MODIS BRDF/Albedo Products from Terra and Aqua - PowerPoint PPT Presentation

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MODIS BRDF/Albedo Products from Terra and Aqua

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MODIS BRDF/Albedo Products from Terra and Aqua Crystal Schaaf Alan Strahler, Xiaowen Li, Jonathan Salomon, Jicheng Liu, Feng Gao et al. Department of Geography – PowerPoint PPT presentation

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Title: MODIS BRDF/Albedo Products from Terra and Aqua


1
MODIS BRDF/Albedo Products from Terra and Aqua
  • Crystal Schaaf
  • Alan Strahler, Xiaowen Li, Jonathan Salomon,
    Jicheng Liu, Feng Gao et al.
  • Department of Geography
  • Boston University
  • (schaaf_at_bu.edu)

2
MODIS BRDF/Albedo Algorithm
  • BRDF modellinear combination of a constant
    (fiso) and two weighted (fvol, fgeo)
    trigonometric functions (kvol, kgeo) derived
    from physical models of volumetric and
    geometric-optical surface scattering.
  • Full model inversions are used when sufficient
    high quality atmospherically-corrected cloud-free
    observations are available over a 16-day period
    to adequately sample the BRDF.
  • Otherwise, lower quality magnitude inversions are
    performed which couple a priori knowledge of the
    surface anisotropy with any high quality MODIS
    observations that are available for a location.

3
MODIS BRDF/Albedo Standard Products
  • Collection 4 (V004) reprocessed MODIS Land
    Products (March 2000 to present).
  • BRDF Model Parameters
  • MODIS bands 1-7 plus three broadbands
  • Albedos
  • white-sky and black-sky (at local solar noon)
  • Nadir BRDF-Adjusted Reflectances (NBAR)
  • MODIS bands 1-7
  • Extensive Quality Assurance Flags
  • Quality of the product, processing method used,
    and whether a snow or snow-free albedo was
    retrieved.
  • Blue-sky albedos
  • Can be computed as an interpolation between
    black-sky and white-sky albedos as a function of
    diffuse skylight.
  • Validated Stage-1
  • Product accuracy has been estimated using a small
    number of independent measurements obtained from
    selected locations and time periods and
    ground-truth/field program effort.

4
MODIS BRDF/Albedo Standard Products
  • V005 Level2G/Level3 Standard Land Products
    (MCD43B)
  • HDF-EOS
  • Sinusoidal equal-area projection
  • Tiles - 1200x1200 pixels for the 1-km products
  • Tiles 2400x2400 pixels for the 500-m products
  • Revised format and QA (snow and mandatory
    separate bytes)
  • V005 Climate Modeling Grid Products (CMG)
    (MCD43C)
  • HDF-EOS
  • Geographic (lat/lon) projection
  • Coarse resolution - 0.05degree (3 arc min or
    5km)
  • Include snow free version
  • Revised format and QA

5
NBAR
January 1-16, 2001 (2001001) April 7-22, 2001
(2001097)
July 12-27, 2001 (2001193) October 16-31, 2001
(2001289)
6
Albedo of Sahara
1 km albedo RGB composite
7

CMG Broadband White-Sky Albedo (0.3-5.0mm)January
2001
No Data
8
CMG Broadband White-Sky Albedo (0.3-5.0mm)June
2001
No Data
9
Spatially Complete Snow-Free MODIS Albedo Product
  • MODIS Atmosphere Group- Eric Moody
  • Fill values, poorest quality results, and
    seasonally snow covered results are replaced with
    temporal estimations and spatial interpolation.
  • 1 arc minute geographic lat/lon
  • http//modis-atmos.gsfc.nasa.gov/ALBEDO/index.html

0.0 0.8
Moody, E. G., M. D. King, S. Platnik, C. B.
Schaaf, F. Gao, Spatially Complete Surface Albedo
Datasets Value-Added Products Derived from Terra
MODIS Land Products, IEEE, Trans Geosci. Remote
Sens., 2005.
10
Spatially Complete White-Sky AlbedoJanuary 1-16,
2002
Snow-free
0.8
0.6
Surface Albedo (0.86 µm)
Snow-covered
0.4
0.2
0.0
11
Combined Aqua Terra Processing
  • BRDF specification requires multiple observations
    to capture anisotropy across viewing/illumination
    geometry
  • Combining observations from Aqua and Terra
  • Increase high-quality inversions
  • Best fit BRDF model retrieved directly from
    observations
  • Fewer lower-quality retrievals using the back-up
    algorithm
  • Back-up method relies on a priori designation of
    BRDF
  • Combined AquaTerra V004 reprocessing completed
    Jan 05
  • V005 MCD43 product only (Terra alone prior to
    May 2002)

12
CMG Broadband Black-sky Albedo (0.3-5.0mm) Terra
(April 2004) Terra Aqua
13
CMG Broadband Black-sky Albedo (0.3-5.0mm) Terra
(April 2004) Terra Aqua
Green high quality Red poorer quality
14
V005 500m White-Sky Albedo
2001193
500m 1km
15
Validation Sites
  • Baseline Surface Radiation Network (BSRN)
  • http//bsrn.ethz.ch/
  • SURFRAD Network (US BSRN sites)
  • http//www.srrb.noaa.gov/surfrad/index.html
  • EOS core validation sites (200x200 pixels
    subsets)
  • http//modis-land.gsfc.nasa.gov/val/coresite_gen.a
    sp
  • MODIS 7x7 pixel subsets in ascii at ORNL
  • 276 sites (BSRN stations archiving albedo, EOS
    core sites, and Flux network sites
  • http//www.modis.ornl.gov/modis/index.cfm
  • Greenland Climate Network (GC-Net) Automatic
    Weather Stations (AWS) -
  • Stroeve, J., J. E. Box, F. Gao, S. Liang, A.
    Nolin, C. Schaaf, Accuracy Assessment of the
    MODIS 16-day Albedo Product for Snow
    Comparisons with Greenland in situ Measurements ,
    doi10.1016/j.rse.2004.09.001, Remote Sens.
    Environ., 2004.
  • Validated Stage-1
  • Product accuracy has been estimated using a small
    number of independent measurements obtained from
    selected locations and time periods and
    ground-truth/field program effort.

16
Fort Peck, Montana V004, 2003
17
ARM SGP Central Site V004, 2003
18
Boulder, CO V004, 2003
19
Desert Rock, NV V004, 2003
20
Validation with Greenland in situ Measurements
  • Description of the Greenland GC-Net AWS Albedo
    Measurements
  • Upward and downward shortwave radiation fluxes
    are measured at several AWS distributed widely in
    latitude and elevation using pairs LI-COR 200SZ
    photoelectric diode pyranometers (0.4 ?m 1.1
    ?m).
  • A correction to the LI-COR albedo are made to
    convert them from a narrowband albedo (e.g. 0.4
    ?m 1.1 ?m) to a broadband (0.285 ?m 2.8 ?m)
    albedo.
  • Comparisons with precision pyranometers suggest a
    residual uncertainty with an RMSE of 0.035
    (absolute albedo).

21
MODIS Albedo Vs Greenland In Situ Albedo
Comparison between MOD43 16-day albedo and 16-day
in situ albedo for both black sky (triangles) and
white sky (squares) albedo for 15 Greenland AWS
stations. MODIS albedo from both the main
(closed symbols) and backup (open symbols)
algorithm results are shown.
Stroeve, J., J. Box, F. Gao, S. Liang, A. Nolin,
C. Schaaf, Accuracy Assessment of the MODIS
16-day Albedo Product for Snow Comparisons with
Greenland in situ Measurements., Remote Sens.
Environ., 94, 46-60, 2005.
22
Albedo/BRDF References
  • Gao, F., C. Schaaf, A. Strahler, A. Roesch, W.
    Lucht, and R. Dickinson, The MODIS BRDF/Albedo
    Climate Modeling Grid Products and the
    Variability of Albedo for Major Global Vegetation
    Types, J. Geophys. Res., 110, D01104,
    doi10.1029/2004JD005190. 2005.
  • Moody, E. G., M. D. King, S., Platnick, C. B.
    Schaaf, and F. Gao, Spatially complete global
    spectral surface albedos Value-added datasets
    derived from Terra MODIS land products. IEEE
    Trans. Geosci. Remote Sens., 43, 144-158, 2005.
  • Stroeve, J., J. Box, F. Gao, S. Liang, A. Nolin,
    C. Schaaf, Accuracy Assessment of the MODIS
    16-day Albedo Product for Snow Comparisons with
    Greenland in situ Measurements., Remote Sens.
    Environ., 94, 46-60, doi10.1016/j.rse.2004.09.001
    , 2005.
  • Roesch, A., C. Schaaf and F. Gao, Use of
    Moderate-Resolution Imaging Spectroradiometer
    bidirectional reflectance distribution function
    products to enhance simulated surface albedos, J.
    Geophys. Res., 109, D12, doi 10.1029/2004JD004552
    , 2004.
  • Tian, Y., R. E. Dickinson, L. Zhou, R. B. Myneni,
    M. Friedl, C. B. Schaaf, M. Carroll, and F. Gao,
    Land boundary conditions from MODIS data and
    consequences for the albedo of a climate model,
    Geophys. Res. Let., 31, doi10.1029/2003GL019104,
    2004.
  • Wang, Z., X. Zeng, M. Barlage, R. E. Dickinson,
    F. Gao, and C. Schaaf, Using MODIS BRDF and
    Albedo Data to Evaluate Global Model Land Surface
    Albedo, J. Hydrometeor., 5, 3-14, 2004.
  • Zhou, L.et al., Comparison of seasonal and
    spatial variations of albedos from
    Moderate-Resolution Imaging Spectroradiometer
    (MODIS) and Common Land Model. J. Geophys. Res.,
    108, D15, 4488, doi10.1029/2002JD003326, 2003.
  • Gao et al., Detecting vegetation structure using
    a kernel-based BRDF model. Remote Sens. Environ.,
    86(2), 198-205, 2003.
  • Oleson et al., Assessment of global climate model
    land surface albedo using MODIS data, Geophys.
    Res. Letters, 30(8), 1443, doi10.1029/2002GL01674
    9, 2003.
  • Jin et al., Consistency of MODIS surface
    BRDF/Albedo retrievals 1. Algorithm performance,
    J. Geophys. Res., 108(D5), 4158,
    doi10.1029/2002JD002803, 2003.
  • Jin et al., Consistency of MODIS surface
    BRDF/Albedo retrievals 2.Validation, J.Geophys.
    Res., 108, 4159, doi10.1029/2002JD002804, 2003.
  • Schaaf et al., First Operational BRDF, Albedo and
    Nadir Reflectance Products from MODIS, Remote
    Sens. Environ., 83, 135-148, 2002.
  • Liang et al., Validating MODIS Land Surface
    Reflectance and Albedo Products Methods and
    Preliminary Results, Remote Sens. Environ., 83,
    149-162, 2002.
  • Jin et al., Improving MODIS Surface BRDF/Albedo
    Retrieval with MISR Multi-angle Observations,
    IEEE Trans. Geosci. Remote Sens., 40, 1593-1604,
    2002.
  • Jin et al., How does snow impact the albedo of
    vegetated land surfaces as analyzed with MODIS
    data?, Geophys. Res. Let., 29, 10.1029/2001GL01413
    2, 2002.
  • Tsvetsinskaya et al., Relating MODIS derived
    surface albedo to soils andlandforms over
    Northern Africa and the Arabian Peninsula,
    Geophys. Res. Let., 29, 10.1029/2001GL014096,
    2002.
  • Gao et al., Bidirectional NDVI and
    Atmospherically Resistant BRDF Inversion for
    Vegetation Canopy, IEEE Trans. Geosci. Remote
    Sens., 40, 1269-1278, 2002.
  • MODIS BRDF/Albedo User Guide (http//geography.bu.
    edu/brdf/userguide/index.html)
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