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Venus surface and near surface anomalies on the Northern hemisphere observed by VIRTIS/VEX: First results

Arnold, Gabriele and Haus, Rainer and Kappel, David and Basilevsky, Alexander and Drossart, Pierre and Piccioni, Giuseppe (2009) Venus surface and near surface anomalies on the Northern hemisphere observed by VIRTIS/VEX: First results. In: Geophysical Research Abstracts, 11. EGU General Assembly 2009, 19.-24. Apr. 2010, Vienna, Austria.


Official URL: http://meetingorganizer.copernicus.org/EGU2009/EGU2009-7878.pdf


Venus nightside emission measurements of VIRTIS on Venus Express provide the opportunity of surface studies in the narrow near infrared atmospheric windows. The measurements as well as detailed new radiative transfer simulations show that radiance ratios in the emission windows between 1.0 and 1.35 micron with respect to the 1.02 micron window can be used to extract information about the surface elevation and temperature. Based on these analyses, first surface and near surface anomalies are identified on the Northern hemisphere of Venus, which are due to deviations of the elevation - temperature correlation in certain small areas. The data are selected from VIRTIS-M-IR nightside measurements. To ensure minimal atmospheric influence on the measured signatures, only pushbroom observations with small observation angles close to nadir are taken into account. The radiative transfer simulation technique considers absorption, emission, and multiple scattering by gaseous and particulate constituents of the atmosphere. Look-up tables of quasi-monochromatic gas absorption cross-sections are calculated using appropriate spectral line data bases and line profiles and a line-by-line procedure. Empirical continuum absorption coefficients are determined from a ’VIRTIS reference spectrum’. In order to derive the parameters of the H2SO4 clouds, Mie theory is applied. Multiple scattering is considered by a Successive Order procedure. The synthetic quasi-monochromatic intensity spectra at the model top level of the atmosphere are convolved with the VIRTIS spectral response function. The surface windows at 1.02, 1.10 and 1.18 micron exhibit a clear dependence of transmitted radiation on topographical features and, thus, on surface thermal emission, since an elevation change of 12 km results in a temperature change of 100 K. In the first approximation, the radiance ratios are affine linear functions of the surface temperature. This is demonstrated by both measurements and simulations. In general, the ratio-based VIRTIS topography correlates well with the Magellan topography, but differences occur in localized areas. Different local surface anomalies do exist. These anomalies are probably a result of the lower atmosphere dynamics, errors in Magellan elevation determinations, or variations in the surface emissivity. Surface emissivity variations are important indicators of the nature of surface material. They may be due to variations in mineralogy and surface texture. While most of Venus’ geologic units are thought to be basaltic in composition, some of them (tessera terrains) could be felsic. The 1 micron emissivity of felsic materials is lower compared to basalts at similar texture conditions. Nevertheless, we found that anomalous areas comprise practically the same geologic units as adjacent non-anomalous terrains. The surface texture (grain size, packing density, surface roughness) is another important factor for emissivity anomalies. Grain size affects the spectral characteristics. Laboratory measurements of basalts and oxidized basalts show significant changes in the contrast of the 1 micron reflectivity band. Although most of the surface of Venus is not very rough, roughness variations exist. Tesserae and rifts show a higher surface roughness compared to other areas. Finally, the Magellan radar data that represent the base of the topography information of the Venus surface result from a surface layer of about 1 m in thickness, whereas the VIRTIS-NIR data describe the optical upper surface layer only. The radiative transfer simulations show the capability of our algorithm to investigate the surface of Venus. Based on these simulations and the VIRTIS/VEX measurements, the extracted anomalies are discussed in the framework of these processes and influences mentioned above. Future improvements will contribute to eliminate the masking of the Venus nightside windows by far wing and pressure-induced absorptions of the deep atmosphere constituents. This will allow a better separation of deep atmosphere, temperature, and emissivity contributions to the Venus nightside emission.

Item URL in elib:https://elib.dlr.de/68403/
Document Type:Conference or Workshop Item (Speech)
Title:Venus surface and near surface anomalies on the Northern hemisphere observed by VIRTIS/VEX: First results
AuthorsInstitution or Email of AuthorsAuthors ORCID iD
Arnold, GabrieleGabriele.Arnold (at) dlr.deUNSPECIFIED
Haus, RainerWestfälische Wilhelms-Universität MünsterUNSPECIFIED
Kappel, DavidWestfälische Wilhelms-Universität MünsterUNSPECIFIED
Basilevsky, AlexanderVernadsky Institute, Moscow, RussiaUNSPECIFIED
Drossart, PierreLESIA, Observatoire de Paris, FranceUNSPECIFIED
Piccioni, GiuseppeINAF-IASF, ItalyUNSPECIFIED
Date:23 April 2009
Journal or Publication Title:Geophysical Research Abstracts
Refereed publication:No
Open Access:Yes
Gold Open Access:No
In ISI Web of Science:No
Keywords:VIRTIS, VEX, Venus, retrieval, surface, anomalies
Event Title:EGU General Assembly 2009
Event Location:Vienna, Austria
Event Type:international Conference
Event Dates:19.-24. Apr. 2010
Organizer:European Geosciences Union
HGF - Research field:Aeronautics, Space and Transport (old)
HGF - Program:Space (old)
HGF - Program Themes:W EW - Erforschung des Weltraums
DLR - Research area:Space
DLR - Program:W EW - Erforschung des Weltraums
DLR - Research theme (Project):W - Vorhaben Venus Express (old)
Location: Berlin-Adlershof
Institutes and Institutions:Institute of Planetary Research > Planetary Physics
Deposited By: Kappel, David
Deposited On:13 Jan 2011 14:19
Last Modified:31 Jul 2019 19:31

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