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Dataset associated with "Cold pool responses to changes in soil moisture"

dc.contributor.authorDrager, Aryeh Jacob
dc.contributor.authorGrant, Leah D
dc.contributor.authorvan den Heever, Susan C
dc.date.accessioned2019-10-11T22:05:58Z
dc.date.available2019-10-11T22:05:58Z
dc.date.issued2019
dc.descriptionThe dataset includes the following: 1) Release 6.2.08 of the Regional Atmospheric Modeling System (RAMS), which was used to conduct the simulations analyzed in the associated manuscript; 2) Modified RAMS source code and scripts necessary to reproduce the simulations; 3) MATLAB analysis scripts and functions for analyzing the data; and 4) A README file with additional details about the contents of the dataset and instructions for running the RAMS model and analysis scripts.en_US
dc.descriptionDepartment of Atmospheric Science
dc.description.abstractThis study examines the role of soil moisture in modulating convective cold pool properties in an idealized modeling framework that uses a cloud-resolving model coupled to an interactive land surface model. Four high-resolution simulations of tropical continental convection are conducted in which the initial soil moisture is varied. The hundreds of cold pools forming within each simulation are identified and composited across space and time using an objective cold pool identification algorithm. Based on the results, a theory for the impacts of soil moisture on cold pools is developed. Lower soil moisture results in greater daytime heating of the surface, which produces a deeper, drier subcloud layer. As a result, latent cooling by the evaporation of precipitation is enhanced, and cold pools are stronger and deeper. Increased propagation speed, combined with wider rain shafts, results in wider cold pools. Finally, the rings of enhanced water vapor that surround each cold pool when soil is wet disappear when the soil moisture is reduced, due to the suppression of surface latent heat fluxes. Instead "puddles" of enhanced water vapor permeate the cold pools. The results are nonlinear in that the properties of the cold pools in the driest-soil simulation depart substantially from the cold pool properties in the three simulations initialized with wetter soil. The dividing line between the resulting wet-soil and dry-soil regimes appears to be the permanent wilting point, below which transpiration is subdued. These results emphasize the role of land surface-boundary layer-cloud interactions in modulating cold pool properties.en_US
dc.description.sponsorshipNational Science Foundation (United States) Graduate Research Fellowship Program under Grant No. DGE-1321845 Amend 5.en_US
dc.description.sponsorshipOffice of Naval Research (Department of Defense, United States) under Grant No. N00014-16-1-3093.en_US
dc.format.mediumZIP
dc.format.mediumPDF
dc.format.mediumDOCX
dc.format.mediumMATLAB
dc.format.mediumHDF5
dc.format.mediumTAR
dc.format.mediumGZIP
dc.format.mediumFortran
dc.format.mediumTXT
dc.format.mediumHTML
dc.format.mediumSH
dc.format.mediumSource Code
dc.format.mediumASCII Grid
dc.identifier.urihttps://hdl.handle.net/10217/198263
dc.identifier.urihttp://dx.doi.org/10.25675/10217/198263
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Librariesen_US
dc.relation.ispartofResearch Data
dc.relation.isreferencedbyDrager, A. J., Grant, L. D., & van den Heever, S. C. (2020). Cold Pool Responses to Changes in Soil Moisture. Journal of Advances in Modeling Earth Systems, https://doi.org/10.1029/2019MS001922en_US
dc.subjectcold pools
dc.subjectsoil moisture
dc.subjectatmospheric convection
dc.subjecttropical convection
dc.subjectconvective processes
dc.subjectcloud processes
dc.subjectdensity currents
dc.subjectgravity currents
dc.subjectland-atmosphere interactions
dc.subjectboundary-layer processes
dc.subjectnumerical modeling
dc.subjectRAMS model
dc.subjectcloud-resolving model
dc.subjecttracking algorithm
dc.titleDataset associated with "Cold pool responses to changes in soil moisture"en_US
dc.typeDataseten_US

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