On the Use of MODIS for Lake and Land Surface Temperature Investigations in the Regions of Great Bear Lake and Great Slave Lake, N.W.T.

Lake surface temperature (LSTlake) can be obtained and studied in different ways: using in situ measurements, satellite imagery and modeling. Collecting spatially representative in situ data over lakes, especially for large and deep ones, is a real challenge. Satellite data products provide the oppo...

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Bibliographic Details
Main Author: Kheyrollah Pour, Homa
Format: Master Thesis
Language:English
Published: University of Waterloo 2011
Subjects:
Online Access:http://hdl.handle.net/10012/6100
id ftunivwaterloo:oai:uwspace.uwaterloo.ca:10012/6100
record_format openpolar
spelling ftunivwaterloo:oai:uwspace.uwaterloo.ca:10012/6100 2023-05-15T16:22:59+02:00 On the Use of MODIS for Lake and Land Surface Temperature Investigations in the Regions of Great Bear Lake and Great Slave Lake, N.W.T. Kheyrollah Pour, Homa 2011-07-15 http://hdl.handle.net/10012/6100 en eng University of Waterloo http://hdl.handle.net/10012/6100 Land Surface Temperature MODIS Great Bear Lake Great Slave Lake Geography Master Thesis 2011 ftunivwaterloo 2022-06-18T22:59:11Z Lake surface temperature (LSTlake) can be obtained and studied in different ways: using in situ measurements, satellite imagery and modeling. Collecting spatially representative in situ data over lakes, especially for large and deep ones, is a real challenge. Satellite data products provide the opportunity to collect continuous data over very large geographic areas even in remote regions. Numerical modeling is also an approach to study the response and the role of lakes in the climate system. Satellite instruments provide spatial information unlike in situ measurements and one-dimensional (1-D) lake models that give vertical information at a single point or a few points in lakes. The advantage of remote sensing also applies to land where temperature measurements are usually taken at meteorological stations whose network is extremely sparse in northern regions. This thesis therefore examined the value of land/lake surface (skin) temperature (LSTland/lake) measurements from satellites as a complement to in situ point measurements and numerical modeling. The thesis is organized into two parts. The first part tested, two 1-D numerical models against in situ and satellite-derived LST measurements. LSTlake and ice phenology were simulated for various points at different depths on Great Slave Lake (GSL) and Great Bear Lake (GBL), two large lakes located in the Mackenzie River Basin in Canada’s Northwest Territories, using the 1-D Freshwater Lake model (FLake) and the Canadian Lake Ice Model (CLIMo) over the 2002-2010 period. Input data from three weather stations (Yellowknife, Hay River and Deline) were used for model simulations. LSTlake model results are compared to those derived from the Moderate Resolution Imaging Spectroradiometer (MODIS) aboard the Earth Observing System Terra and Aqua satellite platforms. The main goal was to examine the performance of the FLake and CLIMo models in simulating LSTlake and ice-cover under different conditions against satellite data products. Both models reveal a good agreement ... Master Thesis Great Bear Lake Great Slave Lake Hay River Mackenzie river Northwest Territories Yellowknife University of Waterloo, Canada: Institutional Repository Deline ENVELOPE(-123.406,-123.406,65.198,65.198) Great Bear Lake ENVELOPE(-120.753,-120.753,65.834,65.834) Great Slave Lake ENVELOPE(-114.001,-114.001,61.500,61.500) Hay River ENVELOPE(-115.847,-115.847,60.787,60.787) Mackenzie River Northwest Territories Yellowknife
institution Open Polar
collection University of Waterloo, Canada: Institutional Repository
op_collection_id ftunivwaterloo
language English
topic Land Surface Temperature
MODIS
Great Bear Lake
Great Slave Lake
Geography
spellingShingle Land Surface Temperature
MODIS
Great Bear Lake
Great Slave Lake
Geography
Kheyrollah Pour, Homa
On the Use of MODIS for Lake and Land Surface Temperature Investigations in the Regions of Great Bear Lake and Great Slave Lake, N.W.T.
topic_facet Land Surface Temperature
MODIS
Great Bear Lake
Great Slave Lake
Geography
description Lake surface temperature (LSTlake) can be obtained and studied in different ways: using in situ measurements, satellite imagery and modeling. Collecting spatially representative in situ data over lakes, especially for large and deep ones, is a real challenge. Satellite data products provide the opportunity to collect continuous data over very large geographic areas even in remote regions. Numerical modeling is also an approach to study the response and the role of lakes in the climate system. Satellite instruments provide spatial information unlike in situ measurements and one-dimensional (1-D) lake models that give vertical information at a single point or a few points in lakes. The advantage of remote sensing also applies to land where temperature measurements are usually taken at meteorological stations whose network is extremely sparse in northern regions. This thesis therefore examined the value of land/lake surface (skin) temperature (LSTland/lake) measurements from satellites as a complement to in situ point measurements and numerical modeling. The thesis is organized into two parts. The first part tested, two 1-D numerical models against in situ and satellite-derived LST measurements. LSTlake and ice phenology were simulated for various points at different depths on Great Slave Lake (GSL) and Great Bear Lake (GBL), two large lakes located in the Mackenzie River Basin in Canada’s Northwest Territories, using the 1-D Freshwater Lake model (FLake) and the Canadian Lake Ice Model (CLIMo) over the 2002-2010 period. Input data from three weather stations (Yellowknife, Hay River and Deline) were used for model simulations. LSTlake model results are compared to those derived from the Moderate Resolution Imaging Spectroradiometer (MODIS) aboard the Earth Observing System Terra and Aqua satellite platforms. The main goal was to examine the performance of the FLake and CLIMo models in simulating LSTlake and ice-cover under different conditions against satellite data products. Both models reveal a good agreement ...
format Master Thesis
author Kheyrollah Pour, Homa
author_facet Kheyrollah Pour, Homa
author_sort Kheyrollah Pour, Homa
title On the Use of MODIS for Lake and Land Surface Temperature Investigations in the Regions of Great Bear Lake and Great Slave Lake, N.W.T.
title_short On the Use of MODIS for Lake and Land Surface Temperature Investigations in the Regions of Great Bear Lake and Great Slave Lake, N.W.T.
title_full On the Use of MODIS for Lake and Land Surface Temperature Investigations in the Regions of Great Bear Lake and Great Slave Lake, N.W.T.
title_fullStr On the Use of MODIS for Lake and Land Surface Temperature Investigations in the Regions of Great Bear Lake and Great Slave Lake, N.W.T.
title_full_unstemmed On the Use of MODIS for Lake and Land Surface Temperature Investigations in the Regions of Great Bear Lake and Great Slave Lake, N.W.T.
title_sort on the use of modis for lake and land surface temperature investigations in the regions of great bear lake and great slave lake, n.w.t.
publisher University of Waterloo
publishDate 2011
url http://hdl.handle.net/10012/6100
long_lat ENVELOPE(-123.406,-123.406,65.198,65.198)
ENVELOPE(-120.753,-120.753,65.834,65.834)
ENVELOPE(-114.001,-114.001,61.500,61.500)
ENVELOPE(-115.847,-115.847,60.787,60.787)
geographic Deline
Great Bear Lake
Great Slave Lake
Hay River
Mackenzie River
Northwest Territories
Yellowknife
geographic_facet Deline
Great Bear Lake
Great Slave Lake
Hay River
Mackenzie River
Northwest Territories
Yellowknife
genre Great Bear Lake
Great Slave Lake
Hay River
Mackenzie river
Northwest Territories
Yellowknife
genre_facet Great Bear Lake
Great Slave Lake
Hay River
Mackenzie river
Northwest Territories
Yellowknife
op_relation http://hdl.handle.net/10012/6100
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