IOP inversion from shallow waters

Slides:



Advertisements
Similar presentations
Atmospheric Correction Algorithm for the GOCI Jae Hyun Ahn* Joo-Hyung Ryu* Young Jae Park* Yu-Hwan Ahn* Im Sang Oh** Korea Ocean Research & Development.
Advertisements

Computer graphics & visualization Global Illumination Effects.
Using a Radiative Transfer Model in Conjunction with UV-MFRSR Irradiance Data for Studying Aerosols in El Paso-Juarez Airshed by Richard Medina Calderón.
GlobColour CDR Meeting ESRIN July 2006 Merging Algorithm Sensitivity Analysis ACRI-ST/UoP.
(a) (b) (c) (d) (e) (a)(b) (c)(d) OPTICAL IMPACTS ON SOLAR TRANSMISSION IN COASTAL WATERS Grace C. Chang and Tommy D. Dickey 1 Ocean Physics Laboratory,
Results Sampling Locations Year 2000 LEO-15 site Methods (1) Satlantic, Inc. SeaWiFS Profiling Multichannel Radiometer (SPMR) on the Suitcase package (
Modelling Bottom Reflectance Image by Fred Voetsch, Death Valley, To develop an analytical.
Shallow Water Bathymetry of Singapore’s Highly Turbid Coastal Waters: A Comparative Approach James F. Bramante, Durairaju Kumaran Raju, Sin Tsai Min Tropical.
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
Rrs Modeling and BRDF Correction ZhongPing Lee 1, Bertrand Lubac 1, Deric Gray 2, Alan Weidemann 2, Ken Voss 3, Malik Chami 4 1 Northern Gulf Institute,
Radiative Transfer Theory at Optical and Microwave wavelengths applied to vegetation canopies: part 2 UoL MSc Remote Sensing course tutors: Dr Lewis
Solving Systems of Equations
Remote Sensing Image Rectification and Restoration
Atmospheric Correction and Adjacency effect (a little) Ken Voss, Ocean Optics Class, Darling Center, Maine, Summer 2011.
Objectives  The objectives of the workshop are to stimulate discussions around the use of 3D (and probably 4D = 3D+time) realistic modeling of canopy.
Inverting In-Water Reflectance Eric Rehm Darling Marine Center, Maine 30 July 2004.
Liane Guild, Brad Lobitz, Randy Berthold, Jeremy Kerr Biospheric Science Branch, NASA Ames Research Center, CA Roy Armstrong, James Goodman University.
L. Guild 1, R. Armstrong 2, B. Lobitz 3, J. Goodman 2, F. Gilbes 2, R. Berthold 1, J. Torres 4, Y. Detres 2, C. Zayas 2, S. Williams 2, O. Tzadik 2, and.
Liane Guild, Brad Lobitz, Randy Berthold, Jeremy Kerr Biospheric Science Branch, NASA Ames Research Center, CA Roy Armstrong, James Goodman, Yasmine Detres,
Solve Systems of Linear Equations Using Elimination Honors Math – Grade 8.
Recent advances for the inversion of the particulate backscattering coefficient at different wavelengths H. Loisel, C. Jamet, and D. Dessailly.
Remote Sensing & Satellite Research Group
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.
Lab 9 Hydrolight and Ecolight. Ex. 1: Inputing measured Chl(z) data.
SCM 330 Ocean Discovery through Technology Area F GE.
Estimating Water Optical Properties, Water Depth and Bottom Albedo Using High Resolution Satellite Imagery for Coastal Habitat Mapping S. C. Liew #, P.
Satellite-derived Sea Surface Temperatures Corey Farley Remote Sensing May 8, 2002.
Digital Imaging and Remote Sensing Laboratory An Atmospheric Correction Algorithm for Hyperspectral Imagery Ph.D. Dissertation Defense by: Lee C. Sanders.
Optical Measurements & K d values Elizabeth Cox 29 November 2010.
Apparent Optical Properties (AOPs) Curtis D. Mobley University of Maine, 2007 (ref: Light and Water, Chapters 3 & 5)
Dr. North Larsen, Lockheed Martin IS&S Dr. Knut Stamnes, Stevens Institute Technology Use of Shadows to Retrieve Water Vapor in Hazy Atmospheres Dr. North.
Radiometric Correction and Image Enhancement Modifying digital numbers.
Use the Distributive Property to: 1) simplify expressions 2) Solve equations.
Inverting In-Water Reflectance Eric Rehm Darling Marine Center, Maine 30 July 2004.
Evaluating Algebraic Expressions 1-7 Solving Equations by Adding or Subtracting Preparation for AF4.0 Students solve simple linear equations and inequalities.
ESA Frascati 31 Oct 1 Determination of the light availability in ocean water utilizing Vibrational Raman Scattering.
Examples of Closure Between Measurements and HydroLight Predictions Curtis D. Mobley Sequoia Scientific, Inc. Bellevue, Washington Maine 2007.
Sensing primary production from ocean color: Puzzle pieces and their status ZhongPing Lee University of Massachusetts Boston.
Retrieving Water Leaving Radiances from MODIS Land and Ocean Color Channels Bo-Cai Gao 1, Marcos J. Montes 1, Rong-Rong Li 1, Heidi M. Dierssen 2, and.
Solving Linear Systems by Substitution
Objectives The Li-Sparse reciprocal kernel is based on the geometric optical modeling approach developed by Li and Strahler, in which the angular reflectance.
The radiance received by a spaceborne or airborne instrument looking at nadir at an altitude of Z (km) is described by the RTE for plane parallel atmospheres.
Chapter 3 Radiative transfer processes in the aquatic medium Remote Sensing of Ocean Color Instructor: Dr. Cheng-Chien LiuCheng-Chien Liu Department of.
NRL 7333 Rb = 1-  1+  1+  2 Non- Linear b1- b2q3 influences We developed improved SeaWIFS coastal ocean color algorithms to derived inherent optical.
Differential Equations Linear Equations with Variable Coefficients.
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,
Lecture 12: Models of IOPs and AOPs Collin Roesler 11 July 2007.
Some refinements for global IOPs products ZhongPing Lee IOPs Workshop, Anchorage, AK, Oct 25, 2010.
Results for Garver-Siegel-Maritorena semi- analytic model (GSM01) when applied to NOMAD dataset. Figures 1-6. The GSM01 model was “linearized” and the.
Chapter 4 Numerical models of radiative transfer Remote Sensing of Ocean Color Instructor: Dr. Cheng-Chien LiuCheng-Chien Liu Department of Earth Science.
Forward and Inverse Modeling of Ocean Color Tihomir Kostadinov Maeva Doron Radiative Transfer Theory SMS 598(4) Darling Marine Center, University of Maine,
Lecture 2 Introduction to Inherent Optical Properties (IOPs) and Radiative Transfer Apparent Optical Properties (AOPs) C. Roesler 3 July 2007.
Hydrolight and Ecolight exercises
D e v e l o p m e n t o f t h e M N I R-S W I R a n d AA a t m o s p h e r I c c o r r e c t I o n a n d s u s p e n d e d s e d I m e n t c.
Group Presentation, July 17, 2013
Coastal Water Algorithms
Investigating Cloud Inhomogeneity using CRM simulations.
High Resolution Time Series Measurements of Bio-Optical and Physical Variability in the Coastal Ocean as Part of HyCODE Dickey Mooring.
Progress toward DCC Demo product
Monitoring Water Chlorophyll-a Concentration (Chl-a) in Lake Dianchi,China from 2003 ~ 2009 by MERIS Data.
Hydrolight and Ecolight
Ke-Sheng Cheng Dept. of Bioenvironmental Systems Engineering
Simulation for Case 1 Water
Solve a system of linear equation in two variables
Downwelling Spectral Solar Irradiance and IR Radiance Measurements ATMS 360 Spring 2008 Preliminary Results.
Steps to solve simple linear simultaneous equations
Fig. 1. Location of the study site (23-28 S, W)
Wei Yang Center for Environmental Remote Sensing
Optical particle sizing in vertically inhomogeneous turbid media
Cases. Simple Regression Linear Multiple Regression.
Presentation transcript:

IOP inversion from shallow waters Peng Wang

Rrs = f(a, bb) Lu(0-): upwelling radiance Ed(0+): downwelling irradiance

PBR approach: • Basis vectors absorption aφ(λ) = aφ(λ0) [Sf*amicro(λ0)+(1-Sf)apico(λ0)] • adg(λ) = adg(λ0) exp(-S(λ-λ0)) backscattering bbp(λ) = bbp(λ0) (λ/λ0)-Y Radiance Reflectance equation [400:10:650] Rrs = 0.0949( bb/(bb+a)) + 0.0794 (bb/(bb+a))2 Linear regression method Data set: simulated by hydrolight (Rrs, a and bb)

Some results: IOP comparison (a and bb) Total Absorption Comparison average of relative difference: 11.9%

total backscattering comparison average of relative difference: 14.2%

Now story changed……

Rrs from shallow waters: Strange rrs Matlab complain No solutions !!!

Ed Lu Ludp LuB Rrs = Lu/Ed = (Ludp + LuB)/Ed = Ludp/Ed + LuB/Ed = Rrsdp + RrsB downwelling irradiance, upwelling radiance from water column and bottom

simple idea, hard application; fortunately…… Semi-Analytical Hyperspectral Model of Lee, et al, 1998 basically: rrs ≈ rrsdp[1-exp(-2KH)] + rrsBexp(-2KH) ≈ rrsdp(1-A0exp{-[(1/cosθw)+D0(1+D1u)0.5]αH}) + A1ρexp{-[(1/cosθw)+D’0(1+D’1u)0.5] αH}. rrs: subsurface remote-sensing reflectance, sr-1 rrsdp:subsurface remote-sensing reflectance for deep waters, sr-1 rrsB: subsurface remote-sensing reflectance for the bottom, sr-1 K: diffuse attenuation, m-1 H: bottom depth, m θw:subsurface solar zenith angle, rad u: bb/(a + bb) α: attenuation coefficient (=a+bb), m-1 ρ: bottom albedo A0,1 D0,1 D’0,1: from Lee et al, 1998

After subtracting the bottom influence, we get… Now matlab smiled and we got solutions !!!

Coefficient of Variance: (express sample variability relative to the mean of the sample) Total absorption: Backscattering:

IOP inversion results from shallow waters: Total Absorption: Total Backscattering:

Conclusions: Bottom reflectance has a huge impact on the remote sensing reflectance; Current semi-analytic algorithm can be successfully applied to invert IOPs after bottom correction; PBR approach can find strange rrs which is caused by the environment or bad measurements?

Acknowledgements