Title: Remote sensing applications in Oceanography: How much we can see using ocean color?
1Remote sensing applications in Oceanography How
much we can see using ocean color?
- Martin A Montes Ph.D
- Rutgers University
- Institute of Marine and Coastal Sciences
Spring 2008
2Main topics
- Introduction
- definitions, sensor characteristics
- Model development
- IOPs, AOPs, Forward and Inversion approach
- Applications
- chl, phytoplankton size structure
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5Ocean color sensors
- Definition
- Types
- Passive vs Active
- Sensor characteristics
- swath, footprint, revisiting time, spectral
resolution
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7 8Ocean color sensors characteristics
- Spectral resolution
- number of channels?, bandwidth?
- Temporal resolution
- revisiting time?
9Ocean color sensors characteristics
http//www.ioccg.org/reports/
10Ocean color sensors characteristics
http//www.ioccg.org/reports/
11Ocean color sensors characteristics
12Ocean color sensors characteristics
Ideally we need to match channels and optical
signatures
SIO PIER
13Ocean color sensors characteristics
14Ocean color sensors Other criteria to keep in
mind
15Ocean color sensors S/N of detectors
16Ocean color sensors types
17Lidar and detection of plankton and fish layers
Spatial Variability in Spatial Variability in
Biological Standing Stocks and SST across the GOA
Basin and Shelves 2003. Evelyn Brown, Martin
Montes, James Churnside. AFSC Symposium
18Model development
- Inherent and apparent Optical properties
- IOPS and biogeochemical parameters
- Forward vs Inversion models
19Inherent and Apparent Optical properties
IOPs not influenced by the light field (e.g.,
a, b, c coefficients)
IOPs influenced by the light field (e.g., Rrs,
Kd)
20IOPS biogeochemical parameters
VSF??
Absorption
Backscattering
Phytoplankton
CDOM
POC
SPM
21Forward vs Inversion models
Forward IOPs
Inversion Rrs
Rrs
IOPs
(Hydrolight or non-commercial code)
(Empirical, analytical, statistical)
22Forward vs Inversion models
Forward Monte Carlo simulations
Montes-Hugo et al. 2006, SPIE
23Inversion models
24Applications
- Chlorophyll a concentration in case II waters of
Alaska - Phytoplankton size structure in Antarctic waters
25Chlorophyll a concentration in case II waters of
Alaska
- Rrs Seawifs, MODIS, Microsas,
- hand-held spectrometer
- bb HydroScat
- Empirical band ratio vs
- spectral curvature
Montes-Hugo et al. 2005. RSE
26TOA
Remote sensing reflectance
200 m height
Spectral curvature
Validation
RMSlog10 0.41
RMSlog10 0.33
No regression
27STAY AWAY FROM CDOM USING LONGER WAVELENGTHS!!
28Phytoplankton size structure in Antarctic waters
- Spectral Backscattering approach
- bb from HS-6
- Rrs from PRR, SeaWiFS
- Phytoplankton size chl fractions , HPLC
bbx (?) M (?o/?) ?bbx
Montes-Hugo et al. 2007. IJRS
29Phytoplankton size structure in Antarctic waters
Field data
PRR
30Phytoplankton size structure in Antarctic waters
31HydroScat-6
32SeaWiFS
33Model validation based on HPLC signatures
34Thank you!!