Category Archives: nature|trees

Valley Oak Sunset

After chugging up the long climb, I pause on the crest of the hill. Open space surrounds me. In a nearby oak, small birds twit and twitter, preparing for the night. In the distance coyotes yip and yell, an announcement on one hilltop, and an answer on another. A cold ribbon of wind brushes against my leg.

I take a deep breath and smile. At sunset the day melds to an end, becoming rich with sights, smells, and sounds. In the moment, senses converge and thoughts coalesce.

There is form in the oak’s twisted limbs. A dove dives from its branches, and I turn for home.

Related post: Return of the Afternoon Sun

Mt. Hawkins Lightning Tree

An unusual, offset lightning scar on a Jeffrey pine in the San Gabriel Mountains, near Los Angeles.

Update. The Mt. Hawkins lightning tree lost it’s crown over the Winter of 2019-2020.

An unusual, offset lightning scar on a Jeffrey pine in the San Gabriel Mountains, near Los Angeles. The tree is located at an elevation of about 8750′, on the ridge east of Mt. Hawkins.

The offset scar is not easily explained. Either the scar was offset when created, became offset as the tree aged, or perhaps multiple strikes have somehow created the appearance of an offset. None of these explanations seem completely satisfactory.

The lightning scar on the Mt. Hawkins tree appears to be older than the scar on the Jeffrey pine on the Three Points – Twin Peaks Saddle trail, and quite a bit older than the scar on the Jeffrey pine on Mt. Baldy’s North Backbone Trail.

Did Lightning Start the 2002 Curve Fire?

Or did the Curve Fire trigger a lightning strike?

These trees — on a section of the Pacific Crest Trail east of Windy Gap — were burned almost six years ago in the 20,857 acre Curve Fire. According to the Curve Fire Burned Area Emergency Report Implementation Plan, the source of ignition for the devastating fire was “a ritual involving the use of fire (candles) and animal sacrifices.” The fire started the afternoon of September 1, 2002.

However, in the document An Exercise Involving Flash Flood and Lightning Potential Forecasts, an alternative ignition source was suggested — an “out of the blue” lightning strike. Forecasters observed a “single positive lightning strike northeast of the Mount Wilson Observatory” about 1:00 PM PDT (2000Z), near the time the Curve Fire started. According to NWS Lightning Safety Outdoors, such bolts from the blue have been documented to travel more than 25 miles from a thunderstorm cloud.

While there is compelling evidence that the blue sky lightning strike occurred, the time of the strike suggests that it was not the initial source of ignition of the Curve Fire. This UCLA Solar Towercam image is time-stamped at 12:58:58, about the time of the strike. It shows the Curve Fire already underway, with a well-developed smoke column. The photograph also shows the cloud development over the San Gabriel Mountains.

An intriguing question comes to mind. Was the lightning strike a coincidence, or was it somehow triggered by the fire, or the smoke?

According to “Forest Fires: Behavior and Ecological Effects” by Edward A. Johnson, Kiyoko Miyanishi (Academic Press, 2001) large scale lightning detection networks have revealed an association between forest fires and the electrification of thunderstorms. Further, “a shift from negative to positive ground flash prevalence in association with fires and forest fire smoke” has been documented.

So it looks like lightning did not start the Curve Fire, but the Curve Fire may have triggered the positive lightning strike observed by the NWS!

The photograph of trees burned in the Curve Fire is from Sunday’s Islip Saddle – Mt. Baden-Powell South Fork run.

Related post: Explosive Growth of the Lake Fire

Technical papers:

CLOUD-TO-GROUND LIGHTNING DOWNWIND OF THE 2002 HAYMAN FOREST FIRE IN COLORADO

Timothy J. Lang* and Steven A. Rutledge
Colorado State University, Fort Collins, Colorado

Enhanced Positive Cloud-to-Ground Lightning in Thunderstorms Ingesting Smoke from Fires

Walter A. Lyons, Thomas E. Nelson, Earle R. Williams, John A. Cramer, and Tommy R. Turner
Science 2 October 1998 282: 77-80 [DOI: 10.1126/science.282.5386.77] (in Reports)