cyndhiasamiah mb presentation

Upload: jpeterson1

Post on 30-May-2018

218 views

Category:

Documents


0 download

TRANSCRIPT

  • 8/14/2019 CyndhiaSamiah MB Presentation

    1/32

    There Is No Bloomin Bloom:There Is No Bloomin Bloom:ANALYSIS OF ALGAL PRE-BLOOMANALYSIS OF ALGAL PRE-BLOOM

    PARAMETERSPARAMETERSIN MONTEREY BAY, CALIFORNIAIN MONTEREY BAY, CALIFORNIA

    ON JULY 22ON JULY 22 ndnd AND 24AND 24 thth

    Phytoplankton are the foundation of the marinefood chain and they can influence Earths climate.

    SARP 2009Samiah Moustafa, UF 2011

    Cyndhia Ramatchandirane, Wellesley 2011

  • 8/14/2019 CyndhiaSamiah MB Presentation

    2/32

    OutlineOutline

    Introduction/Background Motivation Objectives

    Methods Limitations Results Conclusions Acknowledgments

  • 8/14/2019 CyndhiaSamiah MB Presentation

    3/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    4/32

    Underwater terrain of Monterey Bay

  • 8/14/2019 CyndhiaSamiah MB Presentation

    5/32

    Objectives To validate MASTER data with in situ and

    local M1 mooring data Determine favorable pre-bloom

    conditions Determine potential bloom locations Explore/Determine correlations among

    several parameters: Sea SurfaceTemperature (SST), salinity, chlorophyll,dissolved oxygen, nitrates

  • 8/14/2019 CyndhiaSamiah MB Presentation

    6/32

    MotivationMotivation

    Coastal upwellingregions represent adisproportionatelylarge fraction of theoceans primaryproduction

    Phytoplanktonrespond very rapidlyto changes in theirenvironment and canbe used as indicatorsof change (NASA EO)

    Economicincentivefishery production

    Affects health of marineecosystems andhumans

    The increasedfrequency,

  • 8/14/2019 CyndhiaSamiah MB Presentation

    7/32

    Methods Remote sensing:

    MASTER on DC-8 aircraft flyinglaboratory

    In situ ocean sampling Local mooring M1SURF 20km

    offshore Correlation analyses:

    - Time series plots and parameter

    graphs

  • 8/14/2019 CyndhiaSamiah MB Presentation

    8/32

    NASA DC-8 AircraftMASTER instrument (DC-8)

    Moorings in Monterey BayData from M1 surf Station Ship Data from John Ryan at MBARI

  • 8/14/2019 CyndhiaSamiah MB Presentation

    9/32

    LimitationsLimitations M1 SURF station was the only

    available mooring Lack of airborne data from MASTER

    on July 24 th Variability in cloud cover and the

    marine layer Scale measurement (17.7m pixel

    resolution from MASTER while theship has a higher resolution but lessspatial coverage (

  • 8/14/2019 CyndhiaSamiah MB Presentation

    10/32

    Wind Speed over Monterey Bay, CA at 3:00 PM During July 22 nd , 24 th , and 28 th

    July 22 nd July 24 th

    July 28th

  • 8/14/2019 CyndhiaSamiah MB Presentation

    11/32

    July 22nd July 24th

    MODIS Satellite Images

  • 8/14/2019 CyndhiaSamiah MB Presentation

    12/32

    SURFER Contour ImagesSURFER Contour Images

    Chlorophyll Concentrations July 22nd Temperature July 22 nd

    RESULTSRESULTS

  • 8/14/2019 CyndhiaSamiah MB Presentation

    13/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    14/32

    July 22 nd : MASTER thermal band and ship track overlay (white)Blue outline shows our Region of Interest (ROI) for chlorophyll,temperature, and salinity.

  • 8/14/2019 CyndhiaSamiah MB Presentation

    15/32

    Ship data exported & interpolated from Surfer onto ENVI (right) shows layers of warmer (light) and colder (dark) surface water. MASTER thermal band image(left) shows a similar layering effect

    TEMPERATURE

  • 8/14/2019 CyndhiaSamiah MB Presentation

    16/32

    (Right) High chlorophyll concentration interpolated from ship data.

    CHLOROPHYLL

  • 8/14/2019 CyndhiaSamiah MB Presentation

    17/32

    (Right) Highly layered salinity concentration interpolated from ship data.Possibly from upwelling. High salinity concentrations suggest increase in

    nutrient content.

    SALINITY

    l 24 th

  • 8/14/2019 CyndhiaSamiah MB Presentation

    18/32

    July 24 th:Chlorophyllandtemperatureinterpolatedfrom ship data

    CHLOROPHYLL

    CHLOROPHYLL

    TEMPERATURE

  • 8/14/2019 CyndhiaSamiah MB Presentation

    19/32

    July 24 th: Highchlorophyll versussalinity layering

    CHLOROPHYLL

    CHLOROPHYLL

    SALINITY

    SALINITY

  • 8/14/2019 CyndhiaSamiah MB Presentation

    20/32

    FLH bands 678. Red shows highest fluorescence. Red polygon isthe highest chlorophyll from ship data interpolated in surfer. FLHcalculated from expression by Letelier 2005.

  • 8/14/2019 CyndhiaSamiah MB Presentation

    21/32

    Close up view of surfer chlorophyll data from ship and FLH band 678.

  • 8/14/2019 CyndhiaSamiah MB Presentation

    22/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    23/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    24/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    25/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    26/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    27/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    28/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    29/32

  • 8/14/2019 CyndhiaSamiah MB Presentation

    30/32

    Conclusions

    The surface winds we observed suggestupwelling

    July 22 nd and July 24 th ENVI plots exhibit aregion of high chlorophyll and salinityconcentrations corresponding to SSTgradient pattern possibly due to upwelling

    This region of interest was (potentially)

    where the bloom was observed on July28 th Attempts at calculating chlorophyll

    concentrations from the MASTER data

    using FLH were inconclusive

  • 8/14/2019 CyndhiaSamiah MB Presentation

    31/32

    Acknowledgments

  • 8/14/2019 CyndhiaSamiah MB Presentation

    32/32

    References Gower, J. (2005).Detection of intense plankton blooms using the

    709nm band of the MERIS imaging spectrometer. International Journal of Remote Sensing , 26(9) , [2005-2012].

    Kudela, R. (2005). Harmful algal blooms in coastal upwellingsystems. Oceanography , 18(2) , [184-197].

    Olivieri, R., & Chavez, F. (2000). A model of plankton dynamics forthe coastal upwelling system of Monterey Bay, California. Deep SeaResearch , 47 , [1077-1106].

    Ryan, J. (2008). A coastal ocean extreme bloom incubator.Geophysical Research Letters , 35(L12602) , [1-5].

    Ryan, J. (2005). Coastal ocean physics and red tides: an examplefrom Monterey Bay, California. Oceanography , 18(2) , [246-255].