The Lorenz Energy Cycle of the Global Atmosphere during the past 35 Years (1979-2013)

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dc.contributor.advisorLi, Liming
dc.contributor.committeeMemberGunaratne, Gemunu H.
dc.contributor.committeeMemberStokes, Donna W.
dc.contributor.committeeMemberSu, Wu-Pei
dc.contributor.committeeMemberJiang, Xun
dc.creatorPan, Yefeng 1989-
dc.date.accessioned2018-02-15T19:41:18Z
dc.date.available2018-02-15T19:41:18Z
dc.date.createdDecember 2015
dc.date.issued2015-12
dc.date.submittedDecember 2015
dc.date.updated2018-02-15T19:41:18Z
dc.description.abstractThe Lorenz energy cycle (Lorenz 1955) describes how the solar heating generates potential energy that can be converted into kinetic energy to drive Earth’s atmospheric system. Therefore, the studies of the Lorenz energy cycle can help us understand the atmospheric system from a unique energy perspective. Based on two best global meteorological datasets, we systematically study the Lorenz energy cycle of the global atmosphere during the modern satellite era (1979-2013). Our analyses provide the most reliable characteristics of the Lorenz energy cycle of the global atmosphere. The mean state of the 35-year Lorenz energy cycle generates the best global picture of the Lorenz energy cycle. Our analyses also reveal important temporal characteristics of the Lorenz energy cycle of the global atmosphere. Significant positive trends are shown in both the eddy available potential energy (P_E) and the eddy kinetic energy (K_E) especially in the Southern Hemisphere, which are mainly due to the increasing storm activities over the Southern Ocean storm track areas. At the same time, a negative trend is seen in the mean available potential energy (P_M) especially around the North Pole near the surface, which is probably related to the inhomogeneous global warming. As a result, the total mechanical energy does not show any significant trend during the past 35 years, which suggests that the climate system remains close to a dynamical balance. Our analyses also suggest positive trends in all conversion rates and in the dissipation of kinetic energy, which implies that the efficiency of the global atmosphere as a heat engine increased during the modern satellite era. The statistical characteristics of the Lorenz energy cycle revealed in our analyses will provide a powerful tool to validate and develop the atmospheric and climate models. The temporal characteristic of the Lorenz energy cycle will also benefit the monitoring and predicting of climate change, for the atmospheric energetics are an important component of climate system of Earth.
dc.description.departmentPhysics, Department of
dc.format.digitalOriginborn digital
dc.format.mimetypeapplication/pdf
dc.identifier.urihttp://hdl.handle.net/10657/2127
dc.language.isoeng
dc.rightsThe author of this work is the copyright owner. UH Libraries and the Texas Digital Library have their permission to store and provide access to this work. Further transmission, reproduction, or presentation of this work is prohibited except with permission of the author(s).
dc.subjectLorenz energy cycle
dc.subjectAtmospheric energy
dc.titleThe Lorenz Energy Cycle of the Global Atmosphere during the past 35 Years (1979-2013)
dc.type.dcmiText
dc.type.genreThesis
thesis.degree.collegeCollege of Natural Sciences and Mathematics
thesis.degree.departmentPhysics, Department of
thesis.degree.disciplinePhysics
thesis.degree.grantorUniversity of Houston
thesis.degree.levelDoctoral
thesis.degree.nameDoctor of Philosophy

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