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Comparison of MODTRAN5 atmospheric extinction predictions with narrowband astronomical flux observations

机译:MODTRAN5大气消亡预测与窄带天文通量观测值的比较

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Improving the precision of ground-based astronomical observations is an objective of both current (e.g. PanSTARRSl) and future (e.g. Dark Energy Survey and the Large Synoptic Survey Telescope) sky surveys. An important element of this effort is to determine the optical attenuation imposed by the atmosphere. We have obtained atmospheric extinction observations from narrowband photometry (typically 10 nm bandwidth) at central wavelengths of 380 nm, 488 nm, 500 ran, 585 nm, 656 nm, 675 nm and 840 nm. The passbands were selected to measure the continuum component (predominantly from Rayleigh and aerosol scattering) of atmospheric attenuation, and to avoid molecular absorption features in the atmosphere. We compare these atmospheric extinction observations with predictions from MODTRAN5, a commonly used computer model of atmospheric optical transmission. The MODTRAN5 calculations were informed by a satellite-based determination of atmospheric ozone on the night of observations. We also adjusted the MODTRAN5 predictions of Rayleigh scattering to account for the difference between the default pressure and that measured at the observatory on the night of observations. We find excellent agreement across all passbands between the pressure-adjusted MODTRAN5 extinction model and the observations, within our typical extinction uncertainty of 0.013 mag/airmass, but only if we exclude any aerosol scattering component in the MODTRAN5 model. Even though this is a very limited test, with observations of a single star for a single night, the fact that we obtain excellent agreement between extinction measurements and the MODTRAN5 model, with no adjustable fit parameters, bodes well for exploiting MODTRAN5 to increase the precision of ground-based flux measurements.
机译:提高地面天文观测的精度是当前(例如PanSTARRS1)和未来(例如暗能量调查和大型天气观测望远镜)天空调查的目标。这项工作的一个重要因素是确定大气施加的光学衰减。我们已经从窄带光度法(通常为10 nm带宽)在380 nm,488 nm,500 ran,585 nm,656 nm,675 nm和840 nm的中心波长处获得了大气消光的观察结果。选择通带来测量大气衰减的连续分量(主要来自瑞利和气溶胶散射),并避免大气中的分子吸收特征。我们将这些大气灭绝的观测结果与MODTRAN5(大气光学传输的常用计算机模型)的预测结果进行了比较。 MODTRAN5的计算是通过在观测之夜基于卫星的大气臭氧含量测定得出的。我们还调整了Rayleigh散射的MODTRAN5预测值,以解决默认压力与观测之夜在天文台测得的压力之间的差异。在0.013磁极/气团的典型消光不确定度范围内,但在未将MODTRAN5模型中的任何气溶胶散射成分排除在外的情况下,我们发现压力调整后的MODTRAN5消光模型与观测值在所有通带之间都具有极好的一致性。即使这是一个非常有限的测试,只有一个夜晚观察到一颗恒星,但事实是,我们在消光测量和MODTRAN5模型之间获得了很好的一致性,并且没有可调整的拟合参数,这预示着利用MODTRAN5提高精度地面通量测量

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