Field‐Aligned Currents Associated With Pulsating Auroral Patches: Observation With Magneto‐Impedance Magnetometer (MIM) Onboard Loss Through Auroral Microburst Pulsations (LAMP) Sounding Rocket

Author:

Nosé Masahito12ORCID,Hosokawa Keisuke3ORCID,Nomura Reiko4ORCID,Teramoto Mariko5ORCID,Asamura Kazushi4ORCID,Miyoshi Yoshizumi2ORCID,Mitani Takefumi4ORCID,Sakanoi Takeshi6ORCID,Namekawa Taku7ORCID,Kawano Takeshi8,Iwanaga Yoshihiro8,Tatematsu Shunichi8,Hirahara Masafumi2ORCID,Halford Alexa9ORCID,Shumko Mykhaylo10ORCID,Lessard Marc R.11ORCID,Lynch Kristina12ORCID,Paschalidis Nicholaos9ORCID,Jaynes Allison N.13ORCID,McHarg Matthew G.14

Affiliation:

1. School of Data Science Nagoya City University Nagoya Japan

2. Institute for Space‐Earth Environmental Research Nagoya University Nagoya Japan

3. The University of Electro‐Communications Chofu Japan

4. Institute of Space and Astronautical Science Japan Aerospace Exploration Agency Chuo‐ku Japan

5. Kyushu Institute of Technology Kita‐kyushu Japan

6. Tohoku University Sendai Japan

7. National Institute of Information and Communications Technology Tokyo Japan

8. Aichi Steel Corporation Tokai Japan

9. NASA Goddard Space Flight Center Nagoya Japan

10. University of Maryland College Park MD USA

11. University of New Hampshire Durham NH USA

12. Dartmouth College Hanover NH USA

13. University of Iowa Iowa City IA USA

14. US Air Force Academy Colorado Springs CO USA

Abstract

AbstractWe made observations of magnetic field variations in association with pulsating auroras with the magneto‐impedance sensor magnetometer (MIM) carried by the Loss through Auroral Microburst Pulsations (LAMP) sounding rocket that was launched at 11:27:30 UT on 5 March 2022 from Poker Flat Research Range, Alaska. At an altitude of 200–250 km, MIM detected clear enhancements of the magnetic field by 15–25 nT in both the northward and westward components. From simultaneous observations with the ground all‐sky camera, we found that the footprint of LAMP at the 100 km altitude was located near the center of a pulsating auroral patch. The auroral patch had a dimension of ∼90 km in latitude and ∼25 km in longitude, and its major axis was inclined toward northwest. These observations were compared with results of a simple model calculation, in which local electron precipitation into the thin‐layer ionosphere causes an elliptical auroral patch. The conductivity within the patch is enhanced in the background electric field and as a result, the magnetic field variations are induced around the auroral patch. The model calculation results can explain the MIM observations if the electric field points toward southeast and one of the model parameters is adjusted. We conclude that the pulsating auroral patch in this event was associated with a one‐pair field‐aligned current that consists of downward (upward) currents at the poleward (equatorward) edge of the patch. This current structure is maintained even if the auroral patch is latitudinally elongated.

Funder

Japan Society for the Promotion of Science

Yamada Science Foundation

Publisher

American Geophysical Union (AGU)

Reference30 articles.

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2. Swarm observations of field‐aligned currents associated with pulsating auroral patches

3. Observations and modeling of correlated Pi B magnetic and auroral luminosity pulsations

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