Spatial and Temporal Variability of Vertical Velocity under Shallow Cumulus Article Swipe
Gavin C. Cornwell
,
Johannes Mülmenstädt
,
Larry K. Berg
,
Kôichi Sakaguchi
,
Brian Gaudet
,
D. Chand
,
Colleen Kaul
,
Heng Xiao
,
Rob Newsom
,
William I. Gustafson
,
Vincent E. Larson
,
Jerome D. Fast
·
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.1175/mwr-d-24-0055.1
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.1175/mwr-d-24-0055.1
Vertical velocity distribution below cloud is one of the key determinants of cloud life cycle, but observations of this variable are extremely sparse in space. Doppler lidar retrievals and large-eddy simulations at the U.S. Department of Energy’s Atmospheric Radiation Measurement User Facility Southern Great Plains site are used to determine whether vertical velocity statistics from temporally dense profiles at a single location can be substituted for spatial vertical velocity statistics. We show that even a small number (five) of widely distributed [ O (1°) latitude/longitude spacing] lidars is sufficient sampling to reconstruct domainwide spatial vertical velocity variance, but not higher moments of the vertical velocity distribution. Spatial and temporal vertical velocity variances in the Doppler lidar observations are nearly interchangeable as long as the spatial variance is temporally averaged and the temporal variance is averaged across lidars. This is true even though the dominant spatial scales of vertical velocity variability are , more than an order of magnitude smaller than the spacing between the lidars. In the limit where the temporal variance does not vary across a spatial domain (e.g., if the meteorological and surface forcing of the atmospheric turbulence is homogeneous across the domain) and the domain-mean vertical velocity is zero, the commonly available retrieval of temporal vertical velocity variance at one site is equivalent to the spatial variance over the domain. We use an updraft parcel model to show that substituting temporal for spatial vertical velocity statistics will have a relatively minor effect on cloud droplet number concentrations.
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Metadata
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1175/mwr-d-24-0055.1
- https://journals.ametsoc.org/downloadpdf/view/journals/mwre/aop/MWR-D-24-0055.1/MWR-D-24-0055.1.pdf
- OA Status
- bronze
- References
- 62
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4409573356
All OpenAlex metadata
Raw OpenAlex JSON
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- DOI
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https://doi.org/10.1175/mwr-d-24-0055.1Digital Object Identifier
- Title
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Spatial and Temporal Variability of Vertical Velocity under Shallow CumulusWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2025Year of publication
- Publication date
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2025-04-18Full publication date if available
- Authors
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Gavin C. Cornwell, Johannes Mülmenstädt, Larry K. Berg, Kôichi Sakaguchi, Brian Gaudet, D. Chand, Colleen Kaul, Heng Xiao, Rob Newsom, William I. Gustafson, Vincent E. Larson, Jerome D. FastList of authors in order
- Landing page
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https://doi.org/10.1175/mwr-d-24-0055.1Publisher landing page
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https://journals.ametsoc.org/downloadpdf/view/journals/mwre/aop/MWR-D-24-0055.1/MWR-D-24-0055.1.pdfDirect link to full text PDF
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YesWhether a free full text is available
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bronzeOpen access status per OpenAlex
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https://journals.ametsoc.org/downloadpdf/view/journals/mwre/aop/MWR-D-24-0055.1/MWR-D-24-0055.1.pdfDirect OA link when available
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Geology, Climatology, Environmental science, Meteorology, GeographyTop concepts (fields/topics) attached by OpenAlex
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10Other works algorithmically related by OpenAlex
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