TY - JOUR
T1 - Phase correction for ALMA. Investigating water vapour radiometer scaling
T2 - The long-baseline science verification data case study
AU - Maud, L. T.
AU - Tilanus, R. P.J.
AU - Van Kempen, T. A.
AU - Hogerheijde, M. R.
AU - Schmalzl, M.
AU - Yoon, I.
AU - Contreras, Y.
AU - Toribio, M. C.
AU - Asaki, Y.
AU - Dent, W. R.F.
AU - Fomalont, E.
AU - Matsushita, S.
N1 - Funding Information:
Acknowledgements. L.T.M., R.P.J.T., M.R.H., Y.C., and C.T. are part of Allegro, the European ALMA Regional Centre node in The Netherlands (also formerly T.v.K. and M.S.). Allegro is funded by The Netherlands Organisation for Scientific Research (NWO). This paper makes use of the following ALMA data: ADS/JAO.ALMA#2011.0.00013.SV, ADS/JAO.ALMA#2011.0.00014.SV, ADS/JAO.ALMA#2011.0.00015.SV, and ADS/JAO.ALMA#2011.0.00016.SV. ALMA is a partnership of ESO (representing its member states), NSF (USA) and NINS (Japan), together with NRC (Canada) and NSC and ASIAA (Taiwan), and KASI (Republic of Korea), in cooperation with the Republic of Chile. The Joint ALMA Observatory is operated by ESO, AUI/NRAO, and NAOJ. L.T.M and Allegro would like to thank Catherine Vlahakis and Satoko Takahashi for their support during site visits, all parties involved in the ALMA/Allegro Phase Metrics Meeting (held in Leiden May/June 2016), and other Allegri, Ian Stewart, Daniel Harsono and Ciriaco Goddi for helpful and informative discussions.
Publisher Copyright:
© 2017 ESO.
PY - 2017/9/1
Y1 - 2017/9/1
N2 - The Atacama Large millimetre/submillimetre Array (ALMA) makes use of water vapour radiometers (WVR), which monitor the atmospheric water vapour line at 183 GHz along the line of sight above each antenna to correct for phase delays introduced by the wet component of the troposphere. The application of WVR derived phase corrections improve the image quality and facilitate successful observations in weather conditions that were classically marginal or poor. We present work to indicate that a scaling factor applied to the WVR solutions can act to further improve the phase stability and image quality of ALMA data. We find reduced phase noise statistics for 62 out of 75 datasets from the long-baseline science verification campaign after a WVR scaling factor is applied. The improvement of phase noise translates to an expected coherence improvement in 39 datasets. When imaging the bandpass source, we find 33 of the 39 datasets show an improvement in the signal-to-noise ratio (S/N) between a few to ~30 percent. There are 23 datasets where the S/N of the science image is improved: 6 by <1%, 11 between 1 and 5%, and 6 above 5%. The higher frequencies studied (band 6 and band 7) are those most improved, specifically datasets with low precipitable water vapour (PWV), <1 mm, where the dominance of the wet component is reduced. Although these improvements are not profound, phase stability improvements via the WVR scaling factor come into play for the higher frequency (>450 GHz) and long-baseline (>5 km) observations. These inherently have poorer phase stability and are taken in low PWV (<1 mm) conditions for which we find the scaling to be most effective. A promising explanation for the scaling factor is the mixing of dry and wet air components, although other origins are discussed. We have produced a python code to allow ALMA users to undertake WVR scaling tests and make improvements to their data.
AB - The Atacama Large millimetre/submillimetre Array (ALMA) makes use of water vapour radiometers (WVR), which monitor the atmospheric water vapour line at 183 GHz along the line of sight above each antenna to correct for phase delays introduced by the wet component of the troposphere. The application of WVR derived phase corrections improve the image quality and facilitate successful observations in weather conditions that were classically marginal or poor. We present work to indicate that a scaling factor applied to the WVR solutions can act to further improve the phase stability and image quality of ALMA data. We find reduced phase noise statistics for 62 out of 75 datasets from the long-baseline science verification campaign after a WVR scaling factor is applied. The improvement of phase noise translates to an expected coherence improvement in 39 datasets. When imaging the bandpass source, we find 33 of the 39 datasets show an improvement in the signal-to-noise ratio (S/N) between a few to ~30 percent. There are 23 datasets where the S/N of the science image is improved: 6 by <1%, 11 between 1 and 5%, and 6 above 5%. The higher frequencies studied (band 6 and band 7) are those most improved, specifically datasets with low precipitable water vapour (PWV), <1 mm, where the dominance of the wet component is reduced. Although these improvements are not profound, phase stability improvements via the WVR scaling factor come into play for the higher frequency (>450 GHz) and long-baseline (>5 km) observations. These inherently have poorer phase stability and are taken in low PWV (<1 mm) conditions for which we find the scaling to be most effective. A promising explanation for the scaling factor is the mixing of dry and wet air components, although other origins are discussed. We have produced a python code to allow ALMA users to undertake WVR scaling tests and make improvements to their data.
KW - Atmospheric effects
KW - Methods: data analysis
KW - Submillimeter: general
KW - Techniques: high angular resolution
KW - Techniques: interferometric
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U2 - 10.1051/0004-6361/201731197
DO - 10.1051/0004-6361/201731197
M3 - Article
AN - SCOPUS:85029762753
VL - 605
JO - Astronomy and Astrophysics
JF - Astronomy and Astrophysics
SN - 0004-6361
M1 - A121
ER -