研究目的
To observe the vertical fine structures and time evolution of plasma irregularities in the sporadic E (Es) layer using high-resolution Ca+ density measurements to understand the mechanisms behind these irregularities, such as Kelvin–Helmholtz instabilities and the role of Ca+ in Es layer formation.
研究成果
The high-resolution lidar observations revealed detailed fine structures in the Es layer, indicating Kelvin–Helmholtz instabilities and a strong correlation between Ca+ and electron densities. Ca+ plays a significant role in Es layer formation, and observed upward motions are likely due to strong horizontal winds rather than electric fields, though further wind measurements are needed for confirmation.
研究不足
The study relies on lidar and ionosonde data with specific resolutions; background wind measurements were not available, limiting the confirmation of mechanisms like neutral wind effects. The causal relationship with sunrise at the conjugate point remains unclear.
1:Experimental Design and Method Selection:
A resonance scattering lidar was used to measure Ca+ densities with high time-height resolution (5 s and 15 m) to observe fine structures in the Es layer. Ionosonde data were used for simultaneous electron density measurements.
2:Sample Selection and Data Sources:
Observations were conducted at Tachikawa (
3:7°N, 4°E) on December 24, 2014, from
09 to 21:26 UT. Ionosonde data from Kokubunji (35.7°N, 139.5°E) were used for correlation analysis.
4:7°N, 5°E) were used for correlation analysis. List of Experimental Equipment and Materials:
3. List of Experimental Equipment and Materials: Resonance scattering lidar with an injection-seeded alexandrite ring laser, SHG unit with BBO crystals, tunable diode laser, wavelength meter, Nasmyth-Cassegrain telescope, photomultiplier tube, band-pass filter, transient recorder. Ionosonde for electron density measurements.
5:Experimental Procedures and Operational Workflow:
The lidar transmitted laser pulses at 393.477 nm, detected photons with a PMT, recorded counts with 15 m range resolution and 5 s integration. Background noise was subtracted, and Ca+ densities were normalized using Rayleigh signals. Ionosonde ionograms were obtained every 15 min.
6:477 nm, detected photons with a PMT, recorded counts with 15 m range resolution and 5 s integration. Background noise was subtracted, and Ca+ densities were normalized using Rayleigh signals. Ionosonde ionograms were obtained every 15 min. Data Analysis Methods:
5. Data Analysis Methods: Correlation analysis between maximum Ca+ densities and electron densities from foEs, temporal and height variations were analyzed to identify structures like quasi-sinusoidal variations, clumps, and instabilities.
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Tunable diode laser
DL pro 780
Toptica
Used as a seed laser for tuning the laser wavelengths to resonance frequencies.
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Wavelength meter
WSU-10
HighFiness
To calibrate and tune the laser wavelengths.
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Photomultiplier tube
R9880U-210
Hamamatsu
To detect photons at 393.477 nm.
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Resonance scattering lidar
National Institute of Polar Research (NIPR)
To measure Ca+ densities with high time-height resolution for observing plasma irregularities in the Es layer.
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Injection-seeded alexandrite ring laser
Part of the lidar transmitter for generating laser pulses in the range 768–788 nm.
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Second harmonic generation unit
To generate second harmonic wavelengths for the lidar.
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He–Ne laser
Used for calibration of the wavelength meter.
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Nasmyth-Cassegrain telescope
Used as a receiver for the lidar to collect photons.
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Band-pass filter
To reduce background sky brightness by filtering light.
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Transient recorder
PR10-160-P
Licel
To record photon counts with specified range resolution and integration time.
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Ionosonde
National Institute of Information and Communications Technology (NICT)
To measure electron densities and Es layer parameters such as foEs and fbEs.
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