Impact of spatial averaging on radar reflectivity at internal snowpack layer boundaries

Microwave radar amplitude within a snowpack can be strongly influenced by spatial variability of internal layer boundaries. We quantify the impact of spatial averaging of snow stratigraphy and physical snowpack properties on surface scattering from near-nadir frequency-modulated continuous-wave rada...

Full description

Bibliographic Details
Main Authors: N. RUTTER, H.-P. MARSHALL, K. TAPE, R. ESSERY, J. KING
Format: Article
Language:English
Published: Cambridge University Press 2016-12-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S002214301600099X/type/journal_article
_version_ 1811155875461595136
author N. RUTTER
H.-P. MARSHALL
K. TAPE
R. ESSERY
J. KING
author_facet N. RUTTER
H.-P. MARSHALL
K. TAPE
R. ESSERY
J. KING
author_sort N. RUTTER
collection DOAJ
description Microwave radar amplitude within a snowpack can be strongly influenced by spatial variability of internal layer boundaries. We quantify the impact of spatial averaging of snow stratigraphy and physical snowpack properties on surface scattering from near-nadir frequency-modulated continuous-wave radar at 12–18 GHz. Relative permittivity, density, grain size and stratigraphic boundaries were measured in-situ at high resolution along the length of a 9 m snow trench. An optimal range of horizontal averaging (4–6 m) was identified to attribute variations in surface scattering at layer boundaries to dielectric contrasts estimated from centimetre-scale measurements of snowpack stratigraphy and bulk layer properties. Single vertical profiles of snowpack properties seldom captured the complex local variability influencing near-nadir radar surface scattering. We discuss implications of scaling in-situ measurements for snow radiative transfer modelling and evaluation of airborne microwave remote sensing of snow.
first_indexed 2024-04-10T04:42:00Z
format Article
id doaj.art-a1d104fa22d8443d83f4210767a8d6ac
institution Directory Open Access Journal
issn 0022-1430
1727-5652
language English
last_indexed 2024-04-10T04:42:00Z
publishDate 2016-12-01
publisher Cambridge University Press
record_format Article
series Journal of Glaciology
spelling doaj.art-a1d104fa22d8443d83f4210767a8d6ac2023-03-09T12:40:19ZengCambridge University PressJournal of Glaciology0022-14301727-56522016-12-01621065107410.1017/jog.2016.99Impact of spatial averaging on radar reflectivity at internal snowpack layer boundariesN. RUTTER0https://orcid.org/0000-0002-5008-3575H.-P. MARSHALL1K. TAPE2R. ESSERY3J. KING4Department of Geography, Northumbria University, Newcastle upon Tyne, UKCenter for Geophysical Investigation of the Shallow Subsurface, Boise State University, Boise, ID, USAInstitute of Northern Engineering, Water & Environmental Research Center, University of Alaska, Fairbanks, AK, USASchool of GeoSciences, University of Edinburgh, Edinburgh, UKClimate Research Division, Environment and Climate Change Canada, Toronto, CanadaMicrowave radar amplitude within a snowpack can be strongly influenced by spatial variability of internal layer boundaries. We quantify the impact of spatial averaging of snow stratigraphy and physical snowpack properties on surface scattering from near-nadir frequency-modulated continuous-wave radar at 12–18 GHz. Relative permittivity, density, grain size and stratigraphic boundaries were measured in-situ at high resolution along the length of a 9 m snow trench. An optimal range of horizontal averaging (4–6 m) was identified to attribute variations in surface scattering at layer boundaries to dielectric contrasts estimated from centimetre-scale measurements of snowpack stratigraphy and bulk layer properties. Single vertical profiles of snowpack properties seldom captured the complex local variability influencing near-nadir radar surface scattering. We discuss implications of scaling in-situ measurements for snow radiative transfer modelling and evaluation of airborne microwave remote sensing of snow.https://www.cambridge.org/core/product/identifier/S002214301600099X/type/journal_articleradarremote sensingsnow microstructuresnow stratigraphyspatial variability
spellingShingle N. RUTTER
H.-P. MARSHALL
K. TAPE
R. ESSERY
J. KING
Impact of spatial averaging on radar reflectivity at internal snowpack layer boundaries
Journal of Glaciology
radar
remote sensing
snow microstructure
snow stratigraphy
spatial variability
title Impact of spatial averaging on radar reflectivity at internal snowpack layer boundaries
title_full Impact of spatial averaging on radar reflectivity at internal snowpack layer boundaries
title_fullStr Impact of spatial averaging on radar reflectivity at internal snowpack layer boundaries
title_full_unstemmed Impact of spatial averaging on radar reflectivity at internal snowpack layer boundaries
title_short Impact of spatial averaging on radar reflectivity at internal snowpack layer boundaries
title_sort impact of spatial averaging on radar reflectivity at internal snowpack layer boundaries
topic radar
remote sensing
snow microstructure
snow stratigraphy
spatial variability
url https://www.cambridge.org/core/product/identifier/S002214301600099X/type/journal_article
work_keys_str_mv AT nrutter impactofspatialaveragingonradarreflectivityatinternalsnowpacklayerboundaries
AT hpmarshall impactofspatialaveragingonradarreflectivityatinternalsnowpacklayerboundaries
AT ktape impactofspatialaveragingonradarreflectivityatinternalsnowpacklayerboundaries
AT ressery impactofspatialaveragingonradarreflectivityatinternalsnowpacklayerboundaries
AT jking impactofspatialaveragingonradarreflectivityatinternalsnowpacklayerboundaries