PE&RS July 2015 - page 546

its physical sensor model to have parameters and metadata
which are particular to the sensor. Third, the metadata re-
quired to feed many of these models is not passed through the
current lidar processing chains. Finally, the tools and meth-
ods required to exploit such data do not exist. So, while the
theory and literature show the benefits of the sensor modeling
concepts, the detailed implementation of such concepts has
not been addressed.
The goal of the Universal Lidar Error Model (
ULEM
), devel-
oped by the National Geospatial-Intelligence Agency (
NGA
)
Sensor Geopositioning Center (
SGC
), is to address many of
these current shortcomings and provide the utility of sensor
modeling to the users of lidar. Through the
ULEM
Specifica-
tion (
NGA
, 2013), the sensor-specific metadata aspects are
mitigated by mapping these metadata to a few standardized
parameters. Likewise, modeling is provided that allows for
the storage and calculation of correlations among these pa-
rameters. This
ULEM
metadata is stored in existing file formats
such as
LAS
(
ASPRS
, 2011) that are used by the community,
and maintains compliance with those format specifications.
Additionally, the exploitation methods are standardized
based on existing sensor modeling efforts of the community.
While the literature has shown the benefits of the sensor
modeling and error propagation,
ULEM
makes those concepts
accessible to the lidar users.
Concept
ULEM
was developed to provide support for rigorous error
propagation and adjustability in the essential lidar point
cloud scenarios while efficiently storing the requisite meta-
data. It employs two implementation modes,
Sensor-Space
ULEM
and
Ground-Space
ULEM
. Sensor-Space
ULEM
offers an
effectual generic physical sensor model, consolidating the
parameters from the full physical model into a few standard-
ized parameters. In certain cases where this storage of sensor
parameters becomes impractical and/or unwieldy,
ULEM
offers
a ground-space implementation. Ground-Space
ULEM
repre-
sents an efficient strategy for the storage and exploitation of
error covariances in point space that maintains the ability to
generate full covariance matrices among multiple points. Fur-
thermore, the Ground-Space
ULEM
formulation is sufficiently
general to apply to point clouds, dense digital surface models
(
DSM
s), or general 3
D
data derived from any source, e.g., from
overlapping passive electro-optical or
SAR
images.
Many applications, such as precise geopositioning from re-
motely-sensed data, need sensor metadata to generate ground-
point uncertainties using error propagation. Also needed are
rigorous methods to fuse and adjust datasets, even among
differing modalities, which require accurate representations
of correlations and cross-correlations among
adjustable pa-
rameters
(values which define how a dataset may be adjusted,
e.g., translations in geodetic X, Y, and Z). In response to these
needs, the US Air Force Aeronautical Systems Center and
NGA
formed the Community Sensor Model Working Group
(
CSMWG
), which maintains a strict set of rules that define an
application programming interface (
API
) to which many sen-
sor model builders design their sensor models (Rodarmel
et
al
., 2011). As a result, sensor exploitation tool builders can
write photogrammetric processing programs in a sensor-ag-
nostic manner.
ULEM
was designed to be compatible with
CSM
guidelines. The
CSMWG
is working towards expanding the
CSM
3.0.1
API
, which is currently used to exploit imagery (raster, or
2
D
datasets), to handle 3
D
product (e.g., point cloud) datasets
by incorporating
ULEM
into its current suite of sensor models.
CSM
also provides rigorous modeling for correlations using
the Strictly Positive Definite Correlation Function (
SPDCF
) as
discussed by Dolloff (2013). Using a common
CSM
interface
ensures that during exploitation the differences in
ULEM
implementation modes, and the source of the point cloud
data, are imperceptible to the user.
Data storage is a key aspect to implementing the concepts
of sensor modeling and error propagation into existing work-
flows and making the metadata available and exploitable by
the mass of users. The data must be stored in data formats
that users are willing to use, the formats must be transparent
so that anyone can parse the data, and the impact on the total
required storage should be minimized.
ULEM
has addressed
these issues by using the
ASPRS
-developed
LAS
format as a
storage mechanism (although
ULEM
could be applied to other
formats). The
ULEM
metadata, for Sensor-Space or Ground-
Space, is stored in a format compliant with the
LAS
specifica-
tion by encoding the added metadata into Variable Length
Records (
VLR
s) that are included in the
LAS
file with the point
data. The data has been stored using methods that minimize
the storage burden. For example, for Sensor-Space
ULEM
, the
size of a typical
LAS
file grows by less than 0.1 percent when
the
ULEM
metadata is added. Finally, the metadata can be eas-
ily parsed from the
VLR
by exploitation tools and models.
ULEM
supports the storage of adjustable parameters as-
sociated with the dataset as well as the full covariance for
adjustable parameters. The covariance storage is implemented
using the
direct
and
indirect
methods. The direct method
captures the entire covariance matrix by storing all the upper-
diagonal entries (since symmetric), including zeros. For large
numbers of adjustable parameters, this method may prove a
bit unwieldy, take up much space, and be wasteful for sparse
matrices. The indirect method stores only the block-diagonal
covariance entries (e.g.,
Σ
11
, …
Σ
nn
in Equation 2) of the full
covariance matrix. Cross-covariance values are calculated us-
ing correlation coefficients obtained from a correlation model
(i.e.,
SPDCF
(Doucette
et al
., 2013)), the parameters for which
(
A
,
α
,
β
,
τ
) are stored in the
ULEM
metadata. For example, the
correlation coefficient
ρ
of a parameter (
r
) over a time range
(
Δ
t
) is computed from
SPDCF
parameters as follows:
(
)
1 1
ρ
α
α
β
β
Δ τ
=
+
− +
(
)
+
A
e
r r
r
r
r
t
r
[
]
/
(5)
In Equation 5, parameter
A
r
controls the maximum cor-
relation that can be obtained,
A
r
α
r
determines the minimum
correlation value that can be obtained,
β
r
primarily controls
the shape of the correlation curve, and
τ
r
controls the rate of
the decay. It is important to note that while this example used
temporal differences between points, spatial differences are
also used in some of the
ULEM
correlation modeling. Similar-
ly,
τ
may relate to time or distance, depending on the imple-
mentation. Additional detail regarding full-covariance storage
is provided in the Implementations Section.
The intent of this paper is to provide a high-level introduc-
tion to the
ULEM
concept; therefore many of the details are
absent. The reader is encouraged to obtain the
ULEM
Imple-
mentation and Exploitation Document (
NGA
, 2013) for further
information.
Implementations
Sensor-Space ULEM
Sensor-Space
ULEM
approximates the physics of the sensor
during the original data collection. It requires the ability to in-
terpolate the sensor position at which any lidar point was col-
lected. This interpolation is enabled by access to timestamps
for every lidar-point record and time-indexed collection tra-
jectory data. Sensor-Space
ULEM
permits sensor-space param-
eter uncertainties (pointing, ranging, etc.) to be propagated
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July 2015
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