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Recent Posts
- The Cuyahoga River burned today for the first time in 51 years. Here’s what we can learn from it.
- Spooky seismic action at a distance: moderate earthquakes in western US cause submarine landslides in the Gulf of Mexico
- Two reflections on the largest earthquake yet recorded, 60 years later.
- Watershed Hydrology – Complete Compendium of my Online Teaching Resources
- How I taught Flooding online in Spring 2020
- How I taught Streamflow online in Spring 2020
- How I taught Streamflow Generation online in Spring 2020
- How I taught Soil Moisture and Infiltration online in spring 2020
Latest Comments
- On How wet is the unsaturated zone?:
- John Selker: For lot’s more videos on soil moisture topics, see Drs Selker and Or’s text-book... Read
- Chris Rowan: Actually, a (fortunately small) tsunami was generated in the aftermath of the quake:... Read
- Anthony: Wow Chris this was the most excellent explanation of recent Kilauea activity i could find – so... Read
- Lyle: Note 50 years is the average lifetime of a commercial building a single family home tends more to the 75... Read
- Eric J. Fielding: Great blog post! Only suggestion is that the Uniform California Earthquake Rupture Forecast... Read
- Tor B: Hmmm, I refreshed the page and the ‘last parent standing’ changed, but then settled back to... Read
- Tor B: Nice graphics, but the last purple ‘atom’ is always fourth from the right on the top row. I... Read
Tag Archives: runoff
How I taught Streamflow Generation online in Spring 2020
This post is part of a series in which I provide the details of each unit I taught post-transitioning to online in Spring 2020 in the Watershed Hydrology class at Kent State University. For more context about the course and … Continue reading
How does water that falls on land get to streams?
It’s a rainy day and you can see that the water level is rising in your local stream. That’s because of the rain falling on the stream channel and its tributaries, right? Wrong. In most watersheds, <1% of the land … Continue reading
