کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6383478 1626327 2015 13 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Internal tides near the Celtic Sea shelf break: A new look at a well known problem
ترجمه فارسی عنوان
جزر و مد داخلی در نزدیکی قفسه دریای سلت: نگاه جدید به یک مشکل شناخته شده
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات زمین شناسی
چکیده انگلیسی


- Internal waves generated by tides at the Celtic Sea shelf break are investigated.
- Due to large bottom steepness they disintegrated locally over the continental slope.
- Radiated seaward internal waves transform their energy to higher baroclinic modes.
- In the open part of the sea internal waves are generated locally by a tidal beam.
- A large part of tidal beam energy is reflected upward from the layered pycnocline.

Internal waves generated by tides in the Celtic Sea were investigated on the basis of in situ data collected at the continental slope in July 2012, and theoretically using a weakly nonlinear theory and the Massachusetts Institute of Technology general circulation model. It was found that internal solitary waves generated over the shelf break and propagated seaward did not survive in the course of their evolution. Due to the large bottom steepness they disintegrated locally over the continental slope radiating several wave systems seaward and transforming their energy to higher baroclinic modes. In the open part of the sea, i.e. 120 km away from the shelf break, internal waves were generated by a baroclinic tidal beam which was radiated from the shelf break downward to the abyss. After reflection from the bottom it returned back to the surface where it hit the seasonal pycnocline and generated packets of high-mode internal solitary waves. Another effect that had strong implications for the wave dynamics was internal wave reflection from sharp changes of vertical fluid stratification in the main pycnocline. A large proportion of the tidal beam energy that propagated downward did not reach the bottom but reflected upward from the layered pycnocline and returned back to the surface seasonal pycnocline where it generated some extra higher mode internal wave systems, including internal wave breathers.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Deep Sea Research Part I: Oceanographic Research Papers - Volume 103, September 2015, Pages 24-36
نویسندگان
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