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Riverine Thermal Regimes
    An Integral Component of Environmental Flows




Julian D. Olden
School of Aquatic and Fishery Sciences
University of Washington
Ecologically Sustainable
  Water Management
             Meeting the fresh water
             demands of a growing human
             population while ensuring
             ecosystem integrity has
             emerged as one of the world’s
             primary resource issues.

             Shifting focus from humans as
             exploiters of the environment
             to a world where riverine
             systems are legitimate “users”
             of fresh water.
The Science of Environmental Flows
Scientists are becoming increasingly engaged in the development
   of environmental flow recommendations.

An environmental flow is can be defined as the
  quantity, quality and timing of water flows
  required to maintain the components,
  functions, processes and resilience of aquatic
  systems which provide goods and services that
  are valued by society.

Efforts in environmental flow research have thus
   far have focused primarily on water quantity,
   whereas issues involving water quality, such as
   water temperature, have received little
   consideration.
Why has temperature been overlooked
   in environmental flow science?
 Society is largely unaware of the ecological importance of a
     river’s thermal regime for freshwater biodiversity and
     ecosystem function.
 Scientists have their hands full with understanding how
     freshwater ecosystems respond to hydrologic modification
     and how best to use this information to inform the
     science of environmental flows.

 The impacts of river regulation on
    downstream thermal regimes are
    considered to be small compared to the
    potential for flow alteration.
Objectives
The scientific community must broaden its perspective on
   ecologically sustainable water management to include
   aspects of the thermal regime in the science of
   environmental flows.

1. Review the concept of the natural thermal regime.
2. Illustrate how river regulation has modified thermal
   regimes and discuss the ecological impacts.
3. Challenge us to expand our perspective on environmental
   flows to include the management of thermal regimes for
   riverine ecosystem integrity.
Water Temperature

Stream temperature
is dependent on:

Energy budget
- the amount of heat
energy added or loss
to the channel.
Thermal capacity
- the volume of water
to be heated or
cooled.
The Natural Thermal Regime
Stream temperatures show marked annual and diurnal fluctuations
in response to seasonal and daily rhythms in the flux of heat
energy gained and lost by a stream and the volume and source of
runoff contributing to discharge.




                                             Bullpasture River, Virginia, USA
The natural thermal regime can be discomposed into its
components of magnitude, frequency, duration, timing, and rate
of change, and be summarized using statistics that describe the
central tendency and variability in distributions of water
temperatures.
                                           Mean annual T and CV
                                           Predictability/Constancy
                                           Magnitude
                                           Mean monthly T and CV
                                           Frequency
                                           1-/3-/7-/30-day maxima T
                                           1-/3-/7-/30-day minima T
       Descriptors of the Thermal Regime   Duration
                                           High pulse count and duration
                                           Low pulse count and duration
                                           Timing
                                           Maximum and minimum T
                                           Rate of Change
                                           Rise and fall rates
                                           # reversals
Ecological Importance of Temperature

 Water temperature directly influences the metabolic rates,
    physiology, and life-history traits of aquatic species and
    helps determine rates of important ecological processes.

 Freshwater fishes and aquatic macroinvertebrates utilize a
     diverse array of thermal habitats to meet their specific
     temperature requirements for survival, growth and
     reproduction.

 Components of the thermal regime have different ecological
    significance.
Thermal Modification in
               Lotic Ecosystems
Human activities may strongly alter spatial and temporal
   patterns in water temperatures by modifying the energy
   budget and thermal capacity of the river.

Sources of “warmwater pollution”
   Forestry, agriculture, and urbanization
•   Industrial effluents
•   Irrigation diversions
Coldwater Pollution below Dams
River regulation by dams can greatly modify water
    temperatures depending on their mode of operation and
    specific mechanism of water release.

Large dams directly modify thermal
    regimes by releasing water that
    greatly differs in temperature
    from natural conditions (Storage
    Effect).

By changing the volume of water,
    dams also influence temperature
    by affecting energy fluxes
    (Regulation Effect).
                                                  Arthur Rylah Institute
Keepit Dam - Namoi River, Australia
   Annual maximum daily temperature was 5.0°C lower and
    occurred 3 weeks later compared to pre-dam conditions.
   Magnitude of thermal alteration decreased with distance
    downstream from dam.




                                              Preece and Jones (2002)
Blowering Dam – Tumut River, Australia
     Reductions in natural summer temperatures of 13.0°C to
      16.0°C.
     Contributes to coldwater pollution for 80 river km below
      the dam and >200 km in the Murrumbidgee River.




                                                Lugg (1999), Preece (2004)
Vilui Dam - Lena River, Siberia
   Post-dam temperatures were 2-5°C higher in early-
    summer and 2-3°C lower in mid-summer.




                                                    Lui et al. (2005)
Flaming Gorge Dam – Green River, USA
   Summer temperatures (June-Aug) were, on average,
    12.0°C lower compared to pre-dam conditions.
   Annual maximum daily temperature was 14.0°C lower and
    its timing shifted from end-July to mid-December.




                                                   Vinson (2001)
Gathright Dam – Jackson River, USA
   Summer temperatures (June-Aug) were, on average,
    6.0°C lower compared to pre-dam conditions.
   Annual maximum daily temperature was 8.0°C lower.




                                              Olden et al. (in review)
Ecological Implications of
             Coldwater Pollution
Cold water releases can have lethal and sub-lethal effects.

Water temperatures below tolerance limits result in species
   extirpation, and sub-lethal impacts include a slowing of
   physiological processes such as reproduction and growth.

Lower spring/summer water temperatures compromise the structure
   and life-history of stream macroinvertebrate assemblages, and
   decrease the survival of egg, larval and adult fishes.

Delayed timing of peak spring temperatures disrupt critical cues for
    initiating fish spawning and insect reproduction and emergence.
Thermal regimes do not satisfy the
spawning requirements of native fishes

                                                 Pre-dam




                                                 Post-dam




                         Gathright Dam, Jackson River, USA
Five major challenges to developing
 comprehensive environmental flow
  assessments that incorporate the
critical temperature requirements of
         riverine ecosystems.
CHALLENGE 1
Improve our understanding of spatiotemporal
   variability in riverine thermal regimes
   Previous attempts to explore similarities in thermal
    regimes among rivers and develop formal classification
    systems have been limited.

   Quantifying thermal variability in undeveloped rivers is
    essential for establishing regional benchmarks needed to
    successful incorporating water temperature into
    environmental flow management.

   The paucity of continuous water temperature data
    represents a significant information gap, requiring a
    greater dependence on statistical modeling.
CHALLENGE 2
    Quantify the degree to which dams alter
           riverine thermal regimes
   In general, the scientific community has inadequately
    quantified the magnitude and geographic extent of dam-
    induced thermal alteration.

   Formal investigations of how dams are altering the various
    facets of the thermal regime are needed, including
    ecologically-relevant components of magnitude, frequency,
    duration, timing and rate of change in temperature events.

   This research is critical for mounting a convincing
    argument that temperature should play a significant role in
    the science and management of environmental flows.
Flaming Gorge Dam – Green River, USA
                 Green River is the largest tributary
                  of the Colorado River.
                 Flaming Gorge dam was constructed
                  in 1962 for hydroelectric power and
                  flood control.
Degree of Thermal Alteration
                 Daily water temperature records
                 •    Pre-dam: 1958-1962
                 •    Post-dam: 1963-1977

                 Mean annual temperature
                     decreased 2.5°C from
                     8.8°C to 6.3°C.

                 Annual variability in water
                     temperatures (CV) decreased
                     from 89% to 34%.

                 Thermal regimes were >2 times
                     more predictable in post-dam
                     years.
Riverine thermal regimes
Olden and Naiman (in prep)
Why has temperature been overlooked
    in environmental flow science?
Society is largely unaware of the ecological importance of a
    river’s thermal regime for freshwater biodiversity and
    ecosystem function.
Scientists have their hands full with understanding how
    freshwater ecosystems respond to hydrologic modification
    and how best to use this information to inform the
    science of environmental flows.

The effects of river regulation on downstream
   thermal regimes are considered to be
   smaller compared to the potential for
   flow alteration.
Thermal vs. Hydrologic Alteration
       ↑Thermal Alteration
          1-/3-/7-/30-day minimum
                                         Dec (Winter)
                                    Jan (Winter)

                          Feb (Winter)
        90-day minimum

                             Nov (Winter)
                 Mar (Winter)
                                                              ↑Hydrologic
                                                                Alteration
       Date of maximum              July - Oct (Summer)
                                    Date of minimum
                                    Rise and fall rates
                                    Lower pulse count




                                                        Olden and Naiman (in prep)
CHALLENGE 2 …

•   Data limitation is a significant problem.

•   “Desk-top” assessments have been used
    to identify and rank large dams based
    on potential to cause coldwater
    pollution according to intake depth,
    discharge, storage, etc …

    Queensland: 18 dams (Brennan, in prep)
    NSW: 9 dams (Preece 2004)
    Victoria: 24 dams (Ryan et al. 2001)
                                                DIPNR (2004)
CHALLENGE 3
     Quantify the ecological consequences of
            altered thermal regimes
•   Systematic assessments of
    the relationship between
    biological condition and
    the degree of thermal
    alteration are needed.
   Place the ecological
    impacts of thermal
    pollution in the context of
    broader ecological
    disturbances associated
    with dams.
CHALLENGE 4
Demonstrate the availability and success of
 thermal pollution remediation strategies
Various mitigation measures are available:
• Multi-level outlet structures
• Artificial destratification (large propellers that pump cold
  bottom water toward the surface)
• Trunnions (piping system that draw water from different
  levels in the water column)
• Surface pumps (large propellers that pump warm surface
  water into existing outlets)
• Draft tube mixers
• Submerged curtains (large curtains extending upwards from
  the bottom of the reservoir forcing all the release water to
  originate from the surface)
• Stilling basins
Thermal Restoration below
Flaming Gorge Dam – Green River, USA
                     Daily water temperature records
                     Pre-dam: 1958-1962
                     Post-restoration: 1978-2006

                     Mean annual temperature
                         decreased 0.3°C from
                         8.8°C to 8.5°C.

                     Annual variability in water
                         temperatures (CV) decreased
                         from 89% to 42%.

                     Thermal regimes were >2 times
                         more predictable in post-dam
                         years.
Post-dam (1963-1977)   Post-restoration (1978-2006)
CHALLENGE 5
    Develop a multi-faceted perspective on
             environmental flows

   Understand the relationships between flow alteration,
    thermal alteration, (other dam-induced drivers of
    environmental change), and the integrity of riverine
    ecosystems.

   Develop conceptual models and assess different
    environmental flow strategies that include prescriptions for
    both flow and temperature regimes.
B




                                                         A




A. Thermal restoration below Flaming Gorge Dam (Vinson 2001)

B. Flow restoration below Clanwilliam Dam (King et al. 1998)
Riverine thermal regimes
Take Home Message

• Dams can substantially modify riverine thermal regimes,
  which can result in significant ecological impacts.

• The degree of thermal alteration below dams may greatly
  exceed the level of flow alteration.

• The benefits of environment flows may not be fully
  realized unless critical aspects of the thermal regime are
  also considered.

• Incorporating aspects of water quality into environmental
  flow science and management represents a necessary step
  forward in ecologically sustainable water management.
Riverine thermal regimes

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Riverine thermal regimes

  • 1. Riverine Thermal Regimes An Integral Component of Environmental Flows Julian D. Olden School of Aquatic and Fishery Sciences University of Washington
  • 2. Ecologically Sustainable Water Management Meeting the fresh water demands of a growing human population while ensuring ecosystem integrity has emerged as one of the world’s primary resource issues. Shifting focus from humans as exploiters of the environment to a world where riverine systems are legitimate “users” of fresh water.
  • 3. The Science of Environmental Flows Scientists are becoming increasingly engaged in the development of environmental flow recommendations. An environmental flow is can be defined as the quantity, quality and timing of water flows required to maintain the components, functions, processes and resilience of aquatic systems which provide goods and services that are valued by society. Efforts in environmental flow research have thus far have focused primarily on water quantity, whereas issues involving water quality, such as water temperature, have received little consideration.
  • 4. Why has temperature been overlooked in environmental flow science? Society is largely unaware of the ecological importance of a river’s thermal regime for freshwater biodiversity and ecosystem function. Scientists have their hands full with understanding how freshwater ecosystems respond to hydrologic modification and how best to use this information to inform the science of environmental flows. The impacts of river regulation on downstream thermal regimes are considered to be small compared to the potential for flow alteration.
  • 5. Objectives The scientific community must broaden its perspective on ecologically sustainable water management to include aspects of the thermal regime in the science of environmental flows. 1. Review the concept of the natural thermal regime. 2. Illustrate how river regulation has modified thermal regimes and discuss the ecological impacts. 3. Challenge us to expand our perspective on environmental flows to include the management of thermal regimes for riverine ecosystem integrity.
  • 6. Water Temperature Stream temperature is dependent on: Energy budget - the amount of heat energy added or loss to the channel. Thermal capacity - the volume of water to be heated or cooled.
  • 7. The Natural Thermal Regime Stream temperatures show marked annual and diurnal fluctuations in response to seasonal and daily rhythms in the flux of heat energy gained and lost by a stream and the volume and source of runoff contributing to discharge. Bullpasture River, Virginia, USA
  • 8. The natural thermal regime can be discomposed into its components of magnitude, frequency, duration, timing, and rate of change, and be summarized using statistics that describe the central tendency and variability in distributions of water temperatures. Mean annual T and CV Predictability/Constancy Magnitude Mean monthly T and CV Frequency 1-/3-/7-/30-day maxima T 1-/3-/7-/30-day minima T Descriptors of the Thermal Regime Duration High pulse count and duration Low pulse count and duration Timing Maximum and minimum T Rate of Change Rise and fall rates # reversals
  • 9. Ecological Importance of Temperature Water temperature directly influences the metabolic rates, physiology, and life-history traits of aquatic species and helps determine rates of important ecological processes. Freshwater fishes and aquatic macroinvertebrates utilize a diverse array of thermal habitats to meet their specific temperature requirements for survival, growth and reproduction. Components of the thermal regime have different ecological significance.
  • 10. Thermal Modification in Lotic Ecosystems Human activities may strongly alter spatial and temporal patterns in water temperatures by modifying the energy budget and thermal capacity of the river. Sources of “warmwater pollution”  Forestry, agriculture, and urbanization • Industrial effluents • Irrigation diversions
  • 11. Coldwater Pollution below Dams River regulation by dams can greatly modify water temperatures depending on their mode of operation and specific mechanism of water release. Large dams directly modify thermal regimes by releasing water that greatly differs in temperature from natural conditions (Storage Effect). By changing the volume of water, dams also influence temperature by affecting energy fluxes (Regulation Effect). Arthur Rylah Institute
  • 12. Keepit Dam - Namoi River, Australia  Annual maximum daily temperature was 5.0°C lower and occurred 3 weeks later compared to pre-dam conditions.  Magnitude of thermal alteration decreased with distance downstream from dam. Preece and Jones (2002)
  • 13. Blowering Dam – Tumut River, Australia  Reductions in natural summer temperatures of 13.0°C to 16.0°C.  Contributes to coldwater pollution for 80 river km below the dam and >200 km in the Murrumbidgee River. Lugg (1999), Preece (2004)
  • 14. Vilui Dam - Lena River, Siberia  Post-dam temperatures were 2-5°C higher in early- summer and 2-3°C lower in mid-summer. Lui et al. (2005)
  • 15. Flaming Gorge Dam – Green River, USA  Summer temperatures (June-Aug) were, on average, 12.0°C lower compared to pre-dam conditions.  Annual maximum daily temperature was 14.0°C lower and its timing shifted from end-July to mid-December. Vinson (2001)
  • 16. Gathright Dam – Jackson River, USA  Summer temperatures (June-Aug) were, on average, 6.0°C lower compared to pre-dam conditions.  Annual maximum daily temperature was 8.0°C lower. Olden et al. (in review)
  • 17. Ecological Implications of Coldwater Pollution Cold water releases can have lethal and sub-lethal effects. Water temperatures below tolerance limits result in species extirpation, and sub-lethal impacts include a slowing of physiological processes such as reproduction and growth. Lower spring/summer water temperatures compromise the structure and life-history of stream macroinvertebrate assemblages, and decrease the survival of egg, larval and adult fishes. Delayed timing of peak spring temperatures disrupt critical cues for initiating fish spawning and insect reproduction and emergence.
  • 18. Thermal regimes do not satisfy the spawning requirements of native fishes Pre-dam Post-dam Gathright Dam, Jackson River, USA
  • 19. Five major challenges to developing comprehensive environmental flow assessments that incorporate the critical temperature requirements of riverine ecosystems.
  • 20. CHALLENGE 1 Improve our understanding of spatiotemporal variability in riverine thermal regimes  Previous attempts to explore similarities in thermal regimes among rivers and develop formal classification systems have been limited.  Quantifying thermal variability in undeveloped rivers is essential for establishing regional benchmarks needed to successful incorporating water temperature into environmental flow management.  The paucity of continuous water temperature data represents a significant information gap, requiring a greater dependence on statistical modeling.
  • 21. CHALLENGE 2 Quantify the degree to which dams alter riverine thermal regimes  In general, the scientific community has inadequately quantified the magnitude and geographic extent of dam- induced thermal alteration.  Formal investigations of how dams are altering the various facets of the thermal regime are needed, including ecologically-relevant components of magnitude, frequency, duration, timing and rate of change in temperature events.  This research is critical for mounting a convincing argument that temperature should play a significant role in the science and management of environmental flows.
  • 22. Flaming Gorge Dam – Green River, USA  Green River is the largest tributary of the Colorado River.  Flaming Gorge dam was constructed in 1962 for hydroelectric power and flood control.
  • 23. Degree of Thermal Alteration Daily water temperature records • Pre-dam: 1958-1962 • Post-dam: 1963-1977 Mean annual temperature decreased 2.5°C from 8.8°C to 6.3°C. Annual variability in water temperatures (CV) decreased from 89% to 34%. Thermal regimes were >2 times more predictable in post-dam years.
  • 25. Olden and Naiman (in prep)
  • 26. Why has temperature been overlooked in environmental flow science? Society is largely unaware of the ecological importance of a river’s thermal regime for freshwater biodiversity and ecosystem function. Scientists have their hands full with understanding how freshwater ecosystems respond to hydrologic modification and how best to use this information to inform the science of environmental flows. The effects of river regulation on downstream thermal regimes are considered to be smaller compared to the potential for flow alteration.
  • 27. Thermal vs. Hydrologic Alteration ↑Thermal Alteration 1-/3-/7-/30-day minimum Dec (Winter) Jan (Winter) Feb (Winter) 90-day minimum Nov (Winter) Mar (Winter) ↑Hydrologic Alteration Date of maximum July - Oct (Summer) Date of minimum Rise and fall rates Lower pulse count Olden and Naiman (in prep)
  • 28. CHALLENGE 2 … • Data limitation is a significant problem. • “Desk-top” assessments have been used to identify and rank large dams based on potential to cause coldwater pollution according to intake depth, discharge, storage, etc … Queensland: 18 dams (Brennan, in prep) NSW: 9 dams (Preece 2004) Victoria: 24 dams (Ryan et al. 2001) DIPNR (2004)
  • 29. CHALLENGE 3 Quantify the ecological consequences of altered thermal regimes • Systematic assessments of the relationship between biological condition and the degree of thermal alteration are needed.  Place the ecological impacts of thermal pollution in the context of broader ecological disturbances associated with dams.
  • 30. CHALLENGE 4 Demonstrate the availability and success of thermal pollution remediation strategies Various mitigation measures are available: • Multi-level outlet structures • Artificial destratification (large propellers that pump cold bottom water toward the surface) • Trunnions (piping system that draw water from different levels in the water column) • Surface pumps (large propellers that pump warm surface water into existing outlets) • Draft tube mixers • Submerged curtains (large curtains extending upwards from the bottom of the reservoir forcing all the release water to originate from the surface) • Stilling basins
  • 31. Thermal Restoration below Flaming Gorge Dam – Green River, USA Daily water temperature records Pre-dam: 1958-1962 Post-restoration: 1978-2006 Mean annual temperature decreased 0.3°C from 8.8°C to 8.5°C. Annual variability in water temperatures (CV) decreased from 89% to 42%. Thermal regimes were >2 times more predictable in post-dam years.
  • 32. Post-dam (1963-1977) Post-restoration (1978-2006)
  • 33. CHALLENGE 5 Develop a multi-faceted perspective on environmental flows  Understand the relationships between flow alteration, thermal alteration, (other dam-induced drivers of environmental change), and the integrity of riverine ecosystems.  Develop conceptual models and assess different environmental flow strategies that include prescriptions for both flow and temperature regimes.
  • 34. B A A. Thermal restoration below Flaming Gorge Dam (Vinson 2001) B. Flow restoration below Clanwilliam Dam (King et al. 1998)
  • 36. Take Home Message • Dams can substantially modify riverine thermal regimes, which can result in significant ecological impacts. • The degree of thermal alteration below dams may greatly exceed the level of flow alteration. • The benefits of environment flows may not be fully realized unless critical aspects of the thermal regime are also considered. • Incorporating aspects of water quality into environmental flow science and management represents a necessary step forward in ecologically sustainable water management.