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Linking In situ Measurements, Remote Sensing, and Models to Validate MODIS Products Related to the Terrestrial Carbon Cycle. Warren B. Cohen USDA Forest Service. Stith T. Gower University of Wisconsin. David P. Turner Oregon State University. Steven W. Running University of Montana. - PowerPoint PPT Presentation
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Linking In situ Measurements, Remote Sensing, andModels to Validate MODIS Products Related
to the Terrestrial Carbon Cycle
Peter B. Reich, University of Minnesota
Warren B. CohenUSDA Forest Service
Stith T. GowerUniversity of Wisconsin
David P. TurnerOregon State University
Steven W. RunningUniversity of Montana
MODLAND Validation Meeting, January 22 & 23, 2001
Objectives(MODIS Validation & Ecological Science)
• Provide high quality, site-specific data layers at several sites that can be compared to MODIS and other sensor products (land cover, LAI, NPP)
•Develop better understanding of the climatic and ecological controls on totalnet primary production and carbon allocation within and among biomes
• Learn how flux tower-measured NEEand field-measured NPP co-vary in time& how to translate between them using ecological models
• Explore errors and information lossesthat accrue when generalizing detailedecological information through remotelysensed data and models
Sites
BOREAS Northern Old Black Spruce (NOBS)
muskeg (open black spruce),
“closed” black spruce, aspen,
wetlands
Harvard Forest (HARV) LTER
mixed hardwoods, eastern hemlock,
red pine, old-field meadow
Konza Prairie Biological Station (KONZ) LTER
tallgrass, shortgrass, shrub, gallery forest; grazing and burning regimes
Bondville Agricultural Farmland (AGRO) corn, soybeans
Field-BasedSampling Design
100 25m2 plots
80 in a nested spatial series
20 plots broadly distributed
Plot measurements
Vegetation cover
LAI, fAPAR
Aboveground biomass
Aboveground productivity
Belowground productivity
•Ecosystem properties (e.g, LAI)highly variable in space
•Tower footprints notnecessarily representative ofgreater site area
•Specific crop types can havevery different productivity levels
•A given crop can vary inproductivity among years
July August
Overall Accuracy: 95%
2000 AGRO
Corn LAI=4.41+0.63*CCIcj R2=0.61
Soy LAI=1.54+0.49*CCIsj R2=0.58
ETM+ predictions of July LAI
Corn LAI=4.00+0.45*CCIca R2=0.63
Soy LAI=3.44+0.49*CCIsa R2=0.27
ETM+ predictions of Aug. LAI
July LAI
0
1
2
3
4
5
6
7
0 1 2 3 4 5 6 7
Predicted (n-1 jackknife)
Ob
serv
ed
Corn
Soybeans
RMSE=0.45Slope=0.99Intercept=0.01R=0.95
1:1
August LAI
0
1
2
3
4
5
6
7
0 1 2 3 4 5 6 7
Predicted (n-1 jackknife)
Ob
serv
ed
Corn
Soybeans
RMSE=0.71Slope=0.92Intercept=0.27R=0.57
1:1
Crop- and measurement date-specific indices derived from canonical correlationanalyses of 4-date (April-September) ETM+ spectral trajectories
NOBS
LAI
0
1
2
3
4
5
6
7
8
9
10
0 1 2 3 4 5 6 7 8 9 10
Predicted (n-1 jackknife)
Obs
erve
d
Classified Urbn/Blt Brn/Sprse Water Wetland Muskeg Black Spr Hardwood
Urbn/Blt 3 0 0 0 0 0 0
Brn/Sprse 0 1 0 0 1 1 0
Water 0 0 6 1 0 0 0
Wetland 0 0 1 7 1 0 0
Muskeg 0 0 0 2 66 13 0
Black Spr 0 0 0 4 11 99 2
Hardwood 0 0 0 1 0 1 11
Reference
Overall Accuracy = 83.19%Non-burned area error matrix
Conifer Cover (%)
0
10
20
30
40
50
60
70
0 10 20 30 40 50 60 70
Predicted (n-1 jackknife)
Ob
serv
ed
RMSE=9.09Slope=0.98Intercept=1.46R=0.84
1:1 1:1
Canonical indicesETM+ March, June
RMSE=1.19Slope=1.00Intercept=0.10R=0.74
Canonical indicesETM+ March, June
NOBSJuly
BigFoot MODLAND
NOBSJuly
BigFoot MODLAND
AGROJuly
BigFoot MODLAND
AGROJuly
August
BigFoot MODLAND
MODIS GPP Product
GPP (gC m-2 d-1) = PAR * fAPAR * g
Where:
PAR = from DAO climate model
fAPAR = from MODIS reflectances
g ( gC MJ-1) = GPP / APAR
MODIS g from lookup table Spatial Resolution is 1 km Temporal Res. is 8-day mean
AGRO 2000 NPP (using observed July LAIs)
y = 0.8803x + 53.24
R2 = 0.8566
0
200
400
600
800
1000
1200
0 200 400 600 800 1000 1200
Observed NPP
Pred
icte
d N
PP
RMSE = 87.143
AGRO 1999 CORN GPP
0
5
10
15
20
25
30
35
120 140 160 180 200 220 240 260 280
Day of Year
Gro
ss P
rim
ary
Pro
duct
ion (
gC m
-2 d
-1)
Tower-based GPP
Simulated GPP
Final Points
Anticipated quantitative comparisons with MODIS products
• Direct map-to-map comparisons (e.g., freq. dist. fine- vs. coarse-grainedlandcover classes; mean/SD of LAI/fAPAR/NPP/GPP//tree cover); cell, site, multi-site
• Evaluate effects of generalization on modeled productivity estimates by
successive coarsening of site-specific detail (land cover IGBP/6-class;
grain size 1 km; (following land cover generalization)
BigFoot data are freely available via Mercury with minimaldelay
• 21 datasets thus far (field data, derived surfaces, climate data)
Tasseled Cap Correlations: DN vs. Reflectance; Landsat 5 vs. Landsat 7
L5 exoatmospheric reflectance to L5 DN
Brightness: 0.99, Greenness: 0.99, Wetness: 0.95
L5 COST reflectance to L7 COST reflectance
Brightness: 0.97, Greenness: 0.96, Wetness: 0.93