Abstract:[1] A model of Venus' atmosphere permittivity profile up to 300 km is developed in this paper for X band. The model includes both the real and imaginary parts of the atmospheric permittivity, derived using data sets inferred or directly measured from past exploration missions to Venus: the real part is obtained by calculating the total polarization of the mixture of the atmospheric components including CO 2 , N 2 , H 2 O, SO 2 , H 2 SO 4 , CO, etc.; the imaginary part is derived using the superposition of the … Show more
“…One-way absorption through the atmosphere of Venus at the sub-Earth point is ∼5.62 dB at X band [51], which effectively decreases our signal-to-noise ratio by a factor of ∼10 compared to that of a hypothetical atmosphereless Venus.…”
“…One-way absorption through the atmosphere of Venus at the sub-Earth point is ∼5.62 dB at X band [51], which effectively decreases our signal-to-noise ratio by a factor of ∼10 compared to that of a hypothetical atmosphereless Venus.…”
“…As high physical perpendicular baseline to critical baseline ratios have a detrimental effect on InSAR correlation, we believe that longer radar wavelengths are optimal for our lava detection method. Longer radar wavelengths also travel more easily through Venus' atmosphere, reducing the impact of attenuation on the signal to noise of the correlation signal (Duan et al., 2010; Meyer & Sandwell, 2012). A higher radar bandwidth also linearly increases the length of the critical baseline, however higher bandwidth radar produces a higher volume of data, requiring the satellite to have a faster data downlink.…”
We explore the potential for repeat‐pass SAR Interferometry (InSAR) correlation to track volcanic activity on Venus' surface motivated by future SAR missions to Earth's sister planet. We use Hawai'i as a natural laboratory to test whether InSAR can detect lava flows assuming orbital and instrument parameters similar to that of a Venus mission. Hawai'i was chosen because lava flows are frequent, and well documented by the United States Geological Survey, and because Hawai'i is a SAR supersite, where space agencies have offered open radar data sets for analysis. These data sets have different wavelengths (L, C, and X bands), bandwidths, polarizations, look angles, and a variety of orbital baselines, giving opportunity to assess the suitability of parameters for detecting lava flows. We analyze data from ALOS‐2 (L‐band), Sentinel‐1 (C‐band), and COSMO‐SkyMed (X‐band) spanning 2018 and 2022. We perform SAR amplitude and InSAR correlation analysis over temporal baselines and perpendicular baselines similar to those of a Venus mission. Fresh lava flows create a sharp, noticeable decrease in InSAR correlation that persists indefinitely for images spanning the event. The same lava flows are not always visible in the corresponding amplitude images. Moreover, noticeable decorrelation persists in image pairs acquired months after the events due to post‐emplacement contraction of flows. Post‐emplacement effects are hypothesized to last longer on the Venusian surface, increasing the likelihood of detecting Venus lava flows using InSAR. We argue for further focus on repeat‐pass InSAR capabilities in upcoming Venus missions, to detect and quantify volcanic activity on Earth's hotter twin.
“…The base dielectric permittivities of analyzed gases in this work were taken as those of DC values which is valid for nonpolar gases due to the absence of the gas transitions in MW range. [ 40 ] Permittivity values of the pure gas phases at ambient pressure were obtained from [ 41,42 ] and are listed in Table S1, Supporting Information. Quadrupole moment values for gases were taken from Reference [ 43 ] .…”
Permittivity sensing is a critically important analytical tool for bioscience, environmental, and industrial applications. The response time for commonly used plasmonic permittivity sensors is fundamentally set by the reaction kinetics of chemically adsorbed analytes. In this work, the proposal is to overcome this limit by combining plasmonic sensors with phase transition materials possessing a rapid amplified electrostatic response such as quadrupole moment induced molecular helix reversal. As a proof‐of‐concept, rapid sensing of CO2 on a phase transition polytetrafluoroethylene substrate and amplification of permittivity response in plasmonic Fabry–Perot sensor is shown. The demonstrated universal approach holds promise for a wide range of applications in fast, real time sensing and monitoring of biological and environmental processes.
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