vegetation dynamics and seasonal responses of north and ... · vegetation dynamics and seasonal...
TRANSCRIPT
![Page 1: Vegetation Dynamics and Seasonal Responses of North and ... · Vegetation Dynamics and Seasonal Responses of North and South America from EOS-MODIS Vegetation Indices Alfredo Huete1,](https://reader033.vdocuments.mx/reader033/viewer/2022051812/602b7c798c4b5840214a8df2/html5/thumbnails/1.jpg)
Vegetation Dynamics and SeasonalResponses of North and South Americafrom EOS-MODIS Vegetation Indices
Alfredo Huete1, Kamel Didan1, Tomoaki Miura1,Edna P. Rodriguez1, Xiang Gao1,
and Laerte G. Ferreira2
1Department of Soil, Water, and Environmental Science,
University of Arizona, Tucson, AZ2Universidade Federal de Goiás - UFG
Goiânia, GO, 74.001-970 Brazil
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MODIS (MOD 13)Vegetation Index Products
K The MODIS Products include 2 Vegetation Indices(NDVI, EVI) and QA produced at 16-day and monthlyintervals at 250m/ 500m, 1km, and 25km resolutions
K The narrower ‘red’ MODIS band provides increasedchlorophyll sensitivity (band 1),
K The narrower ‘NIR’ MODIS band avoids highly variablewater vapor absorption (band 2),
K Use of the blue channel in the EVI provides aerosolresistance.
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Global EVI composite (Sept. 30 - Oct. 15, 2000)(Spatial and temporal intercomparisons of vegetation
activity)
Hammer Aitoff Projection
1000 km 5000 km
TBRS, University of ArizonaSCF Group, http://tbrs.arizona.edu
water 0.2 0.4 0.6 0.8 1.0
EVI
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TBRS, University of ArizonaSCF Group, http://tbrs.arizona.edu
NDVI
water 0.2 0.4 0.6 0.8 1.0
Colorado River DeltaVegetation Spatial and Temporal Dynamics with MODIS NDVI 2000-
2001
June 9May 25
Apr 7
Mar 22
Mar 6
Feb 18
Feb 2
Jan 17
Jan 1Dec 18 Dec 2
Spring Summer
FallWinter
Sept 13
Sept 29
Oct 15
Oct 31Nov 16
June 25
July 11
Aug 12
Aug 28
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MODIS Vegetation Indices
ARVIAtmosphereResistance
)Re(Re*)1(
LdNIR
dNIRL+ρ+ρ
ρ−ρ+
SAVI
Canopy BackgroundCorrection
Soil-adjusted Vegetation Index
NDVINormalized DifferenceVegetation Index
dNIR
dNIR
Re
Re
ρρ
ρρ
+
−
EVI
Enhanced Vegetation Index
)Re(Re*
21 blueCdCNIRLdNIRG
ρρρ
ρρ
−++
−
)(
,
ReRe dbluedrb
rbNIR
rbNIR
ρ−ργ−ρ=ρρ+ρρ−ρ
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Geographic location of validation activitiesand time series plots.
Cascades
Jornada &White Sands
KonzaPrairieKonzaPrairie
SALSA
Sevilleta
HarvardForestHarvardForest
MODIS MNR (RGB) DOY 225-240
MODIS MNR (RGB) DOY 225-240
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Harvard Forest (mixedhardwood and conifer forests)
Cascades (mixedconifer forest)
Konza TallgrassPrairie
SALSA (semiaridshrub/ grass)
White SandsSevilleta LTER(semiarid shrub/ grass)
Jornada LTER (semiaridshrub/ grass)
North American sites withdiverse vegetationconditions
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Seasonal Patterns of Major Biomesin North America
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Effective LAI0 2 4 6 8
0.0
0.2
0.4
0.6
ZeroDarkBright
25% 50% 95%
Needleleaf Broadleaf
Effective LAI0 2 4 6 8
0.0
0.2
0.4
0.6
0.8
1.0
Broadleaf
Effective LAI0 2 4 6 8
0.0
0.2
0.4
0.6
0.8
1.0
Needleleaf
25% 50% 95%ZeroDarkBright
EVI
NDVI
-30
-20
-10
0
10
20
30
49 70 91 112
133
154
175
196
217
238
259
280
301
322
343
364 19 40 61 82 103
124
145
166
187
208
229
250
271
Tem
pera
ture
, C
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Semi-arid Vegetation DynamicsApril 8 May 26 June 26 July 13
July 29Aug 14Sep 15Oct 1
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WGEW WGEW –– ExotechExotech EVI EVI
Airplane Data
Ground Data
MODIS 250m EVI
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EVI from MODIS & EVI from MODIS & ExotechExotech
300m AGL 150m AGL
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NDVI
EVI
Dry Season(129 ~ 144)
Wet Season(200 ~ 208)
NDVI EVI
JER
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Jornada Jornada –– ExotechExotech EVI EVI
Green = high EVIOrange = low EVI
ETM+ NDVI
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Scaling:ground > mquals > ETM+ > MODIS
Ground ASD MQUALS ASDScaling up
MQUALS UTM ETM+ UTM Scaling up
Band convolution
ASDBand
convolutionETM+
MODIS
ETM+ UTM MODIS ISIN
Scaling up
Reprojection
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MQUALS vs. ETM+ (JER)(May 2000/2001)
MQUALS reflectance/ VIs0.0 0.1 0.2 0.3 0.4
ET
M+
refle
ctan
ce/ V
Is
0.0
0.1
0.2
0.3
0.4
MMMMMMMMMMMMMM
MM MM M
MMMMM MMMM
MMMMMM
MMM M
MMMMM MMMM
MMM
MMMM
MM
M
MMMM
MMMM MM
MMMMMMMMM
MMMMMMMMMMMM
MMMMMMMCCC
CCCCCCCCC CC CCC
CC
CCC
CC CCC
C
CCC
CC
CCC
CCC
CCC
CCCCCC
CCCC
CC
C
CC
CC
C
C
CC
CCC
CCC
C
CCCCC
CCCCC C
CCCCCCCCCC CCCCCC
CCCCCCC
CCCC
CCCCCCCCCCCCCCCC
CCCCCCC
CCCC
M
M
M
MM
grassland transition mesquiteCreosoteC
C
C
CC
BlueRedNIRNDVIEVI
MQUALS reflectance/ VIs0.0 0.1 0.2 0.3 0.4
ET
M+
reflectance/ VIs
0.0
0.1
0.2
0.3
0.4
M
M
M
M
MC
C
C
C
C
ET
M+
Ref
lect
ance
s/ V
I’s
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MQUALS vs. MODIS (JER)(May 2000/2001)
MQUALS reflectances/ VIs0.0 0.1 0.2 0.3 0.4
MO
DIS
reflectances / VIs (250m
)
0.0
0.1
0.2
0.3
0.4
CCCCCCCCCCCC CC
CCCC
C CC
CCC
C
C
CCCC
C CC
CC
C
C
C
CCCCCCCCCCC CC C
CCCCCCCCCCCCCCMMMMMMMMMMMMMMMM
MMMMMMMMMMMMM
M
MM
MMMMMMMM
MM
M
M
MMMMMMMMMMMMMM
MMMMMMMMMMMMMM
MQUALS reflectances/ VIs0.0 0.1 0.2 0.3 0.4
MO
DIS
reflectances / VIs (250m
)
0.0
0.1
0.2
0.3
0.4
C
C
C
C
CM
M
M
M
M
BlueRedNIRNDVIEVI
M
M
M
MM
C
C
C
CC
grassland transition creosotemesquite
MO
DIS
Ref
lect
ance
s/ V
I’s
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Multitemporal VI Comparisons(MODIS, ETM+, MQUALS, Ground)
DOY120 140 160 180 200 220 240 260 280 300
Vegetation Indices
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
E E
E
E
E EE
E
Mesquite
rain
DOY120 140 160 180 200 220 240 260 280 300
Vegetation Indices
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
E E
E
E
E EE
E
composited MODIS (500m)nadir single day (500m)ETM+EMQUALS
Creosote
rain
E
G Ground G
NDVI EVI
DOY120 140 160 180 200 220 240 260 280 300
Vegetation Indices
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
E E
E
E
E E
E
E
G
G G
G
G G
G
G
Transition
rain
DOY120 140 160 180 200 220 240 260 280 300
Vegetation Indices
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
EE
E
E
E E
E
E
G
G GG
GG
GG
GrasslandDOY
240 250 260 270 280 290
Biophysical
0
10
20
30
40
50% Green coverGreen LAI *100
rain
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Seasonal Patterns of Major Biomesin South America
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ETM+DOY 211,2001
(Tapajos)
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Seasonality observed by MODISTapajos National Forest, Brazil
Dry Season
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Brasilia National ParkBrasilia National Park
• Blue = ASD
•Yellow = DigitalImages
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Brazil Olympus Digital ImagesBrazil Olympus Digital Images
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ASD from Brasilia NPASD from Brasilia NP
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Araguaia Araguaia National ParkNational Park
• Red = ASD
•Yellow = DigitalImages
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MODIS VI Long Term Stability MonitoringMODIS VI Long Term Stability Monitoring
Saharan Desert Sites (h18v05)
MOD13A2 (V3)Mar 6 – Mar 21, 2001False Color Composite (1, 2, 3)
TzTzTz2Tz2
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MODIS VI Long Term Stability MonitoringMODIS VI Long Term Stability Monitoring
Atacama Desert Sites (h11v11)
MOD13A1 (V3)Sep 30 – Oct 15, 2001False Color Composite (1, 2, 3)
AtBAtB
AtDAtD
AtMAtM
AtPAtP
AtAt
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MODIS VI Long Term Stability MonitoringMODIS VI Long Term Stability Monitoring
VI vs. Sun Zenith Angle PlotsNDVI (Daily)NDVI (Daily) EVI (Daily)EVI (Daily)
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MODIS VI Long Term Stability MonitoringMODIS VI Long Term Stability Monitoring
VI Comparisons with Time-LagsNDVI (Daily)NDVI (Daily) EVI (Daily)EVI (Daily)
*α – 1 month ~ 1 year time lags with similar geometries.
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MODIS Vegetation Index performanceMODIS Vegetation Index performance
EVI EVI_QA NDVI NDVI_QA
Nov
embe
r 16
-30
1-1
5
NDVI
water 0.2 0.4 0.6 0.8 1.0water 0.2 0.4 0.6 0.8 1.0
EVI
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MODIS Vegetation Index performance
Transect 1
Transect 4
Transect 3
Transect 2
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Transect 1: This transect spans different vegetation types under different atmosphere conditions. It also show the response of both VIs to aerosol, clouds, snow and vegetation activities)
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Transect 1 (pixel 200 to 400):Medium to high aerosol is prevalent is this section of the Transect. EVI response is more stable and shows more resistance to aerosol. NDVI on the other hand is very unstable.
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VI Validation
• VI products are provisionally validated,however,
• Vegetation Indices are widely used inregional to global applications,
• It is these intended uses or product outputs,that need to be validated,
• Product inputs, however, propagate into theoverall uncertainty of the VI (atmospherecorrection, residual clouds, calibration)
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Next Steps in Validation
• Summer 2001 campaigns in Brazil andArgentina need to be analyzed,
• BRDF and cloud effects remain in thecompositing routine,
• Snow/ice problems persist in both VI’s,
• Assessment of feasibility of using snowproduct and BRDF products.