NAME
r.mblend - Blends two rasters of different spatial resolution.
KEYWORDS
raster,
resolution
SYNOPSIS
r.mblend
r.mblend --help
r.mblend [-a] [high=string] [low=string] [output=string] [far_edge=value] [inter_points=value] [--help] [--verbose] [--quiet] [--ui]
Flags:
- -a
- Assign the average difference between the two rasters to the far edge (instead of zero).
- --help
- Print usage summary
- --verbose
- Verbose module output
- --quiet
- Quiet module output
- --ui
- Force launching GUI dialog
Parameters:
- high=string
- High resolution input raster.
- low=string
- Low resolution input raster.
- output=string
- Name of output raster.
- far_edge=value
- Percentage of distance to high resolution raster used to determine far edge. Number between 0 and 100.
- When the blending occurs along a single edge a number closer to 100 tends to produce more even results. With more blending edges (e.g. high resolution DEM sits on the middle of the low resolution DEM) a lower number may produce a more regular blend.
- Default: 95
- inter_points=value
- Number of points to use in interpolation.
- A higher number produces a smoother result but requires a lengthier computation.
- Default: 50
This module implements Mblend, a DEM merging method proposed by Leitão
et al. (2016). It deals with cases where a study area is only partially
covered by a high resolution DEM, with a coarser DEM available for the
remainder (as in the case shown below).
r.mblend merges the two DEMs,
producing a smooth transition from the high resolution DEM to the low
resolution DEM.
The module works by identifying the edge between the two rasters (near edge,
shown in read below) and the edge composed by the cells in the low resolution
DEM farther away from the high resolution raster (far edge, shown in blue
below). To each point along the near edge is assigned the difference between
the two DEMs. To each point in the far edge is assigned the value 0. The
Inverse Distance Weighted (IDW) method is then used to interpolate a new raster
with the points along the two edges. This interpolated differences raster thus
trends from the full difference at the near edge towards zero at the far edge.
The differences raster is finally added to the low resolution DEM given as
input. In the resulting DEM, cells along the near edge take the values in the
high resolution raster. The farther away from the near edge (and closer to to
the far edge) the closer is their value is to the low resolution raster,
producing a smooth transition, without artefacts.
Merge the
best_dem and
other_dem raster maps from the current mapset:
r.mblend high=best_dem low=other_dem output=result
Modifying the far edge distance cut-off:
r.mblend high=best_dem low=other_dem output=result far_edge=90
J.P. Leitão, L.M. de Sousa,
Towards the optimal fusion of high-resolution Digital Elevation Models for detailed urban flood assessment,
Journal of Hydrology, Volume 561, June 2018, Pages 651-661, DOI:
10.1016/j.jhydrol.2018.04.043.
L.M. de Sousa, J.P. Leitão,
Improvements to DEM Merging with r.mblend. In
Proceedings of the 4th International Conference on Geographical Information Systems Theory, Applications and Management - Volume 1: GISTAM, March 2018, pages 42-49. ISBN 978-989-758-294-3 DOI:
10.5220/0006672500420049.
J.P. Leitão, D. Prodanovic, C. Maksimovic,
Improving merge methods for grid-based digital elevation models,
Computers & Geosciences, Volume 88, March 2016, Pages 115-131, ISSN 0098-3004, DOI:
10.1016/j.cageo.2016.01.001.
Luís Moreira de Sousa
ISRIC - World Soil Information
João Paulo Leitão
EAWAG: Swiss Federal Institute of Aquatic Science and Technology.
SOURCE CODE
Available at:
r.mblend source code
(history)
Latest change: Sunday Aug 18 16:05:40 2024 in commit: f9d320e265329f9ec47c8a5ff0ce4876aa53e3e0
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