Media Summary: The process of combining the hydrostatic balance with the ideal gas law to obtain what is referred to as the Hypsometric Equation. An exercise that will check your understanding of the gradient operator discussed in An overview of what atmospheric factors favor strong straight-line wind gusts. Please keep in mind that there are multiple different ...
Metr2023 Lecture 3 Segment 1 - Detailed Analysis & Overview
The process of combining the hydrostatic balance with the ideal gas law to obtain what is referred to as the Hypsometric Equation. An exercise that will check your understanding of the gradient operator discussed in An overview of what atmospheric factors favor strong straight-line wind gusts. Please keep in mind that there are multiple different ... A graphical representation of what we explored in the previous Now that we have this fancy equation, what the heck does it mean for the atmosphere? The answer is in this video... A look at a particularly impactful oscillation pattern in the atmosphere. Pardon the in-e-fish-ent joke...
An exercise to check your understanding of the Hypsometric Equation (and a discussion of the results behind this specific ... As important as fronts are in the atmosphere, there is no universally agreed upon definition of a front. Though, most people ... In the United States, a "severe thunderstorm" is a thunderstorm that produces at least one of the following: tornado, 50+ knot (58+ ... A look at surface warm fronts. Though slow-moving, warm fronts play an important role in destabilizing the atmosphere. Cyclones often form on the east side of the Rocky Mountains. Potential vorticity offers an explanation as to why this occurs. Trough and ridges, shortwaves and longwaves.
Remember the good ol' quadratic equation?
