On my way to upper Las Virgenes Canyon from the Victory Trailhead of Ahmanson Ranch, I had to stop running and marvel at the intricacy and beauty of this cumulus cloud.
The cloud developed as another weak trough was passing through Southern California. For a few weeks the long-range outlooks have been advertising a change to a wetter weather pattern, but the expected transition keeps being delayed.
The clouds were associated with a front that stalled to the north of Los Angeles, resulting in some surprising and substantial rainfall totals in Santa Barbara and San Luis Obispo Counties. No measurable rain was reported in Los Angeles County by the NWS.
From an early morning run at Ahmanson Ranch (Upper Las Virgenes Canyon Open Space Preserve) on September 20th.
The cumulus cloud towered overhead, its size accentuated by a lone oak on the skyline. An extraordinary series of December rainstorms were finally over. The year 2021 would end with Downtown Los Angeles (USC) having recorded the third highest amount of December rainfall on record.
I was running from the Victory Trailhead of Upper Las Virgenes Canyon Open Space Preserve (aka Ahmanson) to Las Virgenes Canyon. With about 5 inches of rain in the area over the past two days, I was curious to see how upper Las Virgenes Creek was flowing.
When I parked at the Wendy Drive trailhead, there was just enough light to see a wide band of high clouds overhead. That was good news. With a well-advertised storm expected to move through the area the next day, I hadn’t been sure what weather to expect for today’s run.
The general forecast was for low clouds and fog in the morning, giving way to partly cloudy skies in the afternoon. I was going to be running one of the more scenic trails in the Santa Monica Mountains — the Ray Miller Trail. High clouds and sunshine were a much better option than running in the fog or with gloomy, overcast skies.
Shortly after leaving the trailhead, the band of high clouds became underlit by the reds, oranges and yellows of the rising sun. It was going to be a good run.
The route-finding on this run is relatively straightforward. From the Wendy Drive trailhead on Potrero Road, run over to the Satwiwa Native American Indian Culture Center (see Satwiwa map). From the Culture Center run 4+ miles on Big Sycamore Canyon Road/Trail toward the beach. Some of this is paved.
Once past the junction of Sycamore Canyon and Wood Canyon fire roads, take either the Wood Canyon Vista Trail (Backbone Trail) or Fireline Trail up to the Overlook fire road. From the top of the Wood Canyon Vista Trail turn left on Overlook fire road, or from the top of Fireline turn right, and follow the road to the top of the Ray Miller Trail. The Fireline option is about 0.4 miles longer. Here’s a map from the State Park website. Note that the La Jolla Canyon Trail is closed.
The Ray Miller Trail drops about 1000′ over 2.6 scenic miles. There is usually water available at the parking lot at the trailhead. Today the conditions were about as good as they get. The trail was in excellent condition. The temperature was in the mid-70s. The marine layer was holding offshore and a few puffy clouds had formed over the higher peaks.
One of the things about the Ray Miller Trail is that run/hike up it is almost as enjoyable as the run down. It is a very popular, and there are almost always runners and hikers on the trail. Running up a section of trail, I thought I recognized someone going down. It was nine-time Badwater finisher Chris Frost. We talked for a while about trails, running and races.
From Overlook Fire road the route back to Wendy was a familiar one — Hell Hill, Wood Canyon Fire Road, Two Foxes Trail, Big Sycamore Canyon Road, Upper Sycamore Canyon Trail, Danielson Road, and the Satwiwa Loop Trail. Including a short jog over to PCH the run was a little over 24 miles with about 3100′ of elevation gain.
Here’s an interactive, 3D terrain view of the Wendy Drive – Ray Miller Out & Back trail run. The map can be zoomed, tilted, rotated, and panned. To change the view, use the control on the upper right side of the screen. Track and placename locations are approximate and subject to errors. Poor weather, and other conditions may make this route unsuitable for this activity.
Fogbows form opposite the sun in a manner similar to rainbows, except the water droplets that create a fogbow are much smaller than raindrops. Because a fog droplet is so small, the physics of the interaction is different. The result is often a diffuse, primarily white bow.
The photograph of the fogbow was taken Sunday morning on an out and back run from Wendy Drive to Mugu Peak. The sun was about 14 degrees above the horizon. More about fogbows and other atmospheric phenomena can be found on Les Cowley’s Atmospheric Optics website.