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arXiv 1105.0975astro-ph.EP
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用WISE/NEOWISE观测小行星的热模型校正

Thermal Model Calibration for Minor Planets Observed with WISE/NEOWISE

A. Mainzer, T. Grav, J. Masiero, J. Bauer, E. Wright, R. M. Cutri, R. S. McMillan, M. Cohen, M. Ressler, P. Eisenhardt

摘要:

借助广角红外巡天探测器(WISE; Wright et al. 2010),我们已经观测到超过157,000颗小行星(Mainzer et al. 2011)。其中包括一些近地天体、主带小行星和不规则卫星,它们通过雷达、掩星和现场成像具有良好的物理特性。我们已经使用这些对象来验证使用WISE测量的热模型的模型,以及Wright等人(2010)中导出的四个WISE带通作为有效温度的函数的颜色校正。我们已经使用了50个物体的直径测量雷达,掩星或原位成像的特点隐含的系统误差使用WISE数据与面球面NEATM模型计算直径和dos。通过使用之前测量的直径和H星等与球形NEATM模型,我们计算预测通量后,应用Wright等人(2010)在WISE波段给出的颜色校正,并将它们与测量的星等进行比较。我们发现最小的系统通量误差为5- 10%,产生最小的相对直径和最小的误差分别为~10%和~ 20%。计算了这些天体的可见光反射率,并与3.4和4.6微米的可见光反射率进行了比较,后者包含了大多数小行星反射的阳光和热辐射的混合物。我们推导出太阳下温度和有效温度之间的线性关系,这使得Wright等人(2010)中给出的颜色校正可以通过仅计算太阳下温度而不是小面的热模型来用于小行星。在本文中推导出的热模型并不打算取代以前的测量使用雷达或航天器成像,而是,我们用它们来描述的错误,应该预期计算直径和WISE小行星的直径时,使用球形NEATM模型。

英文摘要:

With the Wide-field Infrared Survey Explorer (WISE; Wright et al. 2010), we have observed over 157,000 minor planets (Mainzer et al. 2011). Included in these are a number of near-Earth objects, Main Belt Asteroids, and irregular satellites which have well-measured physical properties via radar, occultation and in situ imaging. We have used these objects to validate models of thermal models using the WISE measurements, as well as the color corrections derived in Wright et al. (2010) for the four WISE bandpasses as a function of effective temperature. We have used 50 objects with diameters measured by radar, occultation or in situ imaging to characterize the systematic errors implicit in using the WISE data with a faceted spherical NEATM model to compute diameters and albedos. By using the previously measured diameters and H magnitudes with a spherical NEATM model, we compute the predicted fluxes after applying the color corrections given in Wright et al. (2010) in the WISE bands and compare them to the measured magnitudes. We find minimum systematic flux errors of 5-10%, yielding minimum relative diameter and albedo errors of ~10% and ~20%, respectively. Visible albedos for the objects are computed and compared to the albedos at 3.4 and 4.6 microns, which contain a mix of reflected sunlight and thermal emission for most asteroids. We derive a linear relationship between subsolar temperature and effective temperature, which allows the color corrections given in Wright et al. (2010) to be used for asteroids by computing only subsolar temperature instead of a faceted thermal model. The thermal models derived in this paper are not intended to supplant previous measurements made using radar or spacecraft imaging; rather, we have used them to characterize the errors that should be expected when computing diameters and albedos of WISE asteroids using a spherical NEATM model.

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