Irrigation
and water, crises
faced subsistence farmers and livestock herders in revrineareas of lower Shabelle.
Rivers are major water
resources in the world for domestic use, livestock, wildlife, irrigation, and
other water supply demand by rural and an urbanized populations, as well as
hydropower production. Somalia being a country situates in East of Africa has
two rivers which originate in the highlands of Ethiopia. The country is mutually
sharing these rivers with Ethiopia and Kenya as neighbor riparian sovereignties
in terms of exploiting underground basins, tributary contributions to the
rivers' runoff and other water utilization purpose1.These two rivers
which are the only two perennials and major water resources in southern part of
the country are locally known as "Webi Shabelle and Webi Jubba".
Likewise the rivers are both important water basin in southern Somalia which is
therefore referred as ‘breadbasket’2.
Most of the country's northern part is
typically arid, where the threshold ofevapo-transpiration exceeds the
precipitation with having no permanent water flow, except temporal flows known
as "toggs" particularly when the rainfall is high2’3
"Webi-Shabelle"
which is utilized by riverine farmers as a gravity fed-irrigation, due to
having an altitude higher than the adjacent farm lands covers total distance of
about 2526km. Nearly about two-third (63.5%)of river's basin area lies in
Ethiopian territory and one-third (36.5%) in Somalia1. The river
passes three regions (Hiraan, Middle and Lower Shabelle),those are the
country's major crop and livestock production, particularly being maize and
sesame belt. These three agricultural regions in the revrine accompanied with few
typical rain-fed mainly being sorghum belt had enabled to be the country's
economic sector and employment activity, which contributed to achieve self
sufficiency3. From the state failure emergence era and this current
post-civil war, the country had hosted consecutive droughts faced the rural
communities which caused severe starvations and food insecurity, resulted from anarchy
outbreak reached even in rural land, which caused lacking infrastructural
rehabilitation of the rivers. The country’s agricultural lands are both rain-fed
and irrigation, in the riverine regions, gravity fed irrigations are mainly
practiced as well using pumping engines, during low river flow in dry seasons.
The irrigation availability of the areas along
the river enabled to farmers to grow both rainy and dry seasons, but this is
however impeded by the irrigation crises, because of low river flow. The
subsistence farmers and livestock herders in Lower Shabelle particularly those
live in the area from Doonbural, which places about 15km far away from
southern-word Qoryoley district, to where the river ends are suffering water
and irrigation crisis, due to very low river flow, which couldn't support both gravity
fed and pumping irrigations. This is attributed to low contribution of
tributaries from in and outside river basins, due to low rainfall and even
locking the inside dams to maintain the remaining water and utilize for crop
and livestock production in a particular area, which had caused severe
circumstances to the farmers and the livestock herders those live in southern
ward of riverine areas. Ethiopia is also
suspected to build dams for exploiting the water irrigating remote lands and
hydropower production which can curtail the the river flow.
During the civil war
the people in the riverine had been threatened by consecutive floods for the
reason of high river flow in rainy seasons and lacking depressions for flood protection,
combined by vandalism of the irversides as well as accumulation of sediment,
due to high siltation of the river flow, which had caused the river to flood and
destruct crop fields and rangelands as well as infrastructures.
Likewise in dry seasons,
the farmers would be rarely faced river flow reduction, particularly in the
onset of Gu' seasonsbut in the last year the conditions became so severe, the
river flow had gradually decreased and then eventually dried .The irrigation
crises resulted from this low water flow aggravated by low rain fall in the
region particularly where the farmers and nomadic pastoralists are concentrated
resulted proximally about half of the agriculture land to be uncultivated. "These
irrigation farms are likely to shift into rainfed" says an interviewee,"so
some small farmers had however introduced drilling wells for pumping irrigation
practices" he added. But poor subsistence farmers are still suffering from
severe water shortage.Enormous migration of young men from rural areas are
consequences ofthis dire situation threatened to rural communities,
particularly household farmers and livestock herders, " every household
families' decision is to send one or more of the family members to the big
cities for labor seek". said another interviewee while, he added that some
of the families had sold their assets and entirely fled and joined in the IDP
camps in the country and now live in mediocre
condition.
Numerous young men who
used to engage growing the riverine farms faced frustration and, are currently fleeing
from agricultural areas, and coming to the big cities,such as Mogadishu, Baidoa, Hargeisa, Garowe and Bosaso to seek labor
opportunities. Not only that, they are also getting treacherous migration to
theoutsides, particularly western Europe and Saudi Arabia, some of them had
lost their lives in remorseless sea. Those who had fled inside are engaging
working in construction sites,being vendor, working wheelbarrows as a janitor, barbers
and porter, "the water stream of the river is very low as well as the
rainfall, so the farms became fallow and was filled with acacia trees"
says an interviewee, who now lives in Mogadisho and works in Bakkaro market. Some
of them had fled to Put-land and Somali-land
as a secure regions in a bid to create a small business and support
their families.
To sum up,Shabellariver
is among Somali's most important water resource, in terms of irrigation, and
water supply demand as direct consumption ofboth the people and livestock. The
riverimproves crop and livestock production, which both provide socio-economy
growth and employment activity. Finally the river does not ordinarily flow to
the Indian ocean, it ends to a depression area beyond Baraawe district, but it
sometimes exceptionally adds to the ocean when there are heavy rainfalls in
upper streams of Ethiopia and watersheds or tributaries those contribute the
river flow. Written
by Yasin Mohamed Ibrahim
References
1. AbdullahiElmi
Mohamed (2013). Managing Shared Basins in the Horn of Africa – Ethiopian
Projects on the Juba and Shabelle Rivers and Downstream Effects in Somalia. Natural
Resources and Conservation, 1 ,35 - 49. doi: 10.13189/nrc.2013.010203.
2.Basnyat, D. B. (2007), Water Resources of Somalia. Technical
Report No W-11, FAO-SWALIM, Nairobi, Kenya.
3.Machiri P.W. (2017),
Climate of Somalia Technical Report No. W-01 FOA-SWALIM Nairobi Kenya.
Most of this report had
been collected from the people who fled from the riverine in Lower Shabelle
particular the rural communities live in between Qoryoley and Kurtunwaray
districts.

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