Davids
Engineering prepared a draft report in October of 1998 for the Bureau of
Reclamation titled “Klamath Project Historical Water Use Analysis.”
This report is based on water use data beginning in October of 1961 and
ending in September of 1997. The
following is a quote of Section 5.4, discussion of Project efficiency, from the
report.
The
results of this study indicate that the effectiveness of water use in the
An
implication of the variability evident in the month to month snapshots of
classical efficiencies is that there are important temporal and spatial
interactions within the Klamath Project. For
example, these snapshots suggest that the runoff of diverted water that reduces
efficiencies in upstream subregions leads to increased efficiencies in Subregion
3 where some of the upstream diversions are ultimately consumed.
A consequence of this observation is that a program intended to improve
efficiencies by reducing return flows in Subregions 1 and 2 could have a
negative effect on the classical efficiency of Subregion 3 and have little net
effect on the efficiency of the Project as a whole.
Analysis
of the monthly patterns of classical efficiencies, both for individual
subregions and for combined subregions, indicates that early season irrigation
efficiencies are typically low while efficiencies during the peak use months of
July and August are very high. This
pattern demonstrates how the classical formula penalizes root zone replenishment
as diverted water that is not immediately consumed.
However, the root zone replenishment that is penalized early in the
season leads to the very high efficiencies during the peak demand period when
soil moisture is consumed. This peak
period withdrawal of soil moisture frequently leads to instances when
consumption in July and August is greater than reported diversions and classical
efficiencies are computed to be greater than 100 percent.
The
above observation implies that a sophisticated seasonal pattern of water use has
evolved in the Klamath Project. Early
in the irrigation season the Project’s diversion and conveyance capacity is
used to distribute water to meet immediate irrigation requirements and to
replenish soil moisture throughout the Project area.
Later, soil moisture stored in the first months of the irrigation season
allows the Project to meet peak consumptive use demands even when these demands
exceed the Project’s capacity to divert and deliver surface water.
This
perspective illustrates a relation between operational practices early in the
irrigation season and the Project’s ability to respond to peak period demands.
In particular, this suggests that reduction
of irrigation deliveries during April and May could yield unintended
consequences that might not be apparent until two months later.
In
summary, should hydrologic conditions make adjustments in irrigation diversions
necessary to follow the annual operations plan, decision makers should base
allocation decisions on the understanding that the Klamath Project has developed
into a highly effective, highly interconnected form of water management.
As a result, careful consideration should be given to implementing
operational changes that meet their objectives without setting in motion a chain
of unintended consequences that negate the benefits of the modified operations.
The
subregions identified in the above quote are described in general as follows:
|
Subregion |
Description |
|
1 |
|
|
2 |
Lands
served mostly by the Klamath Irrigation District; downstream of Harpold
Dam and upstream of Anderson Rose Dam. |
|
3 |
Lands
served by Tulelake Irrigation District; downstream of Anderson Rose Dam. |