In California we
have horizontal variation; from the Pacific Northwest to the Desert
Southwest, with Mediterranean-like and a cold desert in between. This
looks like it is going to get more pronounced as climate change
occurs. The Southwestern Deserts are predicted to to get drier and
hotter. The coastal areas are the Mediterranean climate that will have
bigger droughts and bigger storms.
is vertical variation as you go up the Sierra and the Coast Ranges.
California has many, many variables with each valley and hill top creating micro-climates that may be harsher or milder.
We have customers whose mailboxes
are two USDA Zones or Sunset Zones removed from their house, in a
distance of 200 feet. California has climates with temperatures as high
as 130 degrees F.(Death Valley, The Colorado and Mojave Desert) and as
low as -54 degrees F.( a gold mine in the White Mountains,
approximately 30 miles from Death Valley). There are areas only 50
miles from L.A. that have regularly got down to -15 degrees F. and
occasionally down to -30 degrees F..
California was much colder
when the first explorers were being blown around off the coast in the
1500's and 1600's. Those were arctic gales. California was in an
eighty- year drought that intensified the extremes. Ice was hanging off
of the Big Sur coast, and the mountains of Big Sur were covered with
heavy snow. The water aboard ship froze, and the Salinas river was
frozen to the point that a musket couldn't break it. So if Monterey was
like present day Reno, what was Reno like, never mind the Bristlecone
The hottest plant community is probably Creosote Woodland,
particularly in the Salton Sea area (from Indio to El Centro). There
they recorded 124 F in May 1896. But, then there's Death Valley with
their 134 F in July, 1913, and average high summer temperatures of
about 120 F.
The wettest plant community (other
than riparian, of course) is probably the redwood belt. But the wettest
spot was on the edge of the chaparral/southern oak woodland in Campo,
just north of the Mexican border. On August 12, 1891, 11.5 inches of
rain in 80 minutes was recorded. The official one-day record was 13.6
inches at San Andreas Lake. This chaparral/oak woodland interface seems
to have this characteristic, as 9.2 inches of rainfall in 12 hours fell
at the Santa Margarita Nursery site in 1995, the year all the bridges
blew out along the Salinas River.
The driest plant community is probably the alkali sink. The
bottom of Death Valley sometimes does not see rain. Taft, in shadscale
scrub, commonly receives 3 inches, while most of the creosote bush
scrub areas receive 3-7 inches of rainfall per year.
The weirdest plant community is chaparral. Rainfall is very
variable (we range from 4 to 60 inches per year), temperature varies
50-60 degrees F. per day, and slopes and moisture really count. The top
of a slope may be 20 degrees warmer than the bottom of a slope, 100-200
feet away. Ground may be frozen to 12 inches, but the day time
temperature is 60 F
Forget evapotranspiration rates, reference evapotranspiration
and crop coefficients. They have a lot to do with climate, and
ruderals, but little or nothing to do with drought tolerant plants
(stress tolerants). Other factors such as plant establishment, plant
height, mulch, age of plants on the site, or the fact that you
overwatered or fertilized matter a great deal more. Some of the sites
in California that are covered in native vegetation should not have any
living thing there if judged by evapotranspiration rates (Remember,
according to science, bumblebees can't fly!).
Climate feedback and California native plants.
In some of the more marginal areas extra winter and spring
watering may be required for a few years to restart the forest or scrub
plant community. The problem is in fog/cloud drip. The taller
vegetation induces a positive-feedback loop that allows the plant
community to live (Wilson, J.B.
and A.D.Q. Agnew). The plants capture the moisture from
fog, and create more fog. If the taller trees/shrubs
are not there, the site is between 20-200% drier and effectively
creates a negative-feedback that drives succession backwards into a
drier plant community that is unstable and ready for invasion by alien
species (largely annual grasses). For instance, on Vandenberg Ari Force
Base Rainfall is recorded at 14 inches, fog drip adds 24 inches to
this. If the native vegetation is removed the fog drip drops to nearly
nothing and grasses move in. The grasses absorb a lot of that 14 inches
of rainfall and evaporate it off. The Shadscale scrub in the central
valley is similar. A large portion of their rainfall comes from the
tule fog condensing on the vegetation. Many areas of coastal California
including the redwood forest are very sensitive. Once those huge dew
collectors are removed there is not enough rainfall to support new
ones. ( Redwoods can't survive on 15 inches of rainfall without that
huge addition of fog drip) So the plant community moves from Coastal
Redwood forest to chaparral. Oak woodland, pine forest or mixed
evergreen forest will become weedy coastal sage scrub or chaparral,
coastal sage scrub or chaparral declines, is invaded by annual grasses,
and becomes grassland, redwoods become weedy northern scrub, etc.
In other marginal areas provide a wind screen for a few
seasons to allow the first wind-blocking row of trees/shrubs to grow
up. Some areas only have plants as high as the species that tolerates
wind. The climate behind the bush or tree is very pleasant compared to
the sandy/salty gale on the other side of the wind-tolerant plant. This
wind row may only be 2-5 feet high and is common in coastal bluffs or
desert edges. People commonly remove the 'scrub' and plant foo-foo
plants that look like hell and die. Some people do this for years and
are noticed for their lack of intelligence and plastic garden creatures.
Plant communities are driven by the plants, but the plants can
only survive where the plant community is supposed to be, which is
delineated by climate. Climate is dynamically driven by the plant
community AND the plant community is limited by the climate.
Temperature ranges are decreased 10-20 degrees F, by the effects of the
plant community. Precipitation rates can be increased by 50-150% when
the plant community is intact. This feedback loop is the saving of many
marginal sites. Just because the area has no native plants or plant
community left, doesn't mean it cannot be recreated. Areas as small as
a large lot can provide enough of an area to build a small plant
community that only needs the dust washed off to create it's own
'climate'. The soil moisture under one coyote bush is twice that in the
surrounding field of weeds. The oak tree can germinate and survive only
under the resource island created by a plant like that one bush. Plant
a coastal native landscape and oaks become weeds trying to move your
coastal sage scrub garden to an oak forest. You've just doubled
your effective rainfall, lowered your summer and increased your winter
If weeds invade a native plant community, the effective
rainfall is cut in half, or more.
The individual plants have the USDA zones attached to them
primarily for the Easterners.
We have fog, some areas as much as
50% of the year and providing 18.4 to 30.4 cm (7-15 inches) of rainfall
from fog drip, other areas never see clouds or fog. Can you imagine an
area that gets 330+ days of bright sunshine? Our rainfall in the state
ranges from 80 inches, plus 12 inches of fog drip, in the redwoods to
1.5 inches in Death Valley, about 3 inches in Taft, and between in
parts of the Sonoran Desert.
For those of you that are new to gardening, or new to an area, ask a
neighbor that's been there for awhile and keep bringing him (or her)
cookies or bottles of beverage until you figure out what the rainfall
and temperatures have been for the last decade or more. If their yard
lloks good and has plants you like in it ask about those also.
For those of you back east or in other areas of the world remember that
almost all of California does not get summer rain. The only places that
do get rain from April to October are the S.E. Deserts and the northern coastal
fog belt. Most areas of California you would find dry by your standards. In
1841 Santa Barbara had no measurable rainfall and ½inch of fog
drip. One of our customers from the Desert Center area told us she had
had no rain for three years, but the vegetation still looked good.
On the other hand,the "Great Flood of 1862" filled most of the valleys
in California with water after it rained hard for a month around the
first of the year in 1862. With climate change we might get double that,
or it might not rain at all in a period of just a few years. If it stays dry for a decade or so, California can get VERY cold.
The extreme records in the Santa Margarita nursery: 95 degrees F.(35
C.) for a couple of weeks in Feb., followed by a 12 degrees F(-10 C)
night. 118 degrees F (48 degrees C.) for five days in the heavy shade,
it was cool there, at least 10 degrees cooler than out in the sun where
most of the plants were. There was also a 20-30 mph (10 mps) wind with
10% humidity. We've had as little as 4 and 7 inches of rainfall or as
much as 55 inches in the last 40 years. We have had as much as 4-5"(10
cm) of rain or 10"(25 cm) of snow in a morning before and gone for 10
months with no rain. Historical records say California was much drier
and colder 400 years ago with temperatures 30 F degrees cooler in the
winter and slightly hotter in summer. A period of an 80 year drought
ended as the Europeans showed up. Ice hung off Big Sur bluffs and the
Salinas River in Monterey was frozen to 6" or more in 1608. (Cabrillo)
Customers set us to giggles when they tell us how cold a 28F temp is!
ground is regularly bare when the cold hits subtract at least one USDA
zone from what you think you are. If you always have deep fluffy snow
when the cold hits you may be able to add two zones to your climate.