“Sporadic–E (Es)” (90-125km) is a generic term used to describe thin (one to several km) ionization layers that are typically formed in E region ionosphere. The density within the Es layers is several factors to few orders of magnitude higher than the background ionosphere, and can sometimes get higher than the F-region densities. One can think of these layers as ‘clouds of enhanced ionization’. Similar to troposphere clouds, the Es clouds can be patchy puffs or a blanketing overcasting layer. These layers are generally believed to be a result of wind shears in the E-region ionosphere, but this mechanism is overly simplified and does not explain all the observed layer features. And despite decades of observations and modelling efforts of Es layers, there is a lack of complete understanding of Es layers and the role they play in E-F region coupling, especially at low latitudes. Degradation of RF communications and operational anomalies/failures during ionospheric disturbances are a crucial space weather influence on modern life. Es layers are the sole ubiquitous space weather source in the ionosphere that produce scintillations during nighttime and daytime; affecting operational RF transmissions such as HF, VHF and UHF communication links, as well as over the horizon radar and communications.
NASA SEED mission aims to do comprehensive measurements of the electrodynamics associated with Es layers observed at the low latitude location of Kwajalein Atoll in Marshall Islands. In particular, SEED aims to investigate density-temperature anti-correlations as shown below and reported by Barjatya et al . The figure below shows a unique double Es layer situation wherein the electron temperature heats up above and below an Es layer, but not within the layer. The bottom Es layer (107 km) is clearly located at a wind shear but the top layer seems to be associated with electric fields. We believe this is a result of field aligned currents and SEED aims to investigate this hypothesis.
SEED is a comprehensive experiment to address a series of specific but interlinked science questions related to the Es layer phenomena, especially high altitude (>100 km) Es layers, at low latitude location (Kwajalein) during solar-min. Progress on these 3 questions will also contribute to broader science goal of understanding the role of Es layers in ionosphere coupling:
1. Are low-latitude/equatorial Es layers associated with field aligned currents (FAC) of magnitude of 1 to 2 uA/m2 in the presence of a night time F region dynamo?
2. How do electric fields and winds modulate temperatures and conductivities in the E region via field aligned currents?
3. How do these field aligned currents (associated with a Sporadic E) themselves change over time throughthe modulation that they introduce in the electric field?
SEED mission will consist of two comprehensively instrumented rockets launched within 30 minutes of each other from Kwajalein Atoll in the Marshall Islands during the summer of 2022. Figure below presents a conceptual diagram of the payload with a conceptual layout for the proposed instrumentation (Note TMA payload that will separate along with rocket motor is not shown). The four booms under the nosecone will have a Sweeping Langmuir Probe (SLP), a Fast Temperature fixed bias Probes (FTP), multi-needle fixed bias DC Probes (mNLP), Positive Ion Probe (PIP), and a magnetometer from PNI Sensors Corp. Under the aft skirt will be four folding booms for the floating potential measurements (FPP), as well as the Billingsley Ultra Miniature Flight Magnetometer at the end of a boom. The two sets of 180 degree opposite FPP booms then consist of a typical double probe electric field measurement while each of the four also gives payload charging measurements.
The mission started in Summer 2019. It has been delayed due to scheduling issues and is currently slated to launch in Summer 2022. Expected Integration and Testing is at Wallops Flight Facility in Fall 2021.