Coordinated Ground‐Based and Space‐Based Observations of Equatorial Plasma Bubbles

Author:

Aa Ercha12,Zou Shasha1,Eastes Richard3,Karan Deepak K.3,Zhang Shun‐Rong2,Erickson Philip J.2,Coster Anthea J.2

Affiliation:

1. Department of Climate and Space Sciences and Engineering University of Michigan Ann Arbor MI USA

2. Haystack Observatory Massachusetts Institute of Technology Westford MA USA

3. Laboratory for Atmospheric and Space Physics University of Colorado Boulder Boulder CO USA

Abstract

AbstractThis paper presents coordinated and fortuitous ground‐based and spaceborne observations of equatorial plasma bubbles (EPBs) over the South American area on 24 October 2018, combining the following measurements: Global‐scale Observations of Limb and Disk far ultraviolet emission images, Global Navigation Satellite System total electron content data, Swarm in situ plasma density observations, ionosonde virtual height and drift data, and cloud brightness temperature data. The new observations from the Global‐scale Observations of Limb and Disk/ultraviolet imaging spectrograph taken at geostationary orbit provide a unique opportunity to image the evolution of plasma bubbles near the peak height over a large geographic area from a fixed longitude location. The combined multi‐instrument measurements provide a more integrated and comprehensive way to study the morphological structure, development, and seeding mechanism of EPBs. The main results of this study are as follows: (1) The bubbles developed a westward tilted structure with 10–15° inclination relative to the local geomagnetic field lines, with eastward drift velocity of 80–120 m/s near the magnetic equator that gradually decreased with increasing altitude/latitude. (2) Wave‐like oscillations in the bottomside layer and detrended total electron content were observed, which are probably due to upward propagating atmospheric gravity waves. The wavelength based on the medium‐scale traveling ionospheric disturbance signature was consistent with the interbubble distance of 500–800 km. (3) The atmospheric gravity waves that originated from tropospheric convective zone are likely to play an important role in seeding the development of this equatorial EPBs event.

Publisher

American Geophysical Union (AGU)

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