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7.2.2.1 Theoretical impact analysis <strong>of</strong> science data products by mis-registration<br />
The normalized indices (NI) are the normalization <strong>of</strong> two or more spectral b<strong>and</strong>s.<br />
They are usually used for the scene identification with general formula shown in Eq. (7.6),<br />
where Ra <strong>and</strong> Rb are responses <strong>of</strong> b<strong>and</strong>s a <strong>and</strong> b respectively. Commonly, one b<strong>and</strong> in NI<br />
is sensitive to a given matter class <strong>and</strong> the other b<strong>and</strong> is insensitive to it, such as<br />
Normalized Difference Vegetation Index (NDVI) (Rouse et al., 1973; Huete et al., 1994),<br />
Normalized Difference Snow Index (NDSI) (Hall et al., 2002), Normalized Difference<br />
Water Index (NDWI) (Gao, 1996), <strong>and</strong> Normalized Difference <strong>Dust</strong> Index (NDDI) (Qu et<br />
al., 2006). In some indices, Ra or Rb can be the response combination <strong>of</strong> several spectral<br />
b<strong>and</strong>s, such as Normalized <strong>Multi</strong>-b<strong>and</strong> Drought Index (NMDI) (Wang et al., 2007).<br />
R R<br />
NI <br />
R R<br />
a b<br />
a b<br />
114<br />
(7.6)<br />
If there is a small response deviation <strong>of</strong> two b<strong>and</strong>s, ΔRa <strong>and</strong> ΔRb, the change <strong>of</strong> NI<br />
value, ΔNI, is approximately equal to the first order partial derivative with respect to two<br />
variables, Ra <strong>and</strong> Rb. Practically, one <strong>of</strong> b<strong>and</strong>s is designated as reference b<strong>and</strong> in most<br />
cases to simplify the calculation by setting ΔRa=0 (or ΔRb=0). The ΔNI can be computed<br />
with Eq. (7.7)<br />
2Ra<br />
NI R<br />
2<br />
( R R )<br />
a b<br />
'<br />
b<br />
(7.7)<br />
where ΔRb’is the minute response change <strong>of</strong> b<strong>and</strong> b caused by its spatial mis-registration<br />
relative to b<strong>and</strong> a.