Geography Reference
In-Depth Information
Table 15.2 Examples of possible ground-based imagery applications.
Types of photos
Area covered
References
Grain size
Vertical ground photo
Set of stations
Graham et al. 2005 a&b
Grain morphometry
Vertical ground photo
Set of stations
Roussillon et al. 2009
Grain petrography
Vertical ground photo
Experiment
Riquier 2009
Sand coverage over a gravel
surface
Vertical ground photo
Carbonneau et al. 2005
Bank retreat using
photogrammetry
Oblique ground photo
At a station
Lawler, 1993; Barker et al., 1997;
Pyle et al., 1997
Wood raft area or isolated
pieces detection
Oblique ground photo
At a station
Moulin and Piegay, 2004
Light under the canopy
Fish eye/ground photo
Set of stations
Digan and Bren, 2003; Ringold
et al. 2003
Water level fluctuations;
morphological changes
Oblique ground
photo/timelaps video
At a station
Chandler et al., 2002; Hicks
et al., 2002; Ashmore and
Saucks, 2006; Luchi et al.,
2007; Bertoldi et al., 2009;
Bird et al., 2010
Wood censing, bank states
Oblique helicoptere
photos
Continuous reach
Piegay and Landon, 1997
Riparian Landscape
characterisation
Set of stations
Set of stations
Cossin et Piegay, 2001
Landscape changes between
n dates
Oblique ground photo
(present and archived)
Sampling landscape scenes
Start & Handasyde, 2002;
Michel et al. 2010
River ice growth
Oblique ground
Set of stations
Dube, 2009
Subaerial processes on a
river bank
Oblique ground photo
One river bank
Hamel, 2011
River sediment structures
Vertical from balloon
or mast
River channel width, riffle
Church et al., 1998
experiments, is not easily found in field studies,
particularly on large rivers. The Tagliamento River
example discussed briefly above and more fully below,
provides another case study where oblique photography
from fixed locations has provided important reach-scale
insights about a large braided river. A set-up similar
to the one described by Chandler et al. (2002), with
the acquisition of four daily images, allowed Ashmore
and Saucks (2006) to assess the relationship between
discharge and channel width in a braided network. The
analysis showed that it is possible to use this method to
obtain discharge data in a multi-channel system, where
other direct measurements may be impossible.
Imagery can also be used to target smaller features and
focus on a narrower scene. Some authors have used cam-
eras 'at-a-station', focusing on specific river cross sections
or on a morphological unit of interest. Examples of this
include Dube's (2009) quantification of river-ice growth
rate on a riffle and pool sequence during the freezing
season in Quebec and Moulin and Piegay's (2004) exami-
nation of wood accumulations to evaluate wood trapping
at reservoirs (Figure 15.3). In this last case, the reser-
voirs trap and accumulate migrating dead wood, which
allowed the authors to determine the geographical origin
and the transported volumes of dead wood in relation
to river flow regime. In these examples, ground-based
techniques are essential to guarantee a high temporal
resolution, but even more importantly to accommodate
the unpredictable nature of the documented processes.
Oblique close-range photography also has the advan-
tage of providing information on sites or processes that
are not seen by vertical images such as those beneath a
vegetation canopy (e.g. bank profiles and channel beds
in rivers with vegetated banks). For example, Bird et al.
(2010) recently showed how close-range photogramme-
try can overcome the limits of aerial surveys. In narrow
 
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