Shear, Strain, and Richardson Number Variations in the Thermocline. Part I: Statistical Description
نویسندگان
چکیده
منابع مشابه
Generalized Stability of Nongeostrophic Baroclinic Shear Flow. Part I: Large Richardson Number Regime
A generalized stability theory (GST) analysis of baroclinic shear flow is performed using primitive equations (PEs), and typical synoptic-scale midlatitudinal values of vertical shear and stratification. GST is a comprehensive linear stability theory that subsumes modal stability theory and extends it to account for nonmodal interactions such as may occur among the approximately geostrophically...
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This work continues the generalized stability theory (GST) analysis of baroclinic shear flow in the primitive equations (PE), focusing on the regime in which the mean baroclinic shear and the stratification are of the same order. The Eady model basic state is used and solutions obtained using the PE are compared to quasigeostrophic (QG) solutions. Similar optimal growth is obtained in the PE an...
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Approaches to assess copy number variation have advanced rapidly and are being incorporated into genetic studies. While the technology exists for CNV genotyping, a further understanding and discussion of how to use the CNV data for association analyses is warranted. We present the options available for processing and analysing CNV data. We break these steps down into choice of genotyping platfo...
متن کاملNorth Pacific Thermocline Variations on ENSO Timescales
The North Pacific thermocline (250 to 400 m) is studied using XBT observations acquired during the 1970s and 1980s. Interannual variations (3–5 yr timescales) in thermocline temperature, with O(0.18C) amplitude at 400 m, are found to exhibit westward propagation throughout the extratropical North Pacific up to 458N. Southward of 308N, the features propagate intact across the basin from the east...
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ژورنال
عنوان ژورنال: Journal of Physical Oceanography
سال: 1997
ISSN: 0022-3670,1520-0485
DOI: 10.1175/1520-0485(1997)027<0264:ssarnv>2.0.co;2