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Project Idea• Fire potential models can help stratify and
reduce the number of false positive fire ‘detections’ by assigning probability levels to the landscape based on climate, fuels, ignition and topography.
• Fire detection models can serve as an independent validation source for fire potential models, particularly in under-developed regions.
• Fire potential and fire detection models both depend on MODIS data.
Testing VIIRS• Existing eastern fire
potential models • Standardization issues
– AVHRR/MODIS/VIIRS
• Existing fire detection systems – SERVIR– RSAC
FRANKE, Jonas & Gunter MENZRemote Sensing Research Group (RSRG)
Department of Geography, University of Bonn
Bonn, [email protected]
Testing VIIRS
• Existing fire detection systems – SERVIR– RSAC
• Giglio, et al. / Remote Sensing of Environment
87 (2003) 273-282
‘Contextual Fire Detection Algorithm for MODIS’
• Absolute Threshold Test
T4 > 360 K (320 K at night)
• Brightness threshold MODIS 4um (T4) (Bands 21 and 22 [1km]) – No VIIRS exact
replacement
• Brightness threshold MODIS 11um (T11) (Band 31 [1km])– Two VIIRS bands (M15
[742m], I-5 [371m])
t
0.8*
Monthly Rainfall Totals for July 2003
Weather Station LocationsEvaporation Predictions
St. Bernard
St. CharlesJefferson
MobileBaldwin
PerryPikeGreene
Jackson
Washington
Marion Lamar
StonePearl River
Harrison
Tangipahoa
Forrest
Jones
St. Tammany
Lincoln
George
Clarke
Washington
Wayne
Hancock
WalthallAmite
Lawrence
Orleans
Livingston
CovingtonJefferson Davis
St. John the Baptist
St. Helena
LaFourche Plaquemines
Franklin
Monroe
Ascension ±200 0 200100 Kilometers
Legend
stations
InlandEvaporation
CoastalEvaporation
0
0
Evaporation Regression ModelsAccepted: Southeastern Geographer
Stoneville, MS Cumulative P-E (average over 40 years) and 2000 estimates
Cumulative summaries - Starting date January 1st each year
-20
-15
-10
-5
0
5
10
15
20
1 13 25 37 49 61 73 85 97 109
121
133
145
157
169
181
193
205
217
229
241
253
265
277
289
301
313
325
337
349
361P-E
(in
)
2000 P_E 40 yrs Avg. P-E
January December
Precipitation – Evaporation (P-Et) Cumulative Inland
Fairhope, AL Cumulative P-E (40 years average) and 1995 estimates
Cumulative summaries - starting date January 1st each year
-5
0
5
10
15
20
25
30
1
17
33
49
65
81
97
11
3
12
9
14
5
16
1
17
7
19
3
20
9
22
5
24
1
25
7
27
3
28
9
30
5
32
1
33
7
35
3
Jan
P-E
(in
)
1995 P-E 40 yrs. Avg. P-E
January December
Precipitation – Evaporation (P-Et) Cumulative Coastal
Road Density/Gravity and Fire Ignition
Very LowLowMedHighVery High
Fire Risk
Road Density and Fire Ignition
Gravity vs. Road DensityGravity and Road
DensityAnnual
CriticalAnnual p-value
Winter
Critical
Winter
p-value
Summer
CriticalSummer p-value
Very Low Gravity and Very Low Road
Density3.51* 0.0085 3.64* 0.0058 3.58* 0.007
Low Gravity and Low Road Density 1.6 0.11 1.56 0.13 2.0* 0.05
Medium Gravity and Medium Road
Density3.09* 0.003 2.82* 0.0064 2.78* 0.007
High Gravity and High Road Density 0.62 0.534 0.67 0.5 0.29 0.77
Very High Gravity and Very High Road
Density0.44 0.664 0.08 0.58 0.42 0.68
Conclusions:Gravity models yield improved estimates of risk at very low levelsRoad density yields improved estimates of risk at medium levels
18-year Historic AVHRR NDVI 7-day Composites
Departure from average greeness
Physiographic Region Pearson Correlation (NDVI and Average Acre Burned)
0.01 level 0.05 level
Black Prairie -0.842 √
Coastal Zone -0.525
Delta -0.257
Loess Hills -0.817 √
North Central Hills -0.709 √
Pine Belt -0.696 √
South Central Hills -0.581 √
Jackson Prairie -0.534
Tombigbee Hills -0.533
NDVI and fire data averaged by month for each physiographic region
N = 12
Correlation Results – NDVI and Average Acre Burned
Physiographic Region Pearson Correlation (NDVI and Average Acre Burned)
0.01 level
Black Prairie -.390 √
Coastal Zone -.006
Delta -.119
Loess Hills -.293 √
North Central Hills -.383 √
Pine Belt -.212 √
South Central Hills -288 √
Jackson Prairie -.129
Tombigbee Hills -.090
Correlation Results – NDVI and Average Acre Burned
NDVI and fire data averaged by year and month for each physiographic region N = 177
NDVI Departure from Average
June 1Terra
June 2Aqua
June 3Terra
June 4Aqua
June 5Aqua
June 6Aqua
June 7Aqua
June 8Terra
VIIRS Simulation
• ITD and Chuck O’hara
• Florida and Georgia 2007 for tests
• Methods transferrable to Central America?
Comparison of MODIS & VIIRS BandsBand # Band ID Band # Band ID
1 620 - 670 600 - 680 I-1 3.610 Ğ 3.790 M-122 841 - 876 845 - 885 I-2 3.550 Ğ 3.930 I-43 459 - 479 21 3.929 - 3.9894 545 - 565 22 3.940 Ğ 4.0015 1230 - 1250 1230 - 1250 M-8 23 4.020 - 4.080 3.973 Ğ 4.128 M-13
1580 - 1670 M-10 24 4.433 Ğ 4.4981580 - 1610 I-3 25 4.482 Ğ 4.549
7 2105 - 2155 2225 Ğ 2275 M-11 26 1.360 - 1.390 M-98 405 - 420 402-422 M-1 27 6.535 - 6.8959 438 - 448 436-454 M-2 28 7.175 - 7.475
10 483 - 493 478-498 M-3 29 8.400 - 8.700 8.400 Ğ 8.700 M-1411 526 - 536 30 9.580 - 9.88012 546 - 556 545-565 M-4 10.263 Ğ 11.263 M-1513 662 - 672 662-682 M-5 10.050 - 12.400 I-514 673 - 683 32 11.770 - 12.270 11.538 Ğ 12.488 M-1615 743 - 753 739-754 M-6 33 13.185 - 13.48516 862 - 877 846-885 M-7 34 13.485 - 13.78517 890 - 920 35 13.785 - 14.08518 931 - 941 36 14.085 - 14.38519 915 - 965
MODIS Bands 1& 2 are 250 m at nadirMODIS Bands 3-7 are 500 m at nadirMODIS Bands 8-36 are 1,000 m at nadir
VIIRS Bands I-1 & I-2 are 371 m at nadirVIIRS Band I-3 is 371 m at nadir
VIIRS Bands I-4 & I-5 are 371 m at nadir
MODIS VIIRS
6 1628 - 1652
MODIS VIIRS
10.780 - 11.28031
20 3.660 - 3.840
VIIRS Vis/NIR BandsFire detection, spatial resolution
Band Name
SNR/ NEDT
Ltyp Lmin LmaxSNR/
NEDTLtyp Lmin Lmax
GSD Nadir
(m)
M-1 412 nm 20 nm 352 44.9 30 135 316 155 135 615 742
M-2 445 nm 18 nm 380 40 26 127 409 146 127 687 742
M-3 488 nm 20 nm 416 32 22 107 414 123 107 702 742
M-4 555 nm 20 nm 362 21 12 78 315 90 78 667 742
I-1 640 nm 80 nm 119 22 5 718 371
M-5 672 nm 20 nm 242 10 8.6 59 360 68 59 651 742
M-6 746 nm 15 nm 199 9.6 5.3 41 742
M-7 865 nm 39 nm 215 6.4 3.4 29 340 33.4 29 349 742
I-2 865 nm 39 nm 150 25 10.3 349 371
DNB 700 nm 400 nm 5 3.0E-05 2.0E+02 742
Band Ctr
Band Width
Single or High Gain Low Gain
3
SNR values are as specified for un-aggregated pixel.At nadir SNR will be ~ better after aggregation. (Predicted are better still)
VIIRS S/MW & LW IR BandsFire detection, spatial resolution
SNR values are as specified for un-aggregated pixel.At nadir SNR will be ~ better after aggregation. (Predicted are better still)
Band Name
SNR/ NEDT
Ltyp Lmin Lmax
SNR/ NEDT
Ltyp Lmin Lmax
GSD Nadir (m)
M-8 1.24 0.020 74 5.4 3.5 164.9 742M-9 1.378 0.015 83 6 0.6 77.1 742
M-10 1.61 .06 342 7.3 1.2 71.2 742I-3 1.61 .06 6 7.3 1.2 72.5 371
M-11 2.25 .05 10 .12 0.12 31.8 742M-12 3.70 .18 .396 K 270 K 230 K 353 K 742
I-4 3.74 .38 2.5 K 270 K 210 K 353 K 371M-13 4.05 0.155 .107 K 300 K 230 K 343 K .423 K 380 K 343 K 634 K 742M-14 8.55 0.3 .091 K 270 K 190 K 336 K 742M-15 10.8 1.0 .070 K 300 K 190 K 343 K 742M-16 12.0 1.0 .072 K 300 K 190 K 340 K 742
I-5 11.5 1.9 1.5 K 210 K 190 K 340 K 371
Band CtrBand Width
Single or High Gain Low Gain
3