PHENOLOGICAL SPECTRAL INDEX TIME SERIES -...
Transcript of PHENOLOGICAL SPECTRAL INDEX TIME SERIES -...
PHENOLOGICAL SPECTRAL INDEX TIME SERIESfor the dynamic derivation of soil coverage information
Markus Moller
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10121518192124AHMartin Luther University Halle-Wittenberg · Farm Management Group · Germany
Markus Moller PhenoSITS JRC | 21 March 2017 1 / 12
Outline
1 Motivation
2 WorkflowCrop-specific phenological windowsPhenological NDVI time series
3 Conclusion
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Motivation
Monitoring of soil erosion patterns on agricultural land
Up-to-date information about parcel-and phase-specific crop coverage
Phenological spectral index time series
Fused satellite imagery of high spatial (e.g. Landsat) and hightemporal resolution (e.g. MODIS) ⇒ spectral index time series
Interpolated phenological observations ⇒ phenological phases
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Workflow
Phenologial spectral index time series
Phenologicalwindows
raster1 × 1 km
Phenologicalobservations
DWDpoint
ElevationUSGSraster90 × 90 m
PH
AS
E
Spectral indextime series
raster30 × 30 m
LandsatUSGSraster30 × 30 m
MODISUSGSraster250 × 250 m
STA
RF
MParcel
PHENOLOGICAL INDEX TIME SERIES
Y EAR
DOY
V I
2013
170
V I2013,170
b
b
INTRA- and INTER-ANNUAL INDEX DYNAMIC
Gao, F., Anderson, M.C., Zhang, X., Yang, Z., Alfieri, J.G., Kustas, W.P., Mueller, R., Johnson, D.M., Prueger, J.H.
(2017): Toward mapping crop progress at field scales through fusion of Landsat and MODIS imagery. Remote Sensing ofEnvironment 188, 9–25.
Gerstmann, H., Doktor, D., Glaßer, C. & Moller, M. (2016): PHASE: A geostatistical model for the Kriging-based spatial
prediction of crop phenology using public phenological and climatological observations. Computers and Electronics inAgriculture 127, 726–738.
Moller, M., Gerstmann, H., Dahms, T.C., Gao, F. & Forster, M. (2017): Coupling of phenological information and
simulated vegetation index time series: Limitations and potentials for the assessment and monitoring of soil erosion risk.CATENA 150, 192–205.
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Workflow Crop-specific phenological windows
Interpolated phenological events of Winter Wheat in Germany for 2011
55°N
50°N
5°E 10°E 15°E
93
121
DOY
55°N
50°N
5°E 10°E 15°E
5°E 10°E 15°E
180
134
222
195
Phase 1555°N
50°N
5°E 10°E 15°E
DOY
DOY
158
5°E 10°E 15°E
194
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249DO
Y
Phase 21
Phase 1855°N
50°N
5°E 10°E 15°E
DOY
273
291
Phase 19
DOY
Phase 24 Phase 12
Study site
Study site
Study site Study site
Study site Study site
12 – emerging | 15 – shooting | 18 – beginning of ear | 19 – milk ripeness | 21 – yellow ripeness | 24 – harvest
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Workflow Crop-specific phenological windows
Winter Wheat (top) and Maize (bottom)0.
00.
20.
40.
60.
81.
0
DOY1 21 41 61 81 101 121 141 161 181 201 221 241 261 281 301 321 341 361
Phases
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0.0
0.2
0.4
0.6
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1.0
DOY1 21 41 61 81 101 121 141 161 181 201 221 241 261 281 301 321 341 361
Phases
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5 – begin of flowering | 10 – tilling, sowing, drilling | 12 – emergence | 15, 67 – shooting/growth in height | 18 – beginning ofear | 19 – milk ripeness | 20 – wax-ripe stage | 21 – yellow ripeness | 24 – harvest | 65 – tassel emergence
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Workflow Phenological NDVI time series
Winter Wheat (top) and Maize (bottom)0.
00.
20.
40.
60.
81.
0
DOY
ND
VI
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Phases
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5 – begin of flowering | 10 – tilling, sowing, drilling | 12 – emergence | 15, 67 – shooting/growth in height | 18 – beginning ofear | 19 – milk ripeness | 20 – wax-ripe stage | 21 – yellow ripeness | 24 – harvest | 65 – tassel emergence
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Workflow Phenological NDVI time series
Test site-specific and spatial NDVI variation for DOY = 66
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Figure 9: Classification result of parcel-specific NDV I medians for Winter Wheat in 2011and DOY 66 (a), corresponding cluster and NDV I median distribution (b).
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Workflow Phenological NDVI time series
Parcel-specific (left) and phase-specific NDVI median variations (right)
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sity
0.36 0.66 0.78
Median
Daily or phase-specific soil coverage
empirical models
regression models based on classified vertical photographs andcorresponding satellite imagery
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Conclusion
Phenological NDVI time series
Dynamic parametrization of soil erosion models
Definition of phenological windows for the prediction of fractionalvegetation coverage, crop residue coverage or bare soil
Derivation of short- and long-term parcel-specific soil coverageinformation
Temporal and geometric disaggregation of hotspot areas (monitoring)
Limitation
The quality of the spectral index time series depends on the distanceand the phenological representativity of MODIS-Landsat-pairs.
The fusion quality is expected to be improved by using Sentinel-2imagery.
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Conclusion
Satellite imagery: coverage and resolution
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SPECTRAL RANGE [nm]
SE
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OR
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400 600 800 1000 1200 1400 1600 1800 2000 2200 2400
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1 · Sentinel 2 · 10 m2 · 5 days
2 · Sentinel 2 · 20 m2 · 5 days
3 · Sentinel 2 · 60 m2 · 5 days
4 · RapidEye · 5 m2 · max. 5 days
5 · Landsat 8 · 30 m2 · 16 days
6 · MODIS · 250 m2 · 1-2 days
7 · MODIS · 500 m2 · 1-2 days
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Conclusion
Questions?
Markus Moller | [email protected]
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DOY
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10121518192124AHThis study was funded by the German Ministry of Economics and Energy and managed by the
German Aerospace Center (DLR), contract no. 50 EE 1262 and 50 EE 1230.
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