Dar A. Roberts1, Keely Roth1, Michael Alonzo1

Slides:



Advertisements
Similar presentations
Surface Heat Balance Analysis by using ASTER and Formosat-2 data
Advertisements

Beyond Spectral and Spatial data: Exploring other domains of information GEOG3010 Remote Sensing and Image Processing Lewis RSU.
Scaling Biomass Measurements for Examining MODIS Derived Vegetation Products Matthew C. Reeves and Maosheng Zhao Numerical Terradynamic Simulation Group.
Nitrogen Mineralization Across an Atmospheric Nitrogen Deposition Gradient in Southern California Deserts Leela E. Rao 1, David R. Parker 1, Andrzej Bytnerowicz.
VEGETATION MAPPING FOR LANDFIRE National Implementation.
Optical Imaging and Field Spectroscopy: CLPX 2002 and 2003 Thomas H. Painter.
Time series of coarse resolution satellite imagery: some experiences and caveats Agustín Lobo A contribution to the GLOBAL LAND COVER.
The Effects of Site and Soil on Fertilizer Response of Coastal Douglas-fir K.M. Littke, R.B. Harrison, and D.G. Briggs University of Washington Coast Fertilization.
August 5 – 7, 2008NASA Habitats Workshop Optical Properties and Quantitative Remote Sensing of Kelp Forest and Seagrass Habitats Richard C. Zimmerman -
MODIS Science Team Meeting - 18 – 20 May Routine Mapping of Land-surface Carbon, Water and Energy Fluxes at Field to Regional Scales by Fusing Multi-scale.
03/06/2015 Modelling of regional CO2 balance Tiina Markkanen with Tuula Aalto, Tea Thum, Jouni Susiluoto and Niina Puttonen.
Giant Kelp Canopy Cover and Biomass from High Resolution SPOT Imagery for the Santa Barbara Channel Kyle C Cavanaugh, David A Siegel, Brian P Kinlan, Dan.
Remote Mapping of River Channel Morphology March 9, 2003 Carl J. Legleiter Geography Department University of California Santa Barbara.
Department of Geography, University of California, Santa Barbara
Mapping Roads and other Urban Materials using Hyperspectral Data Dar Roberts, Meg Gardner, Becky Powell, Phil Dennison, Val Noronha.
Digital Imaging and Remote Sensing Laboratory Real-World Stepwise Spectral Unmixing Daniel Newland Dr. John Schott Digital Imaging and Remote Sensing Laboratory.
CSIRO LAND and WATER Estimation of Spatial Actual Evapotranspiration to Close Water Balance in Irrigation Systems 1- Key Research Issues 2- Evapotranspiration.
Val Noronha University of California, Santa Barbara Centerline Extraction and Road Condition.
1 Impervious Surface Mapping with Multi-Spectral Remote Sensing Dr. Qihao Weng Associate Professor of Geography; Director, Ctr. Urban & Environmental Change.
Remote Sensing Hyperspectral Remote Sensing. 1. Hyperspectral Remote Sensing ► Collects image data in many narrow contiguous spectral bands through the.
Liane Guild, Brad Lobitz, Randy Berthold, Jeremy Kerr Biospheric Science Branch, NASA Ames Research Center, CA Roy Armstrong, James Goodman University.
Scale Effect of Vegetation Index Based Thermal Sharpening: A Simulation Study Based on ASTER Data X.H. Chen a, Y. Yamaguchi a, J. Chen b, Y.S. Shi a a.
An Introduction to Using Spectral Information in Aerosol Remote Sensing Richard Kleidman SSAI/NASA Goddard Lorraine Remer UMBC / JCET Robert C. Levy NASA.
Introduction To describe the dynamics of the global carbon cycle requires an accurate determination of the spatial and temporal distribution of photosynthetic.
High Spectral Resolution Infrared Land Surface Modeling & Retrieval for MURI 28 April 2004 MURI Workshop Madison, WI Bob Knuteson UW-Madison CIMSS.
PREFER 1 st Annual Review Meeting, 5-6 Dec 2013, Milano-Italy PREFER WP 3.2 Information support to Recovery/Reconstruction Task 7 Damage Severity Map PREFER.
Giant Kelp Canopy Cover and Biomass from High Resolution Multispectral Imagery for the Santa Barbara Channel Kyle C Cavanaugh, David A Siegel, Brian P.
The University of Mississippi Geoinformatics Center NASA MRC RPC – 11 July 2007 Greg Easson, Ph.D. Robert Holt, Ph.D. A. K. M. Azad Hossain University.
Translation to the New TCO Panel Beverly Law Prof. Global Change Forest Science Science Chair, AmeriFlux Network Oregon State University.
L-band Microwave Emission of the Biosphere (L-MEB)
William Crosson, Ashutosh Limaye, Charles Laymon National Space Science and Technology Center Huntsville, Alabama, USA Soil Moisture Retrievals Using C-
Remote Sensing. Vulnerability is the degree to which a system is susceptible to, or unable to cope with, adverse effects of climate change, including.
Generating fine resolution leaf area index maps for boreal forests of Finland Janne Heiskanen, Miina Rautiainen, Lauri Korhonen,
How Do Forests, Agriculture and Residential Neighborhoods Interact with Climate? Andrew Ouimette, Lucie Lepine, Mary Martin, Scott Ollinger Earth Systems.
PREFER 1 st Annual Review Meeting, 5-6 Dec 2013, Milano-Italy PREFER WP 3.2, Task 7.
Canada Centre for Remote Sensing Field measurements and remote sensing-derived maps of vegetation around two arctic communities in Nunavut F. Zhou, W.
VQ3a: How do changes in climate and atmospheric processes affect the physiology and biogeochemistry of ecosystems? [DS 194, 201] Science Issue: Changes.
Remote Analysis of Asian Cold Desert Ecosystems Cheney M. Shreve & Gregory S. Okin: Univ. of Virginia and Univ. of California, Los Angeles Remote Analysis.
Spectral classification of WorldView-2 multi-angle sequence Atlanta city-model derived from a WorldView-2 multi-sequence acquisition N. Longbotham, C.
Remote Sensing of Vegetation. Vegetation and Photosynthesis About 70% of the Earth’s land surface is covered by vegetation with perennial or seasonal.
BIOPHYS: A Physically-based Algorithm for Inferring Continuous Fields of Vegetative Biophysical and Structural Parameters Forrest Hall 1, Fred Huemmrich.
Spectral unmixing of vegetation, soil and dry carbon cover in arid regions: comparing multispectral and hyperspectral observations G.P.Asner and K.B.Heidebrecht.
Disturbance Effects on Carbon Dynamics in Amazon Forest: A Synthesis from Individual Trees to Landscapes Workshop 1 – Tulane University, New Orleans, Late.
Validation of MODIS Snow Mapping Algorithm Jiancheng Shi Institute for Computational Earth System Science University of California, Santa Barbara.
Status of the MODIS Land-Surface Temperature/Emissivity Product: New Validations and Improvements Zhengming Wan University of California, Santa Barbara.
Scaling Up Above Ground Live Biomass From Plot Data to Amazon Landscape Sassan S. Saatchi NASA/Jet Propulsion Laboratory California Institute of Technology.
How Do Forests, Agriculture and Residential Neighborhoods Interact with Climate? Andrew Ouimette, Lucie Lepine, Mary Martin, Scott Ollinger Earth Systems.
LiDAR Remote Sensing of Forest Vegetation Ryan Anderson, Bruce Cook, and Paul Bolstad University of Minnesota.
Characterizing the Physical Environment of Urban Centers in Rondônia with Landsat ETM+ Rebecca L. Powell 1 and Dar A. Roberts 2 Department of Geography,
Spectral and Structural Differences Between Coniferous and Broadleaf Forest derived from LIDAR and AVIRIS Dar A. Roberts 1, Keely L. Roth 2, Eliza Bradley.
Hyperspectral remote sensing
Spectral Discrimination of Plant Functional Types and Species across diverse North American Ecosystems Dar A. Roberts 1, Keely L. Roth 2, Philip E. Dennison.
Ira Leifer 1, Rob Green 2, Randy Albertson 3, Eliza Bradley 1, Roger Clark 4, Philip Dennison 5, Michael Eastwood 2, Michael Goodman 3, Anthony Guillory.
Airborne Hyperspectral Research & Development for Invasive Species Detection and Mapping Kenneth McGwire 1, Timothy Minor 1, Bradley Schultz 2, and Christopher.
Beyond Spectral and Spatial data: Exploring other domains of information: 3 GEOG3010 Remote Sensing and Image Processing Lewis RSU.
SIMULATION OF ALBEDO AT A LANDSCAPE SCALE WITH THE D.A.R.T. MODEL AN EFFICIENT TOOL FOR EVALUATING COARSE SCALE SATELLITE PRODUCTS? Sylvie DUTHOIT*, Valérie.
Science Enabled by New Hyperspectral Observations Related to Physiology and Functional Types (HyspIRI) Dar Roberts, Frank Muller-Karger Reiterate Break.
Water Stress and Fluorescence Detection in Crop Canopies with AHS Thermal Imagery: simulations with FluorMOD Airborne Imaging Spectroscopy Workshop 7 Oct.
References: 1)Ganguly, S., Samanta, A., Schull, M. A., Shabanov, N. V., Milesi, C., Nemani, R. R., Knyazikhin, Y., and Myneni, R. B., Generating vegetation.
Assessing Annual Forest Ecological Change in Western Canada Using Temporal Mixture Analysis of Regional Scale AVHRR Imagery Over a 14 Year Period Joseph.
Remote Sensing Section Global soil monitoring and mineral mapping from emerging remote sensing technologies Sabine Chabrillat and the group “hyperspectral.
Using vegetation indices (NDVI) to study vegetation
HIERARCHICAL CLASSIFICATION OF DIFFERENT CROPS USING
Ungrazed deep grassland
Why LiDAR makes hyperspectral imagery more valuable for forest species mapping OLI 2018 Andrew Brenner, Scott Nowicki & Zack Raymer.
Lecture 9: Spectroscopy
Figure 1. Spatial distribution of pinyon-juniper and ponderosa pine forests is shown for the southwestern United States. Red dots indicate location of.
By: Paul A. Pellissier, Scott V. Ollinger, Lucie C. Lepine
Sources of Variability in Canopy Spectra and the Convergent Properties of Plants Funding From: S.V. Ollinger, L. Lepine, H. Wicklein, F. Sullivan, M. Day.
VALIDATION OF FINE RESOLUTION LAND-SURFACE ENERGY FLUXES DERIVED WITH COMBINED SENTINEL-2 AND SENTINEL-3 OBSERVATIONS IGARSS 2018 – Radoslaw.
Presentation transcript:

Evaluation of Synergies between VNIR-SWIR and TIR imagery in a Mediterranean-climate Ecosystem Dar A. Roberts1, Keely Roth1, Michael Alonzo1 Contributors: Dale A. Quattrochi2, Glynn C. Hulley3, Simon J. Hook3, and Robert O. Green3 1 UC Santa Barbara Dept. of Geography 2 NASA Marshall Space Flight Center 3 NASA Jet Propulsion Laboratory NASA HyspIRI Preparatory Program

Research Questions What is the potential for improved temperature emissivity separation (TES) using VNIR-SWIR column water vapor? What is the relationship between moisture content and emissivity? What is the relationship between common hyperspectral measures of plant stress and physiological function (i.e., PRI, leaf water content) and canopy temperature in imagery and observed in ground-based measurements? How does canopy temperature vary as a function of plant functional type (PFT) and species at native and HyspIRI spatial scales? How is canopy temperature and emissivity impacted by changes in canopy cover, notably changes in green vegetation (GV) fraction, non-photosynthetic vegetation (NPV) and bare soil? How is temperature partitioned among the various components of cover?

General Approach AVIRIS Analysis MASTER Analysis Reflectance Retrieval with 7.5, 15 and 60 m radiance data Reflectance, retrieval products (water vapor, liquid water) Cover Fractions and Species/PFT identification Multiple Endmember Spectral Mixture Analysis Fused field and AVIRIS-derived spectral library (7.5 m) Iterative Endmember Selection, cover class (i.e., bark, composite shingle, oak), species Multi-level fusion (2, 3, 4 em models, selected based on an RMS threshold) AVIRIS water content, hyperspectral stress indices (PRI) MASTER Analysis Atmospheric correction Modtran simulated, AVIRIS column water vapor Temperature Emissivity Separation (TES): TES, using ASTER algorithm (Gillespie et al.) Combined analysis of image pairs Full spectral analysis (VSWIR-TIR) of plant materials seasonally

Santa Barbara Study Site Pre-fire August 6, 2004 (16 m) August 6-12, 2007 (4 m): urban June 19, 2008: AVIRIS-MASTER Pair Post-fire March 10, 2009 (post Gap & Tea, pre-Jesusita) March 31, 2009 (post Gap & Tea, pre-Jesusita) May 8, 2009 (Active Jesusita) June 17, 2009 August 26, 2009 April 30, 2010 October 26, Nov 1, 2010 July 19, 2011: AVIRIS-MASTER Pair True Color: August 6, 2004

AVIRIS Species and Plant Functional Types Existing, accurate maps of species, PFT generated using MESMA and Iterative Endmember Selection Existing network of species polygons Existing reference spectral library of natural and anthropogenic materials

Synergies between VNIR-SWIR and TIR in an urban Environment: RSE, in press Mixed urban-natural systems, ~ 150,000 people AVIRIS-MASTER pair, June 19, 2008 7.5 m AVIRIS, 15 m MASTER Spatial degradation, 15 m AVIRIS, 60 m AVIRIS/MASTER

Methods Preprocessing AVIRIS Analysis AVIRIS-MASTER georectified to high resolution DOQQ AVIRIS Analysis ACORN 5, applied to 7.5, 15 and 60 m radiance data Reflectance, water vapor, liquid water, albedo (Modo 4.3 Irradiance) Surface Composition VIS Model (Vegetation, Impervious, Soil expanded to include NPV) Multiple Endmember Spectral Mixture Analysis Fused field and AVIRIS-derived spectral library (7.5 m) Count-based Endmember Selection, cover class (i.e., bark, composite shingle, oak) Multi-level fusion (2, 3, 4 em models, selected based on 0.007 RMS threshold) Water screened by LST (< 297.15K) MASTER Analysis (Hulley and Hook) Temperature Emissivity Separation (TES) Modtran 5.2 derived atmospheric correction NCEP column water vapor, iteratively adjusted for water over Laguna Blanca TES, using ASTER algorithm (Gillespie et al.) Spectral emissivity, broad band emissivity, LST

Land-Cover Analysis/Mixture Validation (Quattrochi and Roberts) Defined 14 dominant land-cover classes on Google Earth Imagery Residential (high, medium, low), Commercial, Transportation, Roofs Closed canopy forest, Forested park, Golf courses, Grass sports fields, Orchards, Annual crop Bare soil, crop Extracted GV, NPV, Impervious, Soil fractions and land surface energy properties Developed Mixture Validation Data Sets from NAIP 120x120 m polygons (ranges in surface fractions) Large, mixed land-cover polygons

Land-Cover Analysis: Examples

Mixture Validation Utilized 85 polygons 64 land-cover 21 designed Calculated fractions from high-res imagery Manually delineated polygons for GV, NPV, Soil and Impervious Determination aided by AVIRIS A C B Figure showing three validation polygons A: 44% NPV, 11.3% GV, 44.7% Soil B: 50.45%NPV, 1.5% GV, 48%Soil C: 4.8% NPV, 57.4% GV, 34.5% Soil, 3.3% Imp

Results AVIRIS-MASTER Products Fine spatial scale variability in water vapor Elevation gradients clear AVIRIS 1.2 – 1.7 cm, MASTER 0.78 cm Liquid water and emissivity positively correlated Asphalt also high emissiivty Albedo and LST poorly correlated

Reflectance and Emissivity Spectra Biotic Materials – Most Distinct in VSWIR (all unique) NPV low emissivity in TIR (Differs by stature) Abiotic Materials – Varies AVIRIS: Painted roofs, red tile Soils and some road surfaces are not distinct* MASTER: Quartz beach sands, various roof types Asphalt surfaces are near black bodies VSWIR-TIR improves discrimination of abiotic materials

MESMA: Endmember Selections Selected 41 non-water endmembers 4 NPV, 8 GV, 9 soils, 20 Impervious GV strictly AVIRIS, transportation field, roofs, soils, NPV mixed

VIS-NPV Fractions: 15 and 60 m GV and NPV fractions scaled well between all spatial resolutions 7.5, 15 and 60 m Soil tended to be overmapped at the expense of Impervious at coarser scales Two error sources Asphalt – soil Red Tile Roof (so variable requires 3 ems)

Fraction Validation: 15 m a) GV b) NPV c) Impervious d) Soil Phenology Under- mapped Soil Overmapped (red tile/Asphalt)

Fraction Validation: 60 m a) GV b) NPV GV-NPV Fractions good at HyspIRI scales c) Impervious d) Soil

Land-cover Composition Cover fractions follow the expected pattern High GV, low Temperature High Impervious, high Temperature Residential Low density, high GV, Low T, low Imp High density, low GV, High T, High Imp 306K 325K

Green Cover and LST Standard inverse relationship between GV Cover and LST Considerable scatter The scatter is likely to be the most interesting part Moist soils evapotranspiring Closed canopies with variable ET

What’s Next? TES with AVIRIS derived column water vapor Spatial variation in LST in closed canopies VSWIR stress measures Analysis of new AVIRIS-MASTER pair, 2011 Greater areal coverage, including greater elevation range, Gap, Tea and Jesusita Fire scars and a wide diversity of natural vegetation Seasonal VSWIR-TIR spectroscopy JPL Perkin Elmer, ASD and Nicolet 17 tree species, chlorophyll, water First measures late July 2011 Follow up, Nov/Dec 2011, Mar 2012, June 2012 Source: Mike Alonzo, Keely Roth

Example VSWIR-TIR Spectra Quercus agrifolia Coast Live Oak Magnolia grandiflora Southern Magnolia Ceanothus spinosus Green bark Ceanothus Metrosideros excelsa New Zealand Christmas Tree Each plot shows the concatenated Perkin Elmer (VNIR-SWIR) and Nicolet (TIR) spectra for two samples.

Questions?