Category: Fluid Dynamics

Deriving shallow water equations: why is the vertical velocity equal to the material derivative of the surface level?

Getting Started Fluid dynamics plays a critical role in understanding various natural processes on Earth, such as weather patterns, ocean currents, and river flows. A fundamental concept in fluid dynamics is the derivation of the shallow water equations, which provide a simplified mathematical representation of fluid motion in shallow water environments. In this article, we

Exploring the Influence of Friction on Air Velocity: Unraveling the Secrets of Earth’s Fluid Dynamics

Can air be slowed down by friction? Fluid dynamics and the study of the Earth’s atmosphere have long been fascinating subjects for scientists and researchers. One intriguing question that often arises is whether air can be slowed down by friction. In this article, we will explore the concept of air friction and its effects on

Unveiling the Link: Exploring the Definition of Small Layer Thickness in Relation to Bulk Richardson Number and Gradient Richardson Number

Understanding Small Layer Thicknesses in the Context of Bulk Richardson Number Approaching Gradient Richardson Number Fluid dynamics plays a crucial role in understanding various phenomena in Earth science, ranging from atmospheric processes to oceanic movements. An important concept in fluid dynamics is the relationship between small layer thickness and the bulk Richardson number approaching the

Unveiling the Secrets of Mesoscale Cyclones: Calculating Ekman Transport and Vertical Velocity from Wind Stress τ

Mesoscale cyclones are weather systems characterized by their relatively small size compared to synoptic-scale systems, and typically have lifetimes of a few days. These systems can have a significant impact on local weather conditions and can lead to severe weather events such as heavy rainfall, strong winds, and even tornadoes. Understanding the dynamics of mesoscale

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