Thermal Properties of 1847 WISE-observed Asteroids

We present new thermophysical model fits of 1847 asteroids, deriving thermal inertia, diameter, and Bond and visible geometric albedo. We use thermal flux measurements obtained by the Wide-field Infrared Survey Explorer (WISE) during its fully cryogenic phase, when both the 12 μ m ( W3 ) and 22 μ m...

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Main Authors: Denise Hung, Josef Hanuš, Joseph R. Masiero, David J. Tholen
Format: Article
Language:English
Published: IOP Publishing 2022-01-01
Series:The Planetary Science Journal
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Online Access:https://doi.org/10.3847/PSJ/ac4d1f
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author Denise Hung
Josef Hanuš
Joseph R. Masiero
David J. Tholen
author_facet Denise Hung
Josef Hanuš
Joseph R. Masiero
David J. Tholen
author_sort Denise Hung
collection DOAJ
description We present new thermophysical model fits of 1847 asteroids, deriving thermal inertia, diameter, and Bond and visible geometric albedo. We use thermal flux measurements obtained by the Wide-field Infrared Survey Explorer (WISE) during its fully cryogenic phase, when both the 12 μ m ( W3 ) and 22 μ m ( W4 ) bands were available. We take shape models and spin information from the Database of Asteroid Models from Inversion Techniques (DAMIT) and derive new shape models through lightcurve inversion and combining WISE photometry with existing DAMIT lightcurves. When we limit our sample to the asteroids with the most reliable shape models and thermal flux measurements, we find broadly consistent thermal inertia relations with recent studies. We apply fits to the diameters D (km) and thermal inertia Γ (J m ^−2 s ^−0.5 K ^−1 ) normalized to 1 au with a linear relation of the form $\mathrm{log}[{\rm{\Gamma }}]=\alpha +\beta \mathrm{log}[D]$ , where we find α = 2.667 ± 0.059 and β = −0.467 ± 0.044 for our sample alone and α = 2.509 ± 0.017 and β = −0.352 ± 0.012 when combined with other literature estimates. We find little evidence of any correlation between rotation period and thermal inertia, owing to the small number of slow rotators to consider in our sample. While the large uncertainties on the majority of our derived thermal inertia only allow us to identify broad trends between thermal inertia and other physical parameters, we can expect a significant increase in high-quality thermal flux measurements and asteroid shape models with upcoming infrared and wide-field surveys, enabling even more thermophysical modeling of higher precision in the future.
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spelling doaj-art-d74dbf497ae1483393a099fa6147b34b2025-08-20T02:27:39ZengIOP PublishingThe Planetary Science Journal2632-33382022-01-01335610.3847/PSJ/ac4d1fThermal Properties of 1847 WISE-observed AsteroidsDenise Hung0https://orcid.org/0000-0001-7523-140XJosef Hanuš1https://orcid.org/0000-0002-2934-3723Joseph R. Masiero2https://orcid.org/0000-0003-2638-720XDavid J. Tholen3https://orcid.org/0000-0003-0773-1888Institute for Astronomy, University of Hawai’i , 2680 Woodlawn Drive, Honolulu, HI 96822, USAInstitute of Astronomy, Faculty of Mathematics and Physics, Charles University , V Holešovičkách 2, 18000 Prague, Czech RepublicCaltech/IPAC , 1200 E. California Boulevard, MC 100-22, Pasadena, CA 91125, USAInstitute for Astronomy, University of Hawai’i , 2680 Woodlawn Drive, Honolulu, HI 96822, USAWe present new thermophysical model fits of 1847 asteroids, deriving thermal inertia, diameter, and Bond and visible geometric albedo. We use thermal flux measurements obtained by the Wide-field Infrared Survey Explorer (WISE) during its fully cryogenic phase, when both the 12 μ m ( W3 ) and 22 μ m ( W4 ) bands were available. We take shape models and spin information from the Database of Asteroid Models from Inversion Techniques (DAMIT) and derive new shape models through lightcurve inversion and combining WISE photometry with existing DAMIT lightcurves. When we limit our sample to the asteroids with the most reliable shape models and thermal flux measurements, we find broadly consistent thermal inertia relations with recent studies. We apply fits to the diameters D (km) and thermal inertia Γ (J m ^−2 s ^−0.5 K ^−1 ) normalized to 1 au with a linear relation of the form $\mathrm{log}[{\rm{\Gamma }}]=\alpha +\beta \mathrm{log}[D]$ , where we find α = 2.667 ± 0.059 and β = −0.467 ± 0.044 for our sample alone and α = 2.509 ± 0.017 and β = −0.352 ± 0.012 when combined with other literature estimates. We find little evidence of any correlation between rotation period and thermal inertia, owing to the small number of slow rotators to consider in our sample. While the large uncertainties on the majority of our derived thermal inertia only allow us to identify broad trends between thermal inertia and other physical parameters, we can expect a significant increase in high-quality thermal flux measurements and asteroid shape models with upcoming infrared and wide-field surveys, enabling even more thermophysical modeling of higher precision in the future.https://doi.org/10.3847/PSJ/ac4d1fAsteroidsMain belt asteroidsAstronomy data modeling
spellingShingle Denise Hung
Josef Hanuš
Joseph R. Masiero
David J. Tholen
Thermal Properties of 1847 WISE-observed Asteroids
The Planetary Science Journal
Asteroids
Main belt asteroids
Astronomy data modeling
title Thermal Properties of 1847 WISE-observed Asteroids
title_full Thermal Properties of 1847 WISE-observed Asteroids
title_fullStr Thermal Properties of 1847 WISE-observed Asteroids
title_full_unstemmed Thermal Properties of 1847 WISE-observed Asteroids
title_short Thermal Properties of 1847 WISE-observed Asteroids
title_sort thermal properties of 1847 wise observed asteroids
topic Asteroids
Main belt asteroids
Astronomy data modeling
url https://doi.org/10.3847/PSJ/ac4d1f
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