become more likely with
this shift in averages. This also shows
why record cold events, such as the
freeze in early 2007 that severely damaged
the California citrus crop, can
still occur even with global warming
(though they do become less likely as
average temperatures rise because of
the shift of the curve to the warmer
right-hand side). The timing of these
extreme events is also important, as
extremely hot days close to harvest
can be more damaging than such temperatures
earlier in the season.
Precipitation is also likely to be
affected by climate change, with
important implications for viticulture,
although it is more difficult to project
for the future than temperature. The
recent assessment from the IPCC
points toward wetter conditions in
high latitudes and decreased precipitation
in subtropical latitudes such as
the southern U.S. and southern
Europe.
California may experience a little of
both, with a drier south and little
change over much of the state. The
state may also experience changes in
fog patterns. Some climate models
predict increased ocean upwelling
from climate change, which might
intensify fog development and summer
onshore flow, 20 though better
models of fog pattern are needed.
Warming, however, has additional
effects on water availability and
demand, independent of changes in
precipitation. Warmer temperatures
lead to more precipitation falling as
rain rather than snow, reducing the
valuable storage and gradual release
of water that snowpack provides (particularly
in California, where the state
relies on stored water from melting
winter snow to meet its peak water
demands during the dry summer).
Even for growers who do not rely
on snowpack to irrigate vineyards,
increasing future demands for overallocated
water resources are likely to
add stress for winegrowers. In addition,
warming affects soil moisture
through evaporation. Warmer temperatures
lead to drier soils that, in the
absence of increased rainfall, increase
irrigation demand. 6
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WHY CARE ABOUT SOMETHING
THAT MIGHT HAPPEN FAR OUT IN
THE FUTURE? Climate change is not
something that will happen in the
distant
future. It is something that is
occuring now and can already be felt,
and the emissions pathway we follow
over the next few decades will set the
trajectory for big differences at the end
of the century.
The effects of greenhouse gases are
cumulative. The greenhouse gases
from our drive to work today will continue
to exert their full climate-warming
impact for up to a century. This
means that the our climate for the next
several decades is likely to experience
similar amounts of warming, under
every emissions scenario, because differences
in emissions haven't had a
chance to take full effect yet. (Note the
overlap in projected temperatures for
all the scenarios in Figure IV until
about 2040.)
The differences in climate as a
result of different scenarios of human
greenhouse gas emissions begin to
emerge after that time, and these differences
amplify over time, leading to
the large range of projections by the
end of the current century (year 2100),
see Figure IV. Further extending the
time period over which greenhouse
gas impacts are felt is the long time it
takes for the vast ocean to respond to
changes in the atmosphere.
In California, temperatures are projected
to warm an additional 0.6°C
(1°F) by 2020; during this time, climate
conditions will remain within the
range of variability experienced in the
past.9 After that time, the warming
will be more than we have experienced
with historical variability. This
means that we would be experiencing
essentially new climates in familiar
places, climates that behave differently
than they have in the past.
This starts to move outside a range
where past experience is a good guide
for what to do in the vineyard. Given
that the average lifetime of a vine is at
least 20 years in California, this means
that vines in the ground now and
those planted in the future will be
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experiencing new climate regimes that
could affect their growth and quality.
WHAT MIGHT CLIMATE CHANGE
MEAN FOR VITICULTURE? We know
that both the average growing-season
climate and temperature extremes
such as very hot days can affect vine
and fruit development. Generally,
prices are substantially higher for fruit
from even moderately cooler regions.
For example, Cabernet Sauvignon
from the Fresno district sold for about
$260/ton in 2006, compared with fruit
from the Napa district, which sold for
over $4,100/ton. 2 This 15-fold difference
in price was accompanied by
only a 2.7°C (5°F) cooler average
annual temperature.
Up to this point, it appears that the
modest warming experienced has
been positive for grapegrowing in
many regions. For example, the incidence
of frost in Napa and Sonoma
has been substantially reduced with
the warming experienced over the last
50 years, 13 and cooler winegrowing
regions such as the Mosel Valley in
Germany have had more good vintages.
However, further warming is
poised to be a risk for many regions.
For example, D.B. Lobell et al. showed
that wine grapes in California are
already growing within 1°C (1.8°F) of a
modeled optimumfor springtime temperatures,
after which yields were projected
to flatten out and then
decrease. 10
ISN'T THE WINE INDUSTRY PROTECTED
FROM CLIMATE CHANGE
DAMAGE? The wine industry has
some advantages in dealing with climate
change. Much of coastal winegrowing
in California, for example,
does not use water from the Sierra
snowpack, which is projected to
decrease substantially under climate
change. Because of the relatively high
crop value, many growers can afford
to invest in adaptation resources that
might not be feasible for less valuable
crops.
However, winegrowing is highly
climate sensitive. Even small changes
in temperature could have big impacts
on the industry.
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