The M2 Internal Tide Simulated by a 1/10° OGCM

نویسندگان
چکیده

برای دانلود رایگان متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Interdecadal Temperature Variations in the North Pacific Central Mode Water Simulated by an OGCM

Japan Marine Science and Technology Center, Natsushima-cho, Yokosuka 237-0061, Japan 2International Pacific Research Center and Department of Meteorology, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, HI 96822, U.S.A. Frontier Observational Research System for Global Change, Natsushima-cho, Yokosuka 237-0061, Japan 4International Pacific Research Center, Scho...

متن کامل

Unpredictability of internal M2

Current observations from a shelf sea, continental slopes and the abyssal North-East Atlantic Ocean are all dominated by the semidiurnal lunar (M2) tide. It is shown that motions at M2 vary at usually large barotropic and coherent baroclinic scales, >50 km horizontally and >0.5 H vertically. H represents the waterdepth. Such M2-scales are observed even close to topography, the potential source ...

متن کامل

Internal tide generation by arbitrary two-dimensional topography

Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. To date, analytical models of internal tide generation by two-dimensional ridges have considered only idealized sha...

متن کامل

Long-term variability in the solar diurnal tide observed by HRDI and simulated by the GSWM

Observations of the mesosphere and lower thermosphere winds obtained by the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS) during 1991 to 1995 reveal a semiannual variation in the amplitude of the (1,1) diurnal tide. The global-scale wave model (GSWM) represents the first numerical modeling attempt at simulating this seasonal variability, and a prelimina...

متن کامل

a numerical study of internal tide generation due to interaction of barotropic tide with bottom topography in the oman gulf

a major part of tidal energy is usually dissipated by the interaction of tidal currents with bottom topography. gulf of oman is a marginal sea which has variable topography and its dominant tidal constituent is m2 semi-diurnal tide. in this paper, the interaction of barotropic tidal current with bottom topography is evaluated. this phenomenon causes the formation of internal tide. internal tide...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: Journal of Physical Oceanography

سال: 2015

ISSN: 0022-3670,1520-0485

DOI: 10.1175/jpo-d-14-0228.1