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The Impact of Climate Change on California's Marine Ecosystems: Beyond Sea Level Rise Franklin B. Schwing NOAA Fisheries Service SWFSC – Environmental Research Division Pacific Grove CA [email protected] Acknowledgements- COMPASS & Stanford U Jack Barth (Oregon State U) Nathan Mantua (U Washington) Dave Foley, Bill Peterson, Steve Ralston (NOAA) Bill Sydeman (PRBO) and many others

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The Impact of Climate Change on California's Marine Ecosystems:

Beyond Sea Level Rise

Franklin B. Schwing

NOAA Fisheries ServiceSWFSC – Environmental Research Division

Pacific Grove CA

[email protected]

Acknowledgements-COMPASS & Stanford UJack Barth (Oregon State U)Nathan Mantua (U Washington)Dave Foley, Bill Peterson, Steve Ralston (NOAA)Bill Sydeman (PRBO)and many others

Climate Variability and the California Current Ecosystem:

Key QuestionsWhat are the key environmental factors that shape ecosystem structure and productivity?

How are they are influenced by climate events and future climatescenarios?

How does the California Current respond to climate variability?

What are the primary ecological consequences of concern to California's economy and culture?

Large-ScaleCirculation:

The California Current,Part of the north Pacific

Ocean Circulation

(from Jack Barth, OSU)

Coastal upwelling

satellitechlorophyll

andtemperature

(from Jack Barth, OSU)

WHAT FACTORS SHAPE THE CALIFORNIA CURRENT ECOSYSTEM?

“BOTTOM-UP”

SEA LEVELOCEAN TEMPERATURE/FRESHWATERCURRENTS & TRANSPORTSTABILITY & FRONTSWATER QUALITYNUTRIENT AVAILABILITYFOOD TYPE & AVAILABILITY

01

1000 1500 2000

“Bottom-up” Drivers

WHAT FACTORS SHAPE THE CALIFORNIA CURRENT ECOSYSTEM?

“TOP-DOWN”PREDATIONCOMPETITIONFISHINGURBAN RUNOFFEXOTIC SPECIES INVASIONS

CLIMATE EVENTS & CLIMATE CHANGE

0

1

N.H

. Tem

pera

ture

(°C

)

1000 1500 2000

Top down & Human Drivers

El Niño(images from NASA)

Interannual Variability Affects Fish Catch

-

5

1 0

1 5

2 0

2 5

3 0

3 5

2 2 2

M N TS C BTo ta l

2

So CA BightMonterey

Market squidAnnual catch rates, 1981-2005

(from Peterson and Schwing, 2003)

Pacific Decadal Oscillation

warm phase

Interdecadal climate variability (“regime shifts”) changes ecosystem structure and productivity

(from Nathan Mantua, U. Washington)

cool phase

Human activities have changed atmosphere composition since the pre- industrial era

(from IPCC, 2006)

The Future?IPCC

Projections2100 AD

2

4

3

5

6

1

0

Glo

bal

Tem

pera

ture

(°C

)

0

0.5

1

-0.5

N.H

. Tem

pera

ture

(°C

)

1000 1500 2000

Mann et al (1999) and IPCC 2000

Climate Change Projected to ImpactCalifornia Current Ecosystem

• Warmer summer temperatures; greater ocean stratification, weaker upwelling (very likely)

• Warmer & wetter winters; greater freshwater inflow, coastal flooding (very likely)

• Higher coastal sea level (very likely)

• More extreme events; stronger storms, El Nino, hurricanes (likely)

• Delayed seasonal cycle; delayed upwelling (likely)

• Northward species shifts• Lower productivity & food• Exotic species introduced

• Reduced coastal water quality• Toxic blooms• Human health hazards

• Intertidal species displaced

• Greater coastal erosion• Fisheries reduced & displaced• Warm-water fisheries available

• Delayed spring bloom• Reproduction, migration impacted

Projected changes - 21st century Examples of ecological impacts

Less Production in 2005 due to Less Springtime Upwelling

(from David Foley, NOAA NESDIS)

Warmer Climate Favors Southern Intertidal Species

(from Berry et al., 1995)

California Marine Populations Shifting Northward

(from Union of Concerned Scientists)

0.000.250.500.751.001.251.50

1970 1975 1980 1985 1990 1995 2000 2005

2005-2006 - worst years on record for Farallon Island auklets (42 km west of San Francisco)

Mean productivity = 0.70

From Sydeman and Bradley, PRBO

#you

ng/b

reed

ing-

pair

Nests abandoned due to delayed upwelling

Summary and Conclusions

The California Current Marine Ecosystem is shaped by physical processes with time scales of days to decadesClimate variability leads to ecological variability

•Global atmosphere is ultimate source of variabilityModulation by global climate change may include

• delayed spring transition and stronger late-season upwelling• northward shift, favorable for warm-water species• increased variability expected with global warming• fishery winners and losers• more coastal stress

Timing is critical, e.g. rockfish recruitment, seabird breeding,salmon ocean entryMitigate global climate change by avoiding other ecological stressors, e.g. overfishing, coastal pollutionManagement decisions must incorporate climate variability in marine ecosystems