Media Summary: A graphical representation of what we explored in the previous Remember the good ol' quadratic equation? What the acceleration vector looks like in natural coordinates.
Metr2023 Lecture 11 Segment 3 - Detailed Analysis & Overview
A graphical representation of what we explored in the previous Remember the good ol' quadratic equation? What the acceleration vector looks like in natural coordinates. Not all values of V are solutions to the gradient wind balance. Here, we list out what situations are theoretical possible. A first look at the vertical structure of a typical mid-latitude cyclone. A first look at friction and how it affects atmospheric flow.
The observed wind in the atmosphere can be interpreted as having a geostrophic component and a non-geostrophic ... What do all the fancy lines and symbols on a hodograph mean? Link to the splitting storm animation: ... Differential diabetic heating is responsible for sea breezes and land breezes, which can also be referred to as a "sea breeze ... What is the Polar Cell and why does it exist? A look at surface warm fronts. Though slow-moving, warm fronts play an important role in destabilizing the atmosphere. A look at a particularly impactful oscillation pattern in the atmosphere. Pardon the in-e-fish-ent joke...
