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arXiv 1701.03032astro-ph.IM
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ALMA长基线战役:毫米和亚毫米波段长基线大气的相位特性

ALMA Long Baseline Campaigns: Phase Characteristics of Atmosphere at Long Baselines in the Millimeter and Submillimeter Wavelengths

Satoki Matsushita, Yoshiharu Asaki, Edward B. Fomalont, Koh-Ichiro Morita, Denis Barkats, Richard E. Hills, Ryohei Kawabe, Luke T. Maud, Bojan Nikolic, Remo P. … 展开作者

Satoki Matsushita, Yoshiharu Asaki, Edward B. Fomalont, Koh-Ichiro Morita, Denis Barkats, Richard E. Hills, Ryohei Kawabe, Luke T. Maud, Bojan Nikolic, Remo P. J. Tilanus, Catherine Vlahakis, Nicholas D. Whyborn

摘要:

本文介绍了第一次详细的调查毫米/亚毫米相位起伏的特点和相位校正方法获得ALMA与基线长度高达~15公里。大多数的空间结构函数(SSFs)表明,相位起伏增加基线长度的函数,与幂律斜率为~0.6。在许多情况下,我们发现,斜率变浅(平均约0.2-0.3)在基线长度超过1公里,即在SSF的翻转。使用水蒸气辐射计(WVR)的相位校正方法工作良好,特别是对于PWV >1 mm的情况,这在许多情况下将相位波动的程度减小了两倍。然而,相位波动仍然存在后WVR相位校正,这表明存在其他湍流成分,导致相位波动。这是由偶尔的SSF支持的,SSF没有表现出任何翻转;这些仅在PWV低或WVR相位校正后才能看到。这意味着由该湍流成分引起的相位波动固有地小于由水蒸气引起的相位波动。由于SSF在最大基线长度~15 km处没有翻转,因此该湍流成分的尺度高度必须为10 km或更高,因此不可能是水蒸气,其尺度高度约为1 km。这种大尺度高度的湍流成分很可能是水冰或干组分。在基线长度为10 km的情况下,经过WVR相位校正后的剩余路径长度波动较大(>200 μ m),这对于高频(>450 GHz或<700 μ m)观测是显著的。这些结果表明,需要一个额外的相位校正方法,如快速切换,除了WVR相位校正。我们模拟了快速开关,结果表明它工作得很好,较短的周期时间线性地提高了相干性。

英文摘要:

This paper presents the first detailed investigation of the characteristics of mm/submm phase fluctuation and phase correction methods obtained using ALMA with baseline lengths up to ~15 km. Most of the spatial structure functions (SSFs) show that the phase fluctuation increases as a function of baseline length, with a power-law slope of ~0.6. In many cases, we find that the slope becomes shallower (average of ~0.2-0.3) at baseline lengths longer than ~1 km, namely showing a turn-over in SSF. The phase correction method using water vapor radiometers (WVRs) works well, especially for the cases where PWV >1 mm, which reduces the degree of phase fluctuations by a factor of two in many cases. However, phase fluctuations still remain after the WVR phase correction, suggesting the existence of other turbulent constituent that cause the phase fluctuation. This is supported by occasional SSFs that do not exhibit any turn-over; these are only seen when the PWV is low or after WVR phase correction. This means that the phase fluctuation caused by this turbulent constituent is inherently smaller than that caused by water vapor. Since there is no turn-over in the SSF up to the maximum baseline length of ~15 km, this turbulent constituent must have scale height of 10 km or more, and thus cannot be water vapor, whose scale height is around 1 km. This large scale height turbulent constituent is likely to be water ice or a dry component. Excess path length fluctuation after the WVR phase correction at a baseline length of 10 km is large (>200 micron), which is significant for high frequency (>450 GHz or <700 micron) observations. These results suggest the need for an additional phase correction method, such as fast switching, in addition to the WVR phase correction. We simulated the fast switching, and the result suggests that it works well, with shorter cycle times linearly improving the coherence.

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