Engineering topics
Sung, Keeyoon
Publications and source records attributed to Sung, Keeyoon.
FTIR Measurements of Cold Toluene (C7H8) Cross Sections in the 7 – 15 µM for Titan Atmosphere
No abstract provided
OCO-M: Spectroscopy to Support the OCO Missions: P4825: Absorption Coefficient (ABSCO) Tables for the Orbiting Carbon Observatories
No abstract provided
Spectroscopy for the Orbiting Carbon Observatory Missions: Progress and Plans
No abstract provided
Laboratory Measurements of HD Rotational Transitions at Low Temperatures for Gas Giant Atmospheres
No abstract provided
Absorption coefficient (ABSCO) tables for the Orbiting Carbon Observatories: Version 5.1
Not Available
Laboratory spectroscopy of elusive hydrocarbons and nitriles for Cassini/CIRS data analysis
No abstract provided
Spatial and Seasonal Variations in C3Hx Hydrocarbon Abundance in Titan's Stratosphere from Cassini CIRS Observations
Of the C3Hx hydrocarbons, propane (C3H8) and propyne (methylacetylene, CH3C2H) were first detected in Titan’s atmosphere during the Voyager 1 flyby in 1980. Propene (propylene, C3H6) was first detected in 2013 with data from the Composite InfraRed Spectrometer (CIRS) instrument on Cassini. We present the first measured abundance profiles of propene on Titan from radiative transfer modeling, and compare our measurements to predictions derived from several photochemical models. Near the equator, propene is observed to have a peak abundance of 10 ppbv at a pressure of 0.2 mbar. Several photochemical models predict the amount at this pressure to be in the range 0.3–1 ppbv and also show a local minimum near 0.2 mbar which we do not see in our measurements. We also see that propene follows a different latitudinal trend than the other C3 molecules. While propane and propyne concentrate near the winter pole, transported via a global convective cell, propene is most abundant above the equator. We retrieve vertical abundances profiles between 125 km and 375 km for these gases for latitude averages between 60°S–20°S, 20°S–20°N, and 20°N–60°N over two time periods, 2004 through 2009 representing Titan’s atmosphere before the 2009 equinox, and 2012 through 2015 representing time after the equinox. Additionally, using newly corrected line data, we determined an updated upper limit for allene (propadiene, CH2CCH2, the isomer of propyne). We claim a 3-σ upper limit mixing ratio of 2.5 × 10(exp −9) within 30° of the equator. The measurements we present will further constrain photochemical models by refining reaction rates and the transport of these gases throughout Titan’s atmosphere.
Progress in the measurement on temperature-dependence of H2-broadening of cold and hot CH4
UNKNOWN
Far Infrared 14NH3 Line Positions and Intensities Measured with Submm and FT-IR Spectroscopy
No abstract available