نتایج جستجو برای: layer baroclinically unstable midlatitude jet over a 30

تعداد نتایج: 13703768  

Journal: :Journal of Physical Oceanography 2021

Abstract The structure and variations of the North Equatorial Counter Current (NECC) in far western Pacific Ocean during 2014-2016 are investigated using repeated in-situ hydrographic data, altimeter Argo reanalysis data. NECC shifted ~1 degree southward intensified significantly with its transport exceeding 40 Sv (1 = 10 6 m 3 s -1 ), nearly double climatology value, developing phase 2015/16 E...

1995
Joseph Galewsky Richard K. Scott Lorenzo M. Polvani

An initial value problem for testing numerical models of the global shallow water equations is presented. This new test case is designed to address some of the difficulties that have recently been uncovered in the canonical test case suite of Williamson et al (1992). The new test case is simple to set up, yet able to generate a complex and realistic flow. The initial condition consists of an an...

A. R. Pishehvar and H. Ahmadi Kia,

In this study, the missile staging process by implementing a side-injected jet is simulated numerically. The problem is considered to be axisymmetric and the thin shear layer approximation of Navier-Stokes equations along with an algebraic turbulence model is used in a quasi-static form for the calculations. The free stream corresponds to a very high altitude flight condition with a Mach number...

2010
V. A. Sinclair S. L. Gray S. E. Belcher

[1] Midlatitude cyclones are important contributors to boundary layer ventilation. However, it is uncertain how efficient such systems are at transporting pollutants out of the boundary layer, and variations between cyclones are unexplained. In this study 15 idealized baroclinic life cycles, with a passive tracer included, are simulated to identify the relative importance of two transport proce...

پایان نامه :وزارت علوم، تحقیقات و فناوری - دانشگاه تحصیلات تکمیلی علوم پایه زنجان - دانشکده فیزیک 1392

in the first part of this thesis we explored wetting and its dynamics for small droplets. first, we showed how a simple feature of water droplets on a surface, i.e. laplace pressure, can be exploited to build a micropump. we investigated capillary pumping in microchannels both experimentally and numerically. putting two droplets of different sizes at the in/outlet of a microchannel, will ge...

1998
H. CHANSON

In the developing flow region of a plunging jet, the verynear field (i.e. (x-x1)/d1 < 5) is strongly affected by the entrapment process at the impingement. New quantitative results show that, although the distributions of void fraction and mean velocity have smooth shapes, the flow is highly fluctuating and unstable. At a given location in the mixing layer, the probability distribution function...

2012
Ian Grooms K. Shafer Smith Andrew J. Majda

5 Multiscale analysis is used to derive two sets of coupled models, each based on the same distinguished limit, to represent the interaction of the midlatitude oceanic synoptic scale — where coherent features such as jets and rings form — and the mesoscale, defined by the internal deformation scale. The synoptic scale and mesoscale overlap at low and mid latitudes, and are hence synonymous in m...

2010
JIAN LU GANG CHEN DARGAN M. W. FRIERSON

The sensitivity of the midlatitude storm track and eddy-driven wind to the sea surface temperature (SST) boundary forcing is studied over a wide range of perturbations using both simple and comprehensive general circulation models over aquaplanet lower boundary conditions. Under the single-jet circulation regime similar to the conditions of the present climate in the Northern Hemisphere winter ...

2003
R. T. WILLIAMS

The structure of barotropically unstable disturbances in the Tropics is studied with a two-level quasi-geostrophic model. An Ekman layer is attached to the lower boundary. The equations are linearized and the most unstable mode is found numerically by using the initial value technique. Computations are made for a shear-zone wind profile and a jet profile; these fields are independent of height....

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