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David Landry

dblp:152/4806 · DBLP profile ↗
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2ranked-venue papers
1as first author
1since 2021 · last 2022
—ORCID · conflict

Domains — the database's venue-derived domains; a paper can count in several

Artificial intelligence and machine learning · 1 · 1 first-authorSystems, architecture and hardware · 1 · 1 first-authorApplied, interdisciplinary, general and emerging computing · 1 · 1 since 2021

Expertise — from the expertise taxonomy: the topics of the expert's papers under the CCF categories. A weight counts papers with recency: 1 for a paper about the topic, 0.3 when the topic is its context, halved every five years.

Artificial intelligence
1 paper
Robot navigation and mapping · 87% 3D vision · 13%

Topics — the 3 heaviest of 3, each with the papers that count most for it

TopicWeightPapersLastEvidence papers
Robotics › Robot navigation and mapping › scan matching
ICP covariance estimation
0.412019
CELLO-3D: Estimating the Covariance of ICP in the Real World · ICRA 2019
Robotics › Robot navigation and mapping
SLAM
0.412019
CELLO-3D: Estimating the Covariance of ICP in the Real World · ICRA 2019
Computer vision › 3D vision
point cloud registration
0.112019
CELLO-3D: Estimating the Covariance of ICP in the Real World · ICRA 2019

Methods — techniques the papers use, named apart from their topics

iterative closest point · 0.4data-driven covariance estimation · 0.4
YearPublicationVenuePosition
2022 Toward the Detection of Oil Spills in Newly Formed Sea Ice Using C-Band Multipolarization Radar
abstract
Oil spills in the Arctic are becoming more likely as shipping traffic increases in response to climate-related sea ice loss. To improve oil spill detection capability, we used a controlled mesocosm to analyze the multipolarized C-band backscatter response of oil in newly formed sea ice (NI). Artificial sea ice was grown in two cylindrical tubs at the Sea-ice Environmental Research Facility, University of Manitoba. The sea ice physical characteristics, including surface roughness, thickness, temperature, and salinity, were measured before and after oil injection below the ice sheet. Time-series C-band radar backscatter measurements detected the differences in the sea ice evolution and oil migration to the sea ice surface in the oil-contaminated tub, which was compared to uncontaminated ice in a control tub. Immediately prior to the presence of oil on the ice surface, the copolarized backscatter is increased by 13-dB local maximum, while the cross-polarized backscatter is decreased by 9-dB. Ice physical properties suggest that the local backscatter maximum and minimum, which occurred immediately before oil migrated onto the surface, were related to a combination of brine and oil upward migration. The findings of this work provide a baseline data interpretation for oil detection in the Arctic Ocean using current and future C-band multipolarization radar satellites.
Elvis Asihene, Durell S. Desmond, Madison L. Harasyn, David Landry, Cathrin Veenaas, Amirbahador Mansoori, Mark Christopher Fuller, Gary A. Stern, David G. Barber, Colin Gilmore, Dustin Isleifson
IEEE Trans. Geosci. Remote. Sens.4
2019 CELLO-3D: Estimating the Covariance of ICP in the Real World
abstract
The fusion of Iterative Closest Point (ICP) registrations in existing state estimation frameworks relies on an accurate estimation of their uncertainty. In this paper, we study the estimation of this uncertainty in the form of a covariance. First, we scrutinize the limitations of existing closed-form covariance estimation algorithms over 3D datasets. Then, we set out to estimate the covariance of ICP registrations through a data-driven approach, with over 5100000 registrations on 1020 pairs from real 3D point clouds. We assess our solution upon a wide spectrum of environments, ranging from structured to unstructured and indoor to outdoor. The capacity of our algorithm to predict covariances is accurately assessed, as well as the usefulness of these estimations for uncertainty estimation over trajectories. The proposed method estimates covariances better than existing closed-form solutions, and makes predictions that are consistent with observed trajectories.
David Landry, François Pomerleau, Philippe Giguère
ICRA1