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タイトル: | Energy flow exciting field-aligned current at substorm expansion onset |
著者: | Ebihara, Y. Tanaka, T. |
著者名の別形: | 海老原, 祐輔 |
キーワード: | substorm expansion onset MHD simulation convection |
発行日: | Dec-2017 |
出版者: | American Geophysical Union (AGU) |
誌名: | Journal of Geophysical Research: Space Physics |
巻: | 122 |
号: | 12 |
開始ページ: | 12,288 |
終了ページ: | 12,309 |
抄録: | At substorm expansion onset, upward field‐aligned currents (FACs) increase abruptly, and a large amount of electromagnetic energy starts to consume in the polar ionosphere. A question arises as to where the energy comes from. Based on the results obtained by the global magnetohydrodynamics simulation, we present energy flow and energy conversion associated with the upward FACs that manifest the onset. Our simulations show that the cusp/mantle region transmits electromagnetic energy to almost the entire region of the magnetosphere when the interplanetary magnetic field is southward. Integral curve of the Poynting flux shows a spiral moving toward the ionosphere, probably suggesting the pathway of electromagnetic energy from the cusp/mantle dynamo to the ionosphere. The near‐Earth reconnection initiates three‐dimensional redistribution of the magnetosphere. Flow shear in the near‐Earth region results in the generation of the near‐Earth dynamo and the onset FACs. The onset FACs are responsible to transport the electromagnetic energy toward the Earth. In the near‐Earth region, the electromagnetic energy coming from the cusp/mantle dynamo is converted to the kinetic energy (known as bursty bulk flow) and the thermal energy (associated with high‐pressure region in the inner magnetosphere). Then, they are converted to the electromagnetic energy associated with the onset FACs. A part of electromagnetic energy is stored in the lobe region during the growth phase. The release of the stored energy, together with the continuously supplied energy from the cusp/mantle dynamo, contributes to the energy supply to the ionosphere during the expansion phase. |
著作権等: | An edited version of this paper was published by AGU. Copyright 2017 American Geophysical Union. |
URI: | http://hdl.handle.net/2433/237230 |
DOI(出版社版): | 10.1002/2017JA024294 |
出現コレクション: | 学術雑誌掲載論文等 |

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