Mixed effects regression for snow distribution modelling in the central Yukon

To date, remote sensing estimates of snow water equivalent (SWE) in mountainous areas are very uncertain. To test passive microwave algorithm estimations of SWE, a validation data set must exist for a broad geographic area. This study aims to build a data set through field measurements and statistic...

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Bibliographic Details
Main Author: Kasurak, Andrew
Format: Master Thesis
Language:English
Published: University of Waterloo 2009
Subjects:
IPY
Online Access:http://hdl.handle.net/10012/4896
id ftunivwaterloo:oai:uwspace.uwaterloo.ca:10012/4896
record_format openpolar
spelling ftunivwaterloo:oai:uwspace.uwaterloo.ca:10012/4896 2023-05-15T16:55:52+02:00 Mixed effects regression for snow distribution modelling in the central Yukon Kasurak, Andrew 2009 http://hdl.handle.net/10012/4896 en eng University of Waterloo http://hdl.handle.net/10012/4896 Statistics Snow Snow water equivalent Remote sensing Mixed effects model yukon mountain boreal regression model snow distribution net accumulation Geography Master Thesis 2009 ftunivwaterloo 2022-06-18T22:58:43Z To date, remote sensing estimates of snow water equivalent (SWE) in mountainous areas are very uncertain. To test passive microwave algorithm estimations of SWE, a validation data set must exist for a broad geographic area. This study aims to build a data set through field measurements and statistical techniques, as part of the Canadian IPY observations theme to help develop an improved algorithm. Field measurements are performed at, GIS based, pre-selected sites in the Central Yukon. At each location a transect was taken, with sites measuring snow depth (SD), density, and structure. A mixed effects multiple regression was chosen to analyze and then predict these field measurements over the study area. This modelling strategy is best capable of handling the hierarchical structure of the field campaign. A regression model was developed to predict SD from elevation derived variables, and transformed Landsat data. The final model is: SD = horizontal curvature + cos( aspect) + log10(elevation range, 270m) + tassel cap: greenness, brightness (from Landsat imagery) + interaction of elevation and landcover.This model is used to predict over the study area. A second, simpler regression links SD with density giving the desired SWE measurements. The Root Mean Squared Error (RMSE) of this SD estimation is 25 cm over a domain of 200 x 200 km. This instantaneous end of season, peak accumulation, snow map will enable the vali- dation of satellite remote sensing observations, such as passive microwave (AMSR-E), in a generally inaccessible area. Master Thesis IPY Yukon University of Waterloo, Canada: Institutional Repository Yukon
institution Open Polar
collection University of Waterloo, Canada: Institutional Repository
op_collection_id ftunivwaterloo
language English
topic Statistics
Snow
Snow water equivalent
Remote sensing
Mixed effects model
yukon
mountain
boreal
regression
model
snow distribution
net accumulation
Geography
spellingShingle Statistics
Snow
Snow water equivalent
Remote sensing
Mixed effects model
yukon
mountain
boreal
regression
model
snow distribution
net accumulation
Geography
Kasurak, Andrew
Mixed effects regression for snow distribution modelling in the central Yukon
topic_facet Statistics
Snow
Snow water equivalent
Remote sensing
Mixed effects model
yukon
mountain
boreal
regression
model
snow distribution
net accumulation
Geography
description To date, remote sensing estimates of snow water equivalent (SWE) in mountainous areas are very uncertain. To test passive microwave algorithm estimations of SWE, a validation data set must exist for a broad geographic area. This study aims to build a data set through field measurements and statistical techniques, as part of the Canadian IPY observations theme to help develop an improved algorithm. Field measurements are performed at, GIS based, pre-selected sites in the Central Yukon. At each location a transect was taken, with sites measuring snow depth (SD), density, and structure. A mixed effects multiple regression was chosen to analyze and then predict these field measurements over the study area. This modelling strategy is best capable of handling the hierarchical structure of the field campaign. A regression model was developed to predict SD from elevation derived variables, and transformed Landsat data. The final model is: SD = horizontal curvature + cos( aspect) + log10(elevation range, 270m) + tassel cap: greenness, brightness (from Landsat imagery) + interaction of elevation and landcover.This model is used to predict over the study area. A second, simpler regression links SD with density giving the desired SWE measurements. The Root Mean Squared Error (RMSE) of this SD estimation is 25 cm over a domain of 200 x 200 km. This instantaneous end of season, peak accumulation, snow map will enable the vali- dation of satellite remote sensing observations, such as passive microwave (AMSR-E), in a generally inaccessible area.
format Master Thesis
author Kasurak, Andrew
author_facet Kasurak, Andrew
author_sort Kasurak, Andrew
title Mixed effects regression for snow distribution modelling in the central Yukon
title_short Mixed effects regression for snow distribution modelling in the central Yukon
title_full Mixed effects regression for snow distribution modelling in the central Yukon
title_fullStr Mixed effects regression for snow distribution modelling in the central Yukon
title_full_unstemmed Mixed effects regression for snow distribution modelling in the central Yukon
title_sort mixed effects regression for snow distribution modelling in the central yukon
publisher University of Waterloo
publishDate 2009
url http://hdl.handle.net/10012/4896
geographic Yukon
geographic_facet Yukon
genre IPY
Yukon
genre_facet IPY
Yukon
op_relation http://hdl.handle.net/10012/4896
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