CBLAST RU05 glider SAM data 02/02/06. Sampling map.

Slides:

Advertisements

Similar presentations

Beyond Chlorophyll: Ocean color ESDRs and new products S. Maritorena, D. A. Siegel and T. Kostadinov Institute for Computational Earth System Science University.

Advertisements

Backscatter and Chlorophyll Eric Rehm Ocean Optics 2004 Darling Marine Center 16 July 2004.

By: Derrick Griffin. It is a well-known fact that the Dead Sea located in Jordan, Israel is one of the saltiest lakes in the world, whose salinity is.

Index Values NATIONAL STATISTICAL COORDINATION BOARD.

When light passes from vacuum (index of refraction n = 1) into water (n = 1.333), Q33.1 A. the wavelength increases and the frequency is unchanged. B.

Light Scattering Topic 3 Part 2 Biophysics. Single Particle Rough Treatment Sample - dipole Light Source k 0  The scattering angle, , is defined w/r.

Fig Rainbows are formed by refraction, reflection, and dispersion in water drops. (a) Primary rainbow. (b) Secondary rainbow. red violet © 2003.

Atmospheric phase correction for ALMA Alison Stirling John Richer Richard Hills University of Cambridge Mark Holdaway NRAO Tucson.

Presented At AMS Meeting, Long Beach, CA, 2003 Aerosol Phase Function And Size Distributions From Polar Nephelometer Measurements During The SEAS Experiment.

Figure 1.1 The observer in the truck sees the ball move in a vertical path when thrown upward. (b) The Earth observer views the path of the ball as a parabola.

OSMOSIS Primary Production from Seagliders April-September 2013 Victoria Hemsley, Stuart Painter, Adrian Martin, Tim Smyth, Eleanor Frajka-Williams.

1.5 Find Slope and Rate of Change E. Q. How do I find Slope and Rate of Change???

Lidar algorithms to retrieve cloud distribution, phase and optical depth Y. Morille, M. Haeffelin, B. Cadet, V. Noel Institut Pierre Simon Laplace SYMPOSIUM.

Data Processing of IOP Packages Attenuation, Absorption and Backscattering c, a, b b Ian Walsh, Ph.D. Director of Science, Sea-Bird Scientific.

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 aerosol components from multiwavelength/depolarization measurements Nobuo SUGIMOTO, Tomoaki Nishizawa, and Atsushi Shimizu National Institute.

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.

Real part of refractive index ( m r ): How matter slows down the light: where c is speed of light Question 3: Into which direction does the Scattered radiation.

Flow cytometry: characterizing particles towards the submicron scale

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:

VSF as a proxy for Particle Size Distribution Pauline Stephen.

Backscattering Lab Julia Uitz Pauline Stephen Wayne Slade Eric Rehm.

Models for Scattering Curtis Mobley Copyright © 2011 by Curtis D. Mobley Ocean Optics Summer Class Calibration and Validation for Ocean Color Remote Sensing.

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.

When light passes from vacuum (index of refraction n = 1) into water (n = 1.333), Q the wavelength increases and the frequency is unchanged 2. the.

Particulate Organic Carbon (POC) measured from satellites Wilford Gardner Mary Jo Richardson Young Baek Son Alexey Mishonov Texas A&M University Fulbright.

Rick Reynolds and Dariusz Stramski Measurements of IOPs and Characterization of Particle Assemblages for Monterey Bay Experiment Marine Physical Laboratory.

Preliminary results and uncertainties of scattering measurements for SORTIE Michael Twardowski 1, Scott Freeman, Jim Sullivan, Ron Zaneveld, Chuck Trees,

The link between particle properties (size, composition, shape, internal structure) and IOP Emmanuel Boss.

Scattering and attenuation and tracking uncertainties for cal/val.

The Asian Dust Events of April 1998 Prepared by: R. B. Husar, D. Tratt, B. A. Schichtel, S. R. Falke, F. Li D. Jaffe, S. Gassó, T. Gill, N. S. Laulainen,

Drizzle measurements with the HSRL and the KAZR: sensitivity to assumptions Ed Eloranta University of Wisconsin-Madison

AEROSOL CLASSIFICATION RETRIEVAL ALGORITHMS FOR EARTHCARE/ATLID, CALIPSO/CALIOP, AND GROUND-BASED LIDARS Sugimoto, N., T. Nishizawa, I. Matsui, National.

OCEAN ROBOTS: WHAT? HOW? WHY? * Lesson Plan PPT to use with students *

APPLICATIONS Investigate the « particulate biomass » distribution along a size continuum and its variability in relation with W/E gradient or with different.

Remote sensing of coastal habitats: Challenges: Adjacency effects Atmospheric correction (no null NIR band) Currently addressed by Europeans (e.g. Belcolour)

Fluorescence Line Height (FLH) and Fluorescence Quantum Yield (FQY)

Direct Numercal Simulation of two-phase turbulent boundary layer over waved water surface O. A. Druzhinin, Yu.I. Тroitskaya Institute of Applied Physics.

METR Introduction to Synoptic Meteorology Other upper air sounding systems, apart from radiosondes University of Oklahoma 2004.

Refraction Chapter 12 (p ). Refraction Refraction: The bending or change in direction of light when it travels at an angle from one medium into.

Inferring CALIPSO backscattering data over Antarctica during spring Term paper presentation for EAS-6792 Shekhar Chandra, EAS.

Lab 4 Scattering. Samples: Platymonas * Chaetoceros * Arizona 'Dust' *Wikipedia Damariscotta River Estuary.

REFRACTION OF LIGHT. BEHAVIOR OF LIGHT Light acts both as a wave and as a particle Called a “wavicle” Light needs to interact with a surface in order.

Part II: Implementation of a New Snow Parameterization EXPLICIT FORECASTS OF WINTER PRECIPITATION USING AN IMPROVED BULK MICROPHYSICS SCHEME Thompson G.,

Light Scattering Biophysics

Quantifying SPM in estuaries and coastal seas

Feng Peng and Steven Effler

OBJECTIVES Develop an understanding of variability in the relationships between particulate organic carbon (POC), light scattering, and ocean color Develop.

Estimating Suspended Solid Concentration from ADCP measurements

(B.P :51) ( B:P52 ).

'. \s\s I. '.. '... · \ \ \,, I.

Wayne Slade Ocean Optics Summer 2004

Improper localization of the NR2B subunit in synaptic and perisynaptic regions in YF/YF mice. Improper localization of the NR2B subunit in synaptic and.

Backscatter and Chlorophyll

Groundwater Learning objectives

Franklin SS, et al. Circulation 2009;119:243-50

Fig. 1. Location of the study site (23-28 S, W)

Figure S1 - Cunha - de Padua et al

' '· \ ·' ,,,,

Index of Refraction and Speed of Light

Mid Atlantic Water Property Measurements W. S

IOP2b: 2013/12/11.

Generation of Titanic Prime Numbers Through High Performance Computing

Rate of change and slope

CALIPSO First-Light Observations – All 3 Lidar Channels

Fig. 3 Electron PSD in various regions.

Fig. 1 Measurement setup and crystal structure.

Fig. 1 X-ray scattering and EBSD analyses of the bulk Fe25Co25Ni25Al10Ti15 HEA. X-ray scattering and EBSD analyses of the bulk Fe25Co25Ni25Al10Ti15 HEA.

Presentation transcript:

CBLAST RU05 glider SAM data 02/02/06

Sampling map

Time-space coordination of glider and vertical profiling

Water type coordination

Vicarious calibration: backscattering VP glider =s1* – 0.003

Vicarious calibration: attenuation =ln(S1/S2)*0.88 – 0.28 VP glider

Glider SAM: 09/06-10/03 attenuation wind speed (m s -1 )

Glider SAM: 09/06-10/03 backscattering

Glider SAM: 09/06-10/03 b bp /c pg

Glider SAM: 09/06-10/03 bulk particulate refractive index np= *(bbp650/bp650)^0.582 Twardowski et al. 2001

Glider SAM: 09/06-10/03 bulk particle density rho=(np-1.03)/ Twardowski et al. 2004

Glider SAM: 09/06-10/03 visibility visibility=4.8/(cpg650* ) Zaneveld and Pegau 2001

Size distribution slope from current glider measurements…? Fig. 3. Depolarization ratio and nonsphericity index for a sample from 15 m in the western Atlantic, collected October 19, with slope of PSD? ECO-BB3 bbp(532,650) [unpolarized, S11] SAM bbp(650) [polarized, S11-S12]

Testing depolarization with VP data