Articles | Volume 14, issue 8
https://doi.org/10.5194/amt-14-5555-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-14-5555-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
13 Aug 2021
Research article |
| 13 Aug 2021
| 13 Aug 2021
Boundary layer water vapour statistics from high-spatial-resolution spaceborne imaging spectroscopy
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
Department of Atmospheric Science, Colorado State University, Fort Collins, CO 90095, USA
David R. Thompson
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
Marcin J. Kurowski
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
Matthew D. Lebsock
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
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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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Sunlight can pass diagonally through the atmosphere, cutting through the 3-D water vapour field in a way that
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away fromthe Sun, so calculating
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Luis Millán, Richard Roy, and Matthew Lebsock
Atmos. Meas. Tech., 13, 5193–5205, https://doi.org/10.5194/amt-13-5193-2020, https://doi.org/10.5194/amt-13-5193-2020, 2020
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Mark Richardson, Matthew D. Lebsock, James McDuffie, and Graeme L. Stephens
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Short summary
Modern and upcoming hyperspectral imagers will take images with spatial resolutions as fine as 20 m. They can retrieve column water vapour, and we show evidence that from these column measurements you can get statistics of planetary boundary layer (PBL) water vapour. This is important information for climate models that need to account for sub-grid mixing of water vapour near the surface in their PBL schemes.
Modern and upcoming hyperspectral imagers will take images with spatial resolutions as fine as...
