@@ -28,7 +28,8 @@ <h4>Neural network classification</h4>
2828 The IdePix classification algorithm for Sentinel-3 OLCI is based on a neural network approach. A common neural net
2929 is used for both land and water pixels.
3030 As input for the neural net, the square roots of the OLCI TOA reflectances (obtained from an internal
31- radiance-to-reflectance conversion) in all 21 bands are used. < br > < br >
31+ radiance-to-reflectance conversion) in all 21 bands are used. It is described in detail in the ATBD [1].
32+ < br > < br >
3233
3334 As output, the neural net finally provides per pixel one of the properties 'cloud sure',
3435 'cloud ambiguous', 'cloud' (which means sure OR ambiguous) , or 'snow/ice'.< br >
@@ -46,7 +47,7 @@ <h4>Additional properties</h4>
4647 on the full image. The cloud buffer algorithm works on pixel windows of size (2N+1) x (2N+1) with N = cloud buffer
4748 width. Note that the cloud buffer is only applied on cloud-free pixels, i.e. cloudy pixels are not flagged as cloud
4849 buffer of cloudy neighbour pixels.
49- The cloud buffer procedure is described in a bit more detail in the CCI Land Cover ATBD [1 ].
50+ The cloud buffer procedure is described in a bit more detail in the CCI Land Cover ATBD [2 ].
5051 </ li >
5152 < li >
5253 'bright': the pixel is a bright pixel. The information is retained from the quality flags of the L1b product.
@@ -61,7 +62,7 @@ <h4>Additional properties</h4>
6162
6263By default, the 'land' and 'coastline' pixels are identified from the land flag included in the
6364quality flags which come with the L1b product. Optionally, the SRTM (Shuttle Radar Topography Mission) land/water
64- mask[2 ] can be applied instead.
65+ mask [3 ] can be applied instead.
6566The latter is a fractional mask:
6667< ul >
6768 < li >
@@ -88,7 +89,7 @@ <h4>Additional properties</h4>
8889 classification.
8990 </ li >
9091 < li >
91- 'mountain_shadow': a hillshade algorithm [3 ] is implemented, which derives slopes from elevation data and uses a
92+ 'mountain_shadow': a hillshade algorithm [4 ] is implemented, which derives slopes from elevation data and uses a
9293 geometric test with slope, aspect and illumination and satellite observation conditions against a threshold to
9394 find pixel in the (core) shadow of mountainous terrain. The threshold is set to 0.9 by default, and can be adjusted
9495 by the user between 1 (larger terrain shadow extent) and 0 (no terrain shadow).
@@ -158,7 +159,7 @@ <h3>References</h3>
158159
159160 < br > < br >
160161
161- < b > [1 ]</ b >
162+ < b > [2 ]</ b >
162163 CCI Land Cover - Algorithm Theoretical Basis Document: Pre-Processing< br >
163164 Chapter 4.4.11 Cloud shadow and cloud edge detection< br >
164165 < object classid ="java:org.netbeans.modules.javahelp.BrowserDisplayer ">
@@ -169,7 +170,7 @@ <h3>References</h3>
169170
170171 < br > < br >
171172
172- < b > [2 ]</ b >
173+ < b > [3 ]</ b >
173174 Farr, T. G., et al., The Shuttle Radar Topography Mission, Rev. Geophys., 45, RG2004,
174175 doi:10.1029/2005RG000183. (2007)< br >
175176 < object classid ="java:org.netbeans.modules.javahelp.BrowserDisplayer ">
@@ -180,7 +181,7 @@ <h3>References</h3>
180181
181182 < br > < br >
182183
183- < b > [3 ]</ b >
184+ < b > [4 ]</ b >
184185 Hillshade explained< br >
185186 < object classid ="java:org.netbeans.modules.javahelp.BrowserDisplayer ">
186187 < param name ="content " value ="https://desktop.arcgis.com/en/arcmap/latest/tools/spatial-analyst-toolbox/how-hillshade-works.htm ">
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