Captured as part of the 2010-11 CIP, this 10cm georeferenced photography was captured by AAM with their A3 camera system along with the 10cm DOT project then separated out and further processed for use by Casey and Mornington Peninsula Shires. Georeferenced photography has less horizontal spatial accuracy compared with a fully orthorectified product, but the photography is still useful for a wide range of council purposes.

River condition in Victoria is assessed every 5 years using the Index of Stream Condition (ISC). The Department of Environment and Primary Industries (DEPI) has developed a methodology to assess components of the ISC using remote sensing techniques, specifically LIDAR and aerial photography. As such, a State Wide mapping project was undertaken in 2009-12 to accurately map the riparian vegetation and physical form components (metrics) of the ISC using LiDAR and imagery data. Remote sensing data collected includes 15cm true colour infra-red aerial photography and four return multi-pulse LiDAR data. These were used to derive a range of standard and non-standard physical form and riparian vegetation raster datasets. The project was managed on a CMA by CMA basis with all source and derived datasets being organised this way. In addition to the remote sensing and derived raster products, a set of vector products and tabular data has also been generated. These further represent and define the physical form and riparian characteristics of the ISC rivers and contain the ISC scoring data. Keywords: River, ISC, Victoria, LiDAR, Riparian, Physical Form, Vegetation, Elevation

Four return, multi-pulse LiDAR was aquired over the Corrop Lakes Floodplain on the 14th and 15th June 2011 to achieve a vertical accuracy of +/- 10 cm. The LiDAR was used to create a 1m gridded DEM. The intended purpose of the data is to assist with flood modelling and land use planning. Keywords: DEM, LiDAR, +/- 10cm vertical, elevation, floodplains, Goulburn Broken CMA, Corrop Lakes

This photography was captured to assess the flood damage in selected towns in Wimmera CMA. The Georeferenced (reduced accuracy) image includes 3 visible bands and tiled into 1km tiles. It is available in both TIFF and ECW compress format.

This photography was captured to assess flood damage along rivers in selected towns in WCMA & GHCMA: Great Western, Navarre, Beufort, Skipton, and Glenorchy. The Georeferenced (reduced accuracy) image includes 4 bands and tiled into 1km tiles. It is available in both TIFF and ECW compress format.

38-2011 Floods-Rochester,Serpentine,Charlton,Casterton

This photography was captured to assess flood damage in Wimmera CMA. The Georeferenced (reduced accuracy) image includes 4 bands and tiled into 1km tiles. It is available in both TIFF and ECW compress format.

River condition in Victoria is assessed every 5 years using the Index of Stream Condition (ISC). The Department of Environment and Primary Industries (DEPI) has developed a methodology to assess components of the ISC using remote sensing techniques, specifically LIDAR and aerial photography. As such, a State Wide mapping project was undertaken in 2009-12 to accurately map the riparian vegetation and physical form components (metrics) of the ISC using LiDAR and imagery data. Remote sensing data collected includes 15cm true colour infra-red aerial photography and four return multi-pulse LiDAR data. These were used to derive a range of standard and non-standard physical form and riparian vegetation raster datasets. The project was managed on a CMA by CMA basis with all source and derived datasets being organised this way. In addition to the remote sensing and derived raster products, a set of vector products and tabular data has also been generated. These further represent and define the physical form and riparian characteristics of the ISC rivers and contain the ISC scoring data. Keywords: River, ISC, Victoria, LiDAR, Riparian, Physical Form, Vegetation, Elevation

Landsat 2008-09

The purpose of collecting historic air photos is to detect and measure any changes (long term progressive or cyclic) in shorelines over the last 60 years. The sorts of shorelines that may have shown significant change over that sort of time frame include sandy beach-dune shores, scarped 'soft-rock' shores, muddy mangrove shores, and others. The photography will be used to identify an erosion scarp or a seawards vegetation limit (which may move seawards or landwards as a shore erodes or accretes).