Venus coordinated campaign: Difference between revisions
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[[Fichier:Akatsuki_instrumentation.gif|400px|thumb|right|Instrumentation of Akatsuki, Credit: JAXA]] | [[Fichier:Akatsuki_instrumentation.gif|400px|thumb|right|Instrumentation of Akatsuki, Credit: JAXA]] | ||
* IR1 | * IR1 | ||
1. | 1.01µm | ||
cloud (day-night), surface (nightside) | cloud (day-night), surface (nightside) | ||
* IR2 | * IR2 | ||
1.73, 2.26, 2.32 (near-IR) | 1.73, 2.26, 2.32 (near-IR) | ||
2.02 (CO2), 1. | 2.02 (CO2), 1.65µm | ||
* UVI 283, 365 nm | * UVI 283, 365 nm | ||
| Line 74: | Line 74: | ||
* LIR | * LIR | ||
10 | 10 µm | ||
cloud top (day/nightside) | cloud top (day/nightside) | ||
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[http://www.stp.isas.jaxa.jp/venus/E_instrument.html More about the Akatsuki Instruments] | [http://www.stp.isas.jaxa.jp/venus/E_instrument.html More about the Akatsuki Instruments] | ||
==Coordination== | ==Coordination== | ||
==Future meetings== | ==Future meetings== | ||
Revision as of 11:25, 18 May 2010
This wiki page is intended to support the coming coordinated Venus campaign of 2010, to give an overview of teams and techniques involved, and to serve as a tool for synchronized observations between VEx, Akatsuki with specific input or "wish list" from the modeling community.
The main drive of our coordinated ground-based activity is to study the dynamics of the Venus mesosphere (70-120 km) and lower thermosphere ( > 120 km) using techniques that can only be used from the Earth's ground (e.g. Doppler wind measurements on the day and night side of Venus, minor species distribution and abundance, requiring high spectral resolution in the visible, infrared and sub-millimeter range). Ground-based observations also bring a capability for uninterrupted monitoring of atmospheric structures and wave activity as well as other rapidly varying phenomena.
In recent meetings (Koeln, Brussels, Tokyo) we pointed out science objectives than can be reached out of significant coordination between ground-based and in-orbit measurements, such as continuous O2 1.27µm airglow emission mapping in both hemispheres, effects of planetary-scale waves on the nightglow distribution; strongly variable winds direction and amplitude in sub-mm CO and 10-µm non-LTE CO2 using IR heterodyne on the dayside, and their coupling with thermal field measurements (VEx/SPICAV and VeRa), as well as constrains on the vertical extent of cyclostrophic balance in the mesosphere.
Map (under construction)
Instrumentation and Techniques
Link on the table: Instrumentation and Techniques
Observations and Operation Planning
Link on the table: Observations and Operation Planning
In-orbit observations
Venus Express
Instruments
300px|thumb|right|Instrumentation of Venus Express, Credit: ESA
- ASPERA : Analyser of Space Plasma and Energetic Atoms
- MAG : Venus Express Magnetometer
- SPICAV/SOIR : Ultraviolet and Infrared Atmospheric Spectrometer
- VeRa : Venus Radio Science Experiment
- VIRTIS : Ultraviolet/Visible/Near-Infrared mapping spectrometer
- VMC : Venus Monitoring Camera
Akatsuki
The Project
The Venus Climate Orbiter mission (PLANET-C), one of the future planetary missions of Japan, aims at understanding the atmospheric circulation of Venus. Meteorological information will be obtained by globally mapping clouds and minor constituents successively with 4 cameras at ultraviolet and infrared wavelengths, detecting lightning with a high-speed imager, and observing the vertical structure of the atmosphere with radio science technique. The equatorial elongated orbit with westward revolution fits the observations of the movement and temporal variation of the Venusian atmosphere which rotates westward. The systematic, continuous imaging observations will provide us with an unprecedented large dataset of the Venusian atmospheric dynamics. Additional targets of the mission are the exploration of the ground surface and the observation of zodiacal light. The mission will complement the ESA's Venus Express, which also explores the Venusian environment with different approaches.
extract of: http://www.stp.isas.jaxa.jp/venus/top_english.html
The project, a link to JAXA
Instrumentation and Techniques
400px|thumb|right|Instrumentation of Akatsuki, Credit: JAXA
- IR1
1.01µm cloud (day-night), surface (nightside)
- IR2
1.73, 2.26, 2.32 (near-IR) 2.02 (CO2), 1.65µm
- UVI 283, 365 nm
SO2 - UV absorber (dayside)
- LIR
10 µm cloud top (day/nightside)
- LAC
777, 551, 553, 558, 630 nm O2/O airglow (night) lightning (night)
More about the Akatsuki Instruments