Quantifying Tropical Cyclone Vertical Mass Flux in Convection-Permitting Model Simulations

Vertical mass flux (MF) describes the rate at which air and water vapor move upward or downward in an atmospheric column. MF is related to cloud and precipitation formation. This work examines the relationship between MF and characteristics of tropica

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Published
2025-07-18
DOI
https://doi.org/10.22541/essoar.175285262.21830159/v1
Primary Topic
Tropical and Extratropical Cyclones Research
Type
article
Field-Weighted Citation Impact
0.00

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article

Quantifying Tropical Cyclone Vertical Mass Flux in Convection-Permitting Model Simulations

Kristen Lani Rasmussen, Alyssa M. Stansfield
Tropical and Extratropical Cyclones Research
article

Quantifying Tropical Cyclone Vertical Mass Flux in Convection-Permitting Model Simulations

Kristen Lani Rasmussen, Alyssa M. Stansfield
article en

Abstract

Vertical mass flux (MF) describes the rate at which air and water vapor move upward or downward in an atmospheric column. MF is related to cloud and precipitation formation. This work examines the relationship between MF and characteristics of tropica

University of Utah (US), Colorado State University (US)
National Science Foundation, National Aeronautics and Space Administration, Langley Research Center, Science Mission Directorate
Climate action
Openalex Percentile: Top 76%
Tropical and Extratropical Cyclones Research
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