Modelling Lake Ice Phenology with an Examination of Satellite-Detected Subgrid Cell Variability

Lake ice was simulated for the province of Quebec, Canada, for both contemporary and future climate conditions using a one-dimensional thermodynamic ice model. The model was forced with NARR data (32 km) and both the daily IMS product (4 km) and the MODIS snow product (500 m) were assessed for their...

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Main Authors: Laura C. Brown, Claude R. Duguay
Format: Article
Language:English
Published: Hindawi Limited 2012-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2012/529064
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spelling doaj-fbecdba701544b0e8e17a6dadbfad1222020-11-24T22:53:37ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172012-01-01201210.1155/2012/529064529064Modelling Lake Ice Phenology with an Examination of Satellite-Detected Subgrid Cell VariabilityLaura C. Brown0Claude R. Duguay1Department of Geography and Environmental Management and Interdisciplinary Centre on Climate Change (IC3), University of Waterloo, Waterloo, ON, N2L 3G1, CanadaDepartment of Geography and Environmental Management and Interdisciplinary Centre on Climate Change (IC3), University of Waterloo, Waterloo, ON, N2L 3G1, CanadaLake ice was simulated for the province of Quebec, Canada, for both contemporary and future climate conditions using a one-dimensional thermodynamic ice model. The model was forced with NARR data (32 km) and both the daily IMS product (4 km) and the MODIS snow product (500 m) were assessed for their utility at determining lake ice phenology at the subgrid cell level (based on the 32 km NARR grid). Both products were useful for detecting ice-off; however, the MODIS product was advantageous for detecting ice-on, mainly due to the finer resolution and resulting spatial detail. The subgrid cell variability in ice-on/off dates was typically less than 2% of the mean, although it ranged up to 10% for some grid cells. The simulations were found to be within the satellite-detected subgrid cell variability: 62% of the time for ice-off and 80% of the time for ice-on. Forcing the model with future climate scenarios from the Canadian Regional Climate Model predicts the regional ice cover durations will decrease by up to 50 days from the current 1981–2010 means to the 2041–2070 means and decrease from 15 to nearly 100 days shorter from the current means to the 2071–2100 means.http://dx.doi.org/10.1155/2012/529064
collection DOAJ
language English
format Article
sources DOAJ
author Laura C. Brown
Claude R. Duguay
spellingShingle Laura C. Brown
Claude R. Duguay
Modelling Lake Ice Phenology with an Examination of Satellite-Detected Subgrid Cell Variability
Advances in Meteorology
author_facet Laura C. Brown
Claude R. Duguay
author_sort Laura C. Brown
title Modelling Lake Ice Phenology with an Examination of Satellite-Detected Subgrid Cell Variability
title_short Modelling Lake Ice Phenology with an Examination of Satellite-Detected Subgrid Cell Variability
title_full Modelling Lake Ice Phenology with an Examination of Satellite-Detected Subgrid Cell Variability
title_fullStr Modelling Lake Ice Phenology with an Examination of Satellite-Detected Subgrid Cell Variability
title_full_unstemmed Modelling Lake Ice Phenology with an Examination of Satellite-Detected Subgrid Cell Variability
title_sort modelling lake ice phenology with an examination of satellite-detected subgrid cell variability
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2012-01-01
description Lake ice was simulated for the province of Quebec, Canada, for both contemporary and future climate conditions using a one-dimensional thermodynamic ice model. The model was forced with NARR data (32 km) and both the daily IMS product (4 km) and the MODIS snow product (500 m) were assessed for their utility at determining lake ice phenology at the subgrid cell level (based on the 32 km NARR grid). Both products were useful for detecting ice-off; however, the MODIS product was advantageous for detecting ice-on, mainly due to the finer resolution and resulting spatial detail. The subgrid cell variability in ice-on/off dates was typically less than 2% of the mean, although it ranged up to 10% for some grid cells. The simulations were found to be within the satellite-detected subgrid cell variability: 62% of the time for ice-off and 80% of the time for ice-on. Forcing the model with future climate scenarios from the Canadian Regional Climate Model predicts the regional ice cover durations will decrease by up to 50 days from the current 1981–2010 means to the 2041–2070 means and decrease from 15 to nearly 100 days shorter from the current means to the 2071–2100 means.
url http://dx.doi.org/10.1155/2012/529064
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