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Studies of Atmospheric Noise on Mauna Kea at 143 GHz with Bolocam

机译:143 GHz与博洛姆的Mauna Kea的大气噪声研究

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We report measurements of the fluctuations in atmospheric emission (atmospheric noise) above Mauna Kearecorded with Bolocam at 143 GHz. These data were collected in November and December of 2003 with Bolocammounted on the Caltech Submillimeter Observatory (CSO), and span approximately 40 nights. Below= 0.5 Hz,the data time-streams are dominated by the f~(-δ) atmospheric noise in all observing conditions. We were able tosuccessfully model the atmospheric fluctuations using a Kolmogorov-Taylor turbulence model for a thin wind-driven screen in approximately half of our data. Based on this modeling, we developed several algorithms toremove the atmospheric noise, and the best results were achieved when we described the fluctuations using alow-order polynomial in detector position over the 8 arcminute focal plane. However, even with these algorithms,we were not able to reach photon-background-limited instrument photometer (BLIP) performance at frequenciesbelow 0.5 Hz in any observing conditions. Therefore, we conclude that BLIP performance is not possible fromthe CSO below = 0.5 Hz for broadband 150 GHz receivers with subtraction of a spatial atmospheric templateon scales of several arcminutes.
机译:我们在143 GHz报告了Mauna以上Mauna的大气排放(大气噪声)的波动的测量。这些数据于2003年11月和12月收集了CALTECH Subsilimeter天文台(CSO)上的Bolocammounted,并跨越了大约40晚。以下= 0.5Hz,数据时间流在所有观察条件下由F〜(δ)大气噪声主导。我们能够在大约一半的数据中使用Kolmogorov-Taylor湍流模型来定义大气波动的大气波动。基于该造型,我们开发了几种算法徘徊了大气噪声,并且当我们在8个Arcminute焦平面上的检测器位置中使用暑阶多项式描述了波动时,实现了最佳结果。然而,即使使用这些算法,我们在任何观察条件下,我们都无法在频率上达到0.5Hz的光子背景有限的仪表(BLIP)性能。因此,我们得出结论,宽带150GHz接收器的CSO不可能是不可能的,用于减去几个Arcminutes的空间大气模板尺度的减法。

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