Science Perspectives – 2016

The Bay-Delta Science Conference held this past November focused on the topic of “Science for Solutions: Linking Data and Decisions”. There were a diversity of subjects and presentations on the topic. A special series of papers previewed the conference presentations in the San Francisco Estuary and Watershed Science (UC Davis). The conference presentations and journal articles were a lot to take in.

My take on the conference and associated journal articles is that they represent a continuation of a decades-long attempt to avoid and direct focus away from the root cause of the Bay-Delta ecosystem’s greatest problems: high Delta exports, low river flows to the Delta, and low Delta outflows to the Bay under past and present water management. Simply put, there was a lot of the “same-old, same-old” mix of perspectives (excuses), with some new and interesting science.

A previous post covered the conference paper on Delta smelt. Another covered introductory presentations. In this post I focus on one presentation and paper entitled Perspectives on Bay-Delta Science and Policy, a summary of the conference prepared by its sponsor’s (the Delta Stewardship Council) Independent Science Board.

PERSPECTIVES

“Perspectives” focuses on seven themes the Independent Science Board has grown to accept as the causes of the Bay-Delta problems (Figure 1):

  1. Nutrients – Changes in and lack of nutrients are now considered important.
  2. Contaminants – Delta waters are now considered contaminated.
  3. Food Webs – Much less able to support fish than in the past.
  4. Multiple Stressors – Multiple stressors work together to cause the decline in Delta native fishes.
  5. Storms and Droughts Extremes – Extremes in drought and floods wreck havoc on water management.
  6. Landscape Ecology – Restoration has not been pursued on a landscape scale.
  7. Dire Straits of Endangered Species – Regime shifts and climate change have contributed to accelerated spiraling declines in native fishes.

Even if the underlying science on the subjects (factors) is valid, the arguments that relate these factors to the Bay-Delta ecosystem decline are not. At most, these factors are secondary actors in the overall process driven primarily by water management, Central Valley and Bay-Delta water quality standards, and endangered fish “protections in biological opinions.

The focus on these perspectives represents an overall intent to misinform and misdirect science and management away from real causes and effects, and from effective solutions to the Delta’s problems. Some topic examples:

  • “In the past we considered nutrients to be relatively unimportant in Delta productivity.” Untrue. The loss of nutrients that went along with water quality improvement over the past half century were always a concern. Sewage treatment upgrades were considered a factor in declines in Delta fish production. Aerial fertilization of the Delta was considered at least two decades ago.
  • “The low salinity zone, once a food-rich region of the Delta, now provides little food for native fish.” This statement is untrue. The LSZ remains the key rearing area of the Central Valley for smelt, salmon, sturgeon, and splittail, because it has the highest concentrations of “food” in the Bay-Delta Estuary.
  • “Aquatic food webs no longer sustain native fishes.” Untrue. Native fish are sustained if given a chance. Smelt and salmon were nearly recovered in 2000 after six wet years and massive recovery efforts and new protections. The protections simply failed to carry over into dry sequences 01-05, 07-10, and 12-16. Poor food, growth, and survival are caused by man-made drought conditions, and lack of protections of the pelagic food web of the Bay-Delta in drier years.
  • “There are few instances in which a single stressor can be identified as the primary cause of any species’ declines.” Untrue. River flow and exports are often the single most important factors in single events, such as winter-run salmon year-class failures below Shasta.
  • “Effective conservation requires a holistic approach.” Yes, one that does not take most of the fresh water from the rivers, Delta, and Bay.
  • “The aquatic ecosystem has gone through a regime shift that cannot be reversed.” Untrue. Taking most of the water out of the estuary from late winter through fall every year keeps the aquatic ecosystem in a semi-permanent drought, broken only by wet water years when large amounts of unregulated water escape capture by water managers. The patterns of the 2010-2011 water years show that negative patterns can be reversed.
  • “The problems have been caused by invasive clam and aquatic plants, and other non-native animals of the Bay-Delta foodweb.” Untrue. These are for the most part secondary responses to the real cause: greater exports and low river flows.
  • “More frequent and extreme storms and droughts will occur.” Four of last five, seven of last ten, and ten of last sixteen years have been part of drought sequences. From 1987 through 1996, seven of ten years were drought years. Water year 2017, though extreme, is not unlike previous very wet years.
  • “Habitat restoration has cascading effects.” In truth, restoration has as yet been minimal, with minimal evidence that it contributes substantial beneficial effects.
  • “The ecological regime shift and climate change are accelerating decline of native species.” While climate change certainly is not helping, the declines of native species are for the most part avoidable by reducing demands on water. The most important “regime shifts” of the last several decades have been shifts in water management strategies.

FORWARD-THINKING ACTIONS

The Independent Science Board’s editorial board extracted the following forward-thinking actions from their 2016 Perspectives paper:

  1. Incorporate long-range (50 year) thinking into Delta science and management. Acknowledge the accelerating rates of change ahead, and the inability to return to past conditions, in evaluating and planning feasible options for the future. Long-term planning is generally a good idea, but this formulation ignores current reality and the need to (1) return to past levels of protection, and (2) be wary of water management strategies that would further undermine the Bay-Delta ecosystem.
  2. Incorporate more exploratory and forward-looking science into government science programs at all levels, including science not tied to any current policy or crisis. Start planning now for about 15% of the overall Delta science budget to transition into more forward-thinking science. More science is not the answer. More science is more smoke.
  3. Widen science career paths in state agencies so that scientists are not forced to abandon science to advance their careers. More scientists are needed in management to apply the science that is already available.
  4. Plan for variability and extremes in the decades ahead, as well as long-term change. Bolster the ecosystem’s capacity to absorb both drought and deluge by continuing to reduce the state’s demand for water supply from the Delta, as required by the Delta Reform Act of 2009. Replenish Central Valley groundwater reservoirs and promote agricultural practices more resilient to drought. Adjust water management practices to accommodate less predictable sources of supply and more variable flows. Sound advice.
  5. Adapt management practices to take advantage of any ecological, recreational, and economic values to be gained. Yes, take advantage of low cost, high benefit practices.
  6. Begin the scientific and societal groundwork needed to seriously explore alternatives to conservation in place for endangered species. Continue all reasonable efforts to provide for them, including reducing water demand on the Delta, but recognize that the time has come to develop the science and policy foundations for more radical approaches, including assisted relocation, assisted evolution, and cryopreservation. There is also a need to enhance and build conservation hatcheries. But most of all, we need to protect and enhance the resources we have left.
  7. Invest now to develop models of the Delta system, analogous to global climate models, that more fully integrate physical, ecological, and social sciences. Use these models to forecast likely outcomes from changing climate and other external forces acting on the Delta, as well as likely effects of various management policies. Math models of complex ecosystem function are unnecessary – simpler conceptual and statistical (data) models are more realistic and better management tools.
  8. Weave “Delta as an Evolving Place” into all science, planning and management programs. Stop allowing further “evolving” and start de-volving where reasonable. The Bay-Delta is not really evolving; it is just ever-increasingly being disturbed.

Rethinking the above perspectives and actions would be a reasonable first step toward a more progressive strategy for the Delta Science Board.

Figure 1. Perspectives on Bay-Delta Science and Policy. (Independent Science Board)

Juvenile Salmon Survival in the Delta

At its November 2016 Bay-Delta Science Conference, the Delta Science Program addressed salmon survival in the Delta..

The focus of this post is:

PART 1: EFFECTS OF WATER PROJECT OPERATIONS ON JUVENILE SALMON SURVIVAL IN THE DELTA: LITERATURE AND DATA REVIEW. Presenter: Dr. Rebecca Buchanan, Research Scientist with the University of Washington.

The presentation was summarized in Mavens Notebook. Some of the findings are provided with comment below.

“While water export operations contribute to salmonid mortality by way of direct mortality at facilities, this does not account for the majority of the mortality of salmon in the Delta; and the contribution of various stressors to the high mortality is unknown.”

Comment: the contribution of low flows and associated predation and high water temperatures are known, as are effects of hindering migrations of salmon both upstream and downstream. The finding does not take into account salvage inefficiency, especially from Clifton Court Forebay pre-salvage loss, and loss in the south Delta from diverting these fish from their migration routes.

“There’s been some moderate evidence of a positive association between exports and survival through the Delta, based on Delta and ocean recoveries of wire tag data.”

Comment: There is no such evidence. The association is simply between high natural production and/or high hatchery releases on the one hand, and high salvage rates on the other.

“The E:I ratio is found to be useful in a stage-structured life cycle model by Cunningham; they did not find it to be useful for other runs of fish, however,” she said. “Newman and Rice found a small effect, but it was not statistically significant for fall run using code wire tag data.”

Comment: the E:I ratio does not reflect the role of the individual factors in the presence of the other. For example, the low-export/low-inflow scenario is a far different than a high-export/higher-inflow scenario with the same E:I ratio.

“Our primary finding was that salmon survival in the South Delta is low, which is not a big surprise; we knew it was low, but what was somewhat surprising is just how low it is and how consistently low it has been, especially for the San Joaquin fall run chinook”.

Comment: The low survival through the Delta has long been known from tag studies and low run size resulting from dry years, especially in the San Joaquin watershed. Low flows have long been associated with poor habitat conditions and high salvage losses in the Delta.

“Insufficient data on survival in Delta for steelhead, Sacramento River Chinook (all runs).”

Comment: There is a tremendous amount of data on the role of the Delta in the overall production of salmon in the Central Valley. Much of the analyzed effects points to droughts, low reservoir releases, low river flows, low Delta inflows and outflows, and direct and indirect effects of Delta exports. There is sufficient information to support and warrant OMR (exports restrictions) from fall through spring in NMFS’s biological opinion. There is also sufficient information to show that the restrictions do work, an analysis that was not conducted in the study.

“The tag studies that we have available to us represent only part of the life histories in populations that use the Delta, smelt-sized hatchery fish, so we’re missing the smaller fish and we’re missing the wild fish”.

Comment: This is true. Tagging/release of springtime fall run smolts represents a limited fall run life history group forced to navigate the Delta later than they would in the wild. At minimum, a majority of emigrants would naturally leave earlier.

“I haven’t been talking about mechanisms that might explain indirect effects of water project operations on mortality in the Delta, but we did identify some possible mechanisms, and we didn’t find much research on that, so there’s a need for some work there.”

Comment: Indirect effects include water temperature effects, flow effects, habitat effects (e.g., location of X2), predators, etc. There has been much research on these effects, including substantial research on salmon.

“Formal analysis of relationships between inflow, exports, I:E and survival is incomplete for existing data, especially on the San Joaquin.”

Comment: Formal analyses have been conducted over the past half century. All these analyses have led to the same conclusion: salmon survival is low when through-Delta flows are low, when exports are high, and when salmon salvage is high.

“Even when we have those analyses done, there will still be some constraints on our understanding. One, all of the observations that we have are in the presence of the management operations, which is understandable, but it does make it difficult to assess their effectiveness because we’re lacking control and we’re lacking variability in the conditions; without that variability, it’s very difficult to identify a relationship. We also don’t have very many observations at higher levels of exports or inflow. The low overall survival makes it difficult to detect changes in survival because of low effect of sample sizes and the high uncertainty in the results.”

Comment: Again, the available information and analyses are extensive. The range of observed conditions is wide. The range of survival and recruitment into the populations is also wide. These statements are little more than excuses offered to sustain additional decades of the present review process that is reluctant to state conclusions and even more reluctant to take appropriate management action. There has been minimal analysis that highlights the beneficial effects of actions required in the 2009/11 Biological Opinion. The requirements of the Biological Opinion led to significant reductions in winter exports. These reductions have had a marked positive effect on the survival of salmon through the Delta.

Fundamental Needs of Central Valley Fishes – Part 1d: Summer River, Delta, and Bay Freshwater Flows

In the coming months and years, regulatory processes involving water rights, water quality, and endangered species will determine the future of Central Valley fishes.

To protect and enhance these fish populations, these processes will need to address four fundamental needs:

  1. River Flows
  2. River Water Temperatures
  3. Delta Outflow, Salinity, and Water Temperature
  4. Valley Flood Bypasses

In this post, I summarize a portion of the issues relating to River Flows: Summer Flows. Previous posts covered fall, winter, and spring flows.

Summer flows have long been neglected in water management and water quality standards. This absence is a major factor in the decline of salmon, steelhead, sturgeon, Delta smelt, and other Delta native fishes.

Summer River Flows

River flows in summer drive many natural ecological processes in the Central Valley related to reservoir tailwater spawning, egg incubation, and over-summer rearing in Valley rivers. Valley rim dam releases are prescribed to meet these needs as well as water supply demands. All four salmon runs, steelhead, Pacific lamprey, and white and green sturgeon are dependent on river flows in summer. Below Shasta Reservoir on the Sacramento River, flow is necessary to sustain (1) salmon eggs/embryos, fry, fingerlings, and smolts of winter-run salmon, (2) juvenile fall-run, spring-run, and late-fall-run salmon; (3) juvenile steelhead, and (4) newly hatched fry of green and white sturgeon. Below Oroville and Folsom reservoirs, flow is needed to sustain juvenile steelhead as well as numerous over-summering smolts and pre-spawn adults of both spring-run and fall-run salmon. The Sacramento and San Joaquin Basin Plan (Central Valley Basin Plan) prescribes water quality objectives to protect these beneficial uses. The applicable key water quality objectives are for water temperature and streamflow.

During the dry summer season, much of the Central Valley and Bay-Delta water supply and environmental needs depend on water releases from storage reservoirs. Reaches above the reservoirs and non-dammed streams depend on springs and snowmelt. Like spring-run salmon in un-dammed tributaries, spring-run adults downstream of rim dams, most notably on the Sacramento, Feather, and Yuba rivers, must hold over the summer awaiting their September-October spawning season. Winter-run salmon continue to spawn into August in the Sacramento River below Shasta; their progeny, and the progeny of those that spawned earlier in the summer, are sustained by cold-water dam releases as embryos in gravel beds.

Throughout the summer, winter-run fry move out of their redds downstream of Shasta. Water released from Shasta must be sufficient in amount and cold enough to sustain salmon eggs/embryos, fry, fingerlings, smolts, and over-summering and newly arriving adults, as well as young steelhead. Sufficient river flows are necessary in over 200 miles of the lower Sacramento River to keep water temperatures below lethal levels for salmon, trout, and sturgeon. Adult fall-run salmon, whose migration begins in summer, need cool water (<70°F) to commence their run from the Bay up the river.

The Central Valley water quality plan’s limit of 68°F for the river is rarely enforced. Sacramento River flows of 6000-8000 cfs downstream of the major irrigation diversions are necessary to maintain the required water temperature, but these flows and are met only in wet years (Figure 1). The same holds true for the San Joaquin River, where low flows and high temperatures in late summer hinder that river’s salmon runs. Summer river flows into the Delta are also important in maintaining water temperatures within sustaining levels for Delta smelt (<73°F). Under low Delta inflows, not only is the smelt critical habitat warmer (Figure 2), but it is further upstream in the Delta, away from cooler Bay breezes. Further, during the summer, Delta water temperatures reach critical levels (>73°F) far more often under low Delta outflows (~5000 cfs) than moderate outflows (~10,000 cfs) (Figure 3).

In summary, river flows and water temperatures in summer are critical habitat needs. These needs require stronger summer flow standards and additional management attention to protect the salmon, steelhead, sturgeon, smelt and other species dependent on Central Valley and Bay-Delta habitats during summer portions of their life cycles.

Figure 1. River flow (cfs) in lower Sacramento River below major irrigation diversions in four recent years representing four water-year types. Green line represents minimum flow needed to maintain essential ecological processes in the lower river and Bay-Delta. Red line represents preferred minimum level protecting ecological processes. Summer flow is generally depressed even in wet years.

Figure 2. Water temperature in the north Delta channel of the Sacramento River 2008-2016. Red line denotes 73°F limit of sustainability for Delta smelt.

Figure 3. Delta outflow and water temperature (daily average) at Rio Vista in the north Delta channel of the Sacramento River in summer (mid-June to mid-August) of four recent years: critically dry years 2013 and 2015, below normal year 2016, and wet year 2011. Note that the daily averages are not independent from one another within years, and the effect of air temperature is not shown. Regardless, the effect of flow on water temperature, particularly in the readily controllable flow range of 5,000-15,000 cfs, appears significant among years. Source: CDEC.

 

More on Delta Smelt Tidal Surfing

The last post about risk to Delta smelt was on January 9. Adult smelt migrate into the Delta from the Bay in winter to spawn. They take advantage of the flood tide to move upstream. However, with flood flows as high as 100,000 cfs entering the north Delta from the Sacramento River, the Yolo Bypass, and Georgiana Slough in mid- to late January 2017, there are no flood tides to ride into the north Delta spawning areas.

The only option for the adult smelt is thus to ride the incoming tide up the San Joaquin River into the central and south Delta (Figure 1). South Delta export pumping is currently at 14,000 cfs, near maximum capacity, using four rarely used auxiliary pumps. This pumping increases the pull of the incoming tide, reducing the effect of the inflow from the San Joaquin, Calaveras, Mokelumne, and Cosumnes rivers. While Delta inflow from these rivers is relatively high (Figures 2-5), it does not offset the influence of the incoming tide as does the inflow from the Sacramento.

Net tidal flows in lower Old and Middle Rivers (OMR flows) remain at the allowed limit of -5000 cfs, consistent with the smelt Biological Opinion. Several adult Delta smelt were salvaged at the export facilities in mid-January. 1 This scenario is considered a “high risk” to Delta smelt by the Smelt Working Group, because of the continuing risk that the pumps will draw or attract adult smelt into the central Delta and subsequently into the south Delta.

Under lower San Joaquin River flows, the maximum allowed export pumping is 11,400 cfs. High San Joaquin River inflow allows exports of 14,000 cfs that do not generate OMR flows more negative than -5000 cfs. The theoretical benefit of high San Joaquin River flows is that it should keep flow into the central and south Delta moving westward. But a large portion of that inflow is diverted south into the Head of Old River toward the pumping plants (Figure 6).

Figure 1. Approximate flood tide flow in cubic feet per second in mid to late January 2016. Blue arrows represent high Sacramento River, San Joaquin River and Mokelumne River flows (during flood tides). Red arrows depict negative flows of incoming tides. Note the south Delta incoming tide of -20,000 cfs would be less if not for the 14,000 cfs export rate at the south Delta pumping plants.

Figure 1. Approximate flood tide flow in cubic feet per second in mid to late January 2017. Blue arrows represent high Sacramento River, San Joaquin River and Mokelumne River flows (during flood tides). Red arrows depict negative flows of incoming tides. Note the south Delta incoming tide of -20,000 cfs would be less if not for the 14,000 cfs export rate at the south Delta pumping plants.

Figure 2. San Joaquin River flow at Mossdale at the head of the Delta upstream of Stockton and the Head of Old River. Note that on Jan 6 when flow reached about 6,000 cfs, the tidal signal dissipated when flow overcame the tidal forces.

Figure 2. San Joaquin River flow at Mossdale at the head of the Delta upstream of Stockton and the Head of Old River. Note that on Jan 6 when flow reached about 6,000 cfs, the tidal signal dissipated when flow overcame the tidal forces.

Figure 3: Flow from the Calaveras River, upstream of the Delta. The Calaveras enters the Delta at Stockton.

Figure 3: Flow from the Calaveras River, upstream of the Delta. The Calaveras enters the Delta at Stockton.

Figure 4. Release from Camanche Dam to the Mokelumne River. CDEC does not show flow values for the Mokelumne at gages further downstream. The Mokelumne enters the Delta near Jersey Point.

Figure 4. Release from Camanche Dam to the Mokelumne River. CDEC does not show flow values for the Mokelumne at gages further downstream. The Mokelumne enters the Delta near Jersey Point.

Figure 5. Cosumnes River flow well upstream of the Delta. Much of the high flow peaks enters the river’s connected floodplain, roughly between Lodi and Elk Grove, and does not flow immediately to the Delta. Flows in the Cosumnes enter the Mokelumne before passing into the Delta

Figure 5. Cosumnes River flow well upstream of the Delta. Much of the high flow peaks enters the river’s connected floodplain, roughly between Lodi and Elk Grove, and does not flow immediately to the Delta. Flows in the Cosumnes enter the Mokelumne before passing into the Delta

 Figure 6. Flow entering the entrance to Old River from the San Joaquin River near Stockton.


Figure 6. Flow entering the entrance to Old River from the San Joaquin River near Stockton.

  1. https://www.usbr.gov/mp/cvo/vungvari/dsmeltsplitdly.pdf Note: website has changed to this new site.

More on Delta Science

More Delta ScienceI have written often on Delta science and what has been or could be learned from science to support water management.  Yet another biennial Delta science conference, the 9th, was held this past November.  This year’s conference theme was: “Science for Solutions:  Linking Data and Decisions.”  Another year has passed, and more has been studied and learned.  More dots have joined the dozens of previous dots in data charts from annual surveys of Delta organisms and habitat conditions.  More dots lament the loss of water and habitat.  The huge Delta Science Program has progressed yet another year.

Opening Talk

In Phil Isenberg’s opening talk, “A Guide for the Perplexed”, the former legislator and former chair of the Delta Stewardship Council suggested that scientists learn to smile more.  He asked: “Why should science be involved in policy anyway?”  He talked about how policy makers view science.  (Obviously, many are perplexed.)  He forgot that the universe and Mother Nature are vastly mysterious things, which are often more complicated than human understanding, but sensitive to human actions at the same time.  Yes, science is perplexing.

Mr. Isenberg talked about “independent science” and “combat science,” as though they were two different things.  To borrow a legal term, science is not self-executing.  Then he asked: “How do we know when we are using the best-available science”?  His answer: “When it is good enough to avoid doing something stupid.”  Clearly, we have yet to reach that point.  The problem has been in choosing to do the best thing, not that good choices or unknown or not “available.”  He then quoted Churchill:  “America will always do the right thing after trying everything else first”At least we have gotten past the point where we thought the world is flat.  It is all very perplexing.

Mr. Isenberg concluded by suggesting: “It’s the notion that scientists live looking farther out than the rest of us do with the gift of foresight that if properly utilized, can inform, educate, and ultimately motivate policy makers.”   He forgets that ultimately policy makers must trust scientists to get the job done.  Example: the Trinity Project and the atomic bomb in the 1940’s.  As long as water managers and policy makers lead the science, the Delta’s problems will not be solved.

The Delta Science Program

Clifford Dahm, former lead scientist for the Delta Stewardship Council, spoke on his Delta Science Program, which was forced upon us in the 2009 Delta Reform Act to ensure water and environmental policy are guided by the “highest caliber” science.  He spoke on the program’s Independent Science Board, outsiders who meet once a year to review “our science”.  He spoke on their Adaptive Management Program, which ensures that we evaluate everything and learn nothing.  He spoke on the program’s efforts to coordinate science and inform decision makers, and to develop and implement the Delta Science Plan and promote the Science Action Agenda.  He talked about their modeling efforts: “There’s just a lot of ways that modeling could be moved forward, and I hope that in the next two years, we can actually come back to you and say that some of our modeling efforts have shown greater fruition as time goes on.  We were talking about the idea of potentially a modeling center or a co-laboratory to get modelers together.”  Those would be the two years after which we will have new water quality standards, new biological opinions, and new tunnel-boring machines in the Delta, as well as several newly extinct native fish species.  They would also be the two years after 20 years of effort starting with the CalFed Bay-Delta Program.

A Great Question

U.C. Davis fisheries biologist Peter Moyle then addressed the question:  “How has your research program and the data it has produced over the last 35 years been used to develop solutions for conserving aquatic resources in Delta?”  He quoted the 1998 Strategic Plan:

This strategic plan, if followed, should lead to an orderly and successful program of adaptive ecosystem restoration….  The Strategic Plan Core Team has high expectations for the Ecosystem Restoration Program.  There is no turning back and the team anticipates that in 20-30 years many habitats will be restored, endangered species will become abundant enough to be delisted, and conflicts will be lessened , even in the face of population growth and increasing demands on resources.

In addressing the posed question, he then remarked:

In retrospect, now that almost 20 years has past since that was written, the statement almost seems tongue in cheek because clearly that has not happened.  I continue to help write reports that recommend how to improve the Delta ecosystem and frankly I don’t see much progress being made, as the delta smelt trends so eloquently attests…  the reality is that the Delta has continued to deteriorate as a habitat for native fishes, despite my research and despite many proposals for solutions.

His experience, like that of so many other long-time Delta scientists, is that few if any of the specific recommendations in the Strategic Plan have been implemented or completed.  Science has done its job, and scientists have long awaited action.  Policy makers and managers have failed us, not the science.

The use of science in complex public policy decision making

Chair of the State Water Board Felicia Marcus spoke on the use of science in decision making.  She suggested to scientists:  “Dare to recommend, but don’t decree …  Retain your scientific integrity but dare to make recommendations.  At the same time, own your power and be responsible with it and have empathy for the decision makers who have to balance, even as you would have them respect you.”  This is a very tough sell for scientists who have not been listened to for decades.  What will she and her Board do with two more rounds of recommendations on the Delta tunnels and the Bay-Delta Plan?  Will her Board be as transparent and methodical in their balancing as the scientists are in making their recommendations?

Chair Marcus further stated:

We’re entering the era of adaptive management that requires all of the above as well as integrating social sciences into our work … To make adaptive management work, we all have to learn how to be better ‘egosystem’ managers in order to be better ecosystem managers in the real world over time, versus lurching from sound bite to sound bite or wringing our hands that other players just don’t get it.

Sorry, but that’s not the problem.  It gives the policy makers and the managers too much credit and scientists too little.  Very few scientists think that managerial ignorance or lack of cognition is the biggest problem.  Rather, it’s that scientists have endured decades of adaptive management in which their lessons and caveats have on the whole been subsumed to the social sciences of politics and economics.  There are plenty of scientists throughout the resource agencies and non-profit groups who are extremely articulate and who have great senses of humor and social skills.   That hasn’t changed the outcomes: fish and other parts of the Bay-Delta aquatic ecosystem are in crisis, and the agricultural economy and other values against which the ecosystem is “balanced” are thriving..  And that balance sheet is really nothing to smile about.