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Ocean temperature, hypoxia, and acidification: detecting the fingerprint of climate change in California's coastal ocean Drs. Emily B. Rivest, Sarah E. Moffitt, Tessa M. Hill June 16, 2015

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  • Ocean temperature, hypoxia, and acidification: detecting the fingerprint of

    climate change in California's coastal ocean

    Drs. Emily B. Rivest, Sarah E. Moffitt, Tessa M. Hill June 16, 2015

  • Sea Surface Temperature in Coastal CA Sea surface temperature (SST, e.g. upper 20 m) is rising globally.

    How it is measured: Moored and shore-based sensors, and throughout the water column

    Datasets: 317 • ongoing: 48% • ≥ 50 years: 2% • ≥ 10 years: 62%

    Length of time series (years)

    100 75 50 25 10 1

    Metadata are obscured by the extensive spatial and temporal records from the

    California Cooperative Oceanic Fisheries Investigation (CalCOFI)

  • Temperature Time Series Data from CeNCOOS/UCSD Shore Station Hopkins Marine Laboratory

    What you see here: Seasonal variability,

    ENSO variability Inter-decadal variability

    In El Niño years, maximum temperatures change little, but

    winter minima are warmer

  • Biological Indicator for Temperature: Giant Kelp and Black Surfperch

    0

    0.1

    4/19/01 1/14/04 10/10/06 7/6/09 4/1/12Blac

    k Su

    rfpe

    rc(n

    umbe

    r

    0.2

    0.3

    0.4

    0.5Holdfast

    h De

    nsity

    m

    -2)

    0

    4

    8

    12

    16

    5/28/05 7/6/09 8/14/13Ho

    ldfa

    st D

    iam

    eter

    (cm

    )

    DiameterFrond density

    Biological indicators are complex and highly variable. Should be monitored concurrent with physical indicators.

    0

    25

    50

    75

    100

    4/19/01

    Fron

    d De

    nsity

    (num

    ber m

    -2)

  • 30

    20

    15 10 5 1

    Length of time series (years)

    10

    5 1

    Dissolved Oxygen in Coastal CA Oxygen concentrations are declining in the interior of the ocean: • Ocean warming • Increasing stratification • Changing ocean

    circulation

    How it is measured: Moored sensors and throughout the water column in some places

    Datasets: 53 • ongoing: 57% • ≥ 50 years: 0% • ≥ 10 years: 45%

    (CALCOFI)

  • Oxygen Time Series Data from California Cooperative Oceanic Fisheries Investigations (CalCOFI)

    0

    1

    2

    3

    4

    5

    6

    7

    8

    9

    [O2]

    (ml/

    L)

    1950

    1955

    1960

    1965

    1970

    1975

    1980

    1985

    1990

    1995

    2000

    2005

    2010

    20 meters

    300 meters

    500 meters

    20 meters

    300 meters

    500 meters

    CalCOFI is documenting the decline of O2 concentrations in subsurface waters

    (Bograd et al., 2008)

  • Biological Indicator for Oxygen: Humboldt Squid

    ©2003 MBARI

    Zeidberg and Robison, 2007

    Consequence of oxygen loss in the interior of the California Current:

    Invasion of predatory Humboldt Squid

  • 10 7 6 4 3 1

    Length of time series (years)

    Ocean Acidification in Coastal CA The ocean is acidifying as it absorbs anthropogenic CO2. Consequently, pH and carbonate ion concentrations are decreasing.

    How it is measured: Moored, underway, and shore-based sensors record various carbonate chemistry parameters, usually pH and/or pCO2.

    Datasets: 28 • ongoing: 25% • ≥ 50 years: 4% • ≥ 10 years: 11%

  • 7

    7.2

    7.4

    7.6

    7.8

    8

    8.2

    8.4

    8.6

    11/1/12 3/3/13 7/3/13 11/2/13 3/4/14 7/4/14 11/3/14 3/5/15 7/5/15

    Seaw

    ater

    pH

    (tot

    al sc

    ale)

    SeapHOx pH

    Bottle data

    Ocean Acidification Time Series Data from Bodega Marine Laboratory (BML)

    Bodega Marine Lab is measuring

    carbonate chemistry in coastal ocean,

    producing data with signals of seasonal

    upwelling.

    Fall Spring Fall

  • Biological Indicator for Ocean Acidification: Pteropods

    Pteropod monitoring in plankton community

    PMEL, NOAA

    Pteropod shells dissolve when exposed to acidified seawater (we know this from laboratory experiments). This organism is an acidification “canary”.

  • California is a global leader We want to continue to be the leader for documenting

    impacts of climate change in coastal marine ecosystems

    How can we do this? By supporting: • Existing time series to prevent data gaps • Data collection distributed across CA • Expansion of OA monitoring sensor networks • Co-location collection of abiotic and biotic

    data

  • What is ocean acidification (OA)?

    The ocean absorbs ~28% of carbon dioxide emitted by industry and deforestation.

    Sarah R. Cooley ([email protected])

    Carbon Dioxide (CO2)

    Climate change

    Ocean acidification

  • • Harder to calcify skeletons and shells • Disturbed acid/base physiology

    Ocean temperature, hypoxia, and acidification: detecting the fingerprint of climate change in California's coastal oceanSea Surface Temperature in Coastal CATemperature Time Series�Data from CeNCOOS/UCSD Shore Station Hopkins Marine LaboratorySlide Number 4Slide Number 5Oxygen Time Series�Data from California Cooperative Oceanic Fisheries Investigations (CalCOFI)Biological Indicator for Oxygen: Humboldt SquidSlide Number 8Slide Number 9Slide Number 10Slide Number 11What is ocean acidification (OA)?Slide Number 13