Javascript must be enabled to continue!
The Importance of Atmospheric Modeling for Next-Generation Venus Mapping Missions
View through CrossRef
Upcoming Venus missions will feature a range of radar and multispectral instruments to image and map the surface, which is inaccessible to optical sensors due to the thick Venus atmosphere. Of these missions, the X-band VISAR synthetic aperture radar (SAR) instrument on the VERITAS spacecraft will be used to create a global, high-resolution Digital Elevation Map (DEM) with a posting of less than 250 m and a vertical accuracy of better than 10 m. How can the VERITAS mission achieve such performance if the Venus atmosphere, with its high pressure and temperature, introduces consequent apparent range delays to the radar measurements of several hundreds of meters, and only limited in-situ measurements of the deep atmosphere from earlier missions are available?Our answer to this problem is a Venus atmospheric model that combines available data on the atmospheric constituents with wave propagation physics of X-band signals under such conditions. Based on previous work by Duan et al. (2010), we have built a Python-based toolkit to compute the signal delay and attenuation for given atmospheric composition, refraction and absorption models, and instrument viewing geometries. We investigate using simulations how the mismodeling of the atmospheric parameters can lead to an inaccurate georegistration of the SAR imagery (based on work by Gisinger et al., 2015, 2017), which in turn would significantly degrade the quality of the derived DEMs.We perform our investigations on a global scale and over the entire VERITAS science phase of approx. 3 years, and compare our results with analytical expressions. We also show that the expected variability of temperature, pressure, and ionospheric density with latitude and solar time only plays a negligible role in the performance degradation. Finally, we aim to share our atmospheric modeling code with the community, such that we may incorporate improvements to the model, and to help sensitize future users of radar (or multispectral) data from the VERITAS, EnVision, or other missions, to the importance of atmospheric corrections.
Title: The Importance of Atmospheric Modeling for Next-Generation Venus Mapping Missions
Description:
Upcoming Venus missions will feature a range of radar and multispectral instruments to image and map the surface, which is inaccessible to optical sensors due to the thick Venus atmosphere.
Of these missions, the X-band VISAR synthetic aperture radar (SAR) instrument on the VERITAS spacecraft will be used to create a global, high-resolution Digital Elevation Map (DEM) with a posting of less than 250 m and a vertical accuracy of better than 10 m.
How can the VERITAS mission achieve such performance if the Venus atmosphere, with its high pressure and temperature, introduces consequent apparent range delays to the radar measurements of several hundreds of meters, and only limited in-situ measurements of the deep atmosphere from earlier missions are available?Our answer to this problem is a Venus atmospheric model that combines available data on the atmospheric constituents with wave propagation physics of X-band signals under such conditions.
Based on previous work by Duan et al.
(2010), we have built a Python-based toolkit to compute the signal delay and attenuation for given atmospheric composition, refraction and absorption models, and instrument viewing geometries.
We investigate using simulations how the mismodeling of the atmospheric parameters can lead to an inaccurate georegistration of the SAR imagery (based on work by Gisinger et al.
, 2015, 2017), which in turn would significantly degrade the quality of the derived DEMs.
We perform our investigations on a global scale and over the entire VERITAS science phase of approx.
3 years, and compare our results with analytical expressions.
We also show that the expected variability of temperature, pressure, and ionospheric density with latitude and solar time only plays a negligible role in the performance degradation.
Finally, we aim to share our atmospheric modeling code with the community, such that we may incorporate improvements to the model, and to help sensitize future users of radar (or multispectral) data from the VERITAS, EnVision, or other missions, to the importance of atmospheric corrections.
Related Results
Venus Atmospheric Dynamics: Akatsuki UVI and TNG HARPS-N observations
Venus Atmospheric Dynamics: Akatsuki UVI and TNG HARPS-N observations
<p>As the closest planet to Earth, it should be expected Venus to be the most Earth-like planet we know. Both Earth and Venus share almost the same radius, mass and d...
Analysis of lava flow features on Venus for radar sounder simulations
Analysis of lava flow features on Venus for radar sounder simulations
IntroductionPrevious missions to Venus depicted an environment dominated by volcanic landforms and hostile atmospheric conditions. The surface was imaged by the Magellan mission, a...
Giant Impacts on Venus
Giant Impacts on Venus
Venus is similar to Earth in terms of mass and size and is sometimes also referred to as "Earth's twin". Nevertheless, there are some significant differences between the two planet...
Giant Impacts on Venus 
Giant Impacts on Venus 
Venus is similar to Earth in terms of mass and size and is sometimes also referred to as “Earth’s twin”. Nevertheless, there are some significant diff...
The Case for a Mission to Return Cloud Particles from the Lower Atmosphere of Venus
The Case for a Mission to Return Cloud Particles from the Lower Atmosphere of Venus
<p>The possibility of life in the lower Venusian atmosphere has been given serious scientific consideration for many decades (Sagan, 1961; Cockell, 1999; Grinspoon, 1...
Exploring the Venusian Clouds: Dayside Atmospheric Gravity Waves with Akatsuki UVI instrument
Exploring the Venusian Clouds: Dayside Atmospheric Gravity Waves with Akatsuki UVI instrument
As our neighbouring world, Venus stands as a pivotal planet in the study of planetary evolution. Its dense atmosphere, mostly composed of carbon dioxide makes it a unique laborator...
Distribution and Variation of the Venusian Cloud-top Sulfur Dioxide Derived from Akatsuki UV Images
Distribution and Variation of the Venusian Cloud-top Sulfur Dioxide Derived from Akatsuki UV Images
IntroductionThe horizontal distribution of sulfuric acid clouds in the Venusian atmosphere is an essential factor that influences the solar energy absorbed by the planet. The cloud...
Single-image Shape and from Shading with Atmospheric Correction for Precise Topographic Reconstruction on Mars
Single-image Shape and from Shading with Atmospheric Correction for Precise Topographic Reconstruction on Mars
. Introduction Accurate and high-resolution digital elevation models (DEMs) are essential for Martian landing site selection and geological analysis [1]. However, existing photogra...

