Research Highlights

Nicholas Pedatella discusses strong, unexplained echoes returning from altitudes of 130–170 km in the atmosphere; how all radars work by reflecting radio waves off a target and measuring the returned signal. This region (130–170 km) in the upper atmosphere is likely to create and maintain a specific set of plasma waves that act as a coherent structure for radar measurements. 

Y. Zhang, L. Paxton, C. Huang, and W. Wang, observe that the 135.6 nm radiances clearly showed a signature of ionospheric equatorial arcs and their variations during the November 2004 magnetic superstorm. When an intense eastward Interplanetary Electric Field (IEF) occurred, the dayside equatorial arcs were enhanced and their latitude separation increased.

Tingting Yu, Wenbin Wang, Zhipeng Ren, and Jia Yue use TIMED/GUVI limb measurements of FUV airglow emission to investigate thermospheric composition and temperature responses to the 20-21 November 2003 (day of year (DOY) 324 and 325) superstorm. The storm-time composition and temperature responses were global and evolved continuously as the storm progressed.

A. Maute, A.D. Richmond, G. Lu, D. Knipp, Y. Shi, B. Anderson assert that the magnetosphere-ionosphere (MI) coupling is crucial in modeling the thermosphere-ionosphere (TI) response to geomagnetic activity. They introduce a new method  using observed FAC and solve for the interhemispherically asymmetric electric potential distribution. 

A.N. Afanasyev, M.D. Kazachenko, Y. Fan, G.H. Fisher, and B. Tremblay further validate the PDFI SS method, using approximately one–hour long MHD simulation data of magnetic flux emergence from the upper convection zone into the solar atmosphere. They reconstruct photo- spheric electric fields and calculate the Poynting flux, and compare those to the actual values from the simulations.

Kevin Pham, William Lotko, Roger Varney, Binzheng Zhang, Jing Liu have taken a key step in evaluating the importance of ionospheric outflows relative to electrodynamic coupling in the thermosphere’s impact on geospace dynamics.  Their simulation results identify a variety of observed magnetospheric features that are attributable directly to the thermosphere’s material influence.

Alin R. Paraschiv, Alina C. Donea, and Philip G. Judge present comprehensive observations of recurrent active region coronal jets, and derive their thermal and non-thermal properties. We discuss a peculiar penumbral magnetic reconnection site, which we previously identified as a "Coronal Geyser".

Qian Wu, Wenbin Wang, Dong Lin, Chaosong Huang, and Yongliang Zhang use the newly developed, Multiscale Atmosphere-Geospace Environment (MAGE) model to simulate the penetrating electric field in the equatorial region under different interplanetary magnetic field (IMF) BZ conditions during September 2020.

Dr. Nick Pedatella asserts that the advancement of whole atmosphere models has contributed to understanding the significant role terrestrial weather has on generating variability in the ionosphere-thermosphere.