Posted by: Deirdre Des Jardins | April 9, 2013

Update: Bay Delta Conservation Plan & Climate Change

In August, 2012, California Water Research released a report, Incorporating Drought Risk Into California Water Resources Planning.  Since that time we have been waging a quiet campaign for the Department of Water Resources to recognize that their climate modelling for the Bay Delta Conservation Plan has significant limitations and inconsistencies.

The report says that, if the projections of the drier climate change models hold up, then we will see increasing long and increasingly severe droughts in the Sacramento River watershed, and that we are likely already seeing such changes in the San Joaquin River watershed.    Under the drier climate change scenarios, there is simply no way that two 40 foot tunnels can make future CVP or SWP deliveries more reliable.    Thus BDCP cannot meet the co-equal goal of “increasing water supply reliability.”

There is also a problem with sea level rise modelling.    There are major inconsistencies between agencies within Natural Resources — BDCP modellers have projected a likely value of 18 inches by 2060, while the Delta Stewardship Council and the Delta Risk Management Study have used the highest possible value of 55 inches by 2100.

At the meeting on April 4th, Restore the Delta also delivered a coffin to Jerry Meral.

It now appears that the Department of Water Resources has thrown in the towel on BDCP meeting the co-equal goal of “increasing water supply reliability” as well as meeting the mandates for “Delta as place.”  In a blog post on April 5, Nancy Vogel, the spokesperson for DWR, posted a message on the BDCP blog, which said in part,

… The regions that depend upon water exported from the Delta must reduce their future reliance on those supplies, and the state must continue to work with local reclamation districts to protect Delta islands.

Look to the Delta Plan, not BDCP, for the blueprint on how California will improve its statewide water supply reliability and safeguard people and property in the Delta.

They are now saying that the Bay Delta Conservation Plan is primarily a plan to comply with state and federal endangered species laws.

It’s a significant shift, and appears to move the burden for meeting the mandates in the Delta Reform Act to the Delta Stewardship Council.

Posted by: Deirdre Des Jardins | July 25, 2012

An analysis of the claimed benefits for fish in BDCP plus

This is an analysis of the claimed benefits for fish in the BDCP Plus fact sheet, Current Conditions for Fish Compared with the Bay Delta Conservation Plan

BDCP Plus has two claimed benefits for salmon:

1.   Juvenile salmon would have better access to food on the Yolo Bypass floodplain, grow larger, and survive better as they enter the ocean.

The decision to flood the Yolo Bypass is an operating decision by the Department of Water Resources, so it is not necessarily linked to construction of a new conveyance.    The proposed BDCP restoration of habitat in the Yolo Bypass and Cache Slough could help salmon, if there was a significant increase in inundation of the floodplain.   DWR has not proposed to increase bypass flows, but will wait for 12 inches of sea level rise to raise the level of the Sacramento River.    This is forecast for mid-century under climate change models.

2.  95% of juvenile San Joaquin Chinook salmon and 60% of Sacramento River Chinook salmon do not survive the trip through the Delta.

As the February BDCP effects analysis makes clear, major diversions on the Sacramento River would cause signficant entrainment of  migrating spring and fall run Chinook salmon.    DWR’s consultant recommended minimum Sacramento River flows of 7,000 cfs in the fall when the commercially important fall run Chinook are migrating.     This would result in significantly reduced exports, and has been opposed by the water agencies.    The minimum fall flows in the Feburary BDCP effects analysis are 4,000 cfs.

Overall, BDCP benefits for Sacramento River Chinook salmon are unclear, and there is a significant risk to populations from increased entrainment of migrating spring and fall runs.

BDCP plus has three claimed benefits for Delta smelt and Longfin smelt:

1.  Estuary habitat quality and quantity would increase due to improved outflow and habitat restoration

Suisun Bay is important feeding habitat for Delta smelt and Longfin smelt.  Increased diversions since 2000 have increased salinity in the bay to the point that it is not usable in the summer by the pelagic fish, as well as creating an explosion in the population of the invasive clam, Corbula amurensis.    Biologists have recommended reduced diversions and increased outflows in wet and above normal years.   However, this was blocked as a result of a lawsuit by water agencies.     New operating restrictions proposed as part of BDCP will also likely be subject to legal challenge.

Benefits of  proposed BDCP habitat restoration in Suisun Bay are linked to reducing salinity so that the Bay is usable by pelagic fish.

2.     Plankton accumulation would improve through increased residence time in the Central and South delta, potentially enhancing foodweb support for longfin smelt and Delta smelt.

Toxic algae blooms in the Delta first appeared in 2000.   Research links the blooms to increased residence time in the Central and South Delta — low flows and higher water temperatures.     Sampling has also shown that the phytoplankton in the South Delta is almost entirely toxic algae.    This is likely linked to the high level of nitrates in the San Joaquin River in the summer.     Increasing residence time without cleaning up the San Joaquin River will likely increase toxic algal blooms, and could result in eutrophication and fish kills.

Any benefits of BDCP habitat restoration in the South Delta would depend on sufficient flows, as well as reducing nitrates and selenium in the San Joaquin River.    Currently there is no proposal to provide these flows, and reduction of nitrates has been delayed for over a decade.

3.   New intakes in the North Delta would feature state-of-the-art fish screens.

BDCP’s  promise to provide state of the art fish screens is not new.    The 2000 CALFED Record of Decision committed to putting fish screens on the existing pumps in the South Delta.   The water agencies decided not to fund the project.     Provision of adequate funding for BDCP mitigation commitments will be important in ensuring that mitigation commitments are met.

Overall the benefits of BDCP for Delta smelt and Longfin smelt are unclear, and there are significant risks from potential degradation of water quality in the Delta.

The most significant potential benefit for the Peripheral tunnel proposed as part of BDCP is in reducing reverse flows in the Central and South Delta.   However, any reduction in reverse flows is strongly tied to the level of pumping.    Increased water exports could actually increase reverse flows over existing conditions in some months.

Posted by: Deirdre Des Jardins | June 19, 2012

Drought and Climate Change in California — Part I

The June 12, 2012 U.S. Drought Monitor shows continuing extreme drought in many areas of the Southwest, including southwestern Arizona, and eastern New Mexico and western Texas.  The drought monitor also shows severe drought in Nevada and the Central and Southern Sierras.

Map of drought severity in US

June 12, 2012 US Drought Monitor

The final survey of snow water content by the Department of Water Resources showed levels close to the 1976-77 drought in the Central and Southern Sierras.

Many climate change models predict increasing droughts in the Southwest and California.     The graph below is from a 2011 risk assessment by the Bureau of Reclamation, which used an ensemble of 75 global climate models.

USBR 2050s-1990s precipitation change graph

Percent change in annual runoff from 2050s-2090s, USBR 2011

There appears to be a fairly strong correlation between the areas of predicted decrease in precipitation, and current drought patterns.

The graph below shows precipitation decreases in Sacramento under two climate scenarios chosen by Daniel Cayan et. al. for modelling the state of California’s 2009 Climate Adaptation Strategy.

Graph of projected changes in precipitation in the Sacramento Region

Differences in 30-year mean annual total precipitation in Sacramento
of early(2005–2034), middle (2035–2064), and late (2070–2099) 21st century relative to 1961–1990 for each of six GCMs, for A2 and B1 scenarios

Source:   Daniel Cayan et. al.,  Climate Change Scenarios and Sea Level Rise Estimates for the California 2009 Climate Change Scenarios Assessment

The two IPCC climate change scenarios chosen for modelling by Cayan were the A2 scenario, a higher emissions scenario which assumes continuously increasing population, and the B1 scenario, a lower emissions scenario which assumes rapid changes towards resource efficient technologies, and a declining population after 2050.     The A2 scenario is the more likely if current economic and population trends continue.

Under the A2 scenario, all of the global climate models show moderate to significant decreases in precipitation by mid-century.   Under the B1 scenario, two thirds of the global climate models show significant decreases.

The six global climate models (GCMs) used for the modelling were from major research centers around the world:

  1. the French Centre National de Recherches Météorologiques (CNRM) model
  2. the (U.S.) National Oceanic and Atmospheric Administration Geophysical Fluids Dynamics Laboratory (GFDL) model
  3. the MIROC 3.2 medium-resolution model from the Center for Climate
    System Research of the University of Tokyo
  4. the Max Plank Institute ECHAM5/MPI-OM
  5. the (U.S.) National Center for Atmospheric Research,  Community Climate System Model (CCSM)
  6. the National Center for Atmospheric Research,  Parallel Climate Model (PCM)

The models were chosen based on reasonable reproduction of seasonal temperature and precipitation, variability, and the El Nino/Southern Oscillation  (ENSO).

To summarize, the 75 GCM-ensemble model used by the 2011 US Bureau of Reclamation Risk Assessment, and most of the twelve models used in the 2009 California Climate Change Scenarios Assessment point toward a drier California.    This is consistent with recent patterns of drought in the region.   However, only time will tell if these droughts are the beginning of a significant shift in the climate in California and the Southwest.

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