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Sam Brandt

@sambrandt99 • 3,950 subscribers

Meteorologist | M.S. (2024) and B.S. (2022) in Meteorology and Atmospheric Science @penn_state | @StormChaseTeam President ‘20-21

Shorts

Despite being an essential part of a severe weather forecaster’s toolkit, hodographs have a notorious learning curve. So, I have put together this 3D animation as a visual aid to help those new to hodographs understand what they’re showing.

Despite being an essential part of a severe weather forecaster’s toolkit, hodographs have a notorious learning curve. So, I have put together this 3D animation as a visual aid to help those new to hodographs understand what they’re showing.

85,382 просмотров

A 127 mph (!!!) perturbation to the wind at 1 km was sampled at the Bismarck Radar as the rear inflow jet from a derecho passed overhead

A 127 mph (!!!) perturbation to the wind at 1 km was sampled at the Bismarck Radar as the rear inflow jet from a derecho passed overhead

11,797 просмотров

Videos

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An entire weekend of severe weather condensed to under 30 seconds

An entire weekend of severe weather condensed to under 30 seconds

125,338 просмотров • 1 год назад

Drylines are somewhat unique among meteorological boundaries in that they are driven by differences in boundary layer mixing rather than differences in density. Here’s an animation I put together showing how that works:

Drylines are somewhat unique among meteorological boundaries in that they are driven by differences in boundary layer mixing rather than differences in density. Here’s an animation I put together showing how that works:

21,699 просмотров • 1 месяц назад

A defining characteristic of warm core lows is the presence of an anticyclonic circulation of the thermal wind, something that can be made out in satellite loops of Erin this afternoon.

A defining characteristic of warm core lows is the presence of an anticyclonic circulation of the thermal wind, something that can be made out in satellite loops of Erin this afternoon.

33,850 просмотров • 9 месяцев назад

How to identify streamwise vorticity on a hodograph, in 60 seconds

How to identify streamwise vorticity on a hodograph, in 60 seconds

34,575 просмотров • 1 год назад

Tornado formation, explained visually

Tornado formation, explained visually

22,105 просмотров • 1 год назад

Skew-T diagrams are essential for meteorologists to understand, but without formal training it can be difficult to know where to start. Follow along with me as we build one from scratch and try to make sense of what all those lines mean

Skew-T diagrams are essential for meteorologists to understand, but without formal training it can be difficult to know where to start. Follow along with me as we build one from scratch and try to make sense of what all those lines mean

19,413 просмотров • 1 год назад

Using a physical analog to show why variations in fluid density along a pressure surface create vorticity. Referred to as "baroclinicity", the process played an outsized role in providing spin for a tornadic supercell along an outflow boundary near Lubbock TX earlier today.

Using a physical analog to show why variations in fluid density along a pressure surface create vorticity. Referred to as "baroclinicity", the process played an outsized role in providing spin for a tornadic supercell along an outflow boundary near Lubbock TX earlier today.

14,041 просмотров • 1 год назад

Visualizing the vorticity equation

Visualizing the vorticity equation

11,513 просмотров • 1 год назад

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