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Impact of vegetation on the atmospheric boundary layer and convective storms

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dc.contributor.authorLee, Tsengdar J., author
dc.date.accessioned2022-04-27T15:20:22Z
dc.date.available2022-04-27T15:20:22Z
dc.date.issued1992
dc.descriptionFall 1992.
dc.descriptionAlso issued as author's dissertation (Ph.D.) -- Colorado State University, 1992.
dc.description.abstractThe impact of vegetation on atmospheric boundary layer and convective storms is examined through the construction and testing of a soil-vegetation-atmosphere transfer (SVAT) model. The Land Ecosystem-Atmosphere Feedback (LEAF) model is developed using an elevated canopy structure, an above-canopy aerodynamic resistance, two in-canopy aerodynamic resistances, and one stomatal conductance functions. The air temperature and humidity are assumed to be constant in the canopy whereas the wind and radiation follow a specified vertical profile. A simple dump-bucket method is used to parameterize the interception of precipitation and a multi-layer soil model is utilized to handle the vertical transfer of so water. Evaporation from soil and wet leaves and transpiration from dry leaves are evaluated separately. The soil water uptake is based on soil water potential rather than on the length of roots. Separate energy budgets for vegetation and for the soil are used in order to remove unnecessary assumptions on energy partition between the vegetation and the substrate. Primary parameters are LAI, maximum stomata! conductance, and albedo. Secondary parameters include displacement height and environmental controls on stomata! resistance function. Due to the complexity of the LEAF model, statistical methods are used to improve LEAF model performance. The Multi-response Randomized Block Permutation (MRBP) procedure is used to guide the choice of model parameter values. The Fourier Amplitude Sensitivity Test (FAST) is applied to better understand the model behavior in response to the changes in model parameters. Finally, LEAF is used to study the growth of boundary layer and the local thermal circulations generated by surface inhomogeneities. Results show the atmospheric boundary layer is substantially cooler and more moist over unstressed vegetation than over bare dry soil. Thermally forced circulation can result from the juxtaposition of two vegetation types due to different biophysical characteristics. Results from three-dimensional simulations show that the surface spatial heterogeneities made by vegetation play an important role in generating local convective storms.
dc.description.sponsorshipSponsored by NSF ATM-8915265, and USGS 14-08-0001-A0929.
dc.format.mediumreports
dc.identifier.urihttps://hdl.handle.net/10217/234871
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991023630769703361
dc.relationQC852 .C6 no. 509
dc.relation.ispartofAtmospheric Science Papers (Blue Books)
dc.relation.ispartofAtmospheric science paper, no. 509
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectBoundary layer (Meteorology)
dc.subjectConvection (Meteorology)
dc.subjectVegetation and climate
dc.titleImpact of vegetation on the atmospheric boundary layer and convective storms
dc.typeText
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