FOR 474: Forest Inventory LiDAR for DEMs The Main Principal Common Methods Limitations Readings: See Website.

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FOR 474: Forest Inventory LiDAR for DEMs The Main Principal Common Methods Limitations Readings: See Website

The laser pulse travel can travel through trees before hitting the ground. Secondary returns might not be from the ground Lidar DEMs: Understanding the Returns Non ground objects could include: Shrubs Ladder Fuels Seedlings Buildings Wildlife TANKS!!!

The different vertical structure of deciduous and coniferous forests can be highlighted by the returns Lidar DEMs: Understanding the Returns

In modern lidar systems, 1-9 returns are possible depending on sensor. The returns from one pulse are not in the same horizontal or vertical location. 1st 2nd 3rd Lidar DEMs: Understanding the Returns Source: Jeffrey Evans USFS RMRS-Moscow

Intensity Intensity of the object reflecting the laser 8-bit scale (0-255) Adaptive Gain (values are not calibrated) Orthorectified image Source: Jeffrey Evans USFS RMRS-Moscow Lidar DEMs: Understanding the Returns The Intensity is an output of all Lidar acquisitions

Lidar DEMs: Understanding the Returns The Intensity is different for hardwood and coniferous forests

Lidar DEMs: The Raw Data

Lidar DEMs: The General Principal To generate a DEM from Lidar we identify what returns are associated with the ground reflections and delete all the rest. Source: Jeffrey Evans USFS RMRS-Moscow

Lidar DEMs: The General Principal The challenge in forestry is that most of those filtering methods don’t cope well with non-ground objects beneath the first returns: Shrubs, seedlings, wildlife, ladder fuels, coarse woody debris, slash, etc, etc, etc Source: Campbell 2007 Many different methods exist to identify the ground from non- ground returns. They are called “filtering” methods

This process is repeated until the surface stops changing: Lidar DEMs: The General Principal Source: Jeffrey Evans USFS RMRS-Moscow

Lidar DEMs: The General Principal Source: Jeffrey Evans USFS RMRS-Moscow

Lidar DEMs: The General Principal

Lidar DEMs: The Block Minimum Method Block Minimum: The Lidar points are divided into grid cells and the lowest point is chosen as the ground. Easy to Implement Does not work well in high canopy cover forests

Lidar DEMs: The Block Minimum Method Block Minimum: When canopy cover / biomass is high there may be very few ground returns in your “bin” You might need select lowest point in 5x5m area instead of 1x1 m areas If the bin is too large you might miss topographic features!!!

In this case a Block Minimum 6 x 6 meter bin size was still not enough to “see” enough ground returns. Lidar DEMs: The Block Minimum Method Source: Jeffrey Evans USFS RMRS-Moscow

In general, lock Minimum has problems with shrub and understory or when canopy cover is high From Zang et.al, (2000) Lidar DEMs: The Block Minimum Method

Lidar DEMs: The Slope Threshold Method Slope Threshold: Starting at the 1 st point, all points higher than a slope from the first point are deleted. Then repeat at the next point

Problems where features have abrupt edges: buildings/cliffs From Vosselman, (2000) Building Footprint Problems in high canopy cover Lidar DEMs: The Slope Threshold Method

What is a curvature? An aberration from the ground A point higher than the surrounding points Not an edge!!! Curvatures Edges Lidar DEMs: The Progressive Curvature Filter Source: Jeffrey Evans USFS RMRS-Moscow

Lidar DEMs: The Progressive Curvature Filter We have curvatures in Forestry. This method is widely used by the USFS and other agencies (ARS, BLM, etc). Source: Jeffrey Evans USFS RMRS-Moscow

Lidar DEMs: The Progressive Curvature Filter We have curvatures in Forestry. As the filter does each pass, the curvatures in the forest becomes less distinct Source: Jeffrey Evans USFS RMRS-Moscow

Lidar DEMs: The Progressive Curvature Filter We have curvatures in Forestry. This method repeats until a “smooth” surface remains Source: Jeffrey Evans USFS RMRS-Moscow

DEM produced in high biomass area. Lidar DEMs: The Progressive Curvature Filter Source: Jeffrey Evans USFS RMRS-Moscow

Lidar DEMs: Common Errors - Les Moutons Source Lefsky (2005)

Lidar DEMs: Common Errors - Les Moutons

Lidar DEMs: Common Errors – Data Gaps Data Gaps: If too few ground returns are present the ground surface may miss “real” topographic features

Lidar DEMs: Common Errors – Data Gaps Data Gaps: Similar problems can occur when the lowest return is from elevated vegetation

FOR 474: Forest Inventory Next Time … Plot Level Metrics from Lidar