Category Archives: Bay-Delta

Napa River Smelt Sanctuary

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The Napa River and its estuary are an important spawning and rearing area for longfin and Delta smelt, especially in wet years. Wet years, with their high Delta outflows (Figure 1) and modest Napa River flows (Figure 2) provide spawning habitat for the smelt in the Napa River and its estuary (Figures 3-6).

Wet year 2019 shows use by longfin (Figure 3), but little use by Delta smelt (Figure 7), which likely reflects their low population abundance.

Because the smelt populations have strongest recruitment in wet years,1 the Napa River estuary likely is an important contributor to their overall population health and abundance. The Napa River estuary deserves more attention in smelt recovery strategies. However, that should not take away from improving upper Bay-Delta estuary habitat conditions in all water year types.

Figure 1. Delta outflow in recent wet years 2011, 2017, and 2019.

Figure 2. Napa River flows 2009-2019.

Figure 3. 20-mm Survey results for Longfin smelt March 2019. Source

Figure 4. 20-mm Survey results for Longfin smelt March 2017.

Figure 5. 20-mm Survey results for Delta smelt April 2011.

Figure 6. 20-mm Survey results for Delta smelt April 2017.

Figure 7. 20-mm Survey results for Delta smelt April 2019.

 

 

Why is Water Temperature in the Delta so important? Why there should be a water quality objective in the Delta for water temperature.

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The rivers flowing into the Delta are generally cool.  The Bay is generally cool.  But the Delta gets warm (>20oC, 68oF) from late spring into early fall.  Rivers have a water quality standard limit of 68oF.1 The Delta should too.

Salmon, smelt, and steelhead are cool water fish that use the Delta for major portions of their life cycle.  Water temperatures above 68oF are stressful, leading to poorer growth, higher predation, lower survival, and early exits from Delta critical habitats.  One reason for the stress is that warmer water holds less dissolved oxygen.  When water temperature exceeds 68oF, dissolved oxygen falls below 8 parts per thousand (ppt), which is stressful to fish.  In eutrophic (high organic loads with lots of aquatic plants) waters like the Delta, dissolved oxygen can get even lower, near the minimum state standards (6-7ppt), especially at night.

Delta waters are cooler in wet years because of higher flows and generally cooler spring air temperatures.  There is no doubt that low river inflows, higher exports, and low Delta outflows can exacerbate high Delta water temperatures, especially during hot periods of summer.  There is also plenty of evidence that higher inflows, lower exports, and higher outflows during exceptionally warm weather can help minimize high water temperatures.

Delta waters are cooler when inflows are higher and cooler.  The lower reaches of rivers that enter the Delta are cooler with higher flows.  Maintaining high river inflows with the associated cooler water helps maintain Delta water temperatures.  It takes approximately 20,000 cfs of Sacramento River inflow at Freeport to the Delta to maintain inflow water temperature near 68oF in summer (Figures 1-3).

The central Delta flow inputs are also cooler in late spring under higher Delta inflows, as exemplified by water temperature and flow comparisons between dry 2015 and wet 2011, 2017, and 2019 (Figures 4 and 5).  This comparison dispels the argument that that water temperature in the Delta is wholly dependent on air temperature and is not affected by flow.

There is evidence that increasing diversions and decreasing flows in warmer weather (Figures 1 and 3) increases water temperatures.  This is another reason to increase Delta river inflows during warm weather.  A Delta water temperature standard/objective would potentially require episodic higher Delta inflows to offset higher warm weather diversions, in addition to a sustained inflow near 20,000 cfs in summer.

Figure 1. Water temperature and Sacramento River flow in summer 2016.

Figure 2. Water temperature and Sacramento River flow in summer 2017.

Figure 3. Water temperature and Sacramento River flow in summer 2018.

Figure 4. Water temperature in late spring in Georgiana Slough 2011, 2015, 2017, 2019.

Figure 5. Daily average flow in late spring in Sacramento River at Freeport 2011, 2015, 2017, 2019

Winter Trawl Survey – Delta Smelt 2019 Adult Spawning Run Update

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A January 2, 2019 California Department of Fish and Wildlife (CDFW) memo relates that the fall midwater trawl index for Delta smelt was zero (none collected), though an attachment from the U.S. Fish and Wildlife Service (USFWS) shows that some Delta smelt were captured in late 2018 in non-index locations, as was the case in other recent years. The CDFW memo also relates that 5 smelt were captured in the December Kodiak Trawl Survey.

In an effort to update my last winter trawl post, April 2018, I present the winter survey results from 2002 through 2019 in the figure below. The 2018 and 2019 winter indices are consistent with the fall and summer surveys.

The fact that some Delta smelt remain in the Bay-Delta indicates that it might not be too late to save them from extinction, especially with hatchery supplementation. However, there has been no public description of CDFW’s or USFWS’s plan for Delta smelt recovery in 2019-2020. The present recovery plan for Delta smelt is dated 1996. USFWS should update the Delta smelt recovery plan immediately, and USFWS and CDFW should implement it. The State Water Resources Control Board’s effort to update Delta water quality standards should also include measures to recover smelt.

Chart of winter smelt survey results from 2002 through 2019

Improved Yolo Bypass Fish Passage

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Some salmon and sturgeon adults migrating up the Sacramento River this spring have had new help in passing upstream via the Yolo Bypass. With roughly half the Sacramento River’s flood waters flowing through the Yolo Bypass at the beginning of March, many salmon and sturgeon returning to the upper river to spawn likely chose entered the lower end of the Bypass at Rio Vista. These fish had a new notch opening to help them get over the Fremont Weir at the upper end of the 40-mile-long Bypass (Figure 1) and back into the Sacramento River to continue their journey.

The new $6-million gated-notch opening in the Fremont Weir is the first of several to be built into the two-mile-wide weir to help fish passage. The notches will allow an easier passage route over the weir, especially for large sturgeon. The notches are especially important in allowing an extended period for adult fish to finish their passage through the Bypass when Sacramento River water levels fall and the river flow ceases spilling over the weir into the Bypass. In the past, these conditions would have trapped any fish that remained in the Bypass. The notches will also help pass downstream-migrating juvenile salmon to enter the Yolo Bypass, where there is potential beneficial tidal and floodplain rearing habitat.

The first year of the new notch’s operation has not been without some glitches.1 Significant numbers of salmon and sturgeon have died and probably continue to die at the weir and in the Bypass.

But the new notch was not the underlying cause of this problem. The problem lies in flood control and reservoir storage management in the Central Valley. Drastic reductions in river flow and water levels led to fish stranding in the Bypass, the draining of the floodplain, and a rapid rise in water temperatures in the Bypass that stressed migrating fish.

  1. Shasta/Keswick reservoir releases were reduced sharply after two major flood releases this winter/spring (Figure 2).
  2. This led to abrupt ends to Fremont Weir overflows into the Yolo Bypass (Figure 3)
  3. The sharp drops in water levels in the river allowed only one week of extended Bypass inflows through the new notch (Figure 4).
  4. That led to a rapid draining of the Bypass (Figures 5 and 6).
  5. This in turn led to excessive water temperatures in the Bypass (Figure 7) for migrating and rearing salmon (>70oF).

For the new notches to be effective, an extended period of flow through the new notches will be needed to allow time for migrating and rearing salmon and sturgeon to safely exit the Yolo Bypass without being subjected to a sudden draining of warm water from the shallow margins of the Bypass. With a near record snowpack and filling reservoirs, there were sufficient river flows and reservoir storage this year to extend the duration of river flows into the Yolo Bypass.

Figure 1. New Fremont Weir gated notch to help fish passage between Yolo Bypass and Sacramento River.

Figure 1. New Fremont Weir gated notch to help fish passage between Yolo Bypass and Sacramento River.

Figure 2. Reservoir releases from Shasta/Keswick dams in winter-spring 2019.

Figure 2. Reservoir releases from Shasta/Keswick dams in winter-spring 2019.

Figure 3. Flow into Yolo Bypass from Sacramento River at Fremont Weir in winter-spring 2019.

Figure 3. Flow into Yolo Bypass from Sacramento River at Fremont Weir in winter-spring 2019.

Figure 4. Water elevation of Sacramento River at Fremont Weir in winter-spring 2019. Top of weir is at 32-ft elevation. Bottom of new notch is at 25-ft elevation. Extended operation of new notch would have occurred from April 22-28.

Figure 4. Water elevation of Sacramento River at Fremont Weir in winter-spring 2019. Top of weir is at 32-ft elevation. Bottom of new notch is at 25-ft elevation. Extended operation of new notch would have occurred from April 22-28.

Figure 5. Flow in upper Yolo Bypass in winter-spring 2019.

Figure 5. Flow in upper Yolo Bypass in winter-spring 2019.

Figure 6. Water elevation in mid Yolo Bypass during Bypass draining in last week of April 2019.

Figure 6. Water elevation in mid Yolo Bypass during Bypass draining in last week of April 2019.

Figure 7. Water temperature in mid Yolo Bypass at Lisbon Weir during Bypass draining in last week of April 2019.

Figure 7. Water temperature in mid Yolo Bypass at Lisbon Weir during Bypass draining in last week of April 2019.

 

South Delta Salmon Trap

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Unless there are high Delta inflows, south Delta export pumping creates a hydrologic “trap” for emigrating salmon and other Delta fishes. Even under moderate Delta inflows and outflows, as occurred in January 2019 (Figure 1), south Delta pumping traps salmon emigrating from both the Sacramento and San Joaquin river systems. This is because the pumps trap nearly all the water from the San Joaquin and about a third of the Sacramento River water the latter primarily via cross-Delta flow in Georgianna Slough (GS). In contrast, under high flows, the trap is confined only to the immediate area of the south Delta export pumps (Figure 2).

Susceptibility to the “trap” for Sacramento salmon under moderate early winter Delta flows is evident from the collection of smolts from the Coleman fish hatchery at south Delta fish salvage facilities (Figure 3, blue and green dots). Susceptibility of San Joaquin salmon smolts under moderate and high flows is evident from San Joaquin hatchery smolts salvage (Figure 3, orange dots).

Lower export limits in winter-spring since 2009 have helped to minimize the frequency of conditions in which salmon become trapped in the south Delta. Exports and salmon salvage are 30-50 % lower than pre-2009 levels, and sometimes lower still. However, political forces may eliminate these export restrictions and greatly increase the trapping of salmon in the south Delta. This would further limit the potential for salmon recovery in the Central Valley.

The State Water Board’s ongoing process of setting new Delta water quality standards should adopt more stringent measures to minimize the trapping of salmon in the south Delta. Such measures should include further restrictions on exports and increased flows in the lower San Joaquin River. Other options include:

  1. Constructing a barrier or fish screen at the head of Old River;
  2. Opening the Delta Cross Channel to increase net downstream flows in the lower San Joaquin channel within the Delta; and
  3. Increasing Delta outflow.

Figure 1. Delta hydrology 1-15-19. Red arrows denote negative or upstream flows. SR = Sac River. JPT = Jersey Point. GS = Georgianna Sl. MOK = Mokelumne River. DS and FR = Dutch Sl and False River. PPT = Prisoners Pt. OMR = Old and Middle Rivers.

 

Figure 2. Delta hydrology 3-15-19. Red arrows denote negative or upstream flows. SR = Sac River. JPT = Jersey Point. GS = Georgianna Sl. DS and FR = Dutch Sl and False River. PPT = Prisoners Pt. OMR = Old and Middle Rivers.

Figure 3. Salmon salvage in winter-spring 2019. Colored dots represent specific hatchery release groups noted by date of release along top margin of chart. River and Delta flows and exports (SWP+CVP) are shown in bottom chart.