کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
6382987 | 1626102 | 2015 | 44 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
The impacts of stratification on high latitude ocean mixing: A case study of internal waves in Storfjorden, Svalbard
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: The impacts of stratification on high latitude ocean mixing: A case study of internal waves in Storfjorden, Svalbard The impacts of stratification on high latitude ocean mixing: A case study of internal waves in Storfjorden, Svalbard](/preview/png/6382987.png)
چکیده انگلیسی
Hydrographic and velocity measurements were taken over four different time periods from April to May 2005-2007 at adjacent stations in Storfjorden, Svalbard. Different environmental conditions, including winds, ice cover, and water mass contributions, yield notably different stratification (N2) profiles among the time series. When classified according to the Gerkema (2001) classification system, the stratification profiles span the spectrum with two profiles resembling that of a two-layer fluid, one resembling more closely a fluid of constant stratification, and one falling in between the two extremes. The different N2 profiles elicit sharply contrasting modal responses from the internal wave field, which is dominated by mode 1 during the two time series most resembling a two-layer fluid, and nearly evenly spread out among the first five modes during the time series with a nearly constant stratification. Turbulent dissipation rates determined from fine-scale parameterizations reveal an average rate on the order of 10â9Wkgâ1 for all time series with an associated average diapycnal diffusivity of 10â5m2sâ1-10â4m2sâ1. Turbulent heat fluxes, determined from the estimated turbulent dissipation rates, ϵ, were found to have a relative maximum at the tops of the pycnoclines, with values up to 1Wmâ2, typical of ice-covered conditions. The turbulent dissipation rate and diapycnal diffusivities for each time series vary with the Gerkema (2001) stratification profile rankings, and are elevated for the time series most resembling a fluid of constant stratification, and reduced for the time series most similar to a two-layer fluid.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Continental Shelf Research - Volume 110, 1 November 2015, Pages 162-182
Journal: Continental Shelf Research - Volume 110, 1 November 2015, Pages 162-182
نویسندگان
Tamara Beitzel Barriquand, Pascale Bouruet-Aubertot, Yannis Cuypers, Frédéric Vivier, Antonio Lourenço, Hervé Le Goff,