Shibata Kazunari, Nakamura Tahei, Matsumoto Takuma, Otsuji Kenichi, Okamoto Takenori J, Nishizuka Naoto, Kawate Tomoko, Watanabe Hiroko, Nagata Shin'ichi, Ueno Satoru, Kitai Reizaburo, Nozawa Satoshi, Tsuneta Saku, Suematsu Yoshinori, Ichimoto Kiyoshi, Shimizu Toshifumi, Katsukawa Yukio, Tarbell Theodore D, Berger Thomas E, Lites Bruce W, Shine Richard A, Title Alan M
Kwasan and Hida Observatories, Kyoto University, Yamashina, Kyoto 607-8471, Japan.
Science. 2007 Dec 7;318(5856):1591-4. doi: 10.1126/science.1146708.
The heating of the solar chromosphere and corona is a long-standing puzzle in solar physics. Hinode observations show the ubiquitous presence of chromospheric anemone jets outside sunspots in active regions. They are typically 3 to 7 arc seconds = 2000 to 5000 kilometers long and 0.2 to 0.4 arc second = 150 to 300 kilometers wide, and their velocity is 10 to 20 kilometers per second. These small jets have an inverted Y-shape, similar to the shape of x-ray anemone jets in the corona. These features imply that magnetic reconnection similar to that in the corona is occurring at a much smaller spatial scale throughout the chromosphere and suggest that the heating of the solar chromosphere and corona may be related to small-scale ubiquitous reconnection.
太阳色球层和日冕的加热是太阳物理学中一个长期存在的谜题。“日之出”卫星的观测显示,活动区黑子外普遍存在色球层海葵状喷流。它们通常长3至7角秒(相当于2000至5000千米),宽0.2至0.4角秒(相当于150至300千米),速度为每秒10至20千米。这些小喷流呈倒Y形,类似于日冕中的X射线海葵状喷流。这些特征表明,类似于日冕中的磁重联在色球层的整个区域以小得多的空间尺度发生,这表明太阳色球层和日冕的加热可能与普遍存在的小尺度重联有关。