Ice thickness measurements in Lake Erie during the winter of 2010–2011

Hawley, Nathan; Beletsky, Dmitry; Wang, Jia

doi:10.1016/j.jglr.2018.04.004

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The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles, guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the NOAA IR retains documents in their original published format to ensure public access to scientific information.

i

Ice thickness measurements in Lake Erie during the winter of 2010–2011

2018
By Hawley, Nathan ; Beletsky, Dmitry ; Wang, Jia
Source: Journal of Great Lakes Research, 44(3), 388-397

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Journal Title:

Journal of Great Lakes Research
Personal Author:

Hawley, Nathan ; Beletsky, Dmitry ; Wang, Jia

Hawley, Nathan ; Beletsky, Dmitry ; Wang, Jia Less -
NOAA Program & Office:

OAR (Oceanic and Atmospheric Research) ; CIGLR (Cooperative Institute for Great Lakes Research) ; GLERL (Great Lakes Environmental Research Laboratory)

OAR (Oceanic and Atmospheric Research) ; CIGLR (Cooperative Institute for Great Lakes Research) ; GLERL (Great Lakes Environmental Research Laboratory) Less -
Description:

Time series measurements of ice thicknesses were made at either 1 or 2 Hz at 6 locations in the western part of Lake Erie's central basin during the winter of 2010–2011. Ice was observed over approximately 80 days beginning in late December and continuing through mid-March. Deformation and ridging of ice occurred frequently and produced ice thicknesses of up to 10 m, and over 6 m at all stations. The measurements show considerable variability (up to several meters) between stations, even when the distance between them is <500 m. Comparison of the measurements to those generated by the National Ice Center show good agreement for undeformed thicknesses, but the Ice Center analyses do not account for increased thicknesses due to ice ridging. Several different measures of ice thickness (based on different averaging times and the parameter used to characterize the resulting distribution of thicknesses) are used to characterize the data, and the results can vary widely depending upon which measure is used. The best measure to use will depend upon the use for which the data is intended.
Source:

Journal of Great Lakes Research, 44(3), 388-397
DOI:

https://doi.org/10.1016/j.jglr.2018.04.004
ISSN:

0380-1330
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pdf
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Elsevier BV
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Journal Article-Accepted Manuscript
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Accepted Manuscript
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urn:sha-512:660dac0635f49b77a33493af0c7d3807277d472f7ba1b620008f0bcbe5cb3a6f8dd005f57381c448690445db376df067997d782f05734730ae64da3a72ef8f84
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Ice thickness measurements in Lake Erie during the winter of 2010–2011

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