Titan Nitrogen Emissions

Slides:



Advertisements
Similar presentations
Space Weather Observations from the GOLD Mission Richard Eastes and the GOLD Team ( W. E. McClintock, A. G. Burns, S. C. Solomon, D. N. Anderson, L. Andersson,
Advertisements

Temperature Measurements in the Lower Thermosphere Utilizing the RAIDS Near Infrared Spectrometer Physical Sciences Laboratories May 19, 2010 A. B. Christensen.
Zasova L.V., Shakun A.V., Khatuntsev I.V., Ignatiev N.I,(1,2), Brekhovskih U.A.(1), Piccioni G.(3), Drossart P.(4). (1) IKI RAS, Moscow, (2) MIPT, Dolgoprudny,
METO 621 Lesson 6. Absorption by gaseous species Particles in the atmosphere are absorbers of radiation. Absorption is inherently a quantum process. A.
Learning Objectives: To understand what is meant by the term, ‘relative molecular mass’
Saturn’s Aurora from Cassini UVIS Wayne Pryor (Central Arizona College) for the UVIS team.
Shows the data from one orbit This is the page to go to to look at the GUVI data in the form of images.
PHEBUS Probing of Hermean Exosphere By Ultraviolet Spectroscopy PHEBUS Science Performance International Mercury Watch GroupObservatoire de Paris 5-6 April.
Saturn’s Auroras and Polar Atmosphere from Cassini UVIS Wayne Pryor Robert West Kris Larsen Ian Stewart Larry Esposito Joshua Colwell William McClintock.
Spectrum from a Prism. Example of a Spectrum Kirchoff’s Laws.
Hydrogen Peroxide on Mars Th. Encrenaz 1, B. Bezard, T. Greathouse, M. Richter, J. Lacy, S. Atreya, A. Wong, S. Lebonnois, F. Lefevre, F. Forget 1 Observatoire.
Photons of Light The smallest unit of light is a photon A photon is often called a particle of light The Energy of an individual photon depends on its.
Observations of Open and Closed Magnetic Field Lines at Mars: Implications for the Upper Atmosphere D.A. Brain, D.L. Mitchell, R. Lillis, R. Lin UC Berkeley.
AOSC 637 Lesson 24. Uranus Has been visited by Voyager 2 in Plane spins on an axis almost parallel to the ecliptic plane. Polar regions can point.
1 MURI:NADIR Progress on Area 6 solar atmospheric models and spectra October 2010.
Airglow on Titan During Eclipse R. A. West 1, J. M. Ajello 1, M. H. Stevens 2, D. F. Strobel 3, G. R. Gladstone 4, J.S. Evans 5, E.T. Bradley 6 1 Jet Propulsion.
1 The Mighty Weather of Saturn Andrew Ingersoll Winds and temperatures - no longer the windiest planet, or is it just a variation.
COMPARATIVE TEMPERATURE RETRIEVALS BASED ON VIRTIS/VEX AND PMV/VENERA-15 RADIATION MEASUREMENTS OVER THE NORTHERN HEMISPHERE OF VENUS R. Haus (1), G. Arnold.
EARTH & SPACE SCIENCE Chapter 30 Stars, Galaxies, and the Universe
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,
In carbon-13 NMR, what do the number of peaks represent? The number of chemically different carbon atoms present.
Rev 131 Enceladus’ Plume Solar Occultation LW Esposito and UVIS Team 14 June 2010.
Cassini UVIS results from Saturn, Titan, icy satellites and rings LW Esposito and the UVIS team 23 May 2005 American Geophysical Union.
Titan Glows in the Dark – West et al. and Ajello et al., 2012 R. A.. West, J. M. Ajello, M. H. Stevens, D. F. Strobel, G. R. Gladstone, J. S. Evans, and.
R. A. WEST, J. M. AJELLO, M. H. STEVENS, D. F. STROBEL, G. R. GLADSTONE, J.S. EVANS, T. BRADLEY, TITAN AIRGLOW DURING ECLIPSE 19 June 2012R. West 1.
Titan Airglow Spectra From 2004 and 2008 and Laboratory Results for UVIS, ISS and VIMS (800-11,000 Å) JOSEPH AJELLO JPL JACQUES GUSTIN MICHAEL STEVENS.
Titan: FUV Limb Spectra From 2004 and EUV Laboratory Cross Sections and Observations JOSEPH AJELLO JPL MICHAEL STEVENS NRL JACQUES GUSTIN LPAP GREG.
Rev 51 Enceladus Zeta Orionis Occultation Analysis Status 9 January 2008.
Interminimum Changes in Global Total Electron Content and Neutral Mass Density John Emmert, Sarah McDonald Space Science Division, Naval Research Lab Anthony.
Saturn’s Auroras from the Cassini Ultraviolet Imaging Spectrograph Wayne Pryor Robert West Ian Stewart Don Shemansky Joseph Ajello Larry Esposito Joshua.
Titan Airglow: FUV & EUV 2009 UVIS Spectra of Airglow During Day, Night & Eclipse : JOSEPH AJELLO JPL MICHAEL STEVENS NRL ROBERT WEST JPL JACQUES GUSTIN.
UVIS auroral update- June Wayne Pryor -Contributed to Kurth et al., Saturn chapter on “auroral processes” -Mitchell et al paper compared UVIS.
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course
Simulated GOLD Observations of Atmospheric Waves
Titan UVIS Airglow Spectra: Modeling and Laboratory Studies
By: Emma Saal By: Rylee Tinnel
Possible plumes at Europa, Observed by Cassini?
UVIS Saturn Atmosphere Occultation Prospectus
Yucheng Zhao, M. J. Taylor, P.-D. Pautet,
UVIS Data Analysis and Modeling: Saturn FUV images
Akatsuki Mission Update: New Images and Status of the Mission
Saturn’s Auroras from the Cassini Ultraviolet Imaging Spectrograph
Joseph Ajello JPL Alan Heays Leiden Observatory
HDAC analysis: Hydrogen in Titan‘s exosphere
Titan: FUV & EUV Spectra Limb, Dayglow, Nightglow & Eclipse
JOSEPH AJELLO JPL MICHAEL STEVENS NRL ROBERT WEST JACQUES GUSTIN LPAP
Titan tholin properties from occultation and emission observations
Joseph Ajello JPL Alan Heays Leiden Observatory
17.3 – Temperature Controls
HDAC status and analysis: Photometric observations by HDAC onboard Cassini Yuri Skorov, Horst Uwe Keller, Ralf Reulke, Karl-Heinz Glassmeier, Vlad.
Iapetus as measured by Cassini UVIS
­Long-Term Variation of Latitudinal Distribution of Coronal Holes
JOSEPH AJELLO JPL MICHAEL STEVENS NRL ROBERT WEST JACQUES GUSTIN LPAP
Final results of HDAC analysis
UVIS Calibration Update
Mosaic code update: mapping the kronian magnetosphere
Spectral analysis of starlight can tell us about:
UVIS Calibration Update
UVIS Saturn EUVFUV Data Analysis
3.5 Energy levels and spectra
Variation of Protonated Ions and H2 as observed by MAVEN NGIMS
Global wave structures in the thermosphere observed by TIMED/GUVI
Inter-calibration result of COMS/MI using before and after reprocessed CrIS data March 2019 Minju Gu and Dohyeong Kim.
Titan Airglow FUV Limb Spectra From Cassini UVIS Observations
Kristopher Larsen July 26, 2005
Dust Polarization in Galactic Clouds with PICO
UVIS Titan T0, TA Analysis
Fig. 1 CFHT photometry converted into spectral reflectivity obtained on UT (Universal Time) 22 and 25 October 2014, is shown in comparison to the VLT reflectivity.
From January Team Meeting
B. L. Alterman & Justin C. Kasper July 18, 2019
Presentation transcript:

Titan Nitrogen Emissions Where are Nitrogen NI,II and LBH emissions coming from on Titan? Is there a hemispherical or altitudinal trend in the emissions? How strong are nitrogen emissions from the ‘dark’ side of Titan?

T14: EUVFUV001 Atomic + Molecular Nitrogen Atomic Carbon Hydrogen Lyman-alpha Solar Reflection 1598 Å Feature

Dayside Nightside Combination. TA: EUVFUV001 TB: EUVFUV002 T3: MIDIRTMAP003 T3: MIDIRTMAP002 T4: FIRNADCMP002 T6: FIRNADCMP003 T10: MIDIRTMAP010 T26: EUVFUV002 T28: FIRNADCMP002 T29: FIRNADCMP002 T31: FIRNADMAP004 T31: FIRNADCMP002 T32: EUVFUV001 Nightside TB: EUVFUV001 T3: EUVFUV001 T3: NIGHTWAC003 T4: EUVFUV001 T4: FIRNADCMP003 T6: FIRNADMAP002 T8: MIDIRTMAP005 T9: EUVFUV001 T10: NIGHTNAC001 T10: EUVFUV001 T12: AURORA002 T17: FIRNADCMP003 T27: EUVFUV001 T27: MIRLMBINT001 T28: CLOUDMAP002 T28: FIRNADCMP001 T30: CLOUDMAP001 T30: EUVFUV001 T31: FIRNADCMP001 T31: PHOTOWAC001 T31: EUVFUV001 T35: EUVFUV001 Combination. T5: FIRNADCMP002 T5: EUVFUV001 T6: MIDIRTMAP007 T11: EUVFUV002 T13: EUVFUV002 T14: EUVFUV001 T14: EUVFUV002 T17: EUVFUV001 T18: EUVFUV001 T20: CLOUDMAP201 T20: CLOUDMAP001 T21: EUVFUV001 T24: EUVFUV001 T27: EUVFUV002 T29: FIRNADCMP001 T34: EUVFUV001

T14: EUVFUV001 Hemispherical Variation Altitudinal Variation

T14:EUVFUV001

T14: EUVFUV001 Dayside Nightside

Dayside vs. Nightside Intensities Sum over atomic and nitrogen bands on day and nightside to compare intensities of emission through various Titan encounters.

Nitrogen Emission Comparison Dayside N 0.098 ± 0.032 kR Nightside N 0.048 ± 0.019 kR Dayside LBH 0.093 ± 0.033 kR Nightside LBH 0.032 ± 0.013 kR

Dayside kR/bandpass Nightside kR/bandpass Atomic N Nitrogen LBH Carbon

Titan FUV Spectral Decomposition Synthetic Solar Atomic Nitrogen Nitrogen LBH

T14:EUVFUV001 Dayside Decomposition Dayside Spectrum Fitted Solar Spectrum 1.83 kR Fitted Lyman-Alpha 0.095 kR Fitted Atomic Nitrogen 0.014 kR Fitted Nitrogen LBH 0.031 kR

Synthetic Model Spectrum Data Model

Fitted Atomic Nitrogen T14:EUVFUV001 Nightside Decomposition Nightside Spectrum Fitted Lyman-Alpha 0.18 kR Fitted Atomic Nitrogen 0.024 kR Fitted Nitrogen LBH 0.014 kR

Dayside atomic Nitrogen: 0.033 ± 0.015 kR Nightside Atomic Nitrogen: 0.027 ± 0.008 kR Dayside Nitrogen LBH: 0.017 ± 0.024 kR Nightside Nitrogen LBH: 0.012 ± 0.007 kR

Correlations Little correlation between dayside and nightside emissions (R2 < 0.3) No apparent correlation to Titan’s position within the Saturn system. No apparent correlation to solar activity (SEE data)* What is controlling the activity of the nitrogen emissions?

T14: EUVFUV001 Altitudinal Distribution Day Night

Fine Resolution Binning

T14:EUVFUV001 LBH C N Dayside N: 1020 km Nightside N: 950 km Dayside LBH: 970 km Nightside LBH: 940 km Dayside Nightside

T31:EUVFUV001 N C LBH Dayside Nightside

Peak Emission Altitudes

Peak Emission Altitude Offsets

Summary of Altitudinal Variation The altitude of peak nitrogen emission on the day and nightside of Titan is correlated. Atomic nitrogen generally peaks at a higher altitude than molecular nitrogen. Dayside Atomic N: 1058 ± 30 km Nightside Atomic N: 1031 ± 28 km Dayside LBH: 1000 ± 21 km Nightside LBH: 971 ± 40 km