| By John Onu Odihi

A woman in burqa and a boy on donkey advance through on a
riverbed without water for last seven years. Vast areas of the
world receive too little rainfall and are therefore arid or
semi-arid. In these areas water is always in short supply and
costs of providing good quality water may be too high for the
state in such places. AP
Climate change and water resources
are two of the important issues occupying the centre stage of
global environmental and policy agenda over the past decades.
Concerns over them looks
certain to continue well into the new millennium with many
experts warning that the problems could not be arrested easily
even if we practice all the restraints proposed for their
mitigation. A change to a warmer climate would result in the
melting of ice and glaciers that would cause a rise in sea
levels globally.
Also, fresh water pollution
caused by intrusion of seawater would jeopardise supplies of
fresh water for human consumption, industrial and agricultural
production in coastal areas.
Furthermore, climate change
would be capable of causing drastic changes and redefining
agricultural belts globally. If and when that happens, today's
breadbaskets (important food producing areas of the world) could
be turned into "agricultural deserts" as a result of
several factors, which include the inability of crops to cope
with climate change-induced temperature regimes. As more data
becomes available, the fears surrounding climate change
particularly the implications for water resources take on a
renewed urgency.
Not withstanding its abundance
(about two-thirds of the earth's surface), water remains an
elusive resource because of its nature and distribution in both
space and time. Only a small quantity of water available at any
time on earth is of fresh nature.
The bulk of water exists as
seawater, which cannot be directly used by humans or in
agricultural production. Also, water is not well distributed
around the world. Its occurrence in time and space does not
correspond well to demand. The bulk of fresh water occurs as
glaciers, snow or ice in areas too far or too cold for humans to
reach.
Vast areas of the world receive
too little rainfall and are therefore arid or semi-arid. In
these areas, water is always in short supply and costs of
providing good quality water may be too high for the state in
such places. Centuries of exploitation of underground sources
have resulted in their complete exhaustion or near-exhaustion in
many parts of the world.
Water supply has been a thorny
issue in many parts of the world. A potpourri of factors has
been responsible for water supply even before the scientific
community discovered the problem of climate change. Rising human
populations is a key factor of global concern.
The fundamental nature of the
human population problem stems from the multifarious nature of
human dependency on water. Each baby born exerts a demand
pressure on water supplies through its needs for food
(production and preparation), shelter, sanitation and recreation
among others. Additionally, modernisation or "the good
life", wrongly or rightly defined in materialistic terms as
abundance of one's material acquisition, places much pressure on
water resources. Unfortunately, water resources remain finite in
many places even with today's technology because of political,
technological and economic feasibility problems.
Not withstanding these
problems, demand for water keeps growing almost everywhere in
the world. In poorer areas, high demands and low supply lead to
high mortality rates. The inadequacy of supply in terms of
quantity, quality or both cause the poor segments of societies
in poor countries to use polluted water. This has led to very
high incidences of enteric or killer diseases such as diarrhoea,
dysentery and typhoid among others with their high tolls on the
population of such countries.
Water, which is easily one of
the most abundant resources of nature, has created the
phenomenon called "hydropolitics" (politics over
water), and it is frequently a cause of friction between people
divided by a political boundary. This happens when a water
resource such as a river has a transboundary existence.
The cause of such friction is
usually a development policy or programme that skews benefits
and costs across such a political boundary. One side gets the
carrot (benefits) and another gets the stick or sting of the
development. In many cases more than two countries have a stake
in an international river. Major basins of the world such as the
Amazon, Mekong, Congo, Nile, Niger and Rhine are international
basins.
The problem comes when
countries that have a stake in an international river have
different agenda for its development.
Parochial development such as
damming or diverting the waters of international rivers for the
benefits of one country is capable of, and has at one time or
another, strained relationships between countries.
Some examples of unresolved
international river issues as recent as the mid-1990s included
those over Rio Grande and Colorado (USA and Mexico), Eurprates
and Tigris (Iraq, Syria and Turkey) and Nile (Egypt, Sudan and
Ethiopia). Close to home, the Mekong is a source of friction
between Thailand, Vietnam, Kampuchea and Laos.
The unequivocal importance of
water to humans, the widely accepted idea of climate change and
its dire implications for water resources the world over sum up
to the need for good planning and management of water resources.
We cannot plan well without correct understanding of the
situation. While Brunei Darussalam has yet to experience major
problems with water resources, the impacts of climate change are
of global proportions. It may only be a matter of time, given
the country's coastal location, for Brunei Darussalam to
experience some of the adverse impacts of climate change such as
sea level rise.
It is therefore to our good
fortune that Professor C. Gregory Knight will be giving a
lecture to address the issues of climate change and water
resources planning using Bulgaria as a case study during his
short visit to Brunei Darussalam. Gregory Knight is Professor of
Geography and Director, Institute for Integrated Regional
Assessment at the Pennsylvania State University, University
Park, PA, United State of America.
The lecture is open to the
public and invited guests from various organisations and
associations responsible for water supply and climate studies.
His lecture will be given at 2:30 p.m. on 3 February 2003 in
Room 1.27 Computer Service Centre (CSC) Universiti Brunei
Darussalam. It is hoped that anyone with burning questions on
the issue would attend and find some answers in the lecture
and/or in the discussions that follow.
The author of this article is
from the Faculty of Arts & Social Sciences, Universiti
Brunei Darussalam.
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