Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Improved Snow Distribution Estimates Using a Rapid-Response LiDAR and Photogrammetry System

View through CrossRef
Snow plays a critical role in global hydrology, climate systems, and human activities, particularly in mountainous regions where it is a primary source of freshwater, influences the energy balance, and impacts mobility and commerce. Despite its importance, accurately mapping and predicting snow distribution remains a major challenge due to the complex spatial and temporal variability of snowpack and the lack of an ideal observation system. This dissertation aims to advance our monitoring capability, understanding, and prediction capacity of snow distribution using Light Detection and Ranging (LiDAR) and photogrammetry techniques. In chapter 2, I discussed the high-resolution LiDAR-derived datasets of multiple sites in the Western United State that I created, contributing to addressing the scarcity of distributed snow depth data in mountain regions. These datasets, collected during NASA's SnowEx campaigns, provide crucial benchmarks for validating emerging snow monitoring techniques across varied environmental conditions. In chapter 3, I introduced Ice-road-copters (IRC), an open-source Python toolkit designed to automate the processing of LiDAR and photogrammetry point clouds for snow depth mapping, significantly reducing the manual labor traditionally required for such tasks. This toolkit streamlines noise removal, ground segmentation, digital elevation model coregistration, and raster differencing, facilitating more efficient and consistent production of snow depth maps. In Chapter 4, I explored the potential of leveraging snow distribution patterns to predict snow depth across diverse mountain environments in the western United States. I assessed the repeatability of snow distribution patterns and systematically evaluated how prediction accuracy varies with different pattern types, training data quantities, and spatial scales. Results demonstrate high correlation ( r > 0.8) of distribution patterns for snow depths exceeding 0.5 m, while shallow snow conditions during early accumulation or late melt exhibit reduced pattern correlation. Prediction performance is optimized when using temporally consistent patterns—accumulation patterns for pre-peak predictions and ablation patterns for post-peak predictions—yielding mean root mean square errors between 0.2-0.4 m across all sites. Notably, robust predictions can be achieved with as few as 10 observations over a 38 km ² L > area, though prediction confidence improves with increased sampling. Performance degrades with larger spatial extents, with errors approximately doubling when scaling from 38 km ² to 3,741 km ² . Finally, in Chapter 4, I investigated the integration of LiDAR and photogrammetry for enhanced snow monitoring, demonstrating how combining LiDAR's high accuracy with photogrammetry's cost-efficiency could advance operational snow mapping in mountain watersheds. Results show that both Airborne Laser Sanning (ALS) and Unoccupied Aerial Vehicles (UAV) LiDAR provide similar levels of vertical accuracy when validated against reference measurements, with RMSE values of about 15cm. In contrast, photogrammetry exhibited substantially higher uncertainty that increase with vegetation density—from 27 cm in sparse vegetation to over 1m in dense vegetation—highlighting a critical limitation of this approach for comprehensive watershed monitoring. I proposed an enhanced methodology that combines vegetation masking during photogrammetric processing with gap-filling based on historical LiDAR-derived snow distribution patterns. This integrated approach reduces the RMSE of photogrammetric snow depth maps from 44 cm to 27 cm, demonstrating the potential for synergistic combination of these technologies. In summary, this dissertation addresses critical gaps in snow science by providing: (1) Invaluable datasets for understanding snow distribution and validating emerging snow monitoring techniques across varied environmental conditions, (2) open-source tools that democratize LiDAR and photogrammetry point cloud processing capabilities, (3) practical guidelines for leveraging limited observations and distribution pattern for predicting snow depth (4) integrated methodologies that maximize the strengths of LiDAR and photogrammetry technologies.
Boise State University, Albertsons Library
Title: Improved Snow Distribution Estimates Using a Rapid-Response LiDAR and Photogrammetry System
Description:
Snow plays a critical role in global hydrology, climate systems, and human activities, particularly in mountainous regions where it is a primary source of freshwater, influences the energy balance, and impacts mobility and commerce.
Despite its importance, accurately mapping and predicting snow distribution remains a major challenge due to the complex spatial and temporal variability of snowpack and the lack of an ideal observation system.
This dissertation aims to advance our monitoring capability, understanding, and prediction capacity of snow distribution using Light Detection and Ranging (LiDAR) and photogrammetry techniques.
In chapter 2, I discussed the high-resolution LiDAR-derived datasets of multiple sites in the Western United State that I created, contributing to addressing the scarcity of distributed snow depth data in mountain regions.
These datasets, collected during NASA's SnowEx campaigns, provide crucial benchmarks for validating emerging snow monitoring techniques across varied environmental conditions.
In chapter 3, I introduced Ice-road-copters (IRC), an open-source Python toolkit designed to automate the processing of LiDAR and photogrammetry point clouds for snow depth mapping, significantly reducing the manual labor traditionally required for such tasks.
This toolkit streamlines noise removal, ground segmentation, digital elevation model coregistration, and raster differencing, facilitating more efficient and consistent production of snow depth maps.
In Chapter 4, I explored the potential of leveraging snow distribution patterns to predict snow depth across diverse mountain environments in the western United States.
I assessed the repeatability of snow distribution patterns and systematically evaluated how prediction accuracy varies with different pattern types, training data quantities, and spatial scales.
Results demonstrate high correlation ( r > 0.
8) of distribution patterns for snow depths exceeding 0.
5 m, while shallow snow conditions during early accumulation or late melt exhibit reduced pattern correlation.
Prediction performance is optimized when using temporally consistent patterns—accumulation patterns for pre-peak predictions and ablation patterns for post-peak predictions—yielding mean root mean square errors between 0.
2-0.
4 m across all sites.
Notably, robust predictions can be achieved with as few as 10 observations over a 38 km ² L > area, though prediction confidence improves with increased sampling.
Performance degrades with larger spatial extents, with errors approximately doubling when scaling from 38 km ² to 3,741 km ² .
Finally, in Chapter 4, I investigated the integration of LiDAR and photogrammetry for enhanced snow monitoring, demonstrating how combining LiDAR's high accuracy with photogrammetry's cost-efficiency could advance operational snow mapping in mountain watersheds.
Results show that both Airborne Laser Sanning (ALS) and Unoccupied Aerial Vehicles (UAV) LiDAR provide similar levels of vertical accuracy when validated against reference measurements, with RMSE values of about 15cm.
In contrast, photogrammetry exhibited substantially higher uncertainty that increase with vegetation density—from 27 cm in sparse vegetation to over 1m in dense vegetation—highlighting a critical limitation of this approach for comprehensive watershed monitoring.
I proposed an enhanced methodology that combines vegetation masking during photogrammetric processing with gap-filling based on historical LiDAR-derived snow distribution patterns.
This integrated approach reduces the RMSE of photogrammetric snow depth maps from 44 cm to 27 cm, demonstrating the potential for synergistic combination of these technologies.
In summary, this dissertation addresses critical gaps in snow science by providing: (1) Invaluable datasets for understanding snow distribution and validating emerging snow monitoring techniques across varied environmental conditions, (2) open-source tools that democratize LiDAR and photogrammetry point cloud processing capabilities, (3) practical guidelines for leveraging limited observations and distribution pattern for predicting snow depth (4) integrated methodologies that maximize the strengths of LiDAR and photogrammetry technologies.

Related Results

Influence of cohesion on drifting snow investigated in cold wind-tunnel 
Influence of cohesion on drifting snow investigated in cold wind-tunnel 
<p>Aeolian transport of particles occurs in many geophysical contexts such as wind-blown sand or snow drift and is governed by a myriad of physical mechanisms. Most o...
Development of a multimodal imaging system based on LIDAR
Development of a multimodal imaging system based on LIDAR
(English) Perception of the environment is an essential requirement for the fields of autonomous vehicles and robotics, that claim for high amounts of data to make reliable decisio...
Dynamic Snow Distribution Modeling using the Fokker-Planck Equation Approach
Dynamic Snow Distribution Modeling using the Fokker-Planck Equation Approach
<p>The Fokker-Planck equation (FPE) describes the time evolution of the distribution function of fluctuating macroscopic variables.  Although the FPE was...
Snow representation in seasonal forecasts and climate simulations: sensitivities of seasonal snow simulation and impact on frozen soils
Snow representation in seasonal forecasts and climate simulations: sensitivities of seasonal snow simulation and impact on frozen soils
Snow cover is a critical component of the Earth's climate system, covering up to 44 % of the Northern Hemisphere's land during winter and influencing energy exchange, water storage...
Revisiting NASA's Operation IceBridge Snow on Sea Ice Radar Measurements in the Arctic
Revisiting NASA's Operation IceBridge Snow on Sea Ice Radar Measurements in the Arctic
Snow on sea ice plays a critical role in modulating ice mass changes in response to anthropogenic warming, with significant implications for ocean mixed layer processes, the surfac...
Dynamic identification of snow phenology in the Northern Hemisphere
Dynamic identification of snow phenology in the Northern Hemisphere
Abstract. Snow phenology characterizes the cyclical changes in snow and has become an important indicator of climate change in recent decades. Changes in snow phenology can signifi...
Challenges in Alpine Snow and Ice Hydrology
Challenges in Alpine Snow and Ice Hydrology
Advances in alpine snow and ice hydrology have occurred due to the relentless efforts of field researchers to study snow processes in remote research sites, improvements in automat...
A snow reanalysis for Italy: IT-SNOW
A snow reanalysis for Italy: IT-SNOW
Quantifying the amount of snow deposited across the landscape at any given time is the main goal of snow hydrology. Yet, answering this apparently simple question is still elusive ...

Back to Top