4.7 Article

STATISTICAL STUDY OF CHROMOSPHERIC ANEMONE JETS OBSERVED WITH HINODE/SOT

Journal

ASTROPHYSICAL JOURNAL
Volume 731, Issue 1, Pages -

Publisher

IOP PUBLISHING LTD
DOI: 10.1088/0004-637X/731/1/43

Keywords

magnetic fields; magnetic reconnection; magnetohydrodynamics (MHD); plasmas; Sun: activity; Sun: chromosphere

Funding

  1. Ministry of Education, Culture, Sports, Science, and Technology (MEXT) of Japan

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The Solar Optical Telescope on board Hinode has revealed numerous tiny jets in all regions of the chromosphere outside of sunspots. A typical chromospheric anemone jet has a cusp-shaped structure and bright footpoint, similar to the shape of an X-ray anemone jet observed previously with the Soft X-ray Telescope on board Yohkoh. The similarity in the shapes of chromospheric and X-ray anemone jets suggests that chromospheric anemone jets are produced as a result of the magnetic reconnection between a small bipole (perhaps a tiny emerging flux) and a pre-existing uniform magnetic field in the lower chromosphere. We examine various chromospheric anemone jets in the solar active region near the solar limb and study the typical features (e. g., length, width, lifetime, and velocity) of the chromospheric anemone jets. Statistical studies show that chromospheric anemone jets have: (1) a typical length similar to 1.0-4.0 Mm, (2) a width similar to 100-400 km, (3) a lifetime similar to 100-500 s, and (4) a velocity similar to 5-20 km s(-1). The velocity of the chromospheric anemone jets is comparable to the local Alfven speed in the lower solar chromosphere (similar to 10 km s(-1)). The histograms of chromospheric anemone jets near the limb and near the disk center show similar averages and shapes of distributions, suggesting that the characteristic behavior of chromospheric anemone jets is independent of whether they are observed on the disk or at the limb. The observed relationship between the velocity and length of chromospheric anemone jets shows that the jets do not follow ballistic motion but are more likely accelerated by some other mechanism. This is consistent with numerical simulations of chromospheric anemone jets.

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