Much of the western United States has been on fire this
summer. Affected landscapes range from California
chaparral to temperate rainforest in the Pacific Northwest .
Fire danger appears to be elevated this year because of the convergence of a
few important factors. First, much of the western US (but particularly California ) has been
experiencing severe drought over the last few years. Second, climate change
continues to steadily result in higher land temperatures year over year. And
finally, western forests have been subject to a long history of fire
suppression by management agencies that have left more fuel than would
otherwise be present.
Fire is a natural part of some ecosystems. In fact, certain plant
species are dependent on fire for establishment of juveniles or completion of
their life cycle. Examples include many species of pines and the giant sequoia of
the Sierra Nevada . The latter species requires
high light and fires help clear out competitors that might shade young
sequoias.
Stebbins Cold Canyon Reserve in spring 2014 with pine, oak and chaparral habitat. |
Unfortunately, fire management policies have exacerbated the
threat of large intense fires in the west. During the early decades of the
1900s, fire was suppressed at all costs. In some cases this may have led to the
excessive buildup of fuels in dense forests. Once the importance of fire to some
native ecosystems began to be better understood, land management agencies such
as the US Forest Service recognized the importance of allowing some fires to
run their course. Despite this change in attitude about fires in western
ecosystems, fires are still managed in many cases. Continued encroachment of
human development deeper into forests or other wildlands increases the
likelihood that a fire will need to be suppressed to protect human
infrastructure instead of letting it runs its natural course.
The Wragg fire was a moderate sized fire that ignited
earlier this summer and burned through chaparral and pine forest habitat along
state route 128 in the coast range hills of northern California
near Lake Berryessa . The fire consumed the whole
area of the Stebbins Cold Canyon Reserve, a small University of California
research reserve where I have been hiking several times over the last decade.
My most recent hike at the reserve was during April 2014.
Monkeyflowers, Brodiaea, Castilleja and Dichelostemma were in bloom at the time. The most striking plant I
observed was the heartleaf milkweed, Asclepias cordifolia. Emerging stoutly a half meter or so from the short groundcover
of grasses, it had slate green fleshy opposite leaves and bright purple
flowers. The magenta petals were slightly reflexed (bent backwards) and contrasted
vividly with white hoods that form little loops around the center of the flower.
Habit and flowers of Asclepias cordifolia, heartleaf milkweed, spring 2014. |
Cold Canyon in late August 2015, after the Wragg fire. |
The Wragg fire however, transformed the landscape
dramatically this summer. Although the Reserve is currently closed to visitors,
from the highway it is possible to see the scorched hillsides. The ground was
blackened and trees stood like ruins on the hillside. Looking closely, I could
see that not all vegetation was equally affected; many trees had at least some
green in their canopies, suggesting tree damage, but not complete mortality. Of
course, the soil retains a seed bank and perhaps individuals of some species
escaped mortality if the fire moved quickly through an area. It will be very
fascinating over the next few years to hike the trails again and observe how
the ecosystem recovers.
References
- Eckenwalder JE. 2009. Conifers of the World. Timber Press, Portland .
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