dawn in the age of ocean observatories

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    Dawn in the age of ocean observatoriesOscar Schofield, Scott Glenn, Josh Kohut

    Coastal Observation and Prediction Sponsors:

    http://www.sebs.rutgers.edu/
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    Oceans are complex and central to the Earth system

    Thanks to Neptune, John Delaney, and Mark Stoermer

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    Despite heroic efforts, the ocean is chronically under-sampled. We need a permanentsustained presence making SPATIAL time series.

    Scott

    Glenn

    JoshKohut

    OscarSchofield

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    GSFC, NASA

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    Vessels -

    Satellite

    Satellite

    Ships/ Vessels

    REMUS

    Modeling

    Leadership

    CODAR

    Glider

    Data Vis.

    Security

    Education

    CODAR Network Glider FleetL-Band & X-Band Satellite

    Receivers

    3-D Nowcasts

    & Forecasts

    Rutgers University - Coastal Ocean Observation Lab

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    MARACOOS - International Constellation of Satellites Since 1992

    X-Band

    (installed 2003)

    L-Band

    (installed 1992)Sea Surface Temperature - SST

    Ocean Color

    Corporate Partner: SeaSpace

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    Mid-Atlantic Bight HF Radar Network Since 1997

    Mid-Atlantic HF Radar Network14 Long-Range CODARs7 Medium-Range CODARs

    15 Short-Range CODARs

    36 Total

    Triple Nested & Multistatic

    1000 kmAlongshore

    Length Scale

    Corporate Partner:

    CODAR Ocean Sensors

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    MARACOOS - Autonomous Underwater GlidersSince 1998

    Satellite Ocean Color

    Satellite SST

    SubsurfaceGlider

    Data

    < Glider Fleet

    With Global Reach >

    Corporate Partner: Teledyne Webb Research

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    Darwin s Odyssey January 11, 2006

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    ARGO combined with satellites the pre-eminent global ocean sampling array

    OOI in valuablelocations provide

    infrastructurecapable of

    sampling oceanintensely to

    support processstudies and helpdevelop model

    parameterization

    Sargasso SeaFront

    Sargasso SeaFront

    Sargasso SeaFront

    Cold CoreEddy

    Cold CoreEddy

    Cold CoreEddy

    Warm Core

    Remnant

    Warm Core

    Remnant Warm CoreRemnant

    Modelsimproved

    with in situdata via dataassimilation

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    MIDDLE ATLANTIC REGIONAL DRIVERS

    OceanCirculation

    Tropical Storms

    Population Ports

    Northeasters

    Climate Change

    CriticalHabitat

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    Total inches of rainfall

    0 32

    Aug 20-29

    First tropical storm to threaten NYCsince Hurricane Gloria in 1985

    Flooding records broken in 26 rivers

    Caused at least 56 deaths

    Damage nearly $8 billion

    Hurricane Irene

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    39.5N 73W Surface Current Time SeriesTotal Current Near-Inertial Current

    Wave & Wind Direction Time Series

    Hurricane Irene

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    Hurricane Irene

    Direct Wind Forcing Inertial Response

    T Glid

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    Two GlidersDeployed by MARACOOS

    in Hurricane Irene

    RU16 Deployed for EPA. Map bottom dissolvedoxygen. Provided data onmixing during storm.

    RU23 Deployed for MARACOOS. Map subsurface T/S

    structure for fisheries. Damaged early - drifter Recovered by fisherman Provided data on inertialcurrents during storm.

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    14

    33

    29

    105

    60

    salinity

    % oxygen

    temperature55

    55

    0

    0

    55

    depth

    depth

    depth

    8/12 9/07date

    260

    Hurricane IreneHurricane Irene

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    Time Series of Derived Parameters

    Glider RU16

    NOAA Delaware Bay Buoy

    Thermocline Depth

    Surface Temp

    Max S.D. w

    Max S.D. w Depth

    Wind Speed

    Wave Height

    Wave Period

    Wave Bottom Orbital Velocity

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    3540455055606570758085

    Wind

    Speed(kts)

    Date

    Maximum Sustained Wind Speed(10m)

    NHC Best Track

    NHC Forecast

    Warm SST (RTG only)

    RU-WRFAtmospheric

    Forecast Model

    WRF M d l R SST U d t

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    27/120028/0600 28/060029/0600

    WRF Model Run: SST Update

    R n Comparison

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    WARM (RTG only) COLD Update(AVHRR)

    Run Comparison

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    Maximum Wind Speed Error (knots)Date/Time

    (UTC)

    NHC

    Forecast

    Warm (RTG

    only)

    Warm (RTG

    only, OMLModel)

    Cold Update

    (AVHRR)

    27/1200 5 -17.22 -17.23 -6.17

    27/1800 10 4.1 4.2 5.88

    28/0000 10 1.39 -2.14 3.96

    28/0600 5 -1.2 -1.04 -1.21

    28/1200 15 2.39 4.79 0.5

    28/1800 15 4.97 3.51 -2.67

    29/0000 15 3.62 1.93 -0.89

    29/0600 10 10.48 9.84 4.52

    Sum of Squares 800 457 452 118RMSE 9.43 7.13 7.09 3.61

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    Case example 2: Application of observatory technologies for studyingremote and extreme locations, the West Antarctic Peninsula

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    We are using the WAP as zone to study how rapid warming can shift the food web

    Fastest winter warming location on Earth

    Northern WAP perennial ice is gone

    87% glaciers in retreat

    Sea ice duration decreased by ~60 days

    Increase in ocean heat content

    Increase in wind and clouds

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    Heat engine melting the WAPis the ACC

    ACC upwelling is rapid flushingevents (time scale of weeks)

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    28

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    29

    Melt pools on surface of King George

    VI Sound, from BAS twin otter(January 2004)

    Thanks to A. Clarke (BAS)

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    30Photo by Bill Fraser

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    Remote Sensing (Decadal changes) Ship Observed (Decadal changes)

    Montes-Hugo et al. 2009 Vernet et al. 2008

    There are indications in changes in the primary production

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    Cryptomonas cryophila

    Thalassiosira antarctica

    Corethron criophilum

    Palmer Cryptophytes --> 8 2m10m

    100m

    SEM Micrographs fromMcMinn and Hodgson 1993

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    1970s-1980s

    1995-2005

    There are indications in changes in the nature of the phytoplankton

    Montes-Hugo et al. 2009

    Moline et al. 2004

    From satellite From ship

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    Antarctic krill Antarctic Salp

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    Loeb et al. 1997

    There are indications in changes in the zooplankton communities

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    Adaptive Sampling of Penguin Habitats

    PenguinForaginglocations

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    Mark Moline & Bill Frazer

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    48

    Observatory (simulated) data

    Virtual Ocean

    Design, Testing and Deploy

    Models

    Data Assimilation

    DataAnalysis

    Science Questions & Drivers

    ~100 m

    ~3 kmSensor &Platform

    Data Synthesis: Nowcast & Data Impact

    W

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    We

    ath

    er

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    Multiple Satellite passesof varying resolution

    An ensemble of different numerical models run by different laborat

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    Model A Model B

    Model C Model D

    An ensemble of different numerical models run by different laborat

    A fleet of four gliders

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    A fleet of four glidersOctober 30 November 20, 2009

    4 Deployments(3 Rutgers, 1University ofDelaware)

    77 in-water days

    1608 km flown

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    Science Community Workshop 1 53

    Model A Model B Model CModel D

    COMBINING THE FIELD ASSETTS WITH OCEAN FORECASTS

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    COMBINING THE FIELD ASSETTS WITH OCEAN FORECASTSFOR PLANNING AND PROSECUTION EFFORTS

    Known constraints (slow 0.5 knot,Battery, shipping lanes)

    Uncertain constraints (time-varying3D currents)

    Operate autonomously & re-plandaily

    From A to B in the shortest time Follow a time-varying feature

    (shelf-slope salinity intrusion)

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    PLANNING FOR THE PRESENT

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    PLANNING FOR THE PRESENT

    PLANNING IN THE FUTURE

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    Increase model resolution Reduce forecast error

    Science S iScientists

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    Science Community Workshop 1 5959

    Science

    Agents

    Science Event ManagerProcesses alerts and

    Prioritizes response observations

    ASPENSchedules observations on EO-1

    EO-1 Flight DynamicsTracks, orbit, overflights,momentum management

    ScienceAlerts

    ObservationRequests

    Updates toonboard plan

    ScienceCampaigns

    Scientists

    Hyperionon EO-1

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    NEPTUNECanada

    NFS OOINetwork

    NOAA N-WaveNetwork

    Global LambdaIntegrated Facility

    Topology of oceanobservatories will be

    integrated into nationaland international cyber-

    networks. This willfacilitate collaboration

    for developing theinternational oceanobserving network

    STEM education: Undergraduates are active pilots of the observatory

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    During RIMPAC 2008 off Hawaii

    Conclusions:Ocean technologies will use to sample

    the oceans as never beforeThis is critical as the oceans have undergonesignificant change over the last few decades