It is Too Early to Turn On the Delta Pumps

Delta export pumping has increased, jeopardizing endangered Winter Run salmon and Delta smelt. Yes, there is a lot of fresh water (and young salmon) pouring into and through the Delta from the recent storms. Delta outflow has risen from 5000 cfs to 22,700 cfs this month (Figure 1). So the state has started pumping more from the south Delta. State exports have risen from 500 cfs on 12/21 to 4000 on 12/23.

The problem is that the Low Salinity Zone (LSZ, 500-10,000 EC1) so critical to the Delta ecology has yet to be flushed west, out of the Delta. Turning up the pumps has actually increased the concentration of salt in export water (Figure 2) by pulling LSZ water from the north and west into the central and south Delta (Figure 3). Smelt and salmon concentrate in this zone. The LSZ has moved west from Rio Vista in the north Delta on the Sacramento River (Figure 4), but not from the west and central Delta on the San Joaquin side (Figure 5). Export pumps in the south Delta are pulling LSZ waters from the San Joaquin channel through False River and Dutch Slough (Figure 6).

Remnants of the Delta smelt population are in the central Delta.2 Winter Run salmon smolts began showing up at the export fish facilities in Clifton Court on 12/23. Both occurrences should be a stern warning, given the present poor state of these two endangered fish populations. Closure of the Delta Cross Channel earlier in December to protect migrating salmon actually aggravated the problem by limiting flushing of the central and west Delta and by trapping salmon and smelt in the central Delta. Exports should not be increased until the LSZ is west of Jersey Point. The Delta Cross Channel should remain open until the LSZ is west of Jersey Point. It is better for everyone if exports are pumping fresh water (

Graph of Delta outflow 2015

Figure 1. Delta outflow in December 2015.

Graph showing Electrical Conductivity at Clifton Court

Figure 2. EC of water exported from Clifton Court Forebay in south Delta in December 2015.

Map of flows

Figure 3. Aerial photo of Delta showing high Delta freshwater inflow and outflow from Sacramento River (blue arrow) and South Delta exports pulling brackish Low Salinity Zone water from central and west Delta San Joaquin channel to south Delta export pumps at Clifton Court Forebay (center bottom). The two eastward red arrows represent the False River (upper arrow) and Dutch Slough connections.

Graph of electrical conductivity at Rio Vista

Figure 4. EC at Rio Vista in north Delta on Sacramento River 12/19-12/26, 2015.

Graph of electrical conductivity at Jersey Point

Figure 5. EC at Jersey Point in the western Delta on San Joaquin River 12/19-12/26, 2015.

Graph of electrical conductivity at Dutch Slough

Figure 6. EC at Dutch Slough between the west and central Delta 12/19-12/26 2015. Note spike on 12/23 when south Delta exports were increased to 4000 cfs.

  1. EC is electrical conductivity expressed as microsiemens
  2. http://calsport.org/fisheriesblog/?p=570

NMFS on Salmon and the Drought, Part 2

As noted in the first blog of this series, the National Marine Fisheries Service (NMFS) is responsible under the Endangered Species Act for protecting the endangered Winter Run Chinook salmon of the Sacramento River. But when the US Bureau of Reclamation (USBR or Bureau) and the Department of Water Resources (DWR) have asked NMFS to comment on proposed changes in Central Valley Project operations during the present four-year drought, NMFS has consistently concurred, often going against its own previous prescriptions and advice. As a consequence, the Winter Run salmon were put at great risk, decimating the 2014 and 2015 year classes and again placing the population at the brink of extinction.

April 8, 2014 Drought Operations Plan

On April 8, 2014, the Bureau and DWR issued a 2014 Drought Operations Plan, in which they proposed low releases in the Sacramento River in April and May:

Keswick releases will be held to no greater than 3,250 cfs, or as determined necessary to reasonably target no more than 4,000 cfs at Wilkins Slough, unless necessary to meet nondiscretionary obligations or legal requirements;

The critical phrase here is “nondiscretionary obligations.” It is the view of NMFS, as described in its Biological Opinion for the Operation of the State Water Project and Central Valley Project, that the Bureau of Reclamation does not have the discretion to release less water to Sacramento River Settlement Contractors than 75% of contracted amounts. Thus, low April and May flows called for in the 2014 Drought Operations Plan were overwhelmed by calls for water by the Settlement Contractors.

April 8, 2014 NMFS Letter on Sacramento River Water Temperature Management

On April 8, 2014, NMFS wrote a letter1 to the Bureau and DWR in response to their April 8, 2014 Drought Operations Plan. In that letter, NMFS concurred with the Plan, but highlighted a concern regarding deliveries to the Settlement Contractors:

“Winter-run Chinook salmon viability and Sacramento Settlement Contractor deliveries: Reclamation is working with Sacramento River Settlement Contractors on options to shift a significant portion of their diversions this year out of the April and May period and into the time frame where Keswick releases are higher to achieve temperature objectives on the upper Sacramento River. The willingness and cooperation of the settlement contractors in this effort would allow a modified diversion pattern and create the benefit of increased Shasta Reservoir storage at the beginning of the temperature control operations and increased availability of water to these senior water rights holders in this critically-dry year. This deferral of irrigation would allow implementation closer to the lower range of the Keswick release schedule for April and May, as identified in Section V of the DOP (Drought Operations Plan).

Thus the agencies and the Settlement Contractors were left to work out on a voluntary basis a mechanism to keep enough cold water in Lake Shasta to protect Winter Run salmon throughout the summer and fall. The State Water Board approved the Plan.

It didn’t work. Though releases from Shasta in April, 2014 were low, the Bureau ramped up releases from Shasta to the Settlement Contractors in early May (Figures 1 and 2), and cold water in Lake Shasta was depleted by the end of August.

Graph of May 2014 releases from Keswick

Figure 1. May 2014 releases from Keswick to the Settlement Contractors were far above those advised by NMFS (

Graph of releases May 2014

Figure 2. May 2014 releases from Keswick to the Sacramento River were diverted by Settlement Contractors upstream of the Delta. Contrast flow at Wilkins Slough (~25 miles north of Woodland) with releases from Keswick in Figure 1: most flow increases over the month were diverted north of the Delta.

January 29, 2015 Letter on Sacramento River Water Temperature Management

On January 29, 2015, NMFS wrote a letter to the Bureau and DWR in response to a new January Temporary Urgency Change Petition (TUCP) to the State Board.2 In its January 29, 2015 letter, NMFS’s acknowledged lessons from 2014 regarding water temperature:

Temperature management is critical. Salmon rely on cold water, particularly during early life stages when fish are young and vulnerable. Shasta and Keswick dams block endangered winter-run Chinook from accessing their native cold water habitat in the Upper Sacramento and McCloud Rivers, so their eggs and fry are particularly vulnerable to high summer temperatures. Data from the Sacramento River indicate 2014 temperatures were at levels that impact the survival of juvenile salmon and steelhead. We found that the 2014 temperature criterion was exceeded starting in August, resulting in approximately 95% mortality of eggs and fry upstream of Red Bluff Diversion Dam. As of December 16, 2014, an estimated 390,000 juvenile winter-run Chinook salmon passed Red Bluff, compared to 1.8 million in the previous brood year and 850,000 in brood year 2011, the year of the winter-run collapse (see Nov. 18 USFWS/CDFW/NOAA Fisheries presentation to State Water Board). This is the fewest winter-run Chinook juveniles per female spawner passing Red Bluff in 11 years.

March 27, 2015 Letter

However, by the end of March, 2015, NMFS was once again tiptoeing through a proposal by the Bureau to repeat the previous year’s disaster. On March 27, 2015 NMFS once again concurred with the proposed TUCP, even while highlighting the “conflict” between Winter Run salmon and deliveries to the Settlement Contractors. 3

The Project Description meets all of the required aspects of the contingency plan required in Action I.2.3 .C, as follows:

  • Reclamation has provided an assessment of additional technological or operational measures that can increase the ability to manage the cold water pool.
  • Reclamation notified the State Board, through filing the TUC Petition, that meeting the biological needs of winter-run and the needs of resident species in the Delta, delivery of water to nondiscretionary Sacramento Settlement Contractors, and Delta outflow requirements per D-1641 , may be in conflict in the coming season.
  • In conclusion, NMFS concurs that Reclamation’s Project Description is consistent with Action I.2.3.C and meets the specified criteria for a contingency plan. … Furthermore, the best available scientific and commercial data indicate that implementation of the interim contingency plan will not exceed levels of take anticipated for implementation of the RPA specified in the CVP/SWP Opinion.

And once again in 2015, no one stepped up to maintain cold water in Shasta Reservoir in April and May (Figure 3).

Graph of 2015 releases

Figure 3. In 2015, releases to the Settlement Contractors ramped up in April and were high throughout May.

July 1 Letter4

By July 1, 2015, NMFS was already issuing a post-mortem.

“NMFS acknowledges that storage in Shasta Reservoir at the beginning of the temperature management season in June, and the quantity and quality of the cold water pool, will not provide for suitable winter-run habitat needs throughout their egg and alevin incubation and fry rearing periods.”

Final Comment

We should expect more from the federal agency mandated to protect our endangered salmon. At a minimum, NMFS should have not concurred, in 2015 (or in 2014, for that matter), and should have called out the fact that added take of Winter Run would occur, further jeopardizing the viability of the species through direct mortality and degradation of their critical habitat.

Regardless of the legal merit of NMFS’s position that it does not have authority under the Endangered Act to limit deliveries to the Settlement Contractors, its failure to defend listed Winter Run gave cover to the Agency that has that authority: the State Water Board. CSPA, the Bay Institute and others asked the State Water Board in February, 2015 and again in the spring to reduce 2015 deliveries to the Sacramento Valley Settlement Contractors to save the Winter Run (and to protect Delta smelt). In an Order denying Petitions for Reconsideration of the 2015 TUCP’s filed by CSPA and others, the State Water Board offered the rationale:

However, at the time the changes were approved, the tradeoff appeared to be reasonable based on the information available at the time, including biological reviews from DWR and Reclamation and concurrence from the National Marine Fisheries Service (NMFS), U.S. Fish and Wildlife Service (USFWS), and California Department of Fish and Wildlife (DFW) (collectively fisheries agencies) with the changes. For these reasons, the petitions for reconsideration of the past Executive Director actions are denied. 5

NMFS on Salmon and the Drought, Part 1

The National Marine Fisheries Service (NMFS) is responsible under the Endangered Species Act for protecting the endangered Winter Run Chinook salmon of the Sacramento River. But when the US Bureau of Reclamation (USBR or Bureau) and the Department of Water Resources (DWR) have asked NMFS to comment on proposed changes in Central Valley Project operations during the present four-year drought, NMFS has consistently concurred, often going against its own previous prescriptions and advice. As a consequence, the Winter Run salmon were put at great risk, decimating the 2014 and 2015 year classes and again placing the population at the brink of extinction.

January 29, 2015 Letter on Old and Middle River Flows

On January 29, 2015, NMFS wrote a letter in response to the Bureau and DWR’s January Temporary Urgency Change Petition (TUCP) to the State Board.1 The Petition asked the State Board to weaken State water quality standards. NMFS stated:

Here’s what we learned from monitoring salmon in 2014 that will inform our strategies for managing the drought in 2015:

1. Managing Old and Middle River (OMR) flow regimes to protect salmon is critically important. Effectively managing flow regimes allows juveniles to stay in the best habitat in the North Delta, ensuring they are not drawn toward the South Delta pumps where they are frequently killed by predators or the pumps themselves. During a rare rainstorm last March, and under a flexible operation approved as part of the 2014 Drought Contingency Plan, we allowed for higher levels of pumping and reverse OMR flows.  Evaluating the effects of the action this fall, we learned that salvage and loss of juvenile Chinook salmon, including winter-run, at the federal and state fish collection facilities increased when OMR’s 14-day running average was more negative than -5,000 cfs. This confirms the importance of managing OMR flows carefully to ensure pumping is increased when it will be most effective for increasing water supply and least impactful to juvenile fish.

Regardless of whatever NMFS had learned from events in 2014, NMFS had already ignored these lessons in December 2014 when it allowed OMRs to significantly exceed the -5000 cfs limit (Figure 1). NMFS then acquiesced to high reverse flows in the 2015 Drought Operations Plan: “OMR shall be no more negative than -5,000 cfs as a 14-day running average, and no more negative than -6,250 cfs as a 5-day running average, except as needed to capture sporadic storms (increase exports).”

The first winter storms usually trigger emigration of juvenile Winter Run and Late Fall Run Chinook salmon into and through the Delta (Figure 2). The only time during a drought that operators can achieve the highly negative OMR levels is in sporadic storms. Since those are precisely the conditions under which emigrating salmon pass through the Delta, the highly negative OMR flows put migrating juvenile salmon at great risk.

Figure 1. Old and Middle River flows in December 2014. Negative or reverse flows are caused by South Delta Exports, which reached over 10,000 during the second week of December 2014. (Data source: CDEC)

Figure 1. Old and Middle River flows in December 2014. Negative or reverse flows are caused by South Delta Exports, which reached over 10,000 during the second week of December 2014. (Data source: CDEC)

Graph of Occurrence of juvenile salmon

Figure 2. Occurrence of juvenile salmon in winter 2004 in seines and trawls near Sacramento at entrance to tidal Delta. Other years have shown a similar pattern. (Source: http://www.science.calwater.ca.gov/pdf/ewa/ support_docs_110804/Salmon%20Criteria%20Figures%201_2_Chappell.pdf )

Some Delta Smelt Back in the Delta

The US Fish and Wildlife Service’s early winter survey1 recently detected the first adult Delta Smelt of the water year in the Delta at Jersey Point on the lower San Joaquin River (Figure 1). The number collected in the survey through December 15th is 3, compared to 26 for the same period last year. Their appearance is on schedule and likely related to the first storm flow of the winter (Figures 2 and 3), and the freshening of the Delta (Figure 4).

Table of Smelt Count

Figure 1. Catch of adult Delta Smelt in early warning survey at two lower San Joaquin River stations in December 2015.

Graph of Delta freshwater outflow in December 2015

Figure 2. Delta freshwater outflow in December 2015. (Source: CDEC)

Graph of Turbidity of water at Jersey Point in December 2015

Figure 3. Turbidity of water at Jersey Pt in December 2015. (Source: CDEC)

Graph of Salinity (EC) at Jersey Point in December 2015

Figure 4. Salinity (EC) at Jersey Pt in December 2015. (Source: CDEC)

Saving Wild Salmon in Dry Years

I support a radical measure for saving wild salmon production in dry years in some Central Valley rivers under special circumstances: capturing wild juvenile salmon in rivers and transporting them to the Bay. This strategy has been employed in dry years on the Columbia River system, and by East Bay Municipal Utility District (EBMUD) in the present drought on the lower Mokelumne River. Under existing conditions in dry years, over 80% of Central Valley salmon fry, parr, and smolts are lost between spawning grounds and their San Francisco Bay target summer nursery. Without natural winter and spring pulse flows, few young wild salmon are able to navigate and survive to the Bay. Much of the production is lost in winter at the fry stage, which is the natural stage for Central Valley spring-run and fall-run Chinook to migrate to the Bay. Less but still important production is lost during the spring fingerling, pre-smolt, and smolt migration stages. In contrast, the hatcheries bypass the many river and Delta sources of mortality by rearing fry in raceways and trucking smolts to the Bay. It’s no wonder 90% of the salmon along the coast are from hatcheries.

Both practices (transport of hatchery and wild juveniles) should only be used in drier years, when there are minimal winter-spring river flows to naturally transport salmon. However, in drought years when reservoir inflows are low, transporting young salmon to the Bay may be necessary. Millions of wild, naturally-produced fry, parr, and smolts could be saved in each of the Central Valley spawning rivers. Huge numbers of young wild salmon are produced even in drought years in rivers such as the Yuba, American, Mokelumne, and Stanislaus that might otherwise be wasted when the Sacramento and San Joaquin rivers trickle into and through the Delta.

The process of trapping and hauling young salmon was perfected on the Columbia River in recent decades1. Capture of young salmon in the rivers at dams and water diversions is feasible and cost-effective. Many wild salmon fry can be captured at large fish screened diversions with fish bypasses (e.g., Daguerre Dam on Yuba River; GCID diversion on Sacramento River). Young salmon can also be captured in rivers below spawning reaches. For example, on the American River at Watt Avenue and the Yuba River at Hallwood Avenue, there are ideal locations with existing screw traps for indexing young salmon production that could be expanded to capture most of the production in low-flow conditions.

I have seen such bank-to-bank capture systems in Alaska on large very popular fishing rivers. The traps and supporting infrastructure are readily available. Peak trap catch of wild salmon is February-March, when hatchery transport trucks are largely unused, waiting for April-May hatchery transport season ().

Barging from the lower rivers to the Bay in lieu of trucking would help minimize subsequent straying of adults. Sacramento Valley salmon can be “barged” from Knights Landing; Feather-Yuba River salmon from Verona; and American River salmon from Discovery Park.

For more on trap capture systems including the Alaska examples see the following sources:
http://www.sf.adfg.state.ak.us/FedAidPDFs/FRED.011.pdf
http://www.adfg.alaska.gov/static/home/library/PDFs/afrb/toddv1n2.pdf
https://redoubtreporter.wordpress.com/2010/06/30/one-fish-two-fish-red-fish-new-fish-—-smolt-project-monitors-kasilof-river/
http://www.stateofthesalmon.org/fieldprotocols/downloads/SFPH_p8.pdf

trap capture system

  1. Many of the mainstem dams on the Columbia have been retrofitted with smolt capture systems. Captured fish are passed safely downstream around turbines or barged-trucked to the estuary.