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Spatio-temporal landscape analysis in mountainous terrain by means of small format photography: A methodological approach


Abstract and Figures

A method is presented in order to georectify high-oblique terrestrial images of high mountainous terrain taken by means of small-format camera. Using the distinct topographic situation of the study area located in a small alpine valley, an automatic camera has been mounted on the opposing hill slope providing daily photographs of the area of interest. To use the data in a geographic information system (GIS) a specific georectification method (JUKE method) was developed employing a digital elevation model (DEM), several reference and ground control points (GCPs), and the focal length of the lens. The method was useful for single-stage image rectification but was also applied successfully on pre-analyzed time-series images (“summary” images). Hence, the procedure enables the analysis of detailed, dynamic landscape ecological processes. Accuracy was mainly a measure of the quality of the GCPs, which were difficult to define in this remote area. The relatively economic data capturing and transforming procedure makes the method interesting for various applied disciplines in order to gain detailed spatio-temporal data. This method might be of considerable benefit, particularly in mountainous terrain where it is often difficult to capture continuous spatio-temporal information
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Spatio-Temporal Landscape Analysis in Mountainous
Terrain by Means of Small Format Photography: A
Methodological Approach
Janette Aschenwald, Karin Leichter, Erich Tasser, and Ulrike Tappeiner
Abstract—A method is presented in order to georectify
high-oblique terrestrial images of high mountainous terrain taken
by means of small-format camera. Using the distinct topographic
situation of the study area located in a small alpine valley, an
automatic camera has been mounted on the opposing hill slope
providingdaily photographs of the area ofinterest. To usethe data
in a geographic information system (GIS) a specific georectifica-
tion method (JUKE method) was developed employing a digital
elevation model (DEM), several reference and ground control
points (GCPs), and the focal length of the lens. The method was
useful for single-stage image rectification but was also applied
successfully on pre-analyzed time-series images (“summary”
images). Hence, the procedure enables the analysis of detailed,
dynamic landscape ecological processes. Accuracy was mainly a
measure of the quality of the GCPs, which were difficult to define
in this remote area. The relatively economic data capturing and
transforming procedure makes the method interesting for various
applied disciplines in order to gain detailed spatio-temporal
data. This method might be of considerable benefit, particularly
in mountainous terrain where it is often difficult to capture
continuous spatio-temporal information.
Index Terms—Digital elevation model (DEM), georectification,
landscape ecology, mountain areas, oblique terrestrial images,
small format photography, time-series.
NE IMPORTANT aspect concerning landscape analysis
is the investigation of temporal changes of spatial phe-
nomena in mountain ecosystems. In the course of the past years,
this topic has received considerable attention in the literature as
landscape changes can be observed frequently and often lead to
serious alterations of ecosystem processes [1], [2].
However, accurate temporal investigations are rare, though
the analysis of detailed time series can lead to important find-
ings about landscape ecological processes. Integrated in a GIS,
the temporal component enables the analysis and simulation of
substantial dynamic processes [3], [4].
Manuscript received December 16, 1999; revised October 16, 2000. This
work was supported in part by the fourth framework of the EU, Project
ECOMONT (ENV4-CT95-0179), and by the INTERREG-II Project INTE-
J. Aschenwald is with the Department of Economic Policy and Economic
Theory, University of Innsbruck, Innsbruck, Austria (e-mail: janette.aschen-
K. Leichter and E. Tasser are with the European Academy Bolzano, Bolzano,
Italy (e-mail:;
U. Tappeiner is with the Institute of Botany, University of Innsbruck, Inns-
bruck, Austria, and also with the European Academy Bolzano, Bolzano, Italy
Publisher Item Identifier S 0196-2892(01)02153-2.
But the possibilities of capturing time series with high tem-
poral resolution are very limited, particularly in mountain re-
gions. Conventional mapping systems sufferfrom variousdraw-
backs. Mapping in the field is extremely time consuming and
thus not feasible for short, regular time intervals. Aerial cam-
paigns are very costly and hence are usually restricted to only a
few selected dates. Satellite imagery is still not provided at suf-
ficient spatial and temporal resolutions needed for research in
small mountainous areas.
One economic alternative would be the use of a small format
camera that provides terrestrial photographs. High oblique im-
ages are usually captured in such cases due to the camera posi-
tion in relation to the study site. This consequently results in a
problem of georectification which needs to be considered seri-
ously in areas of mountainous terrain [5], [6].
Due to the complex image geometry, high oblique pho-
tographs are normally used for documentation purposes only.
In contrast to aerial photographs, where the optical axis needs
to be near-vertical, the axis is shifted severely (in fact, it can
be close to horizontal). The georectification of such images
for integration in a GIS is rarely pursued. Consequently, it
is not possible to apply any of the standard procedures for
georectification offered by various GIS and remote sensing
packages. With the help of terrestrial photogrammetry [7],
[8] specific procedures need to be developed. Hence, there do
exist a few special programs for the geometric correction of
oblique (aerial and terrestrial) photographs, most of which are
monoplotting procedures. To name a few, the program-system
BUSCH-DHM was applied by Waldhäusl
et al. [9] in order
to map the quality of vegetation on ski slopes from terrestrial
photographs. Aschenbrenner [10] analyzed glacier surfaces
derived from terrestrial and aerial images using the package
SCOP-MONOPLOT. Also, Kirnbauer et al. [11] used digital
monoplotting for examining snow cover patterns from oblique
nonmetric aerial photographs. Warner et al. [12] developed
a monoscopic measurement system for vertical and oblique
All these techniques mainly support the transformation of
selected image information, namely, identified boundary lines,
and hence do not allow the georectification of the entire image
contentina raster data format.Thisstudyhowever,isfocusedon
developing a method that enables the production of orthophotos
from high oblique terrestrial imagery. Moreover, the analysis of
a time series of images is of interest and therefore, the goal of
the developed method is to support the requirements of such an
analysis as well. As snow distribution is a spatio-temporal phe-
0196–2892/01$10.00 © 2001 IEEE
nomenon of crucial importance for high mountain ecosystems
[13], [14], snow pattern analysis is chosen in order to test the
developed model with a detailed time series.
The objective of this study is to develop a simple and eco-
nomic method to:
capture data series of spatial information in mountainous
terrain with any temporal resolution desired by means of
a small-format camera;
georectify terrestrial, high-oblique photographs for input
to a GIS;
apply the developed georectification technique on both
single-stage and pre-analyzed time series (“summary”)
A. Study Area
The study area is situated in the upper Passeier Valley, South
Tyrol, Italy, in the central eastern Alps. It is a narrow, v-shaped
valley with fairly steep slopes. The area of ecological interest
is located on the orographic right, south exposed hill slope,
comprising the alpine meadows of the farmers of the village
Walten and the adjoining forest below. It extends over approx-
imately 3 km
and ranges from 1200 m to 2350 m in altitude.
For details, see [15].
B. Automatic Camera and Position
As a capturing system, a 35 mm single lens reflex camera,
namely a Pentax A-3 with Takumar 28–80 mm objective, was
used with Kodak Elite Chrome 100 color slide films. To be
able to take photographs automatically, an electronic timer was
added to the camera.
The topographic situation of the study area, as described
above, provided an optimal solution for the positioning of the
camera. On the opposing hill slope of the study site the camera,
covered by an open metal box, was mounted within a forest
clearing at an altitude of 1521 m. From this position, the central
and most important section of the study site was clearly visible.
The focal length was adjusted to 35 mm to cover the entire
area of interest. The horizontal distance to the area of interest
ranged between 1250 m and 2350 m. Only approximately 3%
of the photographed area could not be seen due to the position
of the camera in relation to the study site. This was checked
by a calculated visibility map. To avoid confusion within the
georectification procedure, the corresponding areas needed to
be excluded from the calculations.
The lensaperture and the exposure time were set to automatic
to allow adjustment to varying weather conditions. By means of
the timer one photograph was taken every day at noon (12.00 h
CET). As a result, a very detailed time series of more than four
years has been established up to now. The study itself, however,
focuses on the period between November 1996 and September
C. Preparation of Photographs
For further processing and integration with GIS, the color
slides were transformed into digital form. They were scanned
with a resolution of 1100 dpi (1536
1024 pixels) by a com-
Fig. 1. Projection of the three-dimensional (3-D) DEM onto the
two-dimensional (2-D) image plane.
: ground coordinates of
the DEM;
: image coordinates of the projected DEM.
mercial company and saved in Kodak Photo CD format (.pcd).
This resulted in a file size of approximately 4.5 MB for each
image. The geometric resolution varied somewhat within the
images (0.5–2.5 m) due to scale variations. The nominal pixel
size in the center of the image covered an area of about 1
For practical reasons the images needed to be pre-processed.
The extent of the images was reduced somewhat on all sides to
a final image size of 1349
624 pixels.
D. Digital Elevation Model
Working with single images in mountainous terrain required
the use of a high-quality and high-resolution digital elevation
model (DEM) [16]. The DEM was generated from 5 m con-
tour lines and the incorporation of auxiliary line and point data
(e.g., ridges, edges, river network, peaks, and depressions) by
applying a sophisticated linear interpolation technique, namely,
the Stochastic Contour Interpolation Method (SCIM) [17]. As
a result, a DEM with a spatial resolution of 5 m and a sub-
pixel accuracy was available. The DEM was georeferenced to
the Italian grid system (Gauß–Boaga projection, International
Spheroid oriented to Rome M. Mario).
A. JUKE Method
differs significantly from the standard monoplotting procedure.
In monoplotting, the image rays from the camera of the identi-
fiedboundary lines areintersected pointby point with thedigital
elevationmodel to find the
-coordinatesof thelines. In the
JUKE method, however, the DEM is projected onto the image
plane (Fig. 1), which enables the relation of the ground coor-
dinate system (
) with the image coordinate system ( ).
This is an efficient and fast technique to obtain the information
pixel by pixel.
Monoplotting has essential disadvantages.
displacement of objects due to misinterpretation when
identifying boundary lines in the photographs, in partic-
ular when the distance between the object and the camera
position is large;
displacement of objects due to small intersection angles
between the image rays and the DEM, in particular for
terrestrial images;
additional inaccuracies caused by linear interpolation be-
tween the intersected points.
Fig. 2. (a) Digital photo. (b) Projected DEM. (c) Both data superimposed.
Applyingthe JUKE method, these inaccuraciestypical forthe
monoplotting technology do not occur. The intrinsic character-
istic of the JUKE method, namely to project the DEM onto the
image plane, guarantees a definite relation of the points(despite
nonlinear effects). Once the transformation parameters (inner
and outer orientation) are determined, all points are projected
by only a few calculation steps. Therefore, it is also a computa-
tionally efficient method. Furthermore with the help of ground
control points (GCPs) the accuracy of the JUKE method (rela-
tive to the accuracyof the DEM and the GCPs) can be specified.
The necessary mathematical equations and derivations are to
be found in specific photogrammetry text books [7], [8].
B. Input Information
For the calculations, the coordinates of various reference
points and GCPs were necessary as input for the JUKE method.
The exact ground position of the camera was measured by
means of differential GPS surveying (spatial accuracy:
1 m).
As a reference receiver, a Trimble 4000 (L1) was available, and
as mobile receiver, a Trimble Pro XL was used.
The ground location of the perspective center of the images
was needed to identify the direction of the optical axis of the
lens system (outer orientation). Normally, the optical axis
should have been horizontal, but a horizontal orientation could
not be guaranteed in practical operation because of some
technical hitches in mounting the camera. The respective center
point of the images was established by connecting the opposing
corners of the images on the screen with very fine lines (inner
orientation). The corresponding ground coordinates were
determined by defining their position on an already available
orthophoto of the study area (scale 1 : 5.000, date of flight
August 23, 1997) [18]. With this information, the location and
orientation of the respective image plane with regard to the
DEM were obtained.
Some of the essential mathematical computations could only
be carried out with the help of several GCPs. Features that were
clearly identifiable in the image were selected, and their image
coordinates were ascertained. Their ground position was either
located with the highest possible precision on the available
orthophoto or measured by means of GPS. Image as well as
ground coordinates were obtained for 15 GCPs.
C. Procedure
For each pixel corner of the DEM, a unique identification
number (ID) as well as the ground coordinates (
) were
calculated and written to an ASCII-file. Knowing the exact po-
sition of the camera, those pixels that were not visible from the
camera location were calculated and marked on the DEM. All
pixel corners covered by this masked area were then deleted
from the ASCII-file.
By means of the JUKE method and the aforementioned input
information, the necessary parameters were calculated. Conse-
quently, all points of the DEM prepared in the ASCII-file were
reflected, shifted, projected, rotated, and multiplied with the
enlargement scaling factor to get the corresponding points on
the image plane. The output ASCII-file now contained three
columns: the identification number and the
- and -coordi-
nates of the pixel corners of the DEM expressed in the coor-
dinate system of the image.
The resulting point information of the new ASCII-file (pro-
jected DEM) was then converted into an ArcInfo (Workstation
7.2) raster file (grid) with the same extent and pixel size as the
prepared image. It was now possible to superimpose the two
grids (projected DEM and image) spatially and combine their
information (Fig. 2). The digital number of each pixel of the
image, which represented the relevant radiometric information,
was appended to the pixel information (the ID number) of the
projected DEM. These two columns were then written into a
third ASCII-file. By means of the ID number, the ground coor-
dinates (i.e., the
, and coordinates of each pixel corner)
were still known. Consequently, the radiometric information of
the image could be depicted in the national map projection and
ground coordinate system. To provide an adjusted value for the
entire pixel, the values of the four surrounding pixel corners
were averaged. The image was now available for overlay with
other spatial data and for incorporation into landscape models.
Forthis study,thegeorectificationwas conducted with single-
stage images as well as with pre-analyzed “summary” images
(amount of days covered with snow) as the analysis of time se-
ries was focused on.
D. Quality of the JUKE Method
The mean Euclidean distance wasused to evaluatethe quality
of the JUKE method. This measure is defined as the mean de-
viation of the calculated points from their known position, in
contrast to the root mean square error (RMSE), which measures
the root of the mean squared deviation.
The set of GCPs was divided randomly into two disjunct sets,
one of which wasthe training set and the other one of which was
the validation set. The training set was used exclusively to com-
pute the orientation of the optical axis. The points of the vali-
dation set were employed to calculate the mean Euclidean dis-
tance. Because of the random choice of these two sets, the mea-
sure could also be biased in both directions and thus, the mean
Euclidean distance on the validation set was not a consistent
estimator for the model performance. Therefore, the bootstrap
Fig. 3. Summary of the model structure. Gray input data; surrounded by broken line
procedure; and black statistical evaluation.
method was applied to achieve statistically correct statements
about the performance of the JUKE method and its standard de-
viation [19]. The set of reference points was not only divided
once into two sets but
times. The procedure of calculating
the parameters of the JUKE method with the help of the training
points and subsequently the corresponding performance on the
validation set (mean Euclidean distance) was repeated
The average over all these performances gave a consistent esti-
mator of the quality of the method and a consistent estimator of
the standard error could also be achieved.
E. Practical Realization
The model was programmed in Visual Basic 6.0 and can
be downloaded from the homepage with the internet address Minimum
requirement is a 486 computer with Windows NT or 9
operating system.
The program requires the following inputs:
camera position;
center point of the photo;
focal length;
text file of the data (DEM);
text file of reference and GCPs;
number of bootstrap replications (optional);
ratio of the number of training points to the number of
validationpoints (at themoment,this ratio isfixed to 2: 1).
The ground coordinates of the center point of the images,
which was the intersection point of the image diagonals, was
very difficult to measure. On the ground, this intersection point
was located within the forest and it was thus impossible to re-
late it to a specific image object. Consequently, the ground co-
ordinates of the image center point could not be ascertained
with confidence. To obtain still quite good results, a raster with
a cell size of 1 m was put around the supposed center in the
-, -, and -directions in the DEM, each raster point repre-
senting a possible center. With each possible center the model
was calculated 100 times and the one with the smallest mean
Euclidean distance on the validation set was selected as the best
center. This procedure guaranteed a good performance even if
the center was not clearly identifiable.
As a summary, Fig. 3 demonstrates graphically the structure
of the entire procedure.
F. Method for Time Series
The focus of this project was not only to analyze single-stage
images but a time series of photographs. Therefore, a useful
procedure for automation had to be developed.
In this section, two methods of time-series analysis are de-
scribed. On the one hand each single image could be georec-
tified separately by means of the above introduced procedure.
The thematic analysis would then be conducted afterwards.
On the other hand the images of a specific time period could
first be added up pixelwise. Consequently, only the resulting
summary image needed to be georectified. The latter procedure
offered the great advantage of identifying and measuring the
reference and control points just once for the reference image.
Hence, a considerable amount of time could be saved this way.
Due to temperature changes leading to subtle movements of
the metal container, which was used for camera suspension, a
variation of the image extent for the various photographs was
expected. Therefore, it was not possible to add up all single im-
ages without making arrangements. Applying the second anal-
ysis procedure, relative image registration was a prerequisite
as image analysis was carried out before the georectification
procedure. To provide the same properties for all images of a
continuous month series, a relative registration was carried out,
adapting the extent and resolution of each image to one specific
reference image, i.e., a warping was performed. By means of
four control points identifiable in all images, the co-registration
was carried out. It was now possible to superimpose all these
Images which could not be used due to bad weather (fog,
clouds, dust) were taken off the time series and substituted with
images from the day before or after which ever fitted best. Con-
Fig. 4. Locations of 15 GCPs G1–G15 and nine test points T1–T9. The broken line characterizes the used image extent.
sequently, all zones without significance for this study were cut
offand masked out,respectively.Hence, the skywas masked out
defining a threshold using a clear summer photograph. A clear
winter photograph was used for masking out the forest. The ra-
diometric information of thepixel in eachimage was then trans-
ferred into binary data by defining a threshold, “0” standing for
Consequently, all images of a specific snow period were super-
imposed and the digital numbers (0 or 1) were added up pixel-
wise, resulting in an image representing the cumulative score of
days with snow cover at each cell. Finally, the model was calcu-
lated for the reference image only and was then superimposed
with the “summary” image.
This technique would represent a comfortable automation
procedure for time series analysis, but first, the quality of this
procedure needed to be checked. Thus, nine test points were
selected, all of which were not covered with snow during the
whole period. The pixel representation of these selected objects
in the summary image and their appearance in the single images
were compared.
Two main questions are addressed in this section.
How suitable was the model for georectification of single-
stage images?
Was the described method successful and useful for time-
series analysis?
A. Georectification: Single Image
A single image was prepared and the DEM was calculated
correspondingly by means of the developed JUKE method. Fi-
nally, both data sets were superimposed to obtain the informa-
tion of interest (Fig. 2). Fifteen GCPs were available to com-
pute the parameters ofthe model. Great attentionwas paid to the
fact that these points were distributed approximately uniformly
throughout the area (Fig. 4). Theywere randomly separated into
ten points for the training set and five points for the validation
set. The more points included in the training set, the better the
accuracy of the model will be.
As an example, an image taken January 11, 1997 was geo-
rectified. For a quantitative judgement, the mean Euclidean dis-
tance on the validation set was calculated to be 2.78 pixels.
According to the different resolutions of the image, caused by
oblique view and topography, this result represented an average
deviation of approximately 1.4 m in the lower, 2.8 m in the
middle, and 7 m in the upper part of the image. With regard
to the final resolution, which was given by the resolution of the
DEM(5m),the mean Euclidean distance correspondedto a high
quality model.
This remarkable result was also supported by repeating the
calculation 100 times. The mean performance amounted to 2.32
pixels with a standard error of 0.39pixels. These results empha-
sized the quality of the JUKE method.
Furthermore, it was checked if the applied technique of
finding the best center by putting a raster around the supposed
center could improve the performance. The raster width was
-, -, and -direction, and the lateral length of the
entire raster was 100 m. The mean performance could be
improved only slightly. But this fact was not surprising because
of the goodness of the previous results. With the optimized
center, the mean performance amounted to 2.14 pixels with a
standard error of 0.41 pixels.
Furthermore, the quality of the model was checked by ap-
plying the methodto eightsingle images from different filmsse-
lected randomly. The image coordinates ofall GCPswere ascer-
tained for each image separately and a raster as described above
was put aroundthe supposed center point of each photo. The se-
lected photos showedclearly the variation of the center (Table I)
andconsequentlyof the optical axisand the GCPs.Ameandevi-
ation of 1.6 pixels in
-direction and approximately 1.5 pixels
Fig. 5. The “summary” image representing the cumulative score of days with snow cover at each cell (a) before and (b) after the georectification procedure.
in -direction were measured after georectifying the eight se-
lected images separately. As the performance results demon-
strated, this fact was not a problem for single image georecti-
fication because of the flexibility of the model that calculated
the optical axis and the optimal center for each. But it was nec-
essary to identify the image coordinates of the GCPs for each
photograph separately. Therefore, time-series analysis by geo-
rectifyingeachsingle imageof a specificperiod wasshowntobe
possible, but of course this would be a time consuming method.
The slight instability of camera adjustment could be a disad-
vantage for time-series analysis using the second method. But
the following section demonstrates theusefulness of the second,
automated, and less time intensive procedure.
B. Georectification: Time-Series
For all images of a continuous seven month series, a rela-
tive registration was carried out, adapting the extent and reso-
lution of each image to the specific reference image dated from
January 11, 1997. This was done with the help of four control
points identifiable in all images. Consequently, 204 images of
the snow period 1997/98 were superimposed, and the digital
numbers (0 or 1) were added up pixelwise, resulting in an image
representing the cumulative score of days with snow cover at
each cell [Fig. 5(a)].
Finally, the JUKE method was calculated for the reference
image (January 11, 1997) only. The grid of the projected
DEM was then superimposed with the summary image and
consequently retransformed into the national coordinate system
[Fig. 5(b)].
Forcheckingthe quality of the co-registrationprocedure,nine
smallobjects (e.g., trees,rocks) that werenot coveredwith snow
during the whole period were selected to serve as test points
(Fig. 6). The pixel values representing these objects in the sum-
mary image were compared to the desired pixel values, which
Fig. 6. (a) Position of test point T . (b) Magnified illustration of the snow situation around test point T . The pixel values in the summary image (actual values)
differ from the desired pixel values. Instead of the ideal value of zero at the location of T
, the actual values were 105 and 88, i.e., a minimum of 88 images
out of a total of 163 images were positioned slightly incorrectly. (c) Actual and desired snow distribution around test point T
represented diagrammatically. (d)
Superimposed information of the desired and the actual snow distribution around test point T
. Test point T and the mean of all nine test points represented
were deduced from the single images. As an example, consid-
ering only one row of pixels, test point T
[Fig. 6(a)] should be
depicted ideally by two pixels side by side, each with the value
0 (desired values), the adjoining pixels should have values of
163 [Fig. 6(b)].Actually, however,test pointT
with values of 105 and 88 in the summary image (actual values).
The values of the adjoining pixels increased from 124 up to 163
[Fig. 6(b)]. This showed that a minimum of 88 single images
out of a total of 163 images were not positioned exactly. This
resulted in the objects being somewhat blurred in the summary
image with a measured positioning error of four pixels to the
right (east) and of two pixels to the left (west) [Fig. 6(c)].
This procedure was repeated for all nine test points. On av-
erage, the objects were expanded incorrectly two pixels (1–5
m) to the left side and five pixels (2.5–12.5 m) to the right side
[Fig. 6(d)]. This gave evidence that thesummary image wasdis-
torted somewhat to the right side of the photograph. It was thus
inevitable to introduce some simplifications, but the developed
procedure was still robust enough to yield useful results.
V. D
As we have shown, the JUKE method is useful for single
image georectification. One sensitive parameter of the model is
the identification of the ground coordinates of the center point
of the images. Another is the determination of the coordinates
of GCPs. By means of an optimization routine, the respective
center can be slightly optimized.
Table I demonstrates that the performance of the model is dif-
ferent depending on the image. Since the center point is opti-
mized for each image and the optical axis is calculated every
time, the range of the performance is not due to variations of
the center point. Rather, it is caused by the difficult identifica-
tion of the GCPs.
Hence, accuracy is mainly a measure of the quality of the
GCPs. In the investigated area, ground control is somewhat dif-
ficult to define, as it is situated in a rather remote region [20],
[21]. At lower altitudes, there are several buildings that can be
used but at higher altitudes, reliable GCPs are rare. There are
only a few elements, such as huts and path intersections, that
can be identified on the photographs. Moreover, image scale be-
comes smaller toward higher altitudes and thus small errors in
determining the image coordinates of the GCPs result in more
serious positioning errors. It waspossible to measure the ground
coordinates of a few GCPs by means of a differential GPS, thus
providing high quality GCPs. Others were defined by means of
an available orthophoto of the area. The difficulty of defining
reliable GCPs could be facilitated considerably by placing large
signals at the respective position in the terrain in advance [7].
The ground coordinates could then be measured with high ac-
curacy. The GCPs would be clearly identifiable in all digital
photos, and their image coordinates could be ascertained with
highest possible confidence.With such preparations, the perfor-
mance of the JUKE method would improve notably.
The accuracy of the summary image is additionally strongly
influenced by the co-registration procedure. As some posi-
tioning errors are already introduced during this process, the
accuracy of the resulting georectified image is somewhat lower
than the mean accuracy of several images which are georecti-
fied separately. Employing precise, predefined GCPs also for
the co-registration procedure would improve the accuracy of
the summary image as well.
Another critical point is the rather small number of GCPs.
Only 15 GCPs are available, which have to be split into training
and validation sets to be able to obtain consistent estimators
for the performance of the model. Generally, the more training
points available the higher the possibility to fit the model per-
fectly. Fifteen reference points are a minimum requirement but
nevertheless the results are promising.
Because of the accuracy of our model, we did not consider
any calculations for correcting aberrations (for example barrel
or pincushion distortion) which are caused by the optical lens
system. This might be due to the fact that only the inner part
of the images was analyzed. As an advantage, the study area
is situated in the middle of the images where these nonlinear
aberrations are negligible.
However, considering the final resolution of 5 m, the mean
deviation in the middle of the images of about 3 m is within
one pixel and thus is satisfying. This is in particular true for the
fieldof application of this study since snowcoverboundaries are
desired to an accuracy of a few meters. Applying monoplotting
procedures, Aschenbrenner [10] achieved a positional accuracy
of 5 to 10 m, Kirnbauer et al. [11] estimated inaccuracies in the
order of 5 m.
For each application concerning time-series analysis, one
needs to weigh up if the georectification procedure has to be
carried out separately for each image thus being time-con-
suming but providing higher accuracy or if a somewhat less
accurate pre-analyzed image is sufficient as input in the georec-
tification procedure and provides a considerable saving of time.
Up to now, the model performance is computed in units of
pixels. This has not been an imperative problem but a compu-
tational effort which, after we have shown the practicability of
our model, will be solved in a future project.
The spatial resolution of the final product mainly depends on
three parameters: a) the scale and resolution of the original pho-
tograph, b) the scanning resolution, and c) the pixel size of the
DEM. In high oblique photographs, scale variation is severe and
needs to be considered. It is not only a function of relief to-
pography (ground elevation) as it is for true vertical aerial pho-
tographs,butit is alsoaffectedby object distance aswellasposi-
tion and angular orientation of the camera [12]. Hence, scale is
different in all directions. Scale is largest at the bottom of the
images, becoming increasingly smaller toward the top of the
image. This phenomenon is closely related to pixel resolution
of the scanned images. Due to scale variation each pixel covers
a different ground area. Pixels are represented at about the fol-
lowing resolutions: bottom 0.5 m, center 1 m, upper part 2.5 m.
Thechosen image resolution of1536
1024pixelsis acompro-
mise between high detail recognition and storage space. How-
ever, detail recognition is still sufficient for the purpose of this
study. The DEM is represented with a pixelsize of 5 m, i.e., with
anotablycoarser spatial resolution thanthe scanned images,and
consequently, this is the determining factor for the final resolu-
tion. Depending on the respective image scale, every second to
fifth image pixel information only is taken when combining the
projected DEM with the image information. At the top of the
image, where scale is the smallest, the projected points of the
DEM are distributed much closer than throughout the bottom
part. Perspective views influence the spreading of the projected
DEM points. A better final resolution can thus be reached by
improving the spatial resolution of the DEM, and adjusting it to
the image resolution determined by the other two factors men-
tioned above.However,as a higher input resolution would result
in a considerably larger data file and consequently would lead
to a notably increased calculation time, this possibility must be
considered carefully.
Working with high oblique images implies dealing with non-
visible areas. For the JUKE method, these zones do not in-
duce any problems as long as the corresponding pixel corners
are excluded from the data file before calculation. However, as
these areas are lost for analysis it is advisable to choose the
study area and the camera location in a way which avoids large
hidden zones. Hence, study areas with highly variable exposi-
tion should not be favored. In this study only about 3% of the
investigated area was not visible. Although no snow cover in-
formation is available for these hidden zones, it is possible to
predict reliable snow distribution values also for these pixels by
means of a multiple regression analysis [22].
To apply the presented method, no experience in photogram-
metry is required. Beside having available the JUKE method
(software), it is necessary to have access to a raster-GIS in order
to combine the model-output file with the digital photograph
and for visualization. All data transfer is done by the convenient
ASCII format. Data preparation can thus be performed by sev-
eral, commonly available programs. Hence, the method is fea-
sible for anybody with general computing knowledge and some
basic training in GIS and digital image processing.
The developed JUKE method proved successful for single-
stage as well as for time series analysis. Although it is not pos-
sible to reach photogrammetric precision, the georectified data
can be used in a GIS-environment for investigations at scales of
about 1:5000 to 1:10 000. Single-stage images were georecti-
fiedwithhighlysatisfactory accuracy. Including an optimization
procedurefor definingthe imagecenter yielded evena slight im-
provement. For time series analysis, one has to accept a some-
whatloweraccuracy,as additional positioning errors arealready
introduced by the image co-registration procedure. The higher
the quality and the precision of the input data, i.e., the DEM
and the GCPs, the higher the accuracy of the final product. As
high quality DEMs and precisely measured GCPs become more
readily available, these limitations are likely to be made up in
the future.
Particularly in high mountainous terrain, where it can be dif-
ficult and expensive to acquire field data, aerial photographs or
satellite images, this method can be of considerable interest and
benefit to applied field studies in order to gain spatio-temporal
data. The relatively economic data capturing and transforming
procedure enables a successful application of the method within
various disciplines.
The authors would like to thank the input of the anonymous
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JanetteAschenwald received the M.Sc. degree inphysics and the Ph.D. degree
in economics from theUniversity of Innsbruck, Innsbruck, Austria, in 1993 and
2000, respectively.
She is currently an Assistant Professor with the Department of Statistics, So-
cial and Economic Faculty, University of Innsbruck. Her research interests are
concentrated on statistical procedures and the fields of application of artificial
neuronal networks.
Karin Leichter received the M.Sc. degree in geography from the University of
Innsbruck, Innsbruck, Austria, in 1996, and the M.Sc. in environmental remote
sensing from the University of Aberdeen, Aberdeen, U.K., in 1997.
She is a Researcher with the European Academy Bolzano, Bolzano, Italy,
where she is responsible for GIS work. Her research interests are focused on
GIS and remote sensing applications in mountain areas in relation to ecological
and environmental aspects.
Erich Tasser received the M.Sc. and Ph.D. in terrestrial ecology from the Uni-
versity of Innsbruck, Innsbruck, Austria, in 1994 and 2000, respectively.
He is currently a Researcher with the European Academy Bolzano, Bolzano,
Italy. His main research interests are in the field of mountain agriculture, sus-
tainable development in mountain areas, and landscape planning. He focuses
methodically on GIS and statistical procedures.
Ulrike Tappeiner received the Ph.D. degree in biology from the University of
Innsbruck, Innsbruck, Austria, in 1985.
She is qualified as a University Lecturer (habilitation) in the field of ecology
with the University of Innsbruck and is the Head of the research area “Alpine
Environment” with the European Academy Bolzano, Bolzano, Italy. She has a
great deal of experience in ecological research of mountain environments at a
European scale. Her main interests are inthe field of applied research with focus
on ecological effects of land-use changes in mountain ecosystems, ecology of
ski runs, and environmental impact assessment and environmental accounting.
... Recognizing the great value of monoplotting, handy software and codes have been created for the geoscience community, including the OP-XFORM project (Aschenward, Leichter, Tasser, & Tappeiner, 2001), the JUKE method (Corripio, 2004), Georeferencing oblique terrestrial photography (Mitishita, Machado, Habib, & Gonçalves, 2004), the 3D Monoplotter (Fluehler, Niederoest, & Akca, 2005), and the DiMoTeP (Conedera, 2018). Recently, the WSL Monoplotting Tool (WSL-MPT) developed by the Swiss Federal Research Institute (WSL) is gaining popularity and has been applied to the quantitative analysis of natural hazards (Scapozza, Lambiel, Bozzini, Mari, & Conedera, 2014;Triglav-Čekada, Radovan, Gabrovec, & Kosmatin-Fras, 2011), glacial processes (Stockdale, Bozzini, Macdonald, & Higgs, 2015), and land cover changes (Gabellieri & Watkins, 2019;McCaffrey & Hopkinson, 2017;Stockdale, Bozzini, Macdonald, & Higgs, 2015). ...
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Urban flooding is becoming a common and devastating hazard, which causes life loss and economic damage. Monitoring and understanding urban flooding in a highly localized scale is a challenging task due to the complicated urban landscape, intricate hydraulic process, and the lack of high-quality and resolution data. The emerging smart city technology such as monitoring cameras provides an unprecedented opportunity to address the data issue. However, estimating water ponding extents on land surfaces based on monitoring footage is unreliable using the traditional segmentation technique because the boundary of the water ponding, under the influence of varying weather, background, and illumination, is usually too fuzzy to identify, and the oblique angle and image distortion in the video monitoring data prevents geor-eferencing and object-based measurements. This paper presents a novel semi-supervised segmentation scheme for surface water extent recognition from the footage of an oblique monitoring camera. The semi-supervised segmentation algorithm was found suitable to determine the water boundary and the monoplotting method was successfully applied to georeference the pixels of the monitoring video for the virtual quantification of the local drainage process. The correlation and mechanism-based analysis demonstrate the value of the proposed method in advancing the understanding of local drainage hydraulics. The workflow and created methods in this study have a great potential to study other street-level and earth surface processes.
... This characteristic type of snow distribution creates difficulties in monitoring and change detection [66,69]. As small snow patches cannot be mapped with MODIS data, some studies have used Landsat data with a higher spatial but lower temporal resolution [70] or terrestrial cameras for continuous monitoring [22,71,72]. ...
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This article presents the distribution of seasonal snow cover in the Trans-Himalayan region of Ladakh over the observation period of 2000-2019. Seasonal snow cover area and duration have been monitored and mapped based on the MODIS Normalised Difference Snow Index (NDSI). Using different MODIS cloud removal algorithms, monthly mean cloud-covered areas have been reduced to 3%. Pixel-wise approaches using Mann-Kendall (MK) and Sen's slope trend tests allow to assess seasonal and annual trends of snow cover days (SCD) and snow cover area (SCA) across seven delineated subregions of Ladakh. Analyses include the impact of topographical parameters (elevation, slope, aspect). Overall, the mean annual SCA amounts to 42%, varying from 15% in August to 71% in February. However, large differences of SCA have been detected between and within subregions. The trend analysis of SCA shows a non-significant, slight increase for summer as well as for the entire year and a decrease for spring and winter seasons. The SCD trend analysis indicates more pixels with a significant increase than a decrease. In total, 12% of all pixels show an increasing trend in summer, 6% over the entire year, 3% in autumn, and 2% in spring and winter, whereas less than 2% of all pixels show a decreasing trend in all seasons. The results are important for regional irrigated agricultural production and freshwater supply in the context of climate change.
... Since the pioneering work in the 1970s and 1980s [6], [21], efforts have been made to develop software and tools for monoplotting oblique pictures. These include the OP-XFORM project [22], the JUKE method [23], Georeferencing oblique terrestrial photography [24], the 3D Monoplotter [25], and the DiMoTeP [26]. Probably the most applied tool is the WSL Monoplotting Tool (WSL-MPT) developed by the Swiss Federal Research Institute (WSL) to allow the georeferencing and vectorization of topographic photographs. ...
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In the last decades, the development of smartphones, drones, aerial patrols, and digital cameras enabled high-quality photographs available to large populations and, thus, provides an opportunity to collect massive data of the nature and society with global coverage. However, the data collected with new photography tools is usually oblique - they are difficult to be georeferenced, and huge amounts of data is often obsolete. Georeferencing oblique imagery data may be solved by a technique called monoplotting, which only requires a single image and Digital Elevation Model (DEM). In traditional monoplotting, a human user has to manually choose a series of ground control point (GCP) pairs in the image and DEM and then determine the extrinsic and intrinsic parameters of the camera to establish a pixel-level correspondence between photos and the DEM to enable the mapping and georeferencing of objects in photos. This traditional method is difficult to scale due to several challenges including the labor-intensive inputs, the need of rich experience to identify well-defined GCPs, and limitations in camera pose estimation. Therefore, existing monoplotting methods are rarely used in analyzing large-scale databases or near-real-time warning systems. In this paper, we propose and demonstrate a novel semi-automatic monoplotting framework that provides pixel-level correspondence between photos and DEMs requiring minimal human interventions. A pipeline of analyses was developed including key point detection in images and DEM rasters, retrieving georeferenced 3D DEM GCPs, regularized gradient-based optimization, pose estimation, ray tracing, and the correspondence identification between image pixels and real world coordinates. Two numerical experiments show that the framework is superior in georeferencing visual data in 3-D coordinates, paving a way toward fully automatic monoplotting methodology.
... Oblique terrestrial images have been used to analyze mountainous terrain [33], to estimate snow albedo [34], monitor snow cover, and make other measurements such as snow depth [35][36][37][38]. The use of this tool is suggested for snow cover because of its high reflectance values [39]. ...
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Snow cover is an important variable in both climatological and hydrological studies because of its relationship to environmental energy and mass flux. However, variability in snow cover can confound satellite-based efforts to monitor vegetation phenology. This research explores the utility of the PhenoCam Network cameras to estimate Fractional Snow Cover (FSC) in grassland. The goal is to operationalize FSC estimates from PhenoCams to inform and improve the satellite-based determination of phenological metrics. The study site is the Oakville Prairie Biological Field Station, located near Grand Forks, North Dakota. We developed a semi-automated process to estimate FSC from PhenoCam images through Python coding. Compared with previous research employing RGB images only, our use of the monochrome RGB + NIR (near-infrared) reduced pixel misclassification and increased accuracy. The results had an average RMSE of less than 8% FSC compared to visual estimates. Our pixel-based accuracy assessment showed that the overall accuracy of the images selected for validation was 92%. This is a promising outcome, although not every PhenoCam Network system has NIR capability.
... Following the work of Makarovic, several attempts have been made to develop software and tools for monoplotting oblique photographs. These include the OP-XFORM project (Doytsher and Hall, 1995), the JUKE method (Aschenwald, Leichter, Tasser & Tappeiner, 2001), Georeferencing oblique terrestrial photography (Corripio, 2004) Gonçalves, 2004), and the DiMoTeP (Fluehler, Niederoest & Akca, 2005) (Bozzini et al., 2012). However, the widespread use of these products has remained limited due to the subject-specific nature, the lack of operational flexibility and userfriendliness (Conedera et al., 2018). ...
... Thus, grid cell size is an important consideration in designing a study of this type. The best opportunity to resolve the inaccuracies and shortcomings of this technique lies in the integration of this method and those that convert oblique photography to a planar view by georeferencing photographs to a digital elevation model (Aschenwald et al., 2001;Davis et al., 2002;Honda and Nagai, 2002;Corripio, 2004). Although it requires establishment of ground control points in the field, this approach would give spatial attributes to the photo-pairs and allow for the calculation of absolute change in the landscape. ...
Repeat photography is a powerful tool for detection of landscape change over decadal timescales. Here a novel method is presented that applies spatial analysis software to digital photo-pairs, allowing vegetation change to be categorized and quantified. This method is applied to 12 sites within the alpine treeline ecotone of Glacier National Park, Montana, and is used to examine vegetation changes over timescales ranging from 71 to 93 years. Tree cover at the treeline ecotone increased in 10 out of the 12 photo-pairs (mean increase of 60%). Establishment occurred at all sites, infilling occurred at 11 sites. To demonstrate the utility of this method, patterns of tree establishment at treeline are described and the possible causes of changes within the treeline ecotone are discussed. Local factors undoubtedly affect the magnitude and type of the observed changes, however the ubiquity of the increase in tree cover implies a common forcing mechanism. Mean minimum summer temperatures have increased by 1.5°C over the past century and, coupled with variations in the amount of early spring snow water equivalent, likely account for much of the increase in tree cover at the treeline ecotone. Lastly, shortcomings of this method are presented along with possible solutions and areas for future research.
... After the emergence of low-cost computers and cameras, low-cost close range digital photogrammetry has become widely used to obtain high-resolution representations of the Earth's surface, where the elevation of the landforms is targeted (Barker et al., 1997;Aschenwald et al., 2001;Heimsath and Farid, 2002;Remondino and El-Hakim, 2006;Matthews, 2008;Fraser and Cronk, 2009;Eltner et al., 2016) in areas where dense vegetation is not present. ...
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Gully formation and evolution represent important aspects not only of landform evolution, but also of practical interest regarding hydrology and agriculture. The classic methodology of assessing the intensity of these erosion processes, and the volumes of sediments involved, is to use field measurements or classical/digital photogrammetry. These methods were recently completed by the use of high-resolution digital elevation models (DEMs) derived from multitemporal LiDAR data and UAV images. In the Moldavian Plateau (northeastern Romania), gullies are common landforms due to geologic, topographic, climatic, and anthropic factors. Their episodic development and the relationship with high rainfall and/or snowmelt events constitute a key point in the deciphering of the gully evolution. For this work we have chosen the case of four gullies developed in the lacustrine deposits of abandoned anthropic reservoirs which presented an obvious dynamic in the last two decades on remote sensing images. A DJI Phantom 4 Pro UAV was flown over the study case areas and acquired images with 80% side and forward overlap at 20 MP resolution. The UAV point cloud was obtained using the structure from motion (SfM) technique in VisualSFM open source software from overlapping images and was georeferenced with ground control points. Georeferenced LiDAR point clouds acquired in winter 2012 were used as a reference dataset. The filtering of the point clouds for obtaining bare ground points was performed with the multiscale curvature classification algorithm. The point cloud ground data for both the sources and periods were used to interpolate a 0.25-m resolution bare earth DEM for every gully. This LiDAR reference DEM was used together with the UAV SfM DEM for deriving the DEM of differences (DoDs) using the geomorphic change detection (GCD) technique of Wheaton et al. (2010) implemented in SAGA GIS and R stat. GCD was applied with both uniform and spatially variable thresholding, the threshold errors being derived from GCPs and from co-registration of DEMs. Geomorphological mapping was performed for establishing the spatially variable thresholds and for assessing the sediment budget. The results highlighted the areas that were affected by erosion and deposition and allowed us to evaluate the process rate for each studied gully, each gully element, and to derive a raw sediment budget, showing that LiDAR, UAV SfM, and DoD are useful methods in geomorphological mapping and rate of process studies.
... As a result, the pioneering work of Makarovič [25,28] has long remained isolated. Only in the last 20 years have new software and tools been developed based on the monoplotting principle [29][30][31][32]. None of these products, however, really meet the needs of potential end users in terms of operational flexibility and user-friendliness, thus, greatly inhibiting their broad use. ...
Full-text available
Urban flooding is becoming a common and devastating hazard to cause life loss and economic damage. Monitoring and understanding urban flooding in the local scale is a challenging task due to the complicated urban landscape, intricate hydraulic process, and the lack of high-quality and resolution data. The emerging smart city technology such as monitoring cameras provides an unprecedented opportunity to address the data issue. However, estimating the water accumulation on the land surface based on the monitoring footage is unreliable using the traditional segmentation technique because the boundary of the water accumulation, under the influence of varying weather, background, and illumination, is usually too fuzzy to identify, and the oblique angle and image distortion in the video monitoring data prevents georeferencing and object-based measurements. This paper presents a novel semi-supervised segmentation scheme for surface water extent recognition from the footage of an oblique monitoring camera. The semi-supervised segmentation algorithm was found suitable to determine the water boundary and the monoplotting method was successfully applied to georeference the pixels of the monitoring video for the virtual quantification of the local drainage process. The correlation and mechanism-based analysis demonstrates the value of the proposed method in advancing the understanding of local drainage hydraulics. The workflow and created methods in this study has a great potential to study other street-level and earth surface processes.
Full-text available
Auch in Südtirol ist die Landwirtschaft durch eine zunehmende Polarisierung der Landnutzung gekennzeichnet: Intensivierung in den Gunstlagen im Tal und Extensivierung bzw. Aufgabe der unrentablen Randzonen und Almflächen. Die ökologischen Dimensionen dieser Landnutzungsänderungen sind wenig erforscht. Mit den Forschungsarbeiten auf den Waltner Mähdern im Passeiertal wurden einige Wissenslücken geschlossen. Das vorliegende Buch stellt die Ergebnisse dieser Arbeiten vor und versucht die vielfältigen Zusammenhänge von landwirtschaftlicher Nutzung und Naturhaushalt aufzuzeigen. Aufbauend auf den Ergebnissen kommt es durch die Autoren zu einer Bewertung der ökologischen Folgen der untersuchten Bewirtschaftungsformen.
This paper emphases the need for the consideration of terrain information through the integration of a digital elevation model (DEM) representing the Earth's surface when geocoding image data of high-relief terrain. This is shown in a practical application, where a multi-sensor data set of a high-mountain tests area in the Austrian Alps has been used consisting of optical data from SPOT and Landsat TM as well as a microwave SAR image acquired by the JPL multipolarisation and multifrequency SAR sensor carried by a DC-8 aircraft. The geometric performance and the mapping accuracy of the individual images are discussed using statistical and graphical means. Further, the basic geocoding results are presented. -from Authors
Though precise, stereoscopic mapping instruments are expensive and beyond the practical application of most natural resource specialists involved with mapping. Consequently, we developed a simple, inexpensive monoscopic measurement and mapping system for use by those with limited training in photogrammetry. The software is designed for a standard digitizing tablet, and is capable of making measurements from vertical and oblique images, including both large-format (23×23cm) and 35mm aerial photographs. The following describes a study in which we used the system with different camera formats, camera orientations and film types for mapping croplands during a 39yr period. Point location accuracy from 1:6000 to 50 000 photo scales was ~2m on the ground. -Authors
This study applies Markovian transition probability matrices to the problem of characterizing classified multitemporal satellite snow-cover data. Transition probability matrices are used to form hypotheses regarding the effects of snow persistence and ablation patterns on the alpine treeline using an integrated geographic information system. Stratification of the rugged landscape by elevation and slope aspect is achieved through the processing of 1:24 000 base-scale Digital Elevation Models (DEMs) and integrated with the satellite characterizations of snow conditions. Analysis of transition matrices by topographic position and watersheds highlighted areas of significantly late snowmelt, which holds implications for ecological investigations of alpine treeline by considering snow both as a stressor and protector of vegetation, depending upon its spatial pattern and temporal persistence. -from Authors
A general snow accumulation and melt model was developed to (1) determine how accurately snow accumulation and ablation can be modeled over heterogeneous landscapes with routinely available climatologic, topographic, and vegetation data, and (2) improve estimates of annual forest snow hydrology for point and regional calculations of annual forest productivity. The snow model was designed to operate within the Regional Hydroecological Simulation System (RHESSys), a GIS based modeling system to manage spatial data for distributed computer simulations on watershed scales. One feature of the RHESSys Snow Model (RSM) is it can use satellite derived forest leaf area index (LAI) to represent catchment forest cover; difficult to obtain in adequate cover and resolution by any other means. The model was tested over 3 water years (October to September) with data recorded by 10 snow telemetry stations (SNOTEL) in 5 states ranging in meso-climate and elevations from a coastal Oregon site (1067 m) to a continental Colorado site (3261 m).Predictions for the 10 sites were made with identical parameter values and only site climate varied for all sites. The average difference between observed and predicted snow depletion dates for all sites and water years was 6.2 days and 8 of the 30 simulations were within ± 2 days (R² = 0.91). Radiation melt was the dominate snow ablation component at the Colorado site where sublimation was 10% (LAI = 0) to 20% (LAI = 6) of snow loss while air temperature was the dominate component at the Oregon site with sublimation reduced to 1% (LAI = 0) to 6% (LAI = 6) of snow loss. LAI had a greater effect determining snow depletion than site aspect. Aspect increased in importance if the snow depletion occurred during early spring when solar insolation differences between hillslopes is greater than in the late spring.An accurate prediction of daily snowpack water equivalent (SWE) was not a strong determinant for making an accurate prediction of snowpack depletion date. Predicted snowpack depletion dates were more sensitive to timing when the snowpack reached an isothermal condition. Daily estimates of SWE were most sensitive to correctly estimating snowfall from SNOTEL data. This means that for purposes of determining the snow depletion dates which are useful for forest ecosystem modeling, tracking SWE is less important then triggering snowmelt. Comparisons of simulations to published snow depletion dates show that RSM predicted the relative ranking and magnitude of depletion for different combinations of forest cover, elevation, and aspect.
Snow cover patterns in a 9.4 km2 basin in the Austrian Alps were examined during the 1989 ablation period. Nine aerial surveys were conducted at intervals of about two weeks. The oblique aerial photographs were printed and snow boundary lines were identified. The metric restitution of the images was performed by digital monoplotting, making use of a digital terrain model with 25 m grid spacing. The depletion process is documented and snow cover is analyzed as a function of elevation, slope and aspect. The snow cover is found to be better related to elevation and slope during winter conditions than during the late ablation period. Differences in snow cover associated with aspect are more pronounced later in the year.