The influence of snow microstructure on dual-frequency radar measurements in a tundra environment

Research output: Contribution to journalArticlepeer-review

Authors

  • Josh King
  • Chris Derksen
  • Peter Toose
  • Alexandre Langlois
  • Chris Larse
  • Juha Lemmetyinen
  • Phil Marsh
  • Benoit Montpetit
  • Alexandre Roy
  • Nick Rutter
  • Matthew Sturm

External departments

  • Environment and Climate Change Canada
  • Université de Sherbrooke
  • University of Alaska Fairbanks
  • Finnish Meteorological Institute
  • Wilfrid Laurier University

Details

Original languageEnglish
Pages (from-to)242-254
JournalRemote Sensing of Environment
Volume215
Early online date8 Jun 2018
DOIs
Publication statusPublished - 15 Sep 2018
Publication type

Research output: Contribution to journalArticlepeer-review

Abstract

Recent advancement in the understanding of snow-microwave interactions has helped to isolate the considerable potential for radar-based retrieval of snow water equivalent (SWE). There are however, few datasets available to address spatial uncertainties, such as the influence of snow microstructure, at scales relevant to space-borne application. In this study we introduce measurements from SnowSAR, an airborne, dual-frequency (9.6 and 17.2 GHz) synthetic aperture radar (SAR), to evaluate high resolution (10 m) backscatter within a snow-covered tundra basin. Coincident in situ surveys at two sites characterize a generally thin snowpack (50 cm) interspersed with deeper drift features. Structure of the snowpack is found to be predominantly wind slab (65%) with smaller proportions of depth hoar underlain (35%). Objective estimates of snow microstructure (exponential correlation length; l_"ex" ), show the slab layers to be 2.8 times smaller than the basal depth hoar. In situ measurements are used to parametrize the Microwave Emission Model of Layered Snowpacks (MEMLS3&a) and compare against collocated SnowSAR backscatter. The evaluation shows a scaling factor (ϕ) between 1.37 and 1.08, when applied to input of l_"ex" , minimizes MEMLS root mean root mean squared error to less than 1.1 dB. Model sensitivity experiments demonstrate contrasting contributions from wind slab and depth hoar components, where wind rounded microstructures are identified as a strong control on observed backscatter. Weak sensitivity of SnowSAR to spatial variations in SWE is explained by the smaller contributing microstructures of the wind slab.

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