1. Observation of Scintillation Enhancements and Large‐Scale Structures Within the Equatorial Ionization Anomaly During a Sudden Stratospheric Warming Event.
- Author
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Valladares, C. E., Chen, Y.‐J., Hairston, M., Chau, J. L., and Dhanya, R.
- Subjects
EQUATORIAL ionization anomaly ,QUASI-biennial oscillation (Meteorology) ,THERMOSPHERE ,MAGNETIC storms ,MERIDIONAL winds ,GPS receivers ,LUNAR phases - Abstract
Total electron content (TEC) and L‐band scintillations measured by several networks of GPS and GNSS receivers that operate in South and Central America and the Caribbean region are used to observe the morphology of the equatorial ionization anomaly (EIA), examine the evolution of plasma bubbles, and investigate the enhancement of L‐band scintillations that occurred on February 12 and 13, 2016. A few weak and short magnetic storms developed these days, and a minor sudden stratospheric warming (SSW) event was initiated a few days before. During these unusual conditions, TEC maps reported a split of the otherwise continuous crests of the EIA and the formation of a large‐scale (thousands of kilometers) almost‐circular structure. The western part of the southern crest faded, and a north‐south aligned segment developed near the center of the South American continent, joining the north and south crests of the EIA, forming an anomaly that resembled a closed loop on the eastern side of the continent. Concurrently with the anomaly events, several GPS stations reported increases in the L‐band scintillation index from 0.4 to values greater than 1. We analyzed TEC values from receivers between ±6° from the magnetic equator to identify and follow TEC depletions associated with plasma bubbles when they reach different stations. Although the magnetic activity was moderate (Kp = 3°), we believe that the anomaly redistribution and the scintillation enhancements are not related to a prompt penetration electric field but to enhancing the semidiurnal lunar tide propitiated by the onset of the minor SSW event. We found that depending on the lunar tide phase cycle, the neutral wind's meridional component can augment sub‐km scale irregularities and enhance L‐band scintillations through the wind gradient instability when U·∇ $\nabla $n < 0 or the action of wind gradients (∇ $\nabla $U) within the bubbles. Our observations imply that the SSW event enables prominent changes in the thermosphere wind system at F‐region altitudes. Plain Language Summary: GPS receivers can measure the total electron content (TEC) between the satellite and the ground receivers. We have used TEC data collected with several networks of GPS receivers in South America to construct maps of TEC over the continent. These maps are used to examine the variability of the low latitude ionosphere during a special event that originates in the northern polar stratosphere called sudden stratospheric warming (SSW), consisting of an increase in the local temperature. In February 2016, a minor SSW produced prominent changes in the equatorial ionization anomaly. The anomaly consists of a pattern of two regions of enhanced densities on both sides of the magnetic equator that develops during the daytime and early evening. A few days after the initiation of the SSW event, the low‐latitude ionosphere dynamics changed, forming a large‐scale structure resembling a closed loop on the continent's eastern side. Concurrently with the anomaly events, several GPS stations reported increases in the level of fadings of the GPS signal‐to‐noise ratio, a process called scintillation. It is indicated that the neutral wind meridional component developed shears and a reversal increasing the level of plasma irregularities at km and sub‐km‐scale lengths, originating a scintillation enhancement. Key Points: Sudden increases in L‐band scintillations coincide with changes in the geometry of the equatorial ionization anomalyThese events occurred on February 12 and 13, 2016, a few days after a minor sudden stratospheric warming eventThe analysis suggests that a meridional neutral wind associated with an increased lunar tide is responsible for anomaly variability [ABSTRACT FROM AUTHOR]
- Published
- 2023
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