The Color of Rain IV

Mountain biker, tree and clouds

The Mortar Pothole



The “Mortar Pothole” is a water feature in the Simi Hills I’ve been monitoring on runs for more than 13 years. Its likeness to a mud puddle is deceiving; it typically has water from October or November into August — a period of 9 to 10 months!

I’ve never seen the Pothole dry in the middle of a rain season, even during 2006-07, the driest water year on record in Los Angeles. But on February 17, 2014, following a 10 month period in which Los Angeles received only 1.2 inches of rain, the Pothole was dry and would remain dry until recharged by the 4+ inches of rain the area received from February 26 to March 2.

Now that the Pothole has been refilled and its groundwater sources at least partially replenished, water should persist in it well into Summer.

Ahmanson Blue Oak



Because I’ve been doing longer weekday runs I had not run past the blue oak at Ahmanson Ranch in a few months. Located north of Lasky Mesa, the tree may be one of the southernmost blue oaks in California. Regional climate modeling suggests that over the next century the range of blue oak may shift northward and diminish to nearly 60% of its current range, making the Ahmanson blue oak a potentially important bellwether of climate change.

After the recent rainfall I happen to run by the blue oak. Still in Winter dormancy, the tree had dropped many of its leaves and looked threadbare. Valley oaks in the area already had a flush of new, green leaves. Although the blue oak is very drought tolerant I wondered if the long period of dry weather might have claimed another victim.

A closer look at the blue oak’s limbs on another run revealed tiny leaf buds, and some sprouting leaves. That was a relief — the Ahmanson blue oak appears to be surviving the drought and will soon sport a new suit of leaves!

I checked on the blue oak on March 24th and its flush of new leaves were coming along nicely. This natural cistern, in the same drainage as the blue oak, still had water on March 18th.

Las Virgenes Creek

Even before our recent storms, small pools of standing water had developed in a few places along Las Virgenes Creek in Upper Las Virgenes Canyon. There are a number of springs along the creek and perhaps the suppression of plant growth by the drought and lower Winter evaporation rates created the pools.



From late Thursday (Feb 27) until late Saturday (Mar 1), the Cheeseboro Remote Automated Weather Station, located on a ridge on the west side of the canyon, recorded 4.26 inches of rain.

Surprisingly, the pools and the creek didn’t look much different before and after the rain, and there was no evidence of surface water flow in the creek bed at the crossing just north of the Cheeseboro connector. The drainage above this point, dessicated by months of drought, absorbed many millions of gallons of rainfall!

This was not the case for all small creeks. Garapito Creek in Topanga State Park appears to have flowed for a period during the storm, but only puddles remained in the creek bed on Sunday, March 2.

Some larger local creeks peaked at flows not observed since March 2011. According to preliminary USGS data Sespe Creek at Fillmore peaked at 6,180 cfs and Calleguas Creek near Camarillo peaked at 2,970 cfs.

One thing that was very different at Las Virgenes Creek following the rain was the dramatic increase in the number of calling chorus frogs.

Rocky Peak Vernal Pools

The vernal pools on Rocky Peak are another water feature I’ve monitored for many years. They result from small scale aquifers in the sandy soil becoming saturated and occur during most rain seasons with normal rainfall. I have not had a chance to check them yet, but suspect that as in the case of Upper Las Virgenes Creek, most of the rainfall was absorbed by the very dry soil.

On March 19th I checked a group of vernal pools on Rocky Peak. One of the larger pools did contain some water. Based on the recession rings around the pool, it was being quickly absorbed. A week later, March 26th, I checked a pool in another area of Rocky Peak and found that it had recently contained a little water, but none remained.

Trippet Ranch Runner

Runner at Trippet Ranch in Topanga State Park

When I turned the corner at the Trippet Ranch parking lot and started up the hill toward the Musch Trail, I did a double take. The road was wet and it looked like it had been raining!

While it wasn’t impossible that a rogue shower had been spawned from the deep layer of moisture flowing over the area, it was far more likely the road was just wet from on-again, off-again drizzle.

On the way over from the end of Reseda one thing is for sure — there had been no rain. The dirt roads and trails had been in great shape. It would have been an exaggeration to describe them as damp. Although cool and cloudy, the weather was excellent for running and I’d removed my sleeves miles ago.

The Trippet Ranch Loop is a favorite. I’d taken the fire roads out from the end of Reseda, now on the way back it would be almost entirely single track trail.

Some related posts: Trippet Ranch Oaks, Trippet Ranch Mule Deer, The Heavenly Ranch in the Hills, Ferns Along the Garapito Trail, Garapito Trail Runs

Celebrating the 10th Anniversary of the Acquisition of Ahmanson Ranch

Valley oaks and cirrus clouds near sunset at Ahmanson Ranch

Today those instrumental in the acquisition of Ahmanson Ranch and supporters of the open space area gathered at the park — now Upper Las Virgenes Canyon Open Space Preserve — to celebrate its purchase. For more on the festivities see this article in the Simi Valley Acorn.

I’ve been running at Ahmanson Ranch for more than ten years and have spent hundreds of hours in the open space area. Following are a few photographs, stories and wildlife encounters from these runs.

 – Northern Harrier Turning to Strike

 – Moonrises and Sunsets

 – Sunset Shower

 – Ahmanson Ranch Moonrise

 – Red-winged Blackbird Song Spread

 – Racing the Sun, Catching the Moon

 – Coyote Tag and Coyote Tag II

 – Southern Pacific Rattlesnake and Big Southern Pacific Rattlesnake

 – Ahmanson Blue Oak

 – Astronomical Trail Running

 – Ahmanson Ranch Trail Runs

 – September & October are Tarantula Months!

 – Southern California Greenscape

 – A Sunset and Moonrise

 – Dealing With Drought

 – Lenticular Wave Clouds

Signs of Winter

 – King of the Hill

Comet PanSTARRS and the Crescent Moon

The title photograph is from a run at Ahmanson Ranch earlier this November.

Mt. Wilson – Newcomb Pass – Chantry Flat Loop

Santiago Peak (Saddleback) from the Rim Trail on Mt. Wilson

As I ran through the scrub oak near the summit of Mt. Wilson, my footfalls and the distant hum of a generator were the only sounds that disrupted the quiet of the early morning. A patchwork of high clouds covered the sky, muting the rising sun and prolonging the dawn-like light.

Suddenly, I caught the movement of something large off to the side on the trail ahead. It took a moment to decipher the scene, but over a second or two the camouflaged bowhunter emerged from the background of oak leaves and limbs. Never turning to look at me, he continued to creep up a game trail toward the observatory grounds.



I wasn’t sure how the bowhunter fit in the array of hunting seasons and regulations, but if the general deer hunting season was open in Angeles National Forest I hoped my bright blue shirt and yellow “rodeo clown” running shoes would make me appear sufficiently unnatural.

Unlike last week, today I had a plan — to run down the Rim Trail from Mt. Wilson to Newcomb Pass, then down the Gabrielino Trail to Chantry Flat and back up to Wilson on the Upper Winter Creek Trail. I had not done this loop and it would give me a chance to do the stretch of the AC100 course between Newcomb Pass and the Mt. Wilson Toll Road.



The Rim Trail is a key part of several Mt. Wilson loops. The trailhead is about a quarter-mile east of the Skyline parking lot along the lower paved road with the nature trail signs. It is an adventurous and scenic trail that switchbacks steeply down the rocky northeast shoulder of Mt. Wilson and then contours over to Newcomb Pass. The trail has many long stretches of outstanding running in a forest of bigcone Douglas-fir and oak.

I’d been on the Rim Trail a few times this year and today was glad to see the poison oak along the trail was leafless and the patches of Poodle-dog bush had been trimmed. It’s harder to spot the poison oak without its “leaves of three” but it seems when it is dormant it is less of an issue.

At Newcomb Pass I turned right (south) onto the Gabrielino Trail, joining the AC100 course and beginning the descent to Sturtevant Camp in Big Santa Anita Canyon. Of all the trails on today’s loop the Gabrielino was the most technical.



In true Fall fashion the temperature on the sun-facing, chaparral-covered upper reaches of Big Santa Anita Canyon contrasted sharply with the forested north-facing slopes traversed by the Rim Trail and along the streams in the depths of the canyon.

The running between Sturtevant Camp and Roberts Camp was superb. The forests of bigcone Douglas-fir, alder, California bay and bigleaf maple are remarkable and among the most developed in Southern California. The yellows of the bigleaf maples stood out brightly against the greens of the other trees, beacons of Autumn in a mostly evergreen habitat.



The 6 mile, 3100′ climb that starts at the green foot bridge below Chantry Flat and ends at the Mt. Wilson Toll Road is the biggest on the AC100 course. On today’s run it started at a little under the 10 mile point, but during the AC100 comes at about mile 74.

After huffing up the paved road three-quarters of a mile, I refilled my Camelbak at the picnic area at Chantry Flat and continued the loop on the Upper Winter Creek Trail. The uphill on this trail was mostly moderate and runnable, and there is even some downhill to be enjoyed on its descent to the Winter Creek Trail junction near Hoegees.



The climb out on the Winter Creek Trail to Manzanita Ridge is toughest on the loop. Last week I jumped onto the undulating and sunbaked Manzanita Ridge Trail to finish the climb to the Mt. Wilson Trail junction. The “Winton Bypass” extension of the Winter Creek Trail built by Hal Winton and AC100 volunteers is a much better trail and option.

From the turnout near the top of the Kenyon Devore Trail (outside of Skyline Park) the loop worked out to about 17.5 miles, with an elevation gain/loss of about 4500′. Two shorter variations of this loop are possible. At about mile 6.5 the Sturtevant Trail can be taken directly back up to Mt. Wilson or the trail can be used to connect to the Mt. Zion Trail and eventually the Winter Creek Trail near Hoegees.

Some related posts: Mt. Wilson Trail Plus; Bigcone ENSO Prediction, Poodle-dog Bush Blues, and a Surprise on Kenyon Devore; GSU Mt. Wilson CHARA Telescope Array; Mt. Wilson Rim Trail – Kenyon Devore Trail Loop; Twenty-Two Miles and Two Classic Climbs

Mt. Wilson Trail Plus

Sunrise behind San Jacinto Peak from the Mt. Wilson Trail.

As I worked up the Mt. Wilson Trail the first flare of sunlight gleamed from behind Mt. San Jacinto. The entire mountain was backlit by the sun, an aura of sunbeams radiating from its ridges. It was about 7:15 and along with a few other hikers and runners, I was chugging up the well-used trail from its Mira Monte Avenue trailhead.

Other than going to the top of Mt. Wilson, I had no specific plan in mind. I’d see how I felt on top and then decide whether to run back down the Mt. Wilson Trail or do something longer.



The run/hike to the top is a little over 7 miles one way with an elevation gain of about 4700′. It’s a spectacular trail that works up rugged Little Santa Anita Canyon to historic Orchard Camp (about mile 3.5), and then climbs up to Manzanita Ridge and the Winter Creek Trail junction (about mile 5.4). Around mile 6 the trail joins the Mt. Wilson Toll Road for about a half-mile, then forks from it on the right, leading in another half-mile to the main parking lot at Skyline Park.

In addition to the original Mt. Wilson Trail there are four other trails that start/end at the top of Mt. Wilson: the Kenyon Devore Trail, Rim Trail, Sturtevant Trail and the Mt. Wilson Toll Road. Using these trails and interconnecting trails and roads a multitude of Mt. Wilson runs and hikes are possible.



At around 9:30 I topped out at the Skyline parking lot and while filling my Camelbak at a water faucet pondered some options. I could just retrace my steps and run back down the Mt. Wilson Trail. That would be the simplest and would be nearly all downhill. Tempting. But the weather was Autumn perfect and the visibility at least 100 miles. It was early and there was plenty of time to do a longer outing.

I’d been toying with the idea of descending the Sturtevant Trail to the Mt. Zion Trail, taking that trail to Hoegees Camp, and then ascending the Winter Creek Trail back up to the Mt. Wilson Trail at Manzanita Ridge. Variations of this loop are popular and most often done from Chantry Flats.



I didn’t know what it would be like to do the loop from the Mt. Wilson Trail, but I had a pretty good idea. On the way up Wilson I’d peered down, down, down into the canyon ascended by the Winter Creek Trail. It looked like the climb out would add another couple thousand feet to an already stout tally.

And it did! Overall the trails were in great shape and there were many miles of superb running. Near Sturtevant Camp at the Mt. Zion Trail junction (about mile 10.3) and continuing above Spruce Grove on the Mt. Zion Trail the forests of bigcone Douglas-fir, oak, alder and bay were so dense and shady I had to check if my sunglasses were still on.

The difficulty of the ascent of the Winter Creek Trail from Hoegees Camp (about mile 13) on tired legs was offset by the beauty of the canyon. At the top of the Winter Creek Trail, I jumped onto the Manzanita Ridge Trail, so that added a little extra gain. I was happy to finally see the bench at the Mt. Wilson Trail & Manzanita Ridge junction (about mile 15.4).



Although there are several places that a fall could “ruin your whole day,” the run down on the Mt. Wilson Trail is one of my favorite descents in Southern California. It’s generally not super steep and there are long stretches of relatively straightforward trail.

The run worked out to 20+ miles with an elevation gain/loss of about 7200′. Although a bit strenuous, it visited some of the most scenic areas found on Mt. Wilson.

Seventh Driest January 1 to November 1 On Record in Los Angeles

Oak and clouds on the El Escorpion loop near West Hills, California

Updated November 5, 2013. My mistake — a spreadsheet range error — thanks for the heads up Reg! The driest January 1 to November 1 for Downtown Los Angeles was in 1972 with 0.92 inch. Here are the driest ten years for that period:

1. 1972 0.92
2. 2002 1.62
3. 1984 1.93
4. 1961 2.37
5. 1971 2.39
6. 1947 2.45
7. 2013 2.78
8. 1894 2.89
9. 1953 2.89
10. 2007 3.37

As much as I enjoyed running in the showery weather Monday, I barely got wet. What Los Angeles needs is a good soaking.

Year to date Downtown Los Angeles (USC) has only recorded 2.78 inches of rain. This is the seventh driest January 1 – November 1  in Los Angeles over the past 135 years! To get out of the bottom ten for calendar year rainfall Los Angeles needs about 3.5 inches of rain by December 31. Normal rainfall for November is 1.04 inches and for December is 2.33 inches.

Although it’s still early in the rain season Downtown Los Angeles (USC) is already 0.83 inch below normal for water year rainfall. The water year extends from July 1 to June 30.