Many Earth Imaging Journal readers consider themselves to be
photogrammetrists, though they may be in the minority, outnumbered by
remote sensing specialists, GIS professionals and other geospatial
scientists. Yet most geospatial professionals can benefit by expanding
their familiarity with photogrammetry. Toward that end, let’s review a
few of the basic concepts, relating them to current practice, taking
stock of recent trends and considering how photogrammetry is changing as
the demands on it evolve.
Back to Basics
We can start with the definition given by the American Society for
Photogrammetry and Remote Sensing (ASPRS): “Photogrammetry is the art,
science, and technology of obtaining reliable information about physical
objects and the environment, through processes of recording, measuring,
and interpreting images and patterns of electromagnetic radiant energy
and other phenomena.” Interestingly, ASPRS uses the tag line “The
Imaging and Geospatial Information Society,” emphasizing
photogrammetry’s role within the wider world of geospatial information.
Furthermore, the definition highlights the role of remotely sensed
imagery—any thoughts that photogrammetry applies only to standard aerial
photography with classical aerial film cameras have been consigned to
history.
An image, as it is received from a sensor, can’t be used as a map
because the geometries of the two products aren’t the same, and the
image doesn’t show information critical to the map user through
characters or symbols. Aerial photographs can be used to illustrate some
simple geometric
concepts that are central to photogrammetry.
The scale of an aerial photograph is given by
f/(H-h), where f is the principal distance of the camera (the same
as the focal length in most practical cases), H is the flying height
of the aircraft above datum, and h is the height of the ground above
datum (Figure 1). All of the lines from the terrain to the image
pass through the lens; this is a perspective projection, as opposed
to the orthographic projection of a map, where we can think of each
point on Earth’s surface being projected in parallel on to the map,
then being reduced in scale.
An aerial photograph exhibits the well-known characteristic of
“building lean” (Figure 2)—i.e., the top of the building is imaged
in a different place from the bottom, and the extent of the
displacement increases radially from the center of the image.
Moreover, the scale varies according to the distance from the
sensor. Thus, changes in the flying height cause variations in
scale, and hilltops are imaged at a larger scale than valley
bottoms. In addition, when the aircraft tilts so the camera isn’t
pointing vertically down, the geometry of the image is that of a
tilted photo. This is demonstrated heuristically in Figure 3, where
the camera was tilted deliberately to take an oblique photo; the
streets of the city form a grid, but the grid converges in the image
and the scale decreases toward the horizon. This effect exists in
every image and must be taken into account during the
photogrammetric restitution of the imagery into geographic
information.
We can use the effect of relief displacement to extract height
information. Figure 4 illustrates a pair of overlapping photographs.
We can see that the distance oa-o’a’—i.e., the change of position in
point A relative to the center of the image as the aircraft flies
along, taking the first photo then the second—isn’t the same as the
distance ob-o’b’. In other words, this distance varies with the
height of the ground.
The change of position of a point from one
image to the next is called parallax, and we can derive the parallax
formula shown in Figure 4, which relates differences in parallax
between points to differences between their heights on the ground.
This is a simple mathematical way of expressing the everyday
phenomenon of stereoscopic vision, whereby our two eyes see an
object in different ways—the brain uses the parallactic angle, for
example L1AL2 in Figure 4, as well as other evidence, and forms a
3-D image. Similarly, if we view two overlapping images, looking at
one with each eye, our brain will again form a 3-D, stereoscopic
image.
Furthermore, we can introduce into this view a “measuring mark” or
“floating mark.” If we put a dot, or differently colored pixels,
into each image, then when the dots are exactly on corresponding
points in the two images the floating mark will appear to rest
perfectly on the ground. If we vary the x-separation between the
dots, the floating mark will appear to rise or fall relative to the
ground. Thus, we have a convenient method of photogrammetric
measurement.
Photogrammetric Measurement, Workstations and Sensor Models
Now that we’ve condensed chapters of photogrammetric education into
a few paragraphs, let’s consider how these principles are applied.
We can build an instrument for photogrammetric measurement, called a
workstation, in which images can be viewed and measured for creating
various types of geographic information. Until the 1980s, most
workstations were called “analog instruments,” in which complex
optical and mechanical components were precisely manufactured and
used to re-create in miniature the situation when the photos were
taken, reproducing the camera’s geometry and the aircraft’s
movement. These instruments were superseded by analytical plotters,
where the relationships between image and ground were modeled in a
computer interfaced to the viewing system and the XYZ control
movements of the human operator.
Today the industry’s workhorse is the digital photogrammetric
workstation. As shown in the opening image above, such workstations typically consist of a high‑end PC with
some form of stereoscopic viewing. Sometimes there are two displays:
one stereoscopic and one monoscopic. Stereoscopic viewing methods
were covered in “New Visualization Technologies Go Beyond the
Screen,”
Earth Imaging Journal, November/December 2005. The measuring mark
can be controlled by the mouse and keyboard, but often the
workstation is equipped with a large 3-D mouse to control X, Y and Z
movements comfortably.
Routine photogrammetric production is still based on film
photographs scanned in a high-performance, photogrammetric
equivalent of the familiar desktop scanner. But digital
photogrammetric workstations can read imagery from many different
sensors—terrestrial, airborne, satellite—as well as many other kinds
of data, such as LiDAR, IfSAR, and existing digital maps and terrain
models.
The first task after reading imagery into the workstation is
orientation, triangulation, registration or georeferencing. There is
no space here to describe these processes in detail. Suffice it to
say that the workstation must include a sensor model comprising
image-to-ground and ground-to-image equations for each image—i.e., a
mathematical model, which may be generic or may attempt to model the
physical characteristics of the sensor and the image acquisition
process. Then the position and orientation of the sensor must be
established for every image in the project.
Today all satellite and most aircraft missions are flown with GPS
and IMU equipment, which provide direct georeferencing—i.e., the
workstation reads the estimated trajectory generated by the GPS/IMU
post-processing software or provided in the satellite ephemeris
(image metadata), and thus the orientations are established. In some
cases, GPS/IMU data may be unavailable or may not meet accuracy
requirements—especially in the case of large-scale work. In these
cases, a process called triangulation is performed on the
workstation; image points, called tie points, are measured in every
image in which they appear. Points on the ground whose coordinates
are known—i.e., ground control points, are also measured in the
imagery. These points are used to fit the images together—rather
like a vast jigsaw puzzle in the sky—and relate them to the ground
coordinate system.
Triangulation results in estimates of the sensor’s position and
orientation when each image was captured. In the case of a line
sensor, as deployed in most of the commercial Earth observation
satellites, every line has its own position and orientation. After
triangulation, measurements on the imagery can be transformed into
coordinates on the ground, and the images can be viewed comfortably
in stereo. Additional photogrammetric operations can proceed.
Photogrammetric Workflows
Photogrammetry can generate deliverables to suit a wide range of end
users. For example, consider the workflows that create the
deliverables shown in Figure 5. Today’s workstations automate many
photogrammetric processes. The skill and profit lie in linking these
processes together into a productive workflow, permeated with
quality control procedures. Successful photogrammetric enterprises
and departments achieve this linking smoothly and imaginatively.
Indeed, there has been significant growth in the availability of
software to expedite workflow management.
The traditional product from photogrammetry—the major source of
revenue for service companies—has been the large-scale line map, for
which buildings, roads, fields, and other small details are
accurately traced by a human operator, using software designed to
expedite, but not automate, the process (Figure 6). Construction
companies and local governments are among the end users.
Terrain models for computing earthworks are another large-scale
application—for example, for mining or transportation. Today terrain
models can be generated automatically by photogrammetry or from
LiDAR data, followed by software-assisted human editing (Figure 7).
In recent years the trend has been away from the traditional line
map toward image-based deliverables. The centerpiece here is the
orthophoto, which looks like a normal image but has been subtly
modified so its geometry is the same as a map; the inputs to
generate orthorectified imagery are the imagery, orientation data
from triangulation and a digital terrain model, which can be
generated specially or accessed from existing libraries. Individual
images have to be mosaicked for this orthorectified imagery to cover
the area of interest.
The final stages in the process include
radiometric adjustment so the mosaicked image is consistent and
visually pleasing across its entirety, as well as the addition of
title, grid, names, etc. Linear features such as buildngs and roads
may be overlaid on the image base. The orthorectified imagery may be
a product in its own right or may often be destined to be a layer
within a GIS. Though orthophotos have the geometry of a map—i.e.,
consistent, known scale and projection and no displacements due to
the tilt of the aircraft—the “building lean” effect is still there.
This can be improved by using only those portions of individual
images near the nadir, but a more sophisticated solution is the
“true ortho” in which the building lean effects are removed. In this
case each individual building must be measured photogrammetrically,
resulting in a slower, more expensive product (Figure 8). This
measurement of buildings is also required for an increasingly
popular photogrammetric deliverable: visualization (Figure 9).
For planning, defense, computer games and other purposes, there is
growing demand for fly-throughs, with ever more complex
functionality to fly around a scene at the user’s whim, zoom in and
out, etc. The data for this purpose can be generated
photogrammetrically, including the manual measurement of buildings.
Though the buildings’ walls can be generated mathematically to
appear in the visualization, there can be a lack of detail in a
vertical or near-vertical image. Sometimes visualization is assisted
by enhancing the walls wth either texture from a library or detail
from close-range ground photography.
Ongoing Changes
Photogrammetry, therefore, is built on principles dating back more than
100 years, based on the geometry of overlapping images. The
well-established methods have been richly laced with new technology.
Though the aerial film cameras in use outnumber the new generation of
airborne digital sensors by perhaps 10 to one, the latter are selling
fast and number even more if we include simpler, less-expensive sensors
of perhaps 16 megapixels. A study published by Forecast International—a
market research, intelligence and consulting organization for the
aerospace, defense and power systems industry—in May 2006 suggested that
140 Earth imaging satellites worth $16.3 billion are scheduled to be
launched during the next 10 years, with as many as 19 per annum until
2009. Two that are well known to photogrammetrists are the
soon-to-be-launched GeoEye-1 and DigitalGlobe WorldView. Both of these
commercial satellites are designed to acquire imagery at around 40 cm
resolution, so the continuum from airborne to satellite imagery grows
tighter. Today’s digital photogrammetric workstations are networked and
work in parallel, running software that grows increasingly sophisticated
and efficient. Server-oriented architecture offers new approaches to
both software and data.
Many workflows are almost entirely automated,
though it is important to remember those that are not. Triangulation is
automated, but some human intervention may be necessary if the system
struggles to find enough tie points that can be matched in multiple
images. Digital terrain models are generated automatically too, but
considerable human editing may be needed with imagery of certain types
of terrain, where image matching (or correlation) is prone to failure.
Indeed, LiDAR and IfSAR alternatives, which are also improving in
economy, availability and accuracy, need human editing.
Orthorectification and mosaicking are fully automated, though the latter
may need a little human attention to seamlines if the automatically
generated ones choose unwise directions on the imagery. Radiometric
dodging and balancing are addressed by the most ingenious algorithms,
yet sometimes human judgment is the best way to determine whether the
result is aesthetically acceptable. Perhaps feature collection is the
holy grail. To be sure, progress has been made with automatic line
following and automatic building extraction from imagery and LiDAR, but
a totally automated map or GIS layer remains elusive. Similarly, human
measurement remains the best way to collect buildings for visualization.
On
the business side, there’s no question that users of photogrammetric
equipment are paying a fraction of the cost—in real terms—of what they
paid a generation ago for similar performance. Moreover, the range of
capabilities of digital workstations and the content of digital imagery
compared with film simply weren’t available then. Satellite imagery from
continuously orbiting platforms is a popular alternative, at least at
certain resolutions, to the specially commissioned photo flight.
Indeed, the traditional business model of a service company generating
revenue from flying imagery and producing deliverables under a specific
contract won in competition is changing too. Though we don’t yet know
the long-term effect of “Internet mapping,” such as Google Earth or
Microsoft Virtual Earth, we do see, for example, that vendors of oblique
imagery or of buildings used in visualization are committed to “acquire
once, sell many times” business models in which the imagery and the
deliverables no longer become the intellectual property only of the
client awarding the contract. The growth of outsourcing services
offshore changes the business landscape too, sometimes
pressing patriotism and economics into an uneasy dance.
Change can be bewildering, but it’s never boring.
As the film camera moves into the autumn of its life, it’s being
superseded by airborne digital sensors, high-resolution satellite
imagery, LiDAR, radar, hyperspectral scanners, etc., all handled, with
increasing felicity, in highly automated, well-managed workflows within
digital photogrammetric workstations. The skill of the photogrammetrist
involves selecting imagery from which the geometric accuracy and content
specifications of the deliverable can be economically met. Meanwhile
business models undergo transformation. Photogrammetry and the Internet
combine to mutual advantage; the faithful workhorse of the geospatial
information industry has become the trendsetter.