نتایج جستجو برای: troposphere interaction

تعداد نتایج: 570676  

2013
Adam A. Scaife Thomas Spangehl David R. Fereday Ulrich Cubasch Ulrike Langematz Hideharu Akiyoshi Slimane Bekki Peter Braesicke Neal Butchart Martyn P. Chipperfield Andrew Gettelman Steven C. Hardiman Martine Michou Eugene Rozanov Theodore G. Shepherd

2002
David Rind Jean Lerner Judith Perlwitz Chris McLinden Michael Prather

[1] Two sets of sea surface temperature/sea ice changes are used to test the sensitivity of tracer transport to the pattern of warming in the doubled CO2 climate. One set (2CO2WT) has greater tropical and high latitude sea surface temperature changes than the other (2CO2), although both fall within the range of plausible response. Simulations were done both with and without interactive ozone. R...

پایان نامه :وزارت علوم، تحقیقات و فناوری - دانشگاه یاسوج - دانشکده ادبیات و علوم انسانی 1392

an investigation into oral interaction in language classes: a conversation analytic point of view the aim of this thesis is to analyze the interaction between language teachers and students in english language institutes. this work is done in the context of yasuj city. learning another language, which is in most cases english, involves many variables. one of these variables is the linguistic...

2002
R. Alan Plumb Kirill Semeniuk

We show (in confirmation of previous work) using oneand three-dimensional models that extratropical zonal wind anomalies, produced by fluctuating Rossby wave forcing in the troposphere, appear first in the stratosphere, and migrate downward into the troposphere. By systematically eliminating wave reflection and “downward control” through an induced meridional circulation, it is shown that the d...

2004
Joseph A. Biello JOSEPH A. BIELLO ANDREW J. MAJDA

Two-layer equatorial primitive equations for the free troposphere in the presence of a thin atmospheric boundary layer and thermal dissipation are developed here. An asymptotic theory for the resonant nonlinear interaction of long equatorial baroclinic and barotropic Rossby waves is derived in the presence of such dissipation. In this model, a self-consistent asymptotic derivation establishes t...

Journal: :Chemosphere 2002
V Grewe C Reithmeier D T Shindell

The importance of the interaction between chemistry and dynamics in the upper troposphere and lower stratosphere for chemical species like ozone is investigated using two chemistry-climate models and a Lagrangian trajectory model. Air parcels from the upper troposphere, i.e. regions of lightning and aircraft emissions, are able to be transported into the lowermost stratosphere (LMS). Trajectory...

1967
TAKASHI NITTA

The vertical flux of geopotential and the conversion between eddy available potential and eddy kinetic energy due t o non-stationary disturbances are studied by solving numerically the diagnostic as well as the prognostic equations of a linearized 20-level model. The vertical distribution of these quantities thus computed compares well with those obtained by other authors from observed data and...

In this study, the interaction between atmosphere and earth surface and its effect on the simulation of Sistan wind structure in the East of Iranian plateau is investigated. For this purpose, four experiments have been carried out with RegCM4, with horizontal resolution of 20 km. In non-topography experiments, the model was implemented in three different conditions. The results indicated that t...

2009
Hong-Li Ren Fei-Fei Jin Jong-Seong Kug Li Gao Jin L. Gao

Interaction between synoptic eddy and lowfrequency flow (SELF) has been the subject of many studies. In this study, we further examine the interaction by introducing a transformed eddy-potential-vorticity (TEPV) flux that is obtained from eddy-potential-vorticity flux through a quasi-geostrophic potential-vorticity inversion. The main advantage of using the TEPV flux is that it combines the eff...

2012
Daniela I.V. Domeisen Alan Plumb Robert D. van der Hilst

The stratosphere and the troposphere exhibit a strong coupling during the winter months. However, the coupling mechanisms between the respective vertical layers are not fully understood. An idealized spectral core dynamical model is utilized in the present study in order to clarify the coupling timing, location and mechanisms. Since the coupling between the winter stratosphere and troposphere i...

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