Development of the Finite-Volume Dynamical Core on the Cubed-Sphere

The finite-volume dynamical core has been developed for quasi-uniform cubed-sphere grids within a flexible modeling framework for direct implementation as a modular component within the global modeling efforts at NASA, GFDL-NOAA, NCAR, DOE and other interested institutions. The shallow water equatio...

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Other Authors: Putman, William M. (authoraut)
Format: Others
Language:English
English
Published: Florida State University
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Online Access:http://purl.flvc.org/fsu/fd/FSU_migr_etd-0511
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spelling ndltd-fsu.edu-oai-fsu.digital.flvc.org-fsu_1686672019-07-01T03:58:05Z Development of the Finite-Volume Dynamical Core on the Cubed-Sphere Putman, William M. (authoraut) O'Brien, James J. (professor directing dissertation) Lin, Shian-Jiann (outside committee member) Rood, Richard (outside committee member) Krishnamurti, T. N. (committee member) Navon, I. Michael (committee member) Zou, Xiaolei (committee member) Department of Earth, Ocean and Atmospheric Sciences (degree granting department) Florida State University (degree granting institution) Text text Florida State University English eng 1 online resource computer application/pdf The finite-volume dynamical core has been developed for quasi-uniform cubed-sphere grids within a flexible modeling framework for direct implementation as a modular component within the global modeling efforts at NASA, GFDL-NOAA, NCAR, DOE and other interested institutions. The shallow water equations serve as a dynamical framework for testing the implementation and the variety of quasi-orthogonal cubed-sphere grids ranging from conformal mappings to those numerically generated via elliptic solvers. The cubed-sphere finite-volume dynamical core has been parallelized with a 2-dimensional X-Y domain decomposition to achieve optimal scalability to 100,000s of processors on today's high-end computing platforms at horizontal resolutions of 0.25-degrees and finer. The cubed-sphere fvcore is designed to serve as a framework for hydrostatic and non-hydrostatic global simulations at climate (4- to 1-deg) and weather (25- to 5-km) resolutions, pushing the scale of global atmospheric modeling from the climate/synoptic scale to the meso- and cloud-resolving scale. A Dissertation submitted to the Department of Meteorology in partial fulfillment of the requirements for the degree of Doctor of Philosophy. Degree Awarded: Summer Semester, 2007. Date of Defense: May 17, 2007. Cubed-Sphere, Shallow Water, Advection, Dynamical Core, Finite-Volume Includes bibliographical references. James J. O'Brien, Professor Directing Dissertation; Shian-Jiann Lin, Outside Committee Member; Richard Rood, Outside Committee Member; T. N. Krishnamurti, Committee Member; I. Michael Navon, Committee Member; Xiaolei Zou, Committee Member. Meteorology FSU_migr_etd-0511 http://purl.flvc.org/fsu/fd/FSU_migr_etd-0511 http://diginole.lib.fsu.edu/islandora/object/fsu%3A168667/datastream/TN/view/Development%20of%20the%20Finite-Volume%20Dynamical%20Core%20on%20the%20Cubed-Sphere.jpg
collection NDLTD
language English
English
format Others
sources NDLTD
topic Meteorology
spellingShingle Meteorology
Development of the Finite-Volume Dynamical Core on the Cubed-Sphere
description The finite-volume dynamical core has been developed for quasi-uniform cubed-sphere grids within a flexible modeling framework for direct implementation as a modular component within the global modeling efforts at NASA, GFDL-NOAA, NCAR, DOE and other interested institutions. The shallow water equations serve as a dynamical framework for testing the implementation and the variety of quasi-orthogonal cubed-sphere grids ranging from conformal mappings to those numerically generated via elliptic solvers. The cubed-sphere finite-volume dynamical core has been parallelized with a 2-dimensional X-Y domain decomposition to achieve optimal scalability to 100,000s of processors on today's high-end computing platforms at horizontal resolutions of 0.25-degrees and finer. The cubed-sphere fvcore is designed to serve as a framework for hydrostatic and non-hydrostatic global simulations at climate (4- to 1-deg) and weather (25- to 5-km) resolutions, pushing the scale of global atmospheric modeling from the climate/synoptic scale to the meso- and cloud-resolving scale. === A Dissertation submitted to the Department of Meteorology in partial fulfillment of the requirements for the degree of Doctor of Philosophy. === Degree Awarded: Summer Semester, 2007. === Date of Defense: May 17, 2007. === Cubed-Sphere, Shallow Water, Advection, Dynamical Core, Finite-Volume === Includes bibliographical references. === James J. O'Brien, Professor Directing Dissertation; Shian-Jiann Lin, Outside Committee Member; Richard Rood, Outside Committee Member; T. N. Krishnamurti, Committee Member; I. Michael Navon, Committee Member; Xiaolei Zou, Committee Member.
author2 Putman, William M. (authoraut)
author_facet Putman, William M. (authoraut)
title Development of the Finite-Volume Dynamical Core on the Cubed-Sphere
title_short Development of the Finite-Volume Dynamical Core on the Cubed-Sphere
title_full Development of the Finite-Volume Dynamical Core on the Cubed-Sphere
title_fullStr Development of the Finite-Volume Dynamical Core on the Cubed-Sphere
title_full_unstemmed Development of the Finite-Volume Dynamical Core on the Cubed-Sphere
title_sort development of the finite-volume dynamical core on the cubed-sphere
publisher Florida State University
url http://purl.flvc.org/fsu/fd/FSU_migr_etd-0511
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