2.3.
How can water stress be calculated?
Much
like the issue of defining sustainability, which we discussed in Session 1 of
this module, a formal scientific definition of how to calculate water stress
has not fully been agreed. There are, however, two methods that are applied
commonly, to calculate water stress; the “water resources vulnerability index”
and the “water stress indicator”.
2.3.1.
The water resources vulnerability index
An
index of water stress that is often calculated is the “water resources
vulnerability index”. The index is a measure of pressure on water resources and
it can be readily applied to multiple watersheds. The index calculates the
ratio of annual water withdrawals to annual runoff (renewable freshwater
supply). Watersheds where withdrawals are less than 20% of supply (i.e. a ratio
of less than 0.2) have low or no water stress, watersheds with a ratio between
0.2-0.4 have medium stress, and watersheds where withdrawals are greater than 40% of supply
(i.e. a ratio of greater than 0.4) have high stress (Alcamo et al., 2007;
Hanasaki et al., 2008).
The
threshold of withdrawals being greater than 40% of supply, has been arbitrarily
chosen amongst the scientific water resources modelling community as an
indicator of high water stress, since the larger the amount of water that is
withdrawn from the environment and used and discharged back into rivers, the
more degraded and/or depleted the resource becomes, and the higher the water
stress (Alcamo et al., 2007). In this sense, 100% of the resource does not need
to be withdrawn for a watershed to be classed as water stressed.
The
water resources vulnerability index tends to highlight pressures in watersheds
with large amounts of irrigation, because the index is largely based upon
withdrawals. Projections of future withdrawals are contingent upon future
population change and assumptions about future changes in domestic, industrial
and agricultural water use intensity. Note, however, that this metric does not
account for water quality.
2.3.2.
The water stress indicator
The
“water stress indicator” is based on water availability per person. A threshold
of 1000 m3/person/year is generally used to indicate exposed to water resources
stress; i.e. if there is less than 1000
m3 of water available for each person in a year, then that region is classed as
water stressed. The measure is simple to calculate but it assumes that water
resources pressures are a function of the numbers of people only, not the
amount of water that those people actually use.