A Memory-Efficient Finite Volume Method for Advection-Diffusion-Reaction Systems with Non-Smooth Sources Jonas Sch¨ afer,1 Xuan Huang,2 Stefan Kopecz,1,0 Philipp Birken,1 Matthias K. Gobbert,2 and Andreas Meister1

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SEPTEMBERROMPS AND KUANG 2009

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• Atmospheric thermodynamics
• Oceanography
• Aerodynamics
• Atmospheric dynamics
• Advection
• Surface layer
• Turbulence
• Atmospheric convection
• Convective available potential energy
• Meteorology
• Atmospheric sciences
• Fluid dynamics

15 OCTOBERPETERS ET AL.

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• Atmospheric thermodynamics
• Tropical meteorology
• Vortices
• Climatology
• Intertropical Convergence Zone
• Tropical cyclone
• Rain
• Advection
• South Pacific convergence zone
• Atmospheric sciences
• Meteorology
• Atmospheric dynamics

Generated using V3.0 of the official AMS LATEX template The relative humidity in an isentropic advection-condensation model: Limited poleward influence and properties of subtropical minima Paul A. O’Gorman∗ Massachu

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Seventh Framework Programme Theme 6 Environment Collaborative Project (Large-scale Integrating Project) Project noProject acronym: MEECE Project title: Marine Ecosystem Evolution in a Changing Environment

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• Atmospheric dynamics
• Aquatic ecology
• Biological oceanography
• Planktology
• Geology
• Advection
• Plankton
• Primitive equations
• Turbulent diffusion
• Meteorology
• Calculus
• Earth

PDF Document

Source URL: geofizika-journal.gfz.hr

• Fluid dynamics
• Wind power
• Advection
• Convection
• Oceanography
• Vector calculus
• Bora
• Wind
• Anemometer
• Meteorology
• Atmospheric sciences
• Atmospheric dynamics

Jonathan P. Fram, Geno R. Pawlak, Francis J. Sansone, Brian T. Glazer, Angelos K. HannidesMiniature thermistor chain for determining surficial sediment porewater advection. Limnology and Oceanography: Methods 12:

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Q IWA Publishing 2006 Journal of Hydroinformatics | 08.3 | Derivation of high-order advection– diffusion schemes Pavel Tkalich

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TURBULENT DIFFUSION, ADVECTION, AND WATER STRUCTURE IN THE NORTH INDIAN OCEAN A DISSERTATION SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAII IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF

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Higher order Vertical Advection (M. Baldauf, DWD) Motivation: in a convection-permitting model (like COSMO-DE) the vertical advection plays a much bigger role than in a convection-parameterising model
try to achieve hi

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