Chlorophyll Results Ocean Optics 2004 Mike Sauer & Eric Rehm.

Slides:



Advertisements
Similar presentations
Sherwin D. Ladner 1, Robert A. Arnone 2, Richard W. Gould, Jr. 2, Alan Weidemann 2, Vladimir I. Haltrin 2, Zhongping Lee 2, Paul M. Martinolich 3, and.
Advertisements

Satellite Ocean Color Overview Dave Siegel – UC Santa Barbara With help from Chuck McClain, Mike Behrenfeld, Bryan Franz, Jim Yoder, David Antoine, Gene.
Backscatter and Chlorophyll Eric Rehm Ocean Optics 2004 Darling Marine Center 16 July 2004.
Vertical Distribution of Photosynthetic Pigments in Bamfield Inlet and Trevor Channel Ashlee Lillis Eosc 473.
Phytoplankton absorption from ac-9 measurements Julia Uitz Ocean Optics 2004.
GlobColour CDR Meeting ESRIN July 2006 Merging Algorithm Sensitivity Analysis ACRI-ST/UoP.
A novel concept for measuring seawater inherent optical properties in and out of the water Alina Gainusa Bogdan and Emmanuel Boss School of Marine Sciences,
2 Remote sensing applications in Oceanography: How much we can see using ocean color? Adapted from lectures by: Martin A Montes Rutgers University Institute.
1 Remote sensing applications in Oceanography: How much we can see using ocean color? Martin A Montes Ph.D Rutgers University Institute of Marine and Coastal.
Effects of Fluorescence Self Absorption of Algae in Sea Water Candy Barbaran Annie Becerra Mentors: Prof. Fred Moshary Dr. Alex Gilerson NYCRI C N p.
OSMOSIS Primary Production from Seagliders April-September 2013 Victoria Hemsley, Stuart Painter, Adrian Martin, Tim Smyth, Eleanor Frajka-Williams.
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
UNH Coastal Observing Center NASA GEO-CAPE workshop August 19, 2008 Ocean Biological Properties Ru Morrison.
Absorption properties of marine particles and CDOM: Use of special measurement devices: Ultrapath and PSICAM Marcel Babin Annick Bricaud Edouard Leymarie.
In situ science in support of satellite ocean color objectives Jeremy Werdell NASA Goddard Space Flight Center Science Systems & Applications, Inc. 6 Jun.
Spectrophotometry August 2011 SLCC/UVU STEP grant workshop.
Data Processing of IOP Packages Attenuation, Absorption and Backscattering c, a, b b Ian Walsh, Ph.D. Director of Science, Sea-Bird Scientific.
A Comparison of Particulate Organic Carbon (POC) from In situ and Satellite Ocean Color Data Off the Coast of Antarctica Amanda Hyde Antonio Mannino (advisor)
IOPs of suspended sediments in rivers and coastal margins: Towards modeling turbid-water photochemistry from space Margaret L. Estapa University of Maine.
ABSTRACT In situ and modeled water-column primary production (PPeu) were determined from seasonally IMECOCAL surveys and satellite data off Baja.
Inverting In-Water Reflectance Eric Rehm Darling Marine Center, Maine 30 July 2004.
PHYTOPLANKTON ABSORPTION IN RELATION TO PIGMENT COMPOSITION.
The beam attenuation coefficient and its spectra* (also known as beam-c or extinction coefficient ). Emmanuel Boss, U. of Maine *Some of the graphic is.
Determination of the optical thickness and effective radius from reflected solar radiation measurements David Painemal MPO531.
Norm Nelson, UCSB Chantal Swan, UCSB / ETH with assistance of: Julia Gauglitz, Teresa Serrano Catala, Erica Aguilera UltraPath in the Oligotrophic Ocean.
Bio-optical observations of the North Atlantic Spring Bloom Toby K. Westberry 1, Giorgio Dall’Olmo 1, Mike Behrenfeld 1, Emmanuel Boss 2 1 Department of.
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
Satellite Ocean Color Products: What should be produced? ZhongPing Lee, Bryan Franz, Norman Kuring, Sean Baily raise questions, rather to provide definite.
Ocean Color Radiometer Measurements of Long Island Sound Coastal Observational platform (LISCO): Comparisons with Satellite Data & Assessments of Uncertainties.
Soe Hlaing *, Alex Gilerson, Samir Ahmed Optical Remote Sensing Laboratory, NOAA-CREST The City College of the City University of New York 1 A Bidirectional.
The link between particle properties (size, packaging, composition, shape, internal structure) and their IOPs. In order for us to be able to use optical.
Using in-situ measurements of inherent optical properties to study biogeochemical processes in aquatic systems. Emmanuel Boss Funded by:
Applications of Regression to Water Quality Analysis Unite 5: Module 18, Lecture 1.
ASSESSMENT OF OPTICAL CLOSURE USING THE PLUMES AND BLOOMS IN-SITU OPTICAL DATASET, SANTA BARBARA CHANNEL, CALIFORNIA Tihomir S. Kostadinov, David A. Siegel,
VSF as a proxy for Particle Size Distribution Pauline Stephen.
5.3 Notes Light & Spectrometry Pg Theory of Light  Color is a visual indication of the fact that objects absorb certain portions of visible.
Lab 3 Particulate Absorption Collin Roesler 5 July 2007.
Backscattering Lab Julia Uitz Pauline Stephen Wayne Slade Eric Rehm.
Inverting In-Water Reflectance Eric Rehm Darling Marine Center, Maine 30 July 2004.
Scattering: What is it? Who does it? A few demos to get us going Why should you care about it? *includes materials by C. Roesler and C. Mobley.
Optical Water Mass Classification for Interpretation of Coastal Carbon Flux Processes R.W. Gould, Jr. & R.A. Arnone Naval Research Laboratory, Code 7333,
Rick Reynolds and Dariusz Stramski Measurements of IOPs and Characterization of Particle Assemblages for Monterey Bay Experiment Marine Physical Laboratory.
Examples of Closure Between Measurements and HydroLight Predictions Curtis D. Mobley Sequoia Scientific, Inc. Bellevue, Washington Maine 2007.
The link between particle properties (size, composition, shape, internal structure) and IOP Emmanuel Boss.
Scattering and attenuation and tracking uncertainties for cal/val.
Impact of Watershed Characteristics on Surface Water Transport of Terrestrial Matter into Coastal Waters and the Resulting Optical Variability:An example.
SCM 330 Ocean Discovery through Technology Area F GE.
Preparation for CDOM absorption lab (spectrophotometry) Mary Jane Perry.
Correspondence Between Net Oxygen Production and Measurements of Inherent Optical Properties Cedric Hall Elizabeth City State University Mentor: Dr. Joseph.
1 Retrieval of ocean properties using multispectral methods S. Ahmed, A. Gilerson, B. Gross, F. Moshary Students: J. Zhou, M. Vargas, A. Gill, B. Elmaanaoui,
Hydrolight Lab: Part 1 July 18th, 2013.
Lab 4 Scattering. Samples: Platymonas * Chaetoceros * Arizona 'Dust' *Wikipedia Damariscotta River Estuary.
Optical System Review. Lens concept selections Solving the optical parameters (Magnification) (Focal length), Where, S’ is the distance from the lens.
Lecture 2 Introduction to Inherent Optical Properties (IOPs) and Radiative Transfer Apparent Optical Properties (AOPs) C. Roesler 3 July 2007.
Group Presentation, July 17, 2013
OBJECTIVES Develop an understanding of variability in the relationships between particulate organic carbon (POC), light scattering, and ocean color Develop.
Estimation of analyte concentration on the basis of light absorption
Project coordinators: IOC-UNESCO & INGV
Hydrolight and Ecolight
Jian Wang, Ph.D IMCS Rutgers University
RESULTS-1. Validation of chlorophyll algorithms
AC-9/AC-S data analysis from CDOM Lab
Simulation for Case 1 Water
Wayne Slade Ocean Optics Summer 2004
Cedric Hall Elizabeth City State University
Optical Observatory Sampling Frequency for the BB2F
Backscatter and Chlorophyll
J.C.A. CEPEDA-MORALES1 and G. GAXIOLA-CASTRO2 RESULTS AND DISCUSSION
Estapa, Margaret1; Boss, Emmanuel2; Mayer, Lawrence M
Measurement of Absorption in Seawater
Presentation transcript:

Chlorophyll Results Ocean Optics 2004 Mike Sauer & Eric Rehm

Sources of [Chl] Variability Spatial Spatial –Different Dock locations –Dock vs. Buoy Temporal Temporal –Different sampling days / times –Fluorometer sample & BB2F measurements made at different times Diel Cycle differences Diel Cycle differences Tidal influences Tidal influences Sample Sample –Sub-sampling technique –Filtration volume for spec was constant = 400 ml Calibration of instruments Calibration of instruments Chlorophyll / a Φ ratio Chlorophyll / a Φ ratio Spec path length amplification correction (  or C&W) Spec path length amplification correction (  or C&W) Wavelength Wavelength –E.g., Spec data is at 675 nm –Local A max Other sources? Other sources?

Chlorophyll Variability

BB2F Chlorophyll Note: Water sampled different time than other measurements

Chlorophyll / a Φ 676 nm Boss, et al., JGR, 2004, “Particulate backscattering ratio at LEO 15 and its use to study particle composition and distribution” “… relationship developed by C. Roesler (personal communication, 2000). … This relationship derives the chlorophyll concentration (mg/L) by dividing its absorption by a chlorophyll specific absorption at 676 nm assumed to be of mg/L/m. This relationship has been found to have a close fit with chlorophyll a obtained through traditional extraction methods with data off the Oregon coast (r 2 = 0.98, where r 2 denotes the square of the correlation coefficient) (L. Karp-Boss, personal communication, 2001).”

Chlorophyll / a Φ 676 nm This is an estimated relationship based on data set from Oregon coast: This is an estimated relationship based on data set from Oregon coast: [Chl] = a Φ (676) /.014 (μg / L) Chlorophyll / a Φ ratio Chlorophyll / a Φ ratio –Used.014, as per lab handout –In reality, range = depending on phytoplankton packaging (more packaging, smaller ratio, smaller phy tend to have less packaging, large phy near surface tend to have more packaging). Think: do you really need a [Chl] measurement? Think: do you really need a [Chl] measurement? Could we model a better value based on the  we estimate from C p ? Could we model a better value based on the  we estimate from C p ?

Variability of [Chl] between BB2F and (Spec, AC-9, Fluorometer) We are looking at : We are looking at : –Variability between sampling times and –Variability between instruments

Variability of the BB2F [Chl] Observatory vs. Handheld Observatory vs. Handheld –Different sampling locations –Metal piling was dumping water stream one day –Relied on Wetlabs calibration data No cross-calibration between instruments No cross-calibration between instruments

Spectrophotometer Method We used the QFT technique We used the QFT technique –Possible problem: Smaller particles reflect (backscatter) more light, overestimating absorbance.

Spectrophotometer Method T-R (Transmittance-Reflectance) Method T-R (Transmittance-Reflectance) Method –Integrating sphere attached to dual-beam spec – –Uses a model that eliminates the effect of light backscattering by the particles. –“Studies have shown that values of path-length amplification were less widely dispersed in the case of the T-R method” Lohrehnz et al., Journal of Phytoplankton Research, 25/1, p35-61, 2003 “Phytoplankton spectral absorption as influenced by community size structure and pigment composition” – –“…particularly suited for applications to samples containing highly scattering mineral particles that are commonly found in Case 2 waters.” Mitchell et al., Ocean Optics Protocols for Sat Ocean Color Sensor Validation Rev. 4, 2003, Chapter 4 “Determination of spectral absorption coefficients of particles, dissolved material and phytoplankton for discrete water samples”

Data Management & Organization Data and metadata are separated Data and metadata are separated –Data: Spec and AC-9 data in computer files –Metadata: Sample time, location in notebooks, typ. not on-line –Suggestion: Include Metadata in Matlab, e.g. Metadata = ‘Data collected 7/1/2004, 10:00:00 EDT by Eric Rehm’ Data and script storage locations vary Data and script storage locations vary –Some groups stored on shared server –Some groups stored on individual laptops (only some data and scripts made it ot the server) –Suggestion: All groups store all data and all Matlab scripts on server, rather than on individual laptops MATLAB file format annoyances MATLAB file format annoyances –Not backward compatible by default (V6.5 vs. V7.0) Workaround: save –v6 Workaround: save –v6 –Spaces in directory names are a pain in the ….