An examination of snow redistribution over smooth land‐fast sea ice

Abstract An understanding of temporal evolution of snow on sea ice at different spatial scales is essential for improvement of snow parameterization in sea ice models. One of the problems we face, however, is that long‐term climate data are routinely available for land and not for sea ice. In this p...

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Published in:Hydrological Processes
Main Authors: Iacozza, J., Barber, D. G.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.7526
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spelling crwiley:10.1002/hyp.7526 2024-06-23T07:56:01+00:00 An examination of snow redistribution over smooth land‐fast sea ice Iacozza, J. Barber, D. G. 2009 http://dx.doi.org/10.1002/hyp.7526 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.7526 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.7526 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 24, issue 7, page 850-865 ISSN 0885-6087 1099-1085 journal-article 2009 crwiley https://doi.org/10.1002/hyp.7526 2024-06-11T04:51:37Z Abstract An understanding of temporal evolution of snow on sea ice at different spatial scales is essential for improvement of snow parameterization in sea ice models. One of the problems we face, however, is that long‐term climate data are routinely available for land and not for sea ice. In this paper, we examine the temporal evolution of snow over smooth land‐fast first‐year sea ice using observational and modelled data. Changes in probability density functions indicate that depositional and drifting events control the evolution of snow distribution. Geostatistical analysis suggests that snowdrifts increased over the study period, and the orientation was related to the meteorological conditions. At the microscale, the temporal evolution of the snowdrifts was a product of infilling in the valleys between drifts. Results using two shore‐based climate reporting stations (Paulatuk and Tuktoyuktuk, NWT) suggest that on‐ice air temperature and relative humidity can be estimated using air temperature recorded at either station. Wind speed, direction and precipitation on ice cannot be accurately estimated using meteorological data from either station. The temporal evolution of snow distribution over smooth land‐fast sea ice was modelled using SnowModel and four different forcing regimes. The results from these model runs indicate a lack of agreement between observed distribution and model outputs. The reasons for these results are lack of meteorological measurements prior to the end of January, lack of spatially adequate surface topography and discrepancies between meteorological variables on land and ice. Copyright © 2009 John Wiley & Sons, Ltd. Article in Journal/Newspaper Paulatuk Sea ice Wiley Online Library Paulatuk ENVELOPE(-123.985,-123.985,69.325,69.325) Hydrological Processes 24 7 850 865
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract An understanding of temporal evolution of snow on sea ice at different spatial scales is essential for improvement of snow parameterization in sea ice models. One of the problems we face, however, is that long‐term climate data are routinely available for land and not for sea ice. In this paper, we examine the temporal evolution of snow over smooth land‐fast first‐year sea ice using observational and modelled data. Changes in probability density functions indicate that depositional and drifting events control the evolution of snow distribution. Geostatistical analysis suggests that snowdrifts increased over the study period, and the orientation was related to the meteorological conditions. At the microscale, the temporal evolution of the snowdrifts was a product of infilling in the valleys between drifts. Results using two shore‐based climate reporting stations (Paulatuk and Tuktoyuktuk, NWT) suggest that on‐ice air temperature and relative humidity can be estimated using air temperature recorded at either station. Wind speed, direction and precipitation on ice cannot be accurately estimated using meteorological data from either station. The temporal evolution of snow distribution over smooth land‐fast sea ice was modelled using SnowModel and four different forcing regimes. The results from these model runs indicate a lack of agreement between observed distribution and model outputs. The reasons for these results are lack of meteorological measurements prior to the end of January, lack of spatially adequate surface topography and discrepancies between meteorological variables on land and ice. Copyright © 2009 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Iacozza, J.
Barber, D. G.
spellingShingle Iacozza, J.
Barber, D. G.
An examination of snow redistribution over smooth land‐fast sea ice
author_facet Iacozza, J.
Barber, D. G.
author_sort Iacozza, J.
title An examination of snow redistribution over smooth land‐fast sea ice
title_short An examination of snow redistribution over smooth land‐fast sea ice
title_full An examination of snow redistribution over smooth land‐fast sea ice
title_fullStr An examination of snow redistribution over smooth land‐fast sea ice
title_full_unstemmed An examination of snow redistribution over smooth land‐fast sea ice
title_sort examination of snow redistribution over smooth land‐fast sea ice
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1002/hyp.7526
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.7526
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.7526
long_lat ENVELOPE(-123.985,-123.985,69.325,69.325)
geographic Paulatuk
geographic_facet Paulatuk
genre Paulatuk
Sea ice
genre_facet Paulatuk
Sea ice
op_source Hydrological Processes
volume 24, issue 7, page 850-865
ISSN 0885-6087 1099-1085
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/hyp.7526
container_title Hydrological Processes
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