Related Experiment Video
Updated: Jul 18, 2025

10:23
Author Spotlight: Computing the Effects of a Local Radiofrequency Hyperthermia Intervention on Tumor Biomechanics
Published on: December 1, 2023
465
Theoretical and Computational Analysis of the Thermal Quasi-Geostrophic Model
Summary
This study analyzes the thermal quasi-geostrophic (TQG) model in geophysical fluid dynamics. Researchers proved the existence of unique strong solutions for the TQG model and verified convergence rates numerically.
Area of Science:
- Geophysical Fluid Dynamics (GFD)
- Theoretical and Numerical Analysis
- Submesoscale Dynamics
Background:
- The thermal quasi-geostrophic (TQG) model is crucial for understanding submesoscale geophysical fluid dynamics.
- It assumes thermal geostrophic balance where Rossby, Froude, and stratification parameters are of the same asymptotic order.
Purpose of the Study:
- To construct local-in-time unique strong solutions for the TQG model.
- To analyze the convergence of a regularized TQG model to the original TQG model.
- To establish blow-up criteria for the regularized TQG model.
Main Methods:
- Theoretical analysis to prove the existence of unique strong solutions.
- Demonstration of convergence of regularized -TQG solutions to TQG solutions as the smoothing parameter approaches zero.
- Numerical simulations to verify convergence rates in relevant GFD regimes.
Main Results:
- Local-in-time unique strong solutions for the TQG model were successfully constructed.
- Convergence of -TQG solutions to TQG solutions was shown as approaches zero.
- Blow-up criteria for the -TQG model were established.
Conclusions:
- The theoretical and numerical analyses provide a robust foundation for studying the TQG model.
- The findings contribute to a deeper understanding of submesoscale processes in geophysical fluid dynamics.
- The established convergence and blow-up criteria are valuable for future research and simulations.
Related Concept Videos
Thermal Sigmatropic Reactions: Overview
2.1K
Sigmatropic rearrangements are a class of pericyclic reactions in which a σ bond migrates from one part of a π system to another. These are intramolecular rearrangements where the total number of σ and π bonds remain unchanged.
Sigmatropic shifts are classified based on an order term [i, j ], where i and j indicate the number of atoms across which each end of the σ bond migrates. Below are examples of a [3,3] sigmatropic shift in...
Sigmatropic shifts are classified based on an order term [i, j ], where i and j indicate the number of atoms across which each end of the σ bond migrates. Below are examples of a [3,3] sigmatropic shift in...
2.1K
Mechanisms of Heat Transfer II
3.3K
In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
3.3K
Temperature and Thermal Equilibrium
6.8K
Heat and temperature are essential concepts for everyone every day. The study of heat and temperature is part of an area of physics known as thermodynamics. It is not always easy to distinguish heat and temperature.
The concept of temperature has evolved from the common concepts of hot and cold. The scientific definition of temperature explains more than just our sense of hot and cold. Temperature is operationally defined as the quantity measured with a thermometer. Furthermore, temperature is...
The concept of temperature has evolved from the common concepts of hot and cold. The scientific definition of temperature explains more than just our sense of hot and cold. Temperature is operationally defined as the quantity measured with a thermometer. Furthermore, temperature is...
6.8K
Mechanisms of Heat Transfer I
4.3K
Just as interesting as the effects of heat transfer on a system are the methods by which the heat transfer occur. Whenever there is a temperature difference, heat transfer occurs. It may occur rapidly, such as through a cooking pan, or slowly, such as through the walls of a picnic ice box. So many processes involve heat transfer that it is hard to imagine a situation where no heat transfer occurs. Yet, every heat transfer takes place by only three methods: conduction, convection, and radiation.
4.3K
Mechanisms of Heat Transfer
360
Heat transfer between the human body and its environment occurs through four main mechanisms: conduction, convection, radiation, and evaporation.
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant...
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant...
360
Reynolds Transport Theorem
1.2K
The Reynolds transport theorem provides a framework to relate the time rate of change of an extensive property within a system to that in a control volume, which is crucial for analyzing fluid dynamics. Extensive properties, such as mass, velocity, acceleration, temperature, and momentum, can be expressed in terms of the mass of a fluid portion. These properties are called extensive because they depend on the system's size, while intensive properties are their corresponding values per unit...
1.2K

