phytoplankton dynamics and bottom water oxygen during a large bloom in the summer of 2011

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    Phytoplankton Dynamics and Bottom Water OxygenDuring a Large Bloom in the Summer of 2011

    Oscar Schofield, Scott Glenn, Josh Kohut, John Manderson, Grace Saba, Matt Oliver

    TAKE HOME MESSAGE:IOOS WILL IMPROVE

    WATER QUALITYSAMPLING &

    MANAGEMENT

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    Causes? Anthropogenic loading from urbanized coastline?

    Ocean

    Hudson Bay

    Salinity

    P e r c e n

    t O x y g e n

    S a

    t u r a

    t i o n

    undersaturated

    superstaurated

    LATTE April 2005

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    40N

    74W75W

    39N

    TemperatureoC

    19 20 21 22 24

    July 6, 98 - AVHRR

    FieldStation

    LEO

    40N

    74W75W

    39N

    FieldStation

    Chlor-a (mg/m3

    ).1 .3 .5 1 2 4

    July 11, 98 - SeaWiFS

    LEO

    New Jersey Coastal Upwelling

    RecurrentHypoxia/Anoxia

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    SST

    CHL

    CHL

    1996-2001Local scale observatories

    2001-2006Regional scale observatories

    2006-2012-2006Regional scale observatories

    The inability of the static sampling lead to the desire of creatingan observatory network which is capable of resolving spatial and temporal

    dynamics in the Mid-Atlantic

    Upwelling hypoxia &coastal predictive skill

    Schofield et al. 2002Glenn & Schofield et al 2003

    Glenn & Schofield et al 2009 Schofield et al 2011

    Shelf transport &communication with deep sea

    Ecosystemdynamics

    climate scalemediated change

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    U..

    CapeCod

    CapeHatteras

    NJ

    MACT

    VA

    DE

    NY

    NC

    RI

    MD

    PA10 States

    MIDDLE ATLANTIC REGIONAL ASSOCIATION COASTAL OCEAN OBSERVING S YSTEM

    1000 kmCape to Cape

    Gliders Nowcast &Forecasts

    L-Band X-BandCODAR

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    The Event(August 23 2011)

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    The Evolution of the Event

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    upwelling

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    The 2011 bloom was almost 10X standard monthly chlorophyll concentration

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    The Cause?

    River inputs?Upwelling?

    Advection?

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    Year Day

    R i v e r

    O u

    t p u

    t

    Large Bloom Observed

    Variable Upwelling

    Hurricane Irene and aftermath

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    HurricanceIrene

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    U.S. IOOS interactive observatory network allows adaptive sampling ofthe water quality.

    Upwelling drove a large bloom and over time was associated withdeclines in bottom water oxygen.

    The passage of Hurricane Irene did not terminate the bloom, but didincrease the bottom water oxygen.

    U.S. IOOS could help provide improved water quality monitoring now.

    Water Quality - U.S. IOOS as it is designed A multi-agency activity.Make Observations > Advance the Science > Improve the Forecasts

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