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Climate change and food security
Richard A. Betts, Pete D. Falloon, Jemma Gornall, Neil Kaye and Andrew Wiltshire, Met Office Hadley Centre;
Timothy R. Wheeler, Walker Institute for Climate Systems Research, Department of Agriculture, University of Reading, UK
F
ood security has been defined as ‘a situation that exists
when all people, at all times, have physical, social and
economic access to sufficient, safe and nutritious food
that meets their dietary needs and food preferences for an active
and healthy life’.
1
Although the production of food is clearly
fundamental, the concept of food security goes beyond produc-
tion and considers the entire system. It therefore encompasses
other aspects of food availability such as distribution and
exchange, and wider issues of access and utilization.
2
Global food systems are inherently linked to climate in a large number
of complex ways. The productivity of food crops, livestock and
fisheries is highly dependent on climatic conditions and other envi-
ronmental factors linked to climate, such as atmospheric composition.
There is a tradition in agriculture of coping with year-to-year changes
in climate. Nevertheless, human-induced change is expected to push
these managed ecosystems beyond their natural boundaries, requiring
greater adaptation. Climate change and its drivers are therefore likely
to impact on the production aspect of food security. Moreover, since
social and economic systems as a whole are influenced by climate,
food security is also likely to be impacted by climate change through
its wider effects on infrastructure and economies.
Impacts of climate change on food production
Climate change is likely to directly impact on food production across
the globe. At higher latitudes where production is currently limited by
temperature, producers may benefit from longer growing seasons for
moderate warming, although higher levels would be expected to counter
these benefits. Even moderate levels may not necessarily confer benefits
without adaptation by producers, as an increase in the mean seasonal
temperature can bring forward the harvest time of current varieties of
many crops and hence reduce final yield, in the absence of any adapta-
tion to a longer growing season.
3
In areas where temperatures are already
close to the physiological maxima for crops, warming will impact yields
more immediately.
4
In seasonal arid environments higher temperatures
may also be more immediately detrimental by increasing heat stress on
crops and water loss by evaporation.
Changes in short-term temperature extremes can be critical, espe-
cially if these coincide with key stages of crop development. Only a
few days of extreme temperature (greater than 32°C) at the flower-
ing point of many crops can drastically reduce yield.
5
Temperature
extremes also increase the risk of heat stress to livestock. Changes in
the water cycle will be vital to production, whether by a decrease in the
availability of fresh water or increasing damage caused by an excess.
More frequent heat waves and droughts are expected,
6
causing yields
of food crops and fodder for livestock to be more variable from year to
year,
7
decreasing overall.
8
Further development of crop cultivars that
are more tolerant to extreme weather is needed. Other
impacts of drought may be reduced pasture productiv-
ity, increased livestock deaths, soil erosion via wind and
land degradation.
Food production can also be impacted by too much
water. Heavy rainfall events leading to flooding can
wipe out crops and drown livestock over wide areas,
and since an increase in the intensity of extreme rain-
fall is expected in a warmer world,
9
damaging flooding
events may become more frequent.
10
Flooding aside,
direct negative impacts of excess water include soil
water-logging, anaerobicity and reduced plant growth.
Indirect impacts include delayed farming operations
or implementation when they could cause compac-
tion damage, as in livestock treading and ‘poaching’.
11
Agricultural machinery may simply not be adapted
to wet soil conditions. Extreme wind events such as
intense storms and hurricanes can also cause wide-
spread damage across cropland areas.
Changes remote from production areas may also be
critical. Irrigated agricultural land comprises less than
one fifth of all cropped area but produces 40-45 per
cent of the world’s food,
12
and water for irrigation is
often extracted from rivers which depend on distant
climatic conditions. Some key rivers are fed by moun-
tain glaciers, with approximately one-sixth of the
world’s population currently living in glacier-fed river
basins. Populations are projected to rise significantly in
major glacier-fed basins such as the Indo-Gangetic plain
and other major irrigated areas such as those near the
Yangtze and Nile. As such, changes in remote rainfall
and the magnitude and seasonality of glacial meltwaters
could impact food production for many people.
Sea-level rise is another potential indirect influence.
In low-lying coastal areas, rising seas will inundate agri-
cultural lands and salinize groundwater. Short-lived
storm surges can also cause great devastation, even if
land is not permanently lost. These impacts will chal-
lenge the livelihoods of many millions of people who
live near the world’s mega deltas. Both marine and
freshwater fisheries may also be impacted by change.
Positive and negative impacts of warming on fish
have been reported.
13
Marine fisheries may be affected
by general poleward shifts in ranges determined by
temperature, and shifts in the ranges of pathogens and
changes in nutrient supply due to altered oceanic circu-
lation. Freshwater fisheries may benefit from increased
T
he
I
mpacts
and
I
mplications
of
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limate
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hange
and
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ariability