Sites Reservoir —
Potential Benefits for Fish,
Potential to Worsen Conditions for Fish
Working Presumption: Thumbs Down

The proposed Sites Reservoir1 would be a new off-stream storage reservoir covering 12,000 -14,000 surface acres with 1.8 million acre-ft of storage capacity on the west side of the Sacramento Valley (Figure 1). The project would capture and store unregulated Sacramento River winter-spring runoff and some water previously stored in Shasta Reservoir. The diversion capacity to the reservoir would be 5400-6500 cfs, supplied by two existing river diversions (up to 1800 cfs at Red Bluff; up to 2100 cfs at Hamilton City) and a new diversion near Colusa (proponents are evaluating alternative capacities of 1500 and 3000 cfs, in addition to the currently preferred capacity of 2000 cfs). The Sites Authority webpage estimates that it could have diverted over 1 Million acre-ft to storage in Sites in 2018 and 1.8 Million acre-ft to storage in 2017; these figures assume bypass flow requirements at the diversion points and at Freeport, and sufficient storage capacity in the reservoir. The Draft Environmental Impact Report/Environmental Impact Statement (DEIR/DEIS) for the Sites Reservoir Project estimates the average annual diversion to Sites storage at about 500,000 acre-ft; actual diversions would vary depending on hydrology and regulatory constraints.

As an off-stream storage reservoir, Sites would store water behind a dam that is not on a major waterway. Water diverted to the reservoir would be pumped into canals from the Sacramento River, and then pumped into the storage reservoir from small holding reservoirs on the canals. The two existing diversions that would fill Sites have modern fish screening facilities. As currently envisioned, a pump-back hydroelectric operation would allow partial recovery of pumping costs.

The Sites project has potential benefits for fish, but also the potential to worsen conditions for fish.

Potential Benefits for Fish

  1. Under current operations, existing irrigation diversions on the Sacramento River draw water primarily in spring and summer via several major canal systems on the west side of the Sacramento Valley. These diversions draw mainly on water that was previously stored in Shasta Reservoir and released to the Sacramento River in part to keep river water temperatures cool. Shasta Reservoir’s cold-water pool varies in volume depending on storage and other factors, and can run out if it is not managed carefully. If the cold-water pool is depleted at the end of the summer, this threatens the viability of winter-run salmon. Under current operations, spring and summer irrigation diversions from the Sacramento River also cut flow and raise water temperatures in the lower river, which harms salmon, steelhead and sturgeon. Water diverted to storage in Sites in the winter could substitute for some of the spring and summer irrigation deliveries that currently come from Shasta. A greater percentage of water released from Shasta in spring and summer could then flow all the way to the Delta. More water could also be retained in Shasta Reservoir to protect the Shasta cold-water pool into the fall and as carryover for the following year.
  2. If more water were delivered to the Delta from Shasta Reservoir in the spring and summer, less water would theoretically be needed from Folsom and Oroville reservoirs to meet Delta water quality, outflow and other requirements. This could allow more targeted releases of water into the lower American and lower Feather rivers to protect fish in those waters. It could also allow better maintenance of cold-water pools and greater carryover storage in Folsom and Oroville, also very important for the respective fisheries downstream.
  3. Water stored in Sites could be delivered directly to the Delta via the Colusa Basin Drain (CBD) system and Yolo Bypass, reducing outflow demands from other Valley reservoirs. Water delivered directly to the Delta from Sites would be of higher potential productivity and could stimulate winter-spring Bay-Delta plankton blooms that would benefit Delta native fishes.

Potential to Worsen Conditions for Fish

  1. The proposal includes a new point of diversion on the Sacramento River with a capacity to divert 2000 cfs. This would give the project higher diversion capacity and the capability of diverting tributary runoff that would otherwise be unavailable to the two upper river diversions that now enters the Delta. This diversion would also affect flows and water temperatures in the lower Sacramento River, and subject migrating juvenile salmon, sturgeon, and steelhead to a third large screening facility. The new point of diversion would be particularly problematic if it diverted water outside the peak runoff season (late fall through spring).
  2. The new diversion and the reoperation of canal intakes at Red Bluff and Hamilton City to divert water in winter would compete for water with Delta diversions and would affect Delta outflow to the Bay.
  3. Water deliveries and hydropower releases from Sites Reservoir to the lower river at the new diversion site could affect water quality in the lower Sacramento River.
  4. With available winter off-stream storage, the existing diversions at Red Bluff and Hamilton City would be capable of diverting uncontrolled flows from tributaries that have otherwise remained relatively untouched down to the Delta.
  5. The greater diversion capacity may increase demands on Shasta storage and will increase diversion of uncontrolled tributary flows, further compromising fishes in the Sacramento River and the Bay-Delta.
  6. A small but potentially significant amount of water supply stored in Sites Reservoir would be lost to evaporation and groundwater seepage.

Above all, there is too much unknown to evaluate how Sites would affect fish.

As is the case for most proposed water supply projects, the project description in the draft DEIR/DEIS for Sites describes several potential configurations of project infrastructure and a description of proposed constraints. The DEIR/DEIS does not evaluate different constraints, such as different bypass flow requirements past each point of diversion; the DEIR/DEIS only evaluates one value for each point. In spite of numerous requests that the DEIR/DEIS evaluate project diversions with more stringent Delta flow and water quality requirements than the existing inadequate ones, the DEIR/DEIS only evaluates project yield with existing Delta constraints.

The benefit side is even more vague and conceptual. The entire construct of hypothetical Sites benefits would in fact require a new type of proscriptive rules and enforcement mechanisms that would be unprecedented for California water projects. There is simply no clue in any of the Sites literature what those rules would be or even could be.

The project description places no numbers on how much water stored in Sites the project’s operators would dedicate to actions designed to benefit fish. The project description defines no decision-making process for dedicating water to fish, other than to say that on an overarching basis fish agencies will decide. The project description defines no way in which project operators will apportion water for fish against water for water supply. For all the offsets that seem to comprise the lion’s share of fish benefits, the project description does not say how water from Sites will generate improvements in operation of state or federal reservoirs, or whether it will be Sites operators or state and federal operators who make the calls.

Then there is the question of whether there would be any offsets at all. There is no assurance that there will be any decreases at all in water use from Shasta or from other state and federal reservoirs. Water freed up by using Sites to meet Sacramento Valley water supply could simply allow Sac Valley water users to irrigate more land or sell more water for export at the Delta pumps. The DEIR/DEIS proposes no mechanism of enforcing offsets: who would regulate the project’s use of water, who would manage the interaction between Sites water and water from Shasta, Oroville, Folsom and perhaps Trinity reservoirs, and how and against whom any requirements would be enforced.

There are other problems. A shift to winter-spring diversions and use of canal systems would potentially change groundwater recharge and use patterns in the Sacramento Valley. The project would compete for water available to the proposed WaterFix Twin Tunnels project in the Delta. Sites and WaterFix have their “sights” on the heretofore untouched tributary inflows that are also protected by Delta export OMR limits so the flows reach the Bay. There will be a big fight over this uncontrolled water that now makes up a significant portion of the Bay’s freshwater input in drier years. Both projects have claimed future benefits of the same pot of water.

Conclusion

There are potential benefits from Sites project’s main features to Central Valley fishes, including salmon, steelhead, sturgeon, smelt, and striped bass. Most of the benefits would result from switching the diversion time period of the two existing upper river diversions and Shasta reservoir releases to these diversions. The added new diversion and increase in winter diversions will at important times reduce Sacramento River flow and Bay-Delta inflow and outflow, harming fish in certain but sometimes hard to quantify amounts.

Past water developments in the Central Valley have overwhelmingly made conditions for fish worse. The Sites project proponents claim that their project will be different. These proponents have not done themselves, the public, or public policy any favors by relying on generalities and politics as the centerpieces of their efforts to advance their project. At this time, there are too many unknowns to meaningfully evaluate the possibility that benefits might outweigh the harm and justify the costs. In the meantime, it is a reasonable working presumption that the Sites project will worsen conditions for fish as well.

Figure 1. Proposed Sites Reservoir and associated infrastructure on west side of the Sacramento Valley.

Spring 2018 – Unusual at Best

Flow conditions into and through the Delta are creating an unintended adaptive management experiment this spring. The San Joaquin River is providing half of the 20,000 cfs of Delta inflow. Exports and other water diversions are each taking about 3000 cfs from the Delta, leaving 14,000 cfs for outflow to the Bay. The Delta has been free of salt (Collinsville has been fresh at 200 EC, but salt is now encroaching). These are good conditions for the Delta and the San Joaquin, but horrendous for the Sacramento. Such conditions are highly unusual.

The Bureau of Reclamation’s decision to save water in Shasta reservoir, combined with a low water level in Oroville Reservoir because of ongoing repairs, have led to poor flows and high water temperatures in the lower Sacramento River. Flow at Wilkins Slough on the Sacramento River above Feather River confluence has fallen to 4000 cfs (Figure 1). Flow in the Sacramento River at Verona, below Feather River confluence, is only 7000 cfs (Figure 2). Water temperatures have reached 60°F at Red Bluff and 70°F at Wilkins Slough. Water temperatures above 56°F are detrimental to spawning winter-run salmon near Red Bluff. Water temperatures above 65°F are detrimental to out-migrating juvenile salmon, steelhead, and sturgeon.

A recent increase in releases from Shasta Reservoir is accommodating agricultural diversion demand in the upper Sacramento River below Shasta (Figure 3), while flows decline in the lower river. The increase in the upper river has stimulated emigration of wild juvenile salmon from the upper river, as shown by increased catch at the Red Bluff screw traps (Figure 4). The problem is that two-thirds of river flow is being diverted for Sacramento Valley agriculture, and river temperature rises 10°F along the way. Sacramento River salmon that reach the Delta, along with other Central Valley wild and hatchery salmon, are subject to south Delta exports (Figures 5 and 6). Though south Delta exports have been reduced, their effect remains significant because of low Sacramento River inflow to the Delta.

As I have suggested in past posts, Shasta Reservoir releases should be increased or water diversions from the upper Sacramento River reduced by several thousand cfs, in order to increase lower river flows and reduce water temperatures to no higher than the state water quality standard of 68°F. If this action is not taken, we will simply be feeding most of the young salmon to the abundant stripers that thrive in warm water conditions between Redding and the Bay (Figure 7).

Figure 1. Sacramento River flow at Wilkins Slough in spring 2018.

Figure 2. Sacramento River flow at Verona in spring 2018.

Figure 3. Sacramento River flow below Shasta/Keswick dams in spring 2018.

Figure 4. Catch of juvenile salmon in screw traps, water temperature, river flow, and turbidity near Red Bluff in Sacramento River.

Figure 5. Juvenile Chinook salmon salvage at south Delta export facilities in spring 2018. Red circle outlines recent salvage of wild juvenile spring- and fall-run smolts.

Figure 6. Juvenile Chinook salmon salvage at south Delta export facilities in spring 2018.

Figure 7. Striper limits from late April 2018 guide trip on lower Sacramento River. Source: James Stone.

Sacramento River Salmon and Water Right Order 90-5

Operation of the Central Valley Project’s Shasta-Trinity Division is governed in part by the State Water Board’s Water Right Order (WRO) 90-5. Issued in 1990, this Order prescribes reasonable protection for Sacramento River salmon, steelhead, and sturgeon even under today’s conditions. The problem in recent years is that “requirements” are not being met by the Bureau of Reclamation.

Even in the past three non-drought years, including record wet 2017 and this year’s normal classification, Reclamation has not met requirements. This has caused significant impacts to salmon, steelhead, and sturgeon, which I have documented in prior posts. In the past three years, Reclamation has used its poor performance during the 2013-2015 drought and global warming as excuses to prioritize preserving water storage in Lake Shasta over meeting water temperature requirements for the Sacramento River under WRO 90-5. But while Reclamation has argued it must preserve Shasta Reservoir’s cold-water pool, Reclamation has maintained full deliveries to its Sacramento Valley contractors.

The State Board has a whole website dealing with the issue and problems dealing with Reclamation on the issue: (https://www.waterboards.ca.gov/waterrights/water_issues/programs/drought/sacramento_river/ ).

In a March 14, 2018 letter to Reclamation, the State Board’s Deputy Director for Water Rights wrote to Reclamation on compliance with WRO 90-5,1 stating:

As you know, Order 90-5 requires Reclamation to maintain a daily average temperature (DAT) of 56 degrees Fahrenheit (F) in the Sacramento River at Red Bluff Diversion Dam during times when higher temperatures will be detrimental to fish, unless factors beyond Reclamation’s reasonable control prevent it from maintaining such temperatures. If Reclamation is unable to meet the temperature requirement at Red Bluff Diversion Dam throughout the temperature control season, Reclamation must develop an operations plan for approval by the Chief of the State Water Board’s Division of Water Rights (Deputy Director). The plan, which is required to be developed in consultation with the California Department of Fish and Wildlife, U.S. Fish and Wildlife Service, National Marine Fisheries Service (NMFS) (collectively fisheries agencies), and the U.S. Western Area Power Administration (WAPA), must designate a location upstream of Red Bluff Diversion Dam where the temperature requirement will be met. Order 90-5 includes specific monitoring and reporting requirements in addition to a general requirement (Condition 3) that Reclamation conduct such monitoring and reporting as is required by the Deputy Director to ensure compliance with the terms and conditions of Order 90-5.

Given potential concerns with temperature management this year and the degraded status of the winter-run Chinook salmon population following the drought, Reclamation should be aware that operational changes may be needed beyond those proposed by Reclamation in their TMP to minimize impacts to winter-run Chinook salmon and avoid redirected impacts to other native species. Reclamation should acknowledge those needs in its TMP and provide for a process for continually evaluating conditions and operations to ensure that needed adjustments to temperature control operations are considered in a timely manner.

On April 2, 2018, Reclamation responded2:

This response not only states that Reclamation will not meet WRO 90-5 water temperature requirements at Red Bluff (river mile 243), but also that it will not meet these requirements at Balls Ferry (river mile 276), 30 miles upstream and half way to Keswick Dam. In fact, Reclamation to date has blatantly kept the promise of not meeting requirements (Figure 1), despite the fact that Shasta Reservoir is full of cold water. It is not even May yet!

The Coleman Fish Hatchery just stocked 4 million fall-run salmon hatchery smolts at Battle Creek upstream of Red Bluff, with another 2 million soon to follow.3 The recently released hatchery fish (and their wild counterparts) are being subjected to highly stressful conditions in their 200-mile journey to San Francisco Bay (Figures 2 and 3).

There is plenty of cold water in Shasta Reservoir (Figures 4 and 5) to meet the flow and temperature needs of salmon in the lower Sacramento River through the summer, as required by WRO 90-5. It would take a total release of about 6000 cfs from Shasta to meet WRO 90-5 requirements at this time just at Balls Ferry. Reclamation increased releases in the past several days to 5300 cfs to meet water contractor demands. The problem remains that this water is not reaching the lower river, where water temperatures now hit 70°F and exceed the WRO 90-5 limits of 68°F (Figure 3). It will take an added 2000-3000 cfs at Wilkins Slough to keep the lower river below its 68°F limit This added release would represent about one foot of Shasta Reservoir water-surface elevation per week (Figure 4).

Sacramento Valley contractors have been given a 100% water allocation. South of Delta San Joaquin CVP contractors have been allocated only 40%. Reclamation is fully capable of meeting WRO 90-5 requirements, as it did historically. It is up to the State Board to enforce the CVP permit requirements. Given the state of the salmon populations, there should be no compromise on the permit requirements.

Figure 1. Reclamation report on Sacramento River temperatures through 24 April, 2018. Source: https://www.usbr.gov/mp/cvo/vungvari/sactemprpt.pdf

Figure 2. Water temperature at Red Bluff (RM 243), April 2018. Red line is limit requirement in WRO 90-5. Source: cdec.

Figure 3. Water temperature at Wilkins Slough (RM 118) April 2018. WRO 90-5 limit is 68°F. Water temperatures in excess of 65°F are highly stressful to juvenile salmon. Source: cdec.

Figure 4. Shasta storage characterization for water at the dam’s temperature control device (TCD), March 23 – April 22, 2018. Source: https://www.usbr.gov/mp/cvo/vungvari/ShastaTCD2018.pdf (See link for updates.)

Figure 5. Shasta Reservoir storage as of April 24, 2018.
Source: http://cdec.water.ca.gov/resapp/ResDetail?resid=SHA

  1. https://www.waterboards.ca.gov/waterrights/water_issues/programs/drought/sacramento_river/docs/2018/03142018_sac_temp_plan_ltr.pdf
  2. https://www.waterboards.ca.gov/waterrights/water_issues/programs/drought/sacramento_river/docs/2018/04022018response_90_5.pdf
  3. Note that Coleman Fish Hatchery on Battle Creek normally stocks 12 million fall-run smolts, but brood year 2014 salmon did not provide sufficient spawners (eggs for hatchery), and the hatchery thus produced only 6 million smolts in 2017. Hopefully, the 2 million smolts that have not yet been released will be trucked to the Bay.

Miracle March/April for Water Supply and Fish

It has been a “Miracle March-April” for water supply and fish in the Central Valley. Over 2 million acre-feet of water was added to Central Valley storage reservoirs. Many major reservoirs reached flood capacity, with large releases and rivers spilling over into flood bypasses. The snowpack doubled to over 50% of average. Water year 2018 cumulative precipitation nearly doubled (remains 10 inches short of average at about 80% of normal).1 Water Year 2018 will likely stack up as “below normal,” not unlike 2010, 2012, or 2016.

Without the added precipitation so far this spring, water conditions would be similar to critically dry 2015. The prognosis for salmon, smelt, and sturgeon would be poor with yet another drought year. The fish have yet to recover from the 2012-2016 drought.

In the next three months, tens of millions of wild and hatchery juvenile salmon and steelhead will be leaving Valley rivers for the Delta, Bay, and ocean. Millions of young smelt and sturgeon will be trying to reach their Bay low salinity nurseries. Adult fall, winter, and spring run salmon and green and white sturgeon will be seeking their upriver spawning grounds. All of these populations are in real trouble and need help after years of stress.

Some of the Miracle March-April water added to Central Valley storage should be set aside for the fish. Fish need higher river flows and Delta outflow through summer than would normally be allocated in a sub-normal water year like this. Lower Sacramento River flows (Figure 1) should be kept near 8000 cfs, not the projected 5000-6000 cfs. San Joaquin River flows should be kept near 1000 cfs (Figure 2). The Delta outflow minimum should be 8000 cfs (Figure 3), not 5000 cfs, by allowing the added river flows to pass through the Delta. The “extra” water would amount to about a quarter of Mother Nature’s gift to the reservoir supply added so far this spring. That would seem more than reasonable and fair. In most cases it means meeting already prescribed flow and water temperature standards for the Central Valley rivers and Delta. These standards have been more than regularly ignored in recent years. So let’s do the fish a favor for once – call it “adaptive management” – and see if it helps.

Figure 1. Flow in lower Sacramento River at Wilkins Slough over past decade.

Figure 2. Flow in lower San Joaquin River at Vernalis over past decade.

Figure 3. Delta outflow at Pittsburg over past three years.

How do we increase salmon runs in 2018 and beyond?

Over the past few months, I wrote posts on the status of specific runs of salmon in rivers throughout the Central Valley. In this post, I describe the overall status of salmon runs and the general actions to take to increase both escapement and fish available for commercial and sport harvest.

It was just over a decade ago that there were nearly one million adult salmon ascending the rivers of the Central Valley (Figure 1). At the same time, there were a millions more Central Valley salmon being harvested each year in sport and commercial fisheries along the coast and rivers of the Central Valley. Improvements in salmon management in the decade of the 1990s by the Central Valley Project Improvement Act, CALFED, and other programs had paid off handsomely with strong runs from 1999 to 2005. New and upgraded hatcheries, along with trucking hatchery smolts to the Bay, significantly increased harvest and escapement to spawning rivers.

Figure 1. Central Valley salmon runs from 1975 to 2016 including fall, late fall, winter, and spring runs. Source of data: CDFW GrandTab.

By 2008-2009, escapement had fallen by over 90% to a mere 70,000 spawners of the four races of salmon.  Fishery harvests were greatly restricted by 2008.  The winter run, the most threatened of the four runs fell from 17,296 to 827 spawners in just five years.  Drier years from 2001-2005, poor ocean conditions in 2004-2005, record-high Delta water diversions, and the 2007-2009 drought were contributing factors in the declines.  Impacts to coastal communities and the fishing industries were severe.

Extraordinary recovery measures included closing fisheries and trucking most of the hatchery smolt production to the Bay or Delta.  Federal salmon biological opinions (2009, 2011) limited winter-spring water-project exports from the Delta.  Hundreds of millions of new dollars were spent on habitat and fish passage improvements in the Valley to increase salmon survival and turn around the declines in runs.  A look at Figure 1 indicates that these efforts proved effective in limiting run declines from the 2012-2015 drought compared to the 1987-1992 and 2007-2009 droughts.

However, the prognosis for the future is again bleak, especially for wild, naturally produced salmon.  The consequences of the 2012-2015 drought  have not fully played out.  Once again, projected runs are low, and harvests are likely to be restricted.  Actions are needed to minimize long-term effects and to help bring about recovery of wild salmon productivity and fisheries in general.

Actions for 2018:

  1. Reduce harvest: Sadly but necessarily, the Pacific Fisheries Management Council and states are likely to take this first step of– restricting the 2018 harvest in the ocean and rivers to protect wild runs.
  2. Improve spawning, rearing, and migrating conditions: Sadly, this past year’s rearing and migrating conditions in the Sacramento River were unnecessarily compromised.   Water temperature at Red Bluff reached above the 56oF prescribed in the biological opinion and Basin Plan.  The higher temperatures resulted from low Shasta Reservoir releases (less than 5000 cfs – Figure 2) despite a virtually full Shasta Reservoir.  The low flow and higher water temperatures likely affected salmon egg incubation, rearing, and emigration-immigration success.  Reservoir releases will be necessary to meet flow and temperature targets in all Central Valley rivers and the Delta.
  3. Limit Delta exports: Delta exports this past spring reached unprecedented highs not seen in recent decades, resulting in high salmon salvage rates at the Delta fish facilities (Figure 3).1 With high water supplies from this past wet water year 2017, there will be high exports again unless there are some constraints.  If anything, winter-spring exports should be reduced to allow salmon to recover.  April-May exports should be reduced, like they were in the 1990’s and 2000’s, to 1500 cfs.

Near term actions over the coming year:

  1. Transport hatchery smolts to Bay: The transport of millions of fall-run smolts from state hatcheries on the Feather, American, and Mokelumne rivers to the Bay provides higher rates of escapement and contributions to the fishery and low rates of straying.  Barge transport to the Bay offers potentially lower rates of predation and straying for federal hatcheries near Redding.
  2. Raise hatchery fry in natural habitats: Recent research indicates that rearing hatchery fry in more natural habitat conditions increases growth rates, survival, and contributions to escapement and fisheries.  Raising hatchery fry in rice fields is one potential approach.
  3. Restore habitats damaged by recent record high flows in salmon spawning and rearing reaches of the Central Valley rivers and floodplains: In nearly every river, habitats were damaged by the winter 2017 floods, requiring extraordinary repairs and maintenance to ready them again to produce salmon.
  4. Take further actions to enhance flows and water temperatures to enhance salmon survival throughout the Central Valley: Actions may include higher base flows, flow pulses, or simply meeting existing target flow and temperature goals.

In conclusion, managers should take immediate actions to minimize the damage to salmon runs from the recent drought and floods, using this past year’s abundant water supply.  They should avoid efforts to exploit the abundant water in storage for small benefits to water supply at the expense of salmon recovery, and should make every effort to use the water in storage for salmon recovery.

Figure 2. Upper Sacramento River flows and water temperatures in May 2017. The target water temperature for Red Bluff is 56oF. Source of data: USBR.

Figure 3. Export rate and young salmon salvage at South Delta federal and state export facilities in May 2017. The target export rate limit for May should be 1500 cfs. Source of data: USBR.