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Fig. A.1

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RMS as a function of frequency in the spws covering the H2O 183 GHz line imaged with a robust parameter of 0.0. Left: Spectra in topocentric coordinates. The telluric due to the water in the Earth’s atmosphere increases the noise at a velocity of 0 km s−1. Right: Same spectra but in the local standard of rest frame. The number within brackets in the labels indicates the velocity width used for the bandpass calibration.

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