Tom the Weather Geek

Tom the Weather Geek

My name is Tom Nery. Ever since I was a kid, my head's been stuck in the clouds. Not literally, of course, though you'd be surprised by the number of times I've chased thunder with a grin from ear to ear. Meteorology wasn't just a career choice, it was a calling. Years of textbooks and weather models later, I found myself a full-fledged weather geek, and I wouldn't have it any other way. But knowledge, they say, needs to be shared, so I poured my passion onto the pages of weathergeeks.org. So, whether you're a seasoned storm chaser or just curious about the raindrop dancing on your window, pull up a chair, grab a cup of something warm (or cold, depending on the forecast), and join me on this whirlwind adventure through the ever-changing skies. You'll leave knowing a little more, laughing a little louder, and hopefully, appreciating the wild beauty of this crazy, weather-filled world we call home. Cheers! Tom, The Weather Geek (and resident cloud enthusiast)
How to Build and Maintain a Snow Stake & Snow Board for Accurate Snow Measurements

How to Build and Maintain a Snow Stake & Snow Board for Accurate Snow Measurements

Accurate snowfall measurement requires more than stepping outside with a ruler. Snow depth varies dramatically due to wind, drifting, melting, and compaction. That’s why meteorologists and trained observers rely on snow stakes and snow boards — standardized tools designed to capture reliable, repeatable snowfall data. In this comprehensive guide, we explain how to properly build, install, level, mark, and maintain snow stakes and snow boards, along with best practices for recording snowfall and snow depth to professional standards.

What is SWE in snow science

Snow Water Equivalent (SWE): Why “Inches of Snow” Isn’t Enough to Know Water Content

Most people equate heavy snowfall with water abundance. In reality, inches of snow tells only part of the story. The true measure of water stored in seasonal snowpacks is Snow Water Equivalent (SWE) — the depth of water contained in snow if it were melted. SWE varies dramatically by snow density, temperature, crystal structure, and regional climate. Understanding SWE is essential for flood risk forecasting, water resource management, and ecosystem resilience. In this comprehensive exploration, we break down the science of SWE, how it’s measured, why “snow depth” alone can be misleading, and how SWE influences water supply and hazard planning from the Rockies to the Sierra Nevada to the Northeast.