Granulation and Convectional Driving on Stellar Surfaces

Johannes Tschernitz and Philippe-A. Bourdin
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Abstract

Surface convection is important for the presence of magnetic activity at stars. So far, this convection is thought to be a result of heating from below, where convection cells rise and break up. New models reveal that surface convection is instead strongly driven by cooling from above. We compare two simulations of surface convection, one with a significant heating from below and one without. We obtain surface convection in both cases, and they show similar granulation patterns. The deep convection driven by heating from below is still evolving and asymptotically approaches a steady-state solution. We find that convection from below is not needed at all to form typical photospheric granulation. This indicates the possibility of a surface dynamo acting on stars without a convecting envelope. Even stars without a convecting envelope could therefore exhibit stronger magnetic and coronal activity than expected so far.
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恒星表面的粒化和对流驱动
表面对流对恒星磁活动的存在很重要。到目前为止,这种对流被认为是来自地下加热的结果,在那里对流细胞上升和分裂。新的模式显示,表面对流是由上方的冷却所强烈驱动的。我们比较了两种地表对流的模拟,一种有明显的从下面加热,另一种没有。我们在两种情况下都获得了表面对流,它们显示出相似的造粒模式。由下层加热驱动的深层对流仍在演化,并渐近于稳态解。我们发现,形成典型的光球颗粒根本不需要来自下面的对流。这表明了表面发电机作用于没有对流包层的恒星的可能性。因此,即使没有对流包层的恒星也会表现出比目前预期更强的磁场和日冕活动。
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