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NUMERICAL EXPERIMENTS IN SYMMETRIC AND ASYMMETRIC MOTIONS IN THE BAROTROPIC PRIMITIVE EQUATION MODEL ATMOSPHERE
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作者 余海安 廖洞贤 《Acta meteorologica Sinica》 SCIE 1991年第4期465-472,共8页
Three numerical experiments have been carried out by using a spectral barotropic primitive equation mo- del.It is found that the results obtained are quite similar to those with the barotropic filtered model.The main ... Three numerical experiments have been carried out by using a spectral barotropic primitive equation mo- del.It is found that the results obtained are quite similar to those with the barotropic filtered model.The main results read as follows: (1)In the case with symmetric orography or without orography,if the motion is symmetric(with re- spect to the equator,the same is true hereafter)at the initial instant,then it would be symmetric afterwards. (2)The antisymmetric orography distribution could cause antisymmetric motion,and the original sym- metric motion might become asymmetric. In order to explain the above results,it has been proved that they are theoretically valid.And it is found that if the motion is antisymmetric at the initial instant,then it would become asymmetric.Therefore,no pure antisymmetric motion could be maintained. 展开更多
关键词 symmetric motion asymmetric motion OROGRAPHY numerical experiment
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Tectonically asymmetric Earth:From net rotation to polarized westward drift of the lithosphere 被引量:5
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作者 Carlo Doglioni Eugenio Carminati +3 位作者 Mattia Crespi Marco Cuffaro Mattia Penati Federica Riguzzi 《Geoscience Frontiers》 SCIE CAS CSCD 2015年第3期401-418,共18页
The possibility of a net rotation of the lithosphere with respect to the mantle is generally overlooked since it depends on the adopted mantle reference frames, which are arbitrary. We review the geological and geophy... The possibility of a net rotation of the lithosphere with respect to the mantle is generally overlooked since it depends on the adopted mantle reference frames, which are arbitrary. We review the geological and geophysical signatures of plate boundaries, and show that they are markedly asymmetric worldwide. Then we compare available reference frames of plate motions relative to the mantle and discuss which is at best able to fit global tectonic data. Different assumptions about the depths of hotspot sources (below or within the asthenosphere, which decouples the lithosphere from the deep mantle) predict different rates of net rotation of the lithosphere relative to the mantle. The widely used no-net-rotation (NNR) reference frame, and low (〈0.2°-0.4°/Ma) net rotation rates (deep hotspots source) predict an average net rotation in which some plates move eastward relative to the mantle (e.g., Nazca). With fast (〉1°/Ma) net rotation (shallow hotspots source), all plates, albeit at different velocity, move westerly along a curved trajectory, with a tectonic equator tilted about 30° relative to the geographic equator. This is consistent with the observed global tectonic asymmetries. 展开更多
关键词 asymmetric plate tectonics Plate motions Westward drift Mantle convection
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Aerodynamic Performance of a Flapping Foil with Asymmetric Heaving Motion near a Wall 被引量:2
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作者 Xingjian Lin Shuhao Guo +1 位作者 Jie Wu Jingwen Nan 《Journal of Bionic Engineering》 SCIE EI CSCD 2018年第4期636-646,共11页
The effect of asymmetric heaving motion on the aerodynamic performance of a two-dimensional flapping foil near a wall is studied numerically. The foil executes the heaving and pitching motion simultaneously. When the ... The effect of asymmetric heaving motion on the aerodynamic performance of a two-dimensional flapping foil near a wall is studied numerically. The foil executes the heaving and pitching motion simultaneously. When the heaving motion is symmetric, the mean thrust coefficient monotonically increases with the decrease in mean distance between foil and wall. Meanwhile, the mean lift coefficient first increases and then decreases sharply. In addition, the negative mean lift coefficient appears when the foil is very close to the wall. After the introduction of asymmetric heaving motion, the influence of wall effect on the force behavior becomes complicated. The mean thrust coefficient is enhanced when the duration of upstroke is reduced. Moreover, more and more enhancement can be achieved when the foil approaches the wall gradually. On the other hand, the positive mean lift coefficient can be observed when the duration of downstroke is shortened. By checking the flow patterns around the foil, it is shown that the interaction between the vortex shed from the foil and the wall can greatly modify the pressure distribution along the foil surface. The results obtained here might be utilized to optimize the kinematics of the Micro Aerial Vehicles (MAVs) flying near a solid wall. 展开更多
关键词 asymmetric heaving motion wall effect thrust enhancement positive mean lift
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