This site requires Cookies enabled in your browser for login.
Updating ...
WaterNet Home
WaterNet
for
pour le
Canada
Menu
WaterNet
Home
GWFO
Home
Catalogue
Master Index
Data
Centre
X
Find Data By Variable Find Data By Site, Facility, or Deployable Show Near-realtime Telemetry (7 day)
Collections
X
Defaults
Select All
Websites
X
Global Water Futures Observatories (GWFO) Global Water Futures (GWF) Global Institute for Water Security (GIWS) International Network of Alpine Research Catchment Hydrology
Legacy Research Programs
X
Changing Cold Regions Network (CCRN) Drought Research Initiative (DRI) International Network of Alpine Research Catchment Hydrology (Legacy Site) Improving Processes & Parameterization for Prediction in Cold Regions Hydrology (IP3) The Mackenzie Global Energy and Water Cycle Experiment (GEWEX) Study (MAGS)
Legacy sites
Map
Utilities
X
Account Settings Create a New Record Record List Alias List Editor
Edit Data Centre
Data Types
. . .
X
Clear
Select All
Advanced Search
Go to Top⇡
Related items loading ...
Fetching Chart ...
Publication Additional Information Download
Publication Type
Journal Article
Authorship
Murfitt, J., C. Duguay, G. Picard, and G. Gunn.
Title
Investigating the effect of lake ice properties on multifrequency imaging SAR backscatter using the Snow Microwave Radiative Transfer (SMRT) model
Year
2022
Publication Outlet
IEEE Transactions on Geoscience and Remote Sensing
DOI
https://doi.org/10.1109/TGRS.2022.3197109
Citation
Murfitt, J., C. Duguay, G. Picard, and G. Gunn (2022). Investigating the effect of lake ice properties on multifrequency imaging SAR backscatter using the Snow Microwave Radiative Transfer (SMRT) model. IEEE Transactions on Geoscience and Remote Sensing.
Abstract
Recent investigations using polarimetric decom- position and numerical models have helped to improve the understanding of how radar signals interact with lake ice. However, further research is needed on how radar signals are impacted by varying lake ice properties. Radiative trans- fer (RT) models provide one method of improving this under- standing. These are the first published experiments using the snow microwave RT (SMRT) model to investigate the response of different frequencies (L-, C-, and X-band) at horizontal- horizontal (HH) and vertical-vertical (VV) polarizations using various incidence angles (20◦, 30 ◦, and 40 ◦)to changes in ice thickness, porosity, bubble radius, and ice–water interface roughness. This is also the first use of SMRT in combination with a thermodynamic lake ice model. Experiments were for a lake with tubular bubbles and one without tubular bubbles under difference scenarios. An analysis of the backscatter response to different properties indicates that increasing ice thickness and layer porosity have little impact on backscatter from lake ice. X-band backscatter shows increased response to surface ice layer bubble radius; however, this was limited to other frequencies except at shallower incidence angles (40◦). All three frequencies display the largest response to increasing root mean square (rms) height at the ice–water interface, which supports surface scatter- ing at the ice–water interface as being the dominant scattering mechanism. These results demonstrate that the SMRT is a valuable tool for understanding the response of backscatter to changes in freshwater lake ice properties and could be used in the development of inversion models.
Program Affiliations
GWF: Global Water Futures
Project Affiliations
GWF-TSTSW: Transformative Sensor Technologies and Smart Watersheds
Publication Stage
Published
Additional Information
TTSW, Refereed Publications
Download Links
https://doi.org/10.1109/TGRS.2022.3197109

https://ieeexplore.ieee.org/iel7/36/4358825/09851652.pdf
© 2026 - WaterNet Version 2026-08-10
Global Water Futures Observatories
Powered by
G W F Net
T-2022-12-03-M1cpqhlNqSUSocfI66enO5Q Publication 1.0