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            <gco:CharacterString>The effects of solar wind driving conditions on the polar distribution of large-scale, nondispersive AlfvÃ©nic Poynting flux at low altitude during steady magnetosphere convections are studied using three-dimensional global simulations of the solar wind-magnetosphere-ionosphere interaction. Results from 18 test simulations driven by steady upstream solar wind (SW) and interplanetary magnetic field (IMF) conditions are used to investigate the relationship between SW/IMF driving and low-altitude signatures of large-scale AlfvÃ©nic Poynting flux. When the IMF is southward, the intensity of the AlfvÃ©nic Poynting flux increases, and the hemispheric integrated AlfvÃ©nic Poynting flux exhibits a linear relation with the SW electric field. When the IMF has a By component, the simulated hemispheric AlfvÃ©nic power does not fit to the same linear relation. During steady IMF By driving conditions, the low-altitude regions with enhanced AlfvÃ©nic Poynting flux are magnetically connected with magnetospheric dynamo regions on both open and closed field lines. The physical origin of low-altitude AlfvÃ©nic Poynting flux connecting to the closed field line region is similar with that during southward IMF Bz driving. However, the AlfvÃ©nic Poynting flux flowing from the open field line dynamo region may be related to the physical process on the magnetopause, and only shear-mode waves are generated.</gco:CharacterString>
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