PE&RS May 2016 - page 362

as snow and wetlands (uncommon across Australia) on
GLAS
canopy height retrievals are unknown as they were unavail-
able for testing. In terms of specific
GLAS
and
ALS
metrics that
are most compatible for model development, it was found that
in the general case,
GLAS
RH
ROS
was most accurately predicted
from
ALS
p95 from an all returns point cloud (
RMSE
= 8.10 m,
R
2
= 0.69, N = 110). The significance of this result is that plot-
and stand-level forest attributes that are frequently modeled
as a function of
ALS
percentiles, can be directly transferred to
GLAS
waveform metrics, which will facilitate the scaling of
attributes from
ALS
extents to
GLAS
continental-scales.
The suggested “optimal”
GLAS
height dataset identified
in this study may be applicable elsewhere across the globe.
However, it is recommended that studies in other geographic
regions follow a similar testing and model development
framework to identify region-specific
GLAS
/
ALS
canopy height
relationships. As new satelliteborne lidar sensors come
on line in the near future (e.g.,
ICESat
2, Global Ecosystem
Dynamics Investigation, and Lidar Surface Topography), and
as airborne lidar datasets become more widely and publicly
available (e.g.,
)
, such controlled analy-
ses and calibration of canopy height metrics will be necessary
to ensure data consistency and the ability to track biomass
variations in space and time.
Acknowledgments
ICESat
/
GLAS
data were obtained from the National Snow and Ice
Data Center (
NSIDC
),
.
ALS
data for Robson Creek,
and Watts Creek were obtained through
CSIRO
Marine and
Atmosphere Research, and AusCover
(
.
au
). AusCover is the remote sensing data products facility of
the Terrestrial Ecosystem Research network (
TERN
,
.
tern.org.au
). Lidar data for Tumbarumba were collected with
support from
NCEO
EO
mission support 2009. Special thanks to
Jorg Hacker and Airborne Research Australia (
ARA
) for carrying
out the airborne campaigns. The authors greatly appreciate
the feedback and suggestions of the anonymous reviewers.
Mahoney acknowledges postdoctoral funding through the
NSERC CREATE
and Campus Alberta Innovates Programs.
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