G. Brodrick, Matthew D. Lebsock, Mark Richardson, and Robert O. Green
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Cited articles

Agee, E. and Childs, S.: Adjustments in Tornado Counts, F-Scale Intensity, and Path Width for Assessing Significant Tornado Destruction, J. Appl. Meteorol. Clim., 53, 1494–1505, https://doi.org/10.1175/JAMC-D-13-0235.1, 2014.. 
AIRS project: Aqua/AIRS L2 Support Retrieval (AIRS-only) V7.0, Greenbelt, MD, USA, Goddard Earth Sciences Data and Information Services Center (GES DISC) [data set], https://doi.org/10.5067/APJ6EEN0PD0Z, 2019. 
Ali, H. and Mishra, V.: Contributions of Dynamic and Thermodynamic Scaling in Subdaily Precipitation Extremes in India, Geophys. Res. Lett., 45, 2352–2361, https://doi.org/10.1002/2018GL077065, 2018. 
Barthel, F. and Neumayer, E.: A trend analysis of normalized insured damage from natural disasters, Climatic Change, 113, 215–237, https://doi.org/10.1007/s10584-011-0331-2, 2012. 
Bechtold, P., Semane, N., Lopez, P., Chaboureau, J.-P., Beljaars, A., and Bormann, N.: Representing Equilibrium and Nonequilibrium Convection in Large-Scale Models, J. Atmos. Sci., 71, 734–753, https://doi.org/10.1175/JAS-D-13-0163.1, 2014. 
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Short summary
Convection over land often triggers hours after a satellite last passed overhead and measured the state of the atmosphere, and during those hours the atmosphere can change greatly. Here we show that it is possible to reconstruct most of those changes by using weather forecast winds to predict where warm and moist air parcels will travel. The results can be used to better predict where precipitation is likely to happen in the hours after satellite measurements.
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