<eprint id="http://eprints.soton.ac.uk/id/eprint/383135" xmlns="http://eprints.org/ep2/data/2.0"><eprintid>383135</eprintid><rev_number>161</rev_number><documents><document id="http://eprints.soton.ac.uk/id/document/721195"><docid>721195</docid><rev_number>2</rev_number><files><file id="http://eprints.soton.ac.uk/id/file/4988000"><fileid>4988000</fileid><datasetid>document</datasetid><objectid>721195</objectid><filename>FloodingAreas.7z</filename><mime_type>application/x-7z-compressed</mime_type><hash>43f9a2e8814d52ea5592dbff8b1c9a7a</hash><hash_type>MD5</hash_type><filesize>755486</filesize><mtime>2017-06-09 13:13:07</mtime><url>https://eprints.soton.ac.uk/383135/1/FloodingAreas.7z</url></file></files><eprintid>383135</eprintid><pos>1</pos><placement>1</placement><mime_type>application/x-7z-compressed</mime_type><format>other</format><language>en</language><security>public</security><license>cc_by_4</license><main>FloodingAreas.7z</main><content>dataset</content><title>Flooding Areas - Western Kenya 2010, geotiff</title></document><document id="http://eprints.soton.ac.uk/id/document/721196"><docid>721196</docid><rev_number>2</rev_number><files><file id="http://eprints.soton.ac.uk/id/file/4988003"><fileid>4988003</fileid><datasetid>document</datasetid><objectid>721196</objectid><filename>LandCoverClassification.7z</filename><mime_type>application/x-7z-compressed</mime_type><hash>5b844a922e859d45464f7d19c5d2806c</hash><hash_type>MD5</hash_type><filesize>5036430</filesize><mtime>2017-06-09 13:13:08</mtime><url>https://eprints.soton.ac.uk/383135/2/LandCoverClassification.7z</url></file></files><eprintid>383135</eprintid><pos>2</pos><placement>2</placement><mime_type>application/x-7z-compressed</mime_type><format>other</format><language>en</language><security>public</security><license>cc_by_4</license><main>LandCoverClassification.7z</main><content>dataset</content><title>Landcover classification - western Kenya 2010, geotiff</title></document><document id="http://eprints.soton.ac.uk/id/document/721197"><docid>721197</docid><rev_number>2</rev_number><files><file id="http://eprints.soton.ac.uk/id/file/4988006"><fileid>4988006</fileid><datasetid>document</datasetid><objectid>721197</objectid><filename>VegetatedAreas.7z</filename><mime_type>application/x-7z-compressed</mime_type><hash>ecd92a3f306cf147fe1ca87e863a4826</hash><hash_type>MD5</hash_type><filesize>1104201</filesize><mtime>2017-06-09 13:13:09</mtime><url>https://eprints.soton.ac.uk/383135/3/VegetatedAreas.7z</url></file></files><eprintid>383135</eprintid><pos>3</pos><placement>3</placement><mime_type>application/x-7z-compressed</mime_type><format>other</format><language>en</language><security>public</security><license>cc_by_4</license><main>VegetatedAreas.7z</main><content>dataset</content><title>Vegetated Areas - Western Kenya 2010, geotiff</title></document><document id="http://eprints.soton.ac.uk/id/document/721198"><docid>721198</docid><rev_number>2</rev_number><files><file id="http://eprints.soton.ac.uk/id/file/4988009"><fileid>4988009</fileid><datasetid>document</datasetid><objectid>721198</objectid><filename>LandCover_ReadMe.pdf</filename><mime_type>application/pdf</mime_type><hash>3571b7bcab397c5a6e8df13c509540af</hash><hash_type>MD5</hash_type><filesize>315438</filesize><mtime>2017-06-09 13:13:09</mtime><url>https://eprints.soton.ac.uk/383135/4/LandCover_ReadMe.pdf</url></file></files><eprintid>383135</eprintid><pos>4</pos><placement>4</placement><mime_type>application/pdf</mime_type><format>application/pdf</format><language>en</language><security>public</security><license>cc_by_4</license><main>LandCover_ReadMe.pdf</main><content>dataset</content><title>Landcover classification procedure</title></document></documents><eprint_status>archive</eprint_status><userid>34173</userid><dir>foo/00/38/31/35</dir><datestamp>2015-10-22 13:42:14</datestamp><lastmod>2017-06-09 13:13:09</lastmod><status_changed>2015-10-22 13:42:14</status_changed><type>dataset</type><metadata_visibility>show</metadata_visibility><ispublished>unpub</ispublished><full_text_status>public</full_text_status><date>2015</date><publisher>University of Southampton</publisher><id_number>10.5258/SOTON/383135</id_number><data_type>Spatial data</data_type><divisions><item>uos2011-F8-WR-PJ</item></divisions><doi>10.5258/SOTON/383135</doi><creators><item><name><family>Wardrop</family><given>Nicola</given></name><id>8f3a8171-0727-4375-bc68-10e7d616e176</id></item></creators><contributors><item><type>http://www.loc.gov/loc.terms/relators/CRE</type><name><family>Wardrop</family><given>Nicola</given></name><id>8f3a8171-0727-4375-bc68-10e7d616e176</id></item></contributors><people><item>50801</item></people><title>Landcover classification: western Kenya, 2010.</title><abstract>&lt;span style='white-space:pre-line'&gt;Landcover classifications were produced for an area of western Kenya based on ASTER (15m spatial resolution) and Landsat (30m spatial resolution) imagery from 2010 and 2011. The land cover classification was carried out in a hierarchical manner, resulting in two overarching classes (a) vegetated land (versus built up and bare ground) and (b) flooding land (versus non-flooding land); and five lower level classes (c) agricultural land and grassland, (d) swamp, (e) trees and shrubs, (f) rice and (g) water bodies.&lt;/span&gt;</abstract><date_type>pub</date_type><languages_3char><item>eng</item></languages_3char><organisations><item>Geography &amp; Environment</item><item>Population, Health &amp; Wellbeing (PHeW)</item></organisations><pure_uuid>ec0b3177-f3f6-4693-bb59-dbe5c4bdaf4f</pure_uuid><geographic_area><item><latitude>0.853715</latitude><longitude>34.6482</longitude></item><item><latitude>34.6482</latitude><longitude>-0.0747764</longitude></item><item><latitude>-0.0747764</latitude><longitude>33.892</longitude></item><item><latitude>33.892</latitude><longitude>0.853715</longitude></item><item><latitude>0.853715</latitude><longitude>34.6482</longitude></item></geographic_area><projects><item><id>443</id></item></projects><bounding_box><north_edge>0.853715</north_edge><east_edge>34.6482</east_edge><south_edge>-0.0747764</south_edge><west_edge>33.892</west_edge></bounding_box><collection_method>A 10 km by 10 km grid was created in ArcMap to cover the study area. 14 grid cells were selected from this grid at random: the sublocation(s) which formed the major part of these 14 grid cells were used as sampling sites for training data collection, resulting in 24 sublocations for sample site collections. This was carried out to ensure a representative sample of locations was used in the training data collection.&#13;
&#13;
Training data was collected during October 2012. A research assistant with thorough knowledge of the roads and land cover within the study area was employed to assist with the land cover training data collection. During training data collection, the research assistant guided us along roads and paths throughout the sublocations of interest. A GPS, linked to a laptop running ArcMap, allowed real time location tracking. Training data polygons were created in ArcMap, relating to the specified land cover classes that were passed on the route. Manual checking of training data polygons was carried out via cross referencing GoogleEarth (where high resolution imagery was available) to minimise the impact of any training data collection errors.&#13;
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A separate set of training data were created using ArcMap: these identified areas of flooding and non-flooding land via visual inspection of ASTER imagery, from which areas of flooding land can be easily identified. This additional training data was selected due to the inherent difficulty in physically reaching flooded areas of land (e.g. swamps), to ensure good representation of flooding land for classification purposes. A random 10% sample of the training areas was selected for use in validation.&#13;
&#13;
Two ASTER images from 11th March 2010, which had no cloud cover, were selected for use in the classification. These were atmospherically corrected using the FLAASH module of ENVI, and then mosaicked to give a single image. See below for information on the scenes used and the settings used during atmospheric correction.&#13;
Scenes information:&#13;
ASTL1B 1003110806321003140170&#13;
Scene centre: 0.230217, 34.242193	&#13;
Flight date: 11th March 2010	&#13;
Flight time: 08:06:32	08:06:23&#13;
&#13;
ASTL1B 1003110806231003140169&#13;
Scene centre: 0.765325, 34.355913&#13;
Flight date: 11th March 2010&#13;
Flight time: 08:06:23&#13;
&#13;
Radiance scale factor: 10&#13;
Sensor altitude: 705.00&#13;
Pixel size: 15 m&#13;
Average scene altitude: 1,300 m&#13;
Atmospheric model: Tropical, rural&#13;
&#13;
Two Landsat images were also selected for use: one from 3rd July 2011 (Landsat 5 TM sensor) and one from 15th December 2010 (Landsat 7 ETM+ sensor). The Landsat ETM+ image was affected by the scan line corrector failure, resulting in a striped image, therefore, this image was gap filled using a third Landsat image (fill image) from 29th November 2010. Each of these three Landsat images were atmospherically corrected using the FLAASH module of ENVI. See below for information on the scenes used, the bands available and the settings used during atmospheric correction. Following atmospheric correction, the 15th December Landsat image was gap-filled using local histogram matching with the fill image in ENVI (using the Landsat gap-filling algorithm). For clarity, the July Landsat image will be referred to as Jul Landsat and the December image as Dec Landsat.&#13;
&#13;
Landsat 5 TM 06020110703&#13;
Scene centre: -0.00949955, 34.3042565&#13;
Flight date: 3rd July 2011&#13;
Flight time: 07:44:21&#13;
Sun elevation: 52.375&#13;
&#13;
Landsat ETM+ 06020101215 (SLC off)&#13;
Scene centre: 0.00542835, 34.29886655&#13;
Flight date: 15th December 2010&#13;
Flight time: 07:48:10&#13;
Sun elevation: 54.646&#13;
&#13;
Fill image Landsat ETM+ 06020101129&#13;
Scene centre: 0.00407185, 34.3002157&#13;
Flight date: 29th November 2010&#13;
Flight time: 07:48:02&#13;
Sun elevation: 56.954&#13;
&#13;
Radiance scale factor: 10&#13;
Sensor altitude: 705.00&#13;
Pixel size: 30 m&#13;
Average scene altitude: 1,300 m&#13;
Atmospheric model: Tropical, rural&#13;
&#13;
The images selected cover March 2010 (start of the long rains), July 2011 (end of the long rains) and December 2010 (start of the dry season). These were selected to allow optimal differentiation of different land cover classes by providing coverage during different seasons and different sections of the agricultural calendar.</collection_method><provenance>The land cover classification was carried out using eCognition Developer 8, which uses an object orientated classification approach (as opposed to a pixel-based classification). Segmentation was carried out using the ASTER image only (as this image had the highest spatial resolution – 15 m): the image was segmented in a hierarchical manner using scales of 50 and 15 to produce two levels with varying object sizes (scale 50 produces larger objects than scale 15), called level 1 (scale 50) and level 2 (scale 15). The homogeneity criteria were set as 0.8 for colour and 0.2 for shape, with the compactness parameter set at 0.5.&#13;
&#13;
The classification used a hierarchical approach. Four main classification steps were carried out as part of this hierarchical approach: &#13;
1.	Classify water bodies and land areas (level 1)&#13;
2.	Classify vegetated and non-vegetated land&#13;
3.	Classify flooding and non-flooding land &#13;
4.	Classify specific land cover classes (level 2)&#13;
&#13;
Water bodies and land areas – classification at level 1&#13;
No training areas were used in the classification of water bodies versus land areas: visual interpretation was used to identify the most suitable threshold values to classify water bodies (rivers and lakes). Lake was classified as objects with mean ASTER band 3 &lt;1020. River was classified as objects with mean Jul Landsat band 5 &lt; 1500 and contrast to neighbouring pixels ASTER band 3 &lt; -350. These classes were grouped together into a single “water bodies” class. A copy of level 1 with the water body classification was created to allow subsequent classification of the land areas into flooding and non-flooding land, and vegetated and non-vegetated land. To clarify – it is possible for flooding land to be either vegetated or non-vegetated and vice versa.&#13;
&#13;
Flooding and non-flooding land – classification at level 1&#13;
The flooding land training areas were imported into eCognition and used to create samples (overlap parameter set to 0.5). Nearest neighbour classification was performed on the objects which were not classified as water bodies in step 1 using the features: mean and absolute mean difference to neighbours (elevation); mean (ASTER band 2); mean of inner border (Jul Landsat band 5); and mean of outer border (ASTER bands 2 and 3). A subsequent filtering step was carried out to remove noise from the classification: objects classified to flooding land were merged together and if the resulting object was less than 600 pixels they were reclassified as non-flooding.&#13;
&#13;
Vegetated versus non-vegetated areas – classification at level 1&#13;
This classification used the copy of the water bodies classification layer (e.g. this was carried out independently of the flooding and non-flooding land classification). The training areas recorded during fieldwork were reclassified as either vegetated or non-vegetated and imported into eCognition. These were used to create samples for the classification (overlap parameter set to 0.1). Nearest neighbour classification was performed on the objects which were not classified as water bodies in step 1 using the features: maximum pixel value (Jul Landsat band 1); mean (Jul Landsat band 5, ASTER band 2); standard deviation (Jul Landsat band 7); and maximum difference.&#13;
&#13;
Classification of specific land cover classes – classification at level 2&#13;
The final level of classification made use of each of the previous classifications. Objects where the super-object (e.g. level 1 object) was classified as water bodies were also classified as water bodies. Objects where the super-object was classified as non-vegetated land were classified as artificial and bare ground. Training data were used to create samples (overlap parameter set to 0.1) for the remaining classes (swamp, rice, crops and grassland, woodland and shrubs). The feature space optimisation tool was used to select the features which resulted in the best separation of classes, and nearest neighbour classification was performed using these features on objects which were not classified as water bodies or artificial and bare ground. The features used were: area; mean difference to neighbours (Dec Landsat band 2 and ASTER band 2); maximum pixel value (Dec Landsat band 4, Jul Landsat bands 4 and 7); mean (Jul Landsat band 2); standard deviation (Dec Landsat bands 4 and 5); mode (Jul Landsat band 2); minimum pixel value (ASTER band 1 and Dec Landsat band 2); ratio (ASTER band 3 and Jul Landsat band 3). Finally, manual editing was performed on some areas where there were unclassified objects or inconsistencies (e.g. the tops of hills) based on visual interpretation of the remotely sensed imagery and the classification of surrounding objects. &#13;
&#13;
Accuracy assessment&#13;
The results show user and producer accuracies of greater than 0.7 for all classes, with the majority of classes having accuracies of greater than 0.8. This indicates a high level of classification accuracy.</provenance><geographic_cover>Western Kenya</geographic_cover><language>English</language><temporal_cover><date_from>2010</date_from><date_to>2011</date_to></temporal_cover><fp7_type>info:eu-repo/semantics/other</fp7_type><dates><item><date>2015</date><date_type>pub</date_type></item></dates><hoa_date_pub>2015-10-22</hoa_date_pub></eprint>