No.189
1996.12

<研究紹介>   ISASニュース 1996.12 No.189

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Yohkoh and the Physical Origins of "Space Weather"

   Hugh S. Hudson


 The solar wind comes from the hot corona of the Sun and continually blows past the Earth. This "wind" (a flow in a collisionless plasma, not in an ordinary gas!) contains irregular structures, some of them big enough and energetic enough to cause strong perturbations of the Earth's own plasma environment, or even to create spectacular effects at the here on the surface of the Earth such as the aurora borealis and strong Earth currents.
 This article describes briefly how we are using data from Yohkoh to understand the solar origin of these solar-wind structures. This is important for several reasons - for the sake of the physics itself; for the practical purpose of understanding better how to predict terrestrial effects; and as a generalization of the solar example to the stars and possibly beyond. The human side of these phenomena is now commonly termed "space weather".
 Yohkoh was launched five years ago and we've just had an international conference to celebrate that fact. But the data continue to amaze us, and in 1996 Yohkoh has made some remarkable observations. Figure 1 shows a solar active region, with large sunspots, that appeared unexpectedly at the bottom of the sunspot cycle as recently as last July. It produced (or participated in) the events discussed below.


 Figure 1. Four Yohkoh images of the Sun from different rotations, each centered on the longitude of the huge active complex and sunspot group of 1996. The upper right shows its birth, and the lower right shows its configuration after the coronal mass ejection of September 25. This and the other illustrations here have reversed colors for clarity.


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◆How Yohkoh helps

 Readers of the ISAS News generally know Yohkoh well, and have seen many of its nice soft X-ray images of the solar corona. I'd like to explain briefly, though, why the images are important in this particular context. The reason is simple: instead of individual pictures, Yohkoh gives us enough telemetered data to make a "data cube" (two space dimensions plus one time dimension), which we can then view as a movie. In this movie we see large-scale and small-scale motions that we can now begin to associate authoritatively with solar-wind structures.
 The Yohkoh soft X-ray images have a mean photon energy of about 1 keV(a mean wavelength of about 10 A). This is the characteristic energy of radiation from a plasma in the range 1-3 MK. The solar coronal plasma is collisional, so that the particle populations Yohkoh senses remotely are thermal and have basically Maxwellian velocity distributions. The coronal magnetic field is strong, and this fact is responsible for the clear tendency of the images to break up into magnetic loops, which are "closed" in the sense that both ends of a loop return directly to the solar photosphere. But - and this is where the physics begins to get really interesting - neither the collisionality nor the magnetic dominance ("low beta") can be taken for granted. It may be that local or global departures from these conditions have major effects.
 For a glance at a Yohkoh image, please refer to the following World-Wide Web access points:
 http://www.solar.isas.jaxa.jp/
or
 http://www.space.lockheed.com/SXT/homepage.html.
 Figure 1 shows some images from 1996, showing the spectacular complex of activity that curiously appeared at our current minimum phase of the sunspot cycle.
 Of course Yohkoh is important for "space weather", since phenomena causing terrestrial effects begin at the Sun and direct solar observations give the longest possible forecast interval. Until 1996, however, the connection between what Yohkoh sees and what appears at the Earth has been uncertain. Now, because of SOHO and other spacecraft, the situation is changing rapidly.


◆Hot news about Yohkoh and CMEs

 A "coronal mass ejection" (CME) is the largest and most spectacular of the coronal disturbances that affect the solar wind. In a single such event, a coronal mass roughly equal to that of a large comet blows out into the solar wind and is lost to the corona forever, becoming part of the heliosphere. The magnetic field in such a cloud stretches out to the extent that the field lines become "open" in the sense of not closing directly back into the photosphere directly. Such events are detected by white-light coronagraphs, which sense the mass by using the scattering of sunlight off the electrons in the ejection. This is a direct determination of the existence of ejected mass, and the resulting images can be extremely beautiful (for example, Figure 2 shows the first major CME detected by the LASCO coronagraph on SOHO).

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 Figure 2. An example of a coronal mass ejection observed by the LASCO instrument on SOHO (January 15, 1996). The big bubble to the right is a classical CME structure, but quite interestingly these data show a jet-like ejection into the heliospheric neutral sheet to the left as well. The scale can be judged from the inset size of the Sun.

 A coronagraph is not the only way (nor even the best way) to detect a CME - their effects can be studied with in-situ observations by interplanetary spacecraft (GEOTAIL, WIND, SOHO...). They can be studied at the Sun during the process of eruption by Yohkoh (and now also by SOHO). The Yohkoh results are new and I will describe some of them here for the first time anywhere - from very recent data.
 The big news is that, as of late September, Yohkoh has succeeded at last in directly observing solar events that could verifiably be identified as coronal mass ejections. This means that we can begin to study the very initial motions of the matter as it begins to leave the Sun, and to understand the mechanism that drives it outwards.
 The event that occurred on October 5 is illustrated in Figure 3. It shows a complicated magnetic structure that evolves interestingly in time, and it shows "dimming". Dimming means that the X-ray corona becomes fainter with time, with the natural explanation that the disappearing mass actually becomes the source material for the coronal mass ejection.


 Figure 3. The Yohkoh observations of a CME on October 5, also well-observed by SOHO. The coronal brightness at upper right decreases with time, the dimming effect of the actual mass ejection, which the SOHO observations showed preferentially in the north. At this time the active region was two days beyond the solar southwest limb. The detailed evolution of the filamentary structures will provide us with interesting insights into the magnetohydrodynamics of the solar corona.


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◆Conclusion

 We are currently analyzing the September and October CME events. By a rare coincidence, S. Watari (a CME specialist from the Communications Research Laboratory, Koganei) was actually serving as tohban at Uchinoura during the October 5 event. Even more remarkably, K. Shibata(an MHD specialist from NAO, Mitaka) was tohban during the remarkable event of April 14, 1994; this was certainly a CME launcher (although no coronagraph could observe it) because of the magnetic storm that resulted on the Earth. Thanks to Shibata-san's alertness, there was actually a direct warning about the arrival of the CME (usually 1-3 days en route from the Sun to the Earth) in this case. We hope that Yohkoh will show how to make this type of warning more routine, and at the same time we hope that it will provide the knowledge needed to understand the mysteries remaining in CME launching, flare occurrence, and the other solar participants in "space weather".



(ヒュー・S・ハドソン,ハワイ大学)


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