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i Detection of Smoke and Dust Aerosols Using Multi-sensor Satellite ...

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cooperatively: the reflectance at 0.63 µm <strong>and</strong> 3.7 µm channel, the Bright Temperature<br />

(BT) difference between 3.7 µm <strong>and</strong> 11 µm channel, <strong>and</strong> the BT difference between<br />

anticipated clear-sky value <strong>and</strong> measured value at 11 µm channel. Li et al. (2001)<br />

presented a multi-threshold method for automated smoke plume detection using AVHRR<br />

measurements based on the neural networks. The shortcoming <strong>of</strong> using AVHRR is that<br />

AVHRR has only five channels, which is inefficient for smoke detection.<br />

Chrysoulakis et al. (2007) proposed a multi-temporal change detection approach<br />

using two images at the same target area on the different time. By comparing two images<br />

(one is acquired during the fire event <strong>and</strong> the other is acquired before fire event), the<br />

important anomalies in NDVI <strong>and</strong> infrared radiances were detected hence to detect the<br />

core <strong>of</strong> plume. Then the plume core was enlarged to include the complete smoke area<br />

through identifying a pixel as plume pixel if it located spatially <strong>and</strong> spectrally at the<br />

neighborhood <strong>of</strong> the initial plume core. The new developed one <strong>of</strong>fers a novel ways for<br />

smoke monitoring. However, this approach need find a clear day before the occurrence <strong>of</strong><br />

smoke. The Bidirectional Reflectance Distribution Function (BRDF) issue is also need to<br />

be taken into account.<br />

The current MODIS aerosol retrieval algorithm uses the dark target approach<br />

(Kaufman et al. 1997, Kaufman et al. 1997) with two assumptions: 1) the aerosol is<br />

transparent to most aerosol types (except dust) at 2.1 µm so that this channel can be used<br />

to detect dark surface targets; 2) the surface reflectance at 0.47 µm <strong>and</strong> 0.64 µm channel<br />

could be retrieved by that at 2.1 µm with the ratio 0.25 <strong>and</strong> 0.5. With the assumptions, the<br />

Aerosol Optical Thickness (AOT) <strong>and</strong> particle size parameters were retrieved at 0.47 µm<br />

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