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Rainfed agriculture : ウィキペディア英語版
Rainfed agriculture

The term Rainfed agriculture is used to describe farming practises that rely on rainfall for water. It provides much of the food consumed by poor communities in developing countries. For example, rainfed agriculture accounts for more than 95% of farmed land in sub-Saharan Africa, 90% in Latin America, 75% in the Near East and North Africa; 65% in East Asia and 60% in South Asia.〔(Managing water for rainfed agriculture ) International Water Management Institute, 2010, Issue 10. 〕
Levels of productivity, particularly in parts of sub-Saharan Africa and South Asia, are low due to degraded soils, high levels of evaporation, droughts, floods and a general lack of effective water management. A major study into water use by agriculture, known as the Comprehensive Assessment of Water Management in Agriculture, coordinated by the International Water Management Institute, noted a close correlation between hunger, poverty and water. However, it concluded that there was much opportunity to raise productivity from rainfed farming.
The authors considered that managing rainwater and soil moisture more effectively, and using supplemental and small-scale irrigation, held the key to helping the greatest number of poor people. It called for a new era of water investments and policies for upgrading rainfed agriculture that would go beyond controlling field-level soil and water to bring new freshwater sources through better local management of rainfall and runoff.〔Molden, D. (Ed). ''Water for food, Water for life: A Comprehensive Assessment of Water Management in Agriculture.'' Earthscan/IWMI, 2007.〕
The importance of rainfed agriculture varies
regionally but produces most food for poor
communities in developing countries. In subSaharan Africa more than 95% of the farmed
land is rainfed, while the corresponding figure
for Latin America is almost 90%, for South Asia
about 60%, for East Asia 65% and for the Near
East and North Africa 75% (FAOSTAT, 2005).
Most countries in the world depend primarily on
rainfed agriculture for their grain food. Despite
large strides made in improving productivity and
environmental conditions in many developing
countries, a great number of poor families in
Africa and Asia still face poverty, hunger, food
insecurity and malnutrition where rainfed agriculture is the main agricultural activity. These
problems are exacerbated by adverse biophysical growing conditions and the poor socioeconomic infrastructure in many areas in the semi-arid tropics (SAT). The SAT is the home to
38% of the developing countries’ poor, 75% of
whom live in rural areas. Over 45% of the
world’s hungry and more than 70% of its
malnourished children live in the SAT

There is a correlation between poverty, hunger
and water stress (Falkenmark, 1986). The UN
Millennium Development Project has identified
the ‘hot spot’ countries in the world suffering from
the largest prevalence of malnourishment. These
countries coincide closely with those located in
the semi-arid and dry subhumid hydroclimates in
the world (Fig. 1.1), i.e. savannahs and steppe
ecosystems, where rainfed agriculture is the
dominating source of food and where water
constitutes a key limiting factor to crop growth
(SEI, 2005). Of the 850 million undernourished
people in the world, essentially all live in poor,
developing countries, which predominantly are
located in tropical regions (UNSTAT, 2005).

Since the late 1960s, agricultural land use has
expanded by 20–25%, which has contributed
to approximately 30% of the overall grain
production growth during the period (FAO,
2002; Ramankutty et al., 2002). The remaining
yield outputs originated from intensification
through yield increases per unit land area.
However, the regional variation is large, as is
the difference between irrigated and rainfed
agriculture. In developing countries rainfed
grain yields are on average 1.5 t/ha, compared
with 3.1 t/ha for irrigated yields (Rosegrant et
al., 2002), and increase in production from
rainfed agriculture has mainly originated from
land expansion.
Trends are clearly different for different
regions. With 99% rainfed production of main
cereals such as maize, millet and sorghum, the
cultivated cereal area in sub-Saharan Africa has
doubled since 1960 while the yield per unit of
land has been nearly stagnant for these staple
crops (FAOSTAT, 2005). In South Asia, there
has been a major shift away from more
drought-tolerant, low-yielding crops such as
sorghum and millet, while wheat and maize hasapproximately doubled in area since 1961
(FAOSTAT, 2005). During the same period, the
yield per unit of land for maize and wheat has
more than doubled (Fig. 1.2). For predominantly rainfed systems, maize crops per unit of
land have nearly tripled and wheat more than
doubled during the same time period.
Rainfed maize yield differs substantially
between regions (Fig. 1.2a). In Latin America
(including the Caribbean) it exceeds 3 t/ha, while
in South Asia it is around 2 t/ha and in subSaharan Africa it only just exceeds 1 t/ha. This
can be compared with maize yields in the USA or
southern Europe, which normally amount to
approximately 7–10 t/ha (most maize in these
regions is irrigated). The average regional yield
per unit of land for wheat in Latin America
(including the Caribbean) and South Asia is similar to the average yield output of 2.5–2.7 t/ha in
North America (Fig. 1.2b). In comparison, wheat
yield in Western Europe is approximately twice
as large (5 t/ha), while in sub-Saharan Africa it
remains below 2 t/ha. In view of the historic
regional difference in development of yields,
there appears to exist a significant potential for
raised yields in rainfed agriculture, particularly in
sub-Saharan Africa and South Asia.

Rural development through sustainable management of land and water resources gives a plausible solution for alleviating rural poverty and improving the livelihoods of the rural poor.
In an effective convergence mode for improving the rural livelihoods in the target districts,
with watersheds as the operational units, a holistic integrated systems approach by drawing attention to the past experiences, existing
opportunities and skills, and supported partnerships can enable change and improve the livelihoods of the rural poor. The well-being of the
rural poor depends on fostering their fair and
equitable access to productive resources. The
rationale behind convergence through watersheds has been that these watersheds help in
‘cross-learning’ and drawing on a wide range of
experiences from different sectors. A significant
conclusion is that there should be a balance
between attending to needs and priorities of
rural livelihoods and enhancing positive directions of change by building effective and
sustainable partnerships. Based on the experience and performance of the existing integrated
community watersheds in different socioeconomic environments, appropriate exit
strategies, which include proper sequencing of
interventions, building up of financial, technical
and organizational capacity of local communities to internalize and sustain interventions, and the requirement for any minimal external technical and organizational support needs to be
identified.
While absolute grain yield variations exist between different global locations as cited in this article, the potential for improved rain fed grain yields may be less than is suggested by a comparison between sub-Saharan and European locations for example, this applies particularly in areas where grain yield is primarily determined by the growing season rainfall. A more accurate formula for measuring yield potential is y x a = X, where X is grain yield in Kg/hectare, y is millimetres of growing season rainfall and a is the variable yield factor, a number that may vary somewhere between 5 and 20. Thus assuming a variable yield factor of 15 and a growing season rainfall of 220mm the formula would express as 220mm x 15 = 3300kg/ha yield potential.
This formula, while not taking account of either the carryover benefits of stored rainfall in the soil profile resulting from out of season rainfall or the impact of temperature or soil fertility, still gives a more accurate picture of the degree to which actual grain yields are matching the region's potential yields and is a better basis for comparison between very different regions such as Europe and the sub-Sahara.
A European yield of 5000kg/ha from a rainfall of 500mm results in a variable yield factor of 10 while a yield of 2500kg/ha in a 200mm rainfall area has a variable yield factor of 12.5, in such an example the lower yielding crop has actually been 25% more efficient in its rainfall utilisation than the higher yielding crop. Agronomy needs to be based on attaining the highest possible variable yield factor rather than the highest absolute yield, factor numbers as high as 17+ are achievable.
==See also==

*Water, Land and Ecosystems

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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