UVIS Goals for CSM R. West.

Slides:



Advertisements
Similar presentations
Nitrogen Chemistry in Titan’s Upper Atmosphere J. A. Kammer 1, D. E. Shemansky 2, X. Zhang 1, Y. L. Yung 1 1 Division of Geological and Planetary Sciences,
Advertisements

During which month does the Sun appear to rise the highest in the sky for an observer in New York State? (1) December (3) June (2) September (4)
SCILOV-10 Validation of SCIAMACHY limb operational NO 2 product F. Azam, K. Weigel, Ralf Bauer, A. Rozanov, M. Weber, H. Bovensmann and J. P. Burrows ESA/ESRIN,
PHEBUS Probing of Hermean Exosphere By Ultraviolet Spectroscopy PHEBUS Science Performance International Mercury Watch GroupObservatoire de Paris 5-6 April.
Titan’s Photochemical Model: Oxygen Species and Comparison with Triton and Pluto Vladimir Krasnopolsky Initial data: N 2 and CH 4 densities near the surface.
2002 PLUTO OCCULTATIONS J. Elliot et al. Observations were made of an occultation of the star by Pluto. Previous observations in 1988 showed an isothermal.
Rosetta_CD\PR\what_is_RS.ppt, :39AM, 1 Mars Express Radio Science Experiment MaRS MaRS Radio Science Data: Level 3 & 4 The retrieval S.Tellmann,
The Oceans Composition. The Oceans There are five main oceans: –Pacific, Atlantic, Indian, Arctic, Antarctic.
LATITUDE AND LONGITUDE
TRENDS IN ATMOSPHERIC OZONE FROM A LONG-TERM OZONE CLIMATOLOGY Jane Liu 1,2, D. W. Tarasick 3, V. E. Fioletov 3, C. McLinden 3, J. H. Y. Jung 1, T. Zhao.
Lesson 01 Atmospheric Structure n Composition, Extent & Vertical Division.
Unit 1 Review Quiz The Oceans & Continents QUESTION #1.
Solar Site Assessment Why the variation in solar radiation? Amount of atmosphere sun’s energy must travel through to reach earth – Time of day, Time.
The ionosphere of Mars never looked like this before Paul Withers Boston University Space Physics Group meeting, University of Michigan.
1 The Organic Aerosols of Titan’s Atmosphere Christophe Sotin, Patricia M. Beauchamp and Wayne Zimmerman Jet Propulsion Laboratory, California Institute.
Page 1 HEND science after 9 years in space. page 2 HEND/2001 Mars Odyssey HEND ( High Energy Neutron Detector ) was developed in Space Research Institute.
Moons of Saturn 14 October Iapetus Mimas.
Planet Earth A Grand Oasis in the vastness of Space
Earth, Sun, Moon and the Seasons Topic 4 and 6 Discussion Question Review Question.
Navigation Unit 1-Planet Earth. What is Navigation?  The science of locating a position on earth.
1 Volatile Exchange on Mars Maria T. Zuber MIT David E. Smith NASA/GSFC 16 th International Workshop on Laser Ranging Poznan, Poland 13 October 2008 NASA/MRO/HiRISE.
Yuk Yung (Caltech), M. C. Liang (Academia Sinica), X. Zhang (Caltech),
Aerosol distribution and physical properties in the Titan atmosphere D. E. Shemansky 1, X. Zhang 2, M-C. Liang 3, and Y. L. Yung 2 1 SET/PSSD, California,
Heating of the Earth. Temperature Layers of the Atmosphere.
© Oxford University Press, All rights reserved. 1 Chapter 3 CHAPTER 3 THE GLOBAL ENERGY SYSTEM.
Enceladus water jet models from UVIS star occultations 2 April 2013.
Earth in Space EARTH, THE SUN, AND THE SEASONS. Earth, the Sun, and the Seasons  Why is Earth colder in winter than in the summer?  Not because Earth.
Nitrogen Chemistry in Titan’s Upper Atmosphere J. A. Kammer †, D. E. Shemansky ‡, X. Zhang †, and Y. L. Yung † † California Institute of Technology, Pasadena,
Rev 131 Enceladus’ Plume Solar Occultation LW Esposito and UVIS Team 14 June 2010.
Enceladus Plume Update C. J. Hansen, I. Stewart, L. Esposito, A. Hendrix June 2009.
Methane Distribution in Titan’s Atmosphere Spica + Shaula Occultations. Candidate Observations Symmetrical Methane Distribution Flatfield Issues Asymmetrical.
Quarterly 1 NASA Quarterly UVIS Q (February – April 2014)
Titan and Saturn reports June, TOST agenda.
UVIS Team Meeting Berlin 2009 Saturn and Titan Planning Bob West Working with Don Shemansky.
Tour Re-planning and Upcoming Observations
Using the Mars climate Database for aerobraking ( km)
Static Stability in the Global UTLS Observations of Long-term Mean Structure and Variability using GPS Radio Occultation Data Kevin M. Grise David W.
D. E. Shemansky† , J. A. Kammer ‡ , X. Zhang ‡ & Y. L. Yung‡
GOMOS measurements of O3, NO2, and NO3 compared to model simulations
UVIS Saturn Atmosphere Occultation Prospectus
XM Status and Plans, XXM Activities Icy Satellite Science
XXM Status, Priorities, Plans, and Activities Icy Satellite Science
Sarah M. Milkovich UVIS Team Meeting, Pasadena 8 January 2009
Global Winds.
Photochemical processes on Titan
RTWT and Science Planning Report
Sarah M. Milkovich UVIS Team Meeting, DLR, Berlin 10 June 2009
Titan tholin properties from occultation and emission observations
CSU Sodium Lidar Program: Temperature and winds in the Mesopause Region of the Atmosphere Joe She and David Krueger, Physics Steve.
Saturn upper atmosphere structure
Earth-Sun Relationships
Analysis of Extreme and Far Ultraviolet Observations of Saturn’s Atmosphere Christopher D. Parkinson Cassini UVIS Team Meeting January 09, 2014.
Iapetus as measured by Cassini UVIS
XXM Status, Priorities, Plans, and Activities Icy Satellite Science
XM Status, Priorities and Plans, XXM Activities Icy Satellite Science
* 07/16/96 Constraints on Titan’s Hign Haze from Cassini UVIS/ISS and Huygens DISR Observations *
Saturn's temperature profiles at high, medium and low latitudes derived from UVIS EUV solar occultations - updates Jacques Gustin LPAP ULg UVIS team meeting.
Enceladus Plume Simulations
Saturn temperature and H2 profiles from Solar EUV occultations
XM Status, Priorities and Plans, XXM Activities Icy Satellite Science
Cassini UVIS solar occultation
Upcoming Events Cassini Equinox Mission
UVIS Saturn EUVFUV Data Analysis
Dione’s O2 Exosphere C. J. Hansen January 2013.
Factors Determining the Climate of India
UVIS PRIME Requests T55-T61
Sun, Earth & Relationships
GEOMETER Update Get new version of GEOMETER from Team web site after August 8. Some new parameters now computed (illum angles for “near point” of non-intersecting.
Evaluation of IRI-2012 by comparison with JASON-1 TEC and incoherent scatter radar observations during the solar minimum period Eun-Young Ji,
UVIS Titan T0, TA Analysis
Presentation transcript:

UVIS Goals for CSM R. West

Solar and Stellar Occultations Occultations provide N2 density profiles, compositional information on some hydrocarbons and haze structure in the region 300-3000 km altitude (in the ‘ignorosphere’ between 400 and 900 km UVIS provides the only information Detailed vertical profiles but point locations in lat, lon. EUV (solar) for N2; FUV (star occs) for hydrocarbons and haze Advocacy for VIMS solar occs – hydrocarbons, CO, and haze down to the surface

Criteria Need a distribution in latitude, with attention to high latitudes where the winter polar vortex is expected to be present in the south Need time coverage to assess seasonal and solar variations Need approximately radial occs For stellar occs, slower is better

Stellar Occ Opportunities

Solar Occ Opportunities

Specifics ‘Penciled-in’ opportunities T78 Low/mid latitude, early opportunity, CIRS and CAPS get most of the time T103 High latitude in both hemispheres, good stellar occ T116 High priority stellar occs, and high priority solar occs for VIMS T118 joint with INMS Star occs outside of +- 2 hr. on T101, 105, 116