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7th Workshop on Forest Fire Management - EARSeL, European ...

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262<br />

IV - BURNED LAND MAPPING, FIRE SEVERITY DETERMINATION, AND VEGETATION RECOVERY ASSESSMENT<br />

Sensor TerraSAR-X Sensor ASAR<br />

Polarizati<strong>on</strong> HH HV HH&HV Polarizati<strong>on</strong> VV HH HV HH&HV<br />

Scene data 12.1908 Scene data 09.12.08 01.08.09 03.19.09<br />

All pseudo-plots 0.529 0.085 0.546 0.101 0.176 0.539 0.542<br />

Pseudo-plots grouped by local incidence angle<br />

26°-30° 0.833 0.291 0.916 6°-10° 0.359 0.768 0.700 0.843<br />

31°-35° 0.707 0.234 0.861 10°-15° 0.338 0.555 0.733 0.758<br />

36°-40° 0.732 0.050 0.857 16°-20° 0.361 0.449 0.609 0.648<br />

41°-45° 0.666 0.291 0.815 21°-25° 0.186 0.354 0.693 0.752<br />

46°-50° 0.621 0.402 0.792 26°-30° 0.001 0.198 0.699 0.699<br />

51°-55° 0.612 0.520 0.824 31°-35° 0.007 0.154 0.767 0.767<br />

56°-60° 0.584 0.464 0.833 36°-40° 0.001 0.174 0.715 0.715<br />

61-65 0.476 0.582 0.843 41-45 0.050 0.109 0.744 0.744<br />

Table 1 - Determinati<strong>on</strong> coefficients explaining the agreement between dNBR and radar<br />

backscatter at X- and C-band.<br />

5 - Discussi<strong>on</strong><br />

Both sensors showed similar trends of the backscatter with respect to dNBR<br />

for co- and cross-polarized beams. Figures 1 and 2 show that for co-polarized<br />

beams the backscattering coefficient increased with burn severity. For<br />

X-band HH-polarizati<strong>on</strong>, the backscattering coefficient increased (Figure 2)<br />

from low to medium burn severity reaching saturati<strong>on</strong> for high burn severities<br />

(i.e. dNBR 800). The HV-backscatter<br />

decreased with the increase of burn severity at both frequencies<br />

(Figures 1 and 2). This is explained by the larger amount of gaps in the<br />

canopy and the increased transmissivity with the increase of burn severity.<br />

Figure 3 shows the str<strong>on</strong>g effects of the local incidence angle <strong>on</strong> the<br />

backscatter at all SAR frequencies and polarizati<strong>on</strong>s. For increasing local<br />

incidence angle decreasing trends were registered for co-polarized beams.<br />

This decrease is the result of a decreasing proporti<strong>on</strong> of direct scatter from<br />

the ground to the total forest backscatter. Cross-polarized beams showed<br />

increase of the backscatter coefficient with increasing local incidence angle<br />

explained by the l<strong>on</strong>ger path traveled by the radar wave within the canopy.<br />

The strength of associati<strong>on</strong> (i.e. R 2 ) for co-polarized beams decreased with<br />

increasing incidence angle while the error increased (Table 1). The simultaneous<br />

use of cross and co-polarized channels (HH and HV) provided the<br />

highest R 2 coefficients and the smallest errors.

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