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Fisheries in the Southern Border Zone of Takamanda - Impact ...

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Landcover change<br />

an operator with knowledge <strong>of</strong> <strong>the</strong> imagery manually<br />

del<strong>in</strong>eates sites (groups <strong>of</strong> pixels) <strong>of</strong> each class on <strong>the</strong><br />

imagery. Based on <strong>the</strong> spectral character <strong>of</strong> <strong>the</strong>se tra<strong>in</strong><strong>in</strong>g<br />

sites, <strong>the</strong> maximum likelihood algorithm <strong>the</strong>n makes<br />

probability-based class assignments <strong>of</strong> all image pixels.<br />

To generate landcover change classes us<strong>in</strong>g <strong>the</strong>se<br />

classification methods, <strong>the</strong> tra<strong>in</strong><strong>in</strong>g sites were selected to<br />

<strong>in</strong>clude both change classes (such as “forest to nonforest”)<br />

and non-change classes (“unchanged lowland<br />

forest”), and <strong>the</strong> spectral bands from both dates <strong>of</strong><br />

imagery were <strong>in</strong>put to <strong>the</strong> classification procedure<br />

simultaneously. This is sometimes termed composite<br />

multi-date classification, s<strong>in</strong>ce images from both dates<br />

are composited and used toge<strong>the</strong>r, as if from a s<strong>in</strong>gle date.<br />

The prelim<strong>in</strong>ary orthorectification step makes this<br />

approach possible as it ensures <strong>the</strong> precise overlay <strong>of</strong><br />

images from different dates. After runn<strong>in</strong>g <strong>the</strong><br />

classification, some post-classification process<strong>in</strong>g and<br />

manual edit<strong>in</strong>g were conducted to clean up and f<strong>in</strong>alize<br />

<strong>the</strong> classification map.<br />

Various statistics were calculated from this f<strong>in</strong>al<br />

classification map to quantify changes <strong>in</strong> landcover. To<br />

provide better <strong>in</strong>sight <strong>in</strong>to where changes might be<br />

occurr<strong>in</strong>g most rapidly, <strong>the</strong>se measures were calculated<br />

for several regions: <strong>the</strong> entire 1600 x 1740 image subset;<br />

<strong>the</strong> area with<strong>in</strong> <strong>the</strong> TFR boundaries (exclud<strong>in</strong>g enclave<br />

communities); <strong>the</strong> areas <strong>of</strong> <strong>the</strong> two enclave communities<br />

(Obonyi and Kekpane); and <strong>the</strong> area with<strong>in</strong> a 5-km buffer<br />

zone surround<strong>in</strong>g <strong>the</strong> TFR.<br />

3 Results<br />

3.1 Change Classification<br />

Tra<strong>in</strong><strong>in</strong>g sites for n<strong>in</strong>e different classes were <strong>in</strong>itially<br />

def<strong>in</strong>ed (see Sunderland et al. this volume) to <strong>in</strong>clude<br />

eight static classes (lowland forest, ridge forest, midelevation<br />

forest, montane forest, grassland/bare,<br />

secondary forest/farms, water, shadow), and one change<br />

class <strong>in</strong>dicat<strong>in</strong>g forest conversion (forest → secondary<br />

forest/farms). Note that <strong>in</strong> a static <strong>in</strong>terpretation <strong>of</strong> <strong>the</strong><br />

output classification (e.g. for a year 2000 landcover<br />

map), <strong>the</strong> forest conversion class would be added to <strong>the</strong><br />

secondary forest/farms class. No dist<strong>in</strong>ction was made<br />

175<br />

between secondary forest and farms because <strong>the</strong>se two<br />

landcover types are fluid and difficult to dist<strong>in</strong>guish;<br />

farms usually have a scatter<strong>in</strong>g, or more, <strong>of</strong> larger trees,<br />

and due to <strong>the</strong> agricultural practices <strong>in</strong> <strong>the</strong> region, areas<br />

<strong>of</strong> secondary forest will be farmed aga<strong>in</strong> after several<br />

years <strong>of</strong> forest regrowth. The four different types <strong>of</strong><br />

undisturbed forest (lowland, ridge, mid-elevation, and<br />

montane) were <strong>in</strong>cluded <strong>in</strong> <strong>the</strong> classification both<br />

because we wanted to map <strong>the</strong> extent <strong>of</strong> <strong>the</strong>se forest types<br />

(see Sunderland et al. this volume), and because lump<strong>in</strong>g<br />

<strong>the</strong>m toge<strong>the</strong>r produces an overly broad and poorly<br />

def<strong>in</strong>ed forest class, which becomes confused with<br />

secondary forest <strong>in</strong> <strong>the</strong> classification results. Several<br />

o<strong>the</strong>r types <strong>of</strong> change might have also been <strong>in</strong>cluded, but<br />

were not, such as grassland → burned grassland, and<br />

forest regrowth (farms → secondary forest); <strong>the</strong>se were<br />

ei<strong>the</strong>r not <strong>of</strong> <strong>in</strong>terest (<strong>the</strong> former) or too difficult to<br />

consistently differentiate (<strong>the</strong> latter). In ei<strong>the</strong>r case, we<br />

verified that <strong>the</strong>se areas were satisfactorily classified with<br />

<strong>the</strong> exist<strong>in</strong>g scheme. For example, <strong>the</strong> grassland →<br />

burned grassland areas were rout<strong>in</strong>ely classified as<br />

grassland, and <strong>the</strong> areas <strong>of</strong> possible regrowth (farms →<br />

secondary forest) were classified as secondary forest. A<br />

class for shadow was necessary because <strong>the</strong> poor and<br />

variable illum<strong>in</strong>ation on <strong>the</strong> shadowed sides <strong>of</strong> hills<br />

makes differentiation <strong>of</strong> different landcovers much more<br />

difficult.<br />

The result<strong>in</strong>g classification was <strong>the</strong>n visually<br />

<strong>in</strong>spected, and <strong>in</strong> an iterative process, m<strong>in</strong>or adjustments<br />

were made to <strong>the</strong> tra<strong>in</strong><strong>in</strong>g classes and certa<strong>in</strong><br />

classification parameters. Despite many such<br />

adjustments, it became apparent that an additional class<br />

would be useful to <strong>in</strong>dicate areas <strong>of</strong> “possible” secondary<br />

forest. These areas can typically be classified as ei<strong>the</strong>r<br />

lowland forest, secondary forest, or ridge forest,<br />

depend<strong>in</strong>g on <strong>the</strong> set <strong>of</strong> tra<strong>in</strong><strong>in</strong>g sites and classification<br />

parameters. However, as <strong>the</strong>se areas do not appear to be<br />

separable solely from image reflectances, it was decided<br />

to create a separate “possible secondary forest” (PSF)<br />

class. Generally, firsthand knowledge <strong>of</strong> <strong>the</strong> area is<br />

required to assign def<strong>in</strong>itive labels to <strong>the</strong>se regions, but<br />

many can be labeled based on a closer <strong>in</strong>spection <strong>of</strong> <strong>the</strong><br />

imagery; for example, <strong>the</strong> areas on hillsides not <strong>in</strong> <strong>the</strong><br />

vic<strong>in</strong>ity <strong>of</strong> villages are most likely undisturbed forest<br />

SI/MAB Series #8, 2003

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