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4 - Searching for a Site

Published online by Cambridge University Press:  03 August 2023

Paul A. Vanden Bout
Affiliation:
National Radio Astronomy Observatory, Virginia
Robert L. Dickman
Affiliation:
National Radio Astronomy Observatory, Virginia
Adele L. Plunkett
Affiliation:
National Radio Astronomy Observatory, Virginia

Summary

The search for the best site for the Millimeter Array is the subject of this chapter. It begins in the continental United States, moves to Mauna Kea in Hawaii, and ends in the Atacama Desert of northern Chile. After detailed study, the Chajnantor site above the village of San Pedro de Atacama is approved. Protection of the site is secured from mining claims, a gas pipeline, and radio interference.

Information

Figure 0

Figure 4.1 The transmission of radiation through the atmosphere as a function of observing frequency (GHz) for 0.25 mm of precipitable water vapor (PWV). The plot is from a model atmosphere for the Chajnantor ALMA site at an elevation of 5,000 m. The ALMA observing bands are indicated at the top for Bands 2–10. (Band 1 covers frequencies around 30 GHz, not shown in this plot.) A PWV column of 0.25 mm is typical of the best observing conditions on the ALMA site.

Courtesy of Juan Ramón Pardo, reproduced by permission.
Figure 1

Figure 4.2 The MMA array configurations on the Mt. Baldy (left), Alpine (center), and Springerville (right) sites. The antenna locations are shown as black dots along tracks over which the antennas would be moved. The areas are approximately 3 km east–west by 5 km north–south.

Credit: Adapted from topographic maps of the US Geological Survey; NRAO/AUI/NSF, CC BY 3.0.
Figure 2

Figure 4.3 An open view of an MMA tipper showing the receiver electronics and computer control and communications circuits. The moving parabolic surface mounted on the side rotates (tips) in elevation to make the observations. The radiometer front end, or receiver, is in the left half of the box, and the intermediate frequency and digital sections are in the right half. The box can be closed for ease of shipment and to preserve temperature stability during operation.

Credit: NRAO/AUI/NSF, CC BY 3.0.
Figure 3

Figure 4.4 The weather station on the Springerville site. The shed held the tipping radiometer and recording equipment. Battery power was maintained by solar panels and a windmill.

Credit: Frazer Owen, NRAO/AUI/NSF, CC BY 3.0.
Figure 4

Figure 4.5 A picture looking south at the Atacama Desert in northern Chile, one of the most arid places on Earth, taken from the International Space Station by Swiss astronaut Claude Nicollier, showing the location of the site selected for the MMA, and in time ALMA. The moisture trapped in off-shore clouds by the cold Humboldt Current are clearly seen from this perspective, as are the clouds in the Amazon Basin blocked by the Andes. The swath of gray that crosses the image diagonally is the Atacama Desert.

Credit: Claude Nicollier; ESO, CC BY 4.0.
Figure 5

Figure 4.6 Left panel: Roy Booth and Masato Ishiguro on a visit to the Vega Valley near Paranal in February 1992.

Courtesy of M. Ishiguro, used by permission. Right panel: The LMSA site search team enjoying a meal. They appear to be camping out. (left to right) Nick Whyborn, Wolfgang Wild, Angel Otárola, Kimiaki Kawara, and Naomasa Nakai. Courtesy of Nagayoshi Ohashi, reproduced by permission.
Figure 6

Figure 4.7 The site identified by SAO’s Raffin and Kusonoki as “Ollagüe Area, #19/20” elevation 4,650 m near Cerro Aucanquilcha. It was their top choice for the SMA. Left to right: Hernán Quintana, Angel Otárola, Paul Vanden Bout, and Bob Brown.

Credit: Riccardo Giovanelli; NRAO/AUI/NSF, CC BY 3.0.
Figure 7

Figure 4.8 The 5,000 m (16,400 ft) elevation site as seen from a point on Cerro Toco. M. Gordon named it the Llano de Chajnantor, after a neighboring peak, Cerro Chajnantor. In general usage, the site name is usually shortened to “Chajnantor,” a word that means “place of departure” in the Kunza language of the Atacameños.

Credit: Simon Radford; NRAO/AUI/NSF, CC BY 3.0.
Figure 8

Figure 4.9 The first MMA site survey team and their equipment: tipping radiometer in the entrance to the tent and solar panels for charging the batteries that powered the tipper in front. Left to right: Peter Napier, Frazer Owen, and Angel Otárola.

Credit: Simon Radford; NRAO/AUI/NSF, CC BY 3.0
Figure 9

Figure 4.10 The atmospheric monitoring laboratory in the center of the Chajnantor site. It was built into a standard shipping container. The array of solar panels leaning on the back side of the container provided power. The tipping mirror mechanism of the 225 GHz radiometer can be seen mounted on the top right-hand side of the container. The small antenna on the end of the container provided a data connection via SatPhone.

Credit: Paul Vanden Bout; NRAO/AUI/NSF, CC BY 3.0.
Figure 10

Figure 4.11 Launching a radiosonde balloon during an August 2005 study of the variation of atmospheric temperature across the ALMA site. Left to right: Rubén Bravo (behind balloon), Roberto Rivera, Angel Otárola, Jorge Riquelme.

Courtesy of Alison Stirling, reproduced by permission.
Figure 11

Figure 4.12 A portion of the “signature wall” in the monitoring station, a modified shipping container on the Chajnantor site. Note that on 10 April 1995 when Moran and Guido Garay (U. Chile) visited, the atmospheric opacity was 0.04, or an atmospheric transparency at 225 GHz of 96 percent.

Courtesy of James Moran, reproduced by permission.
Figure 12

Figure 4.13 Contour maps of the two candidate sites, Maunakea (left panel) and Chajnantor (right panel). A small dotted oval in each map shows the possible locations and extents of a nominal 3 km array. The Chajnantor site clearly offers much more level ground for more extended baselines.

Credits: Left panel –Adapted from a topographic map of the US Geological Survey; NRAO/AUI/NSF, CC BY 3.0; Right panel –Adapted from a topographic map of the Instituto Geográfico Militar, NRAO/AUI/NSF, CC BY 3.0.
Figure 13

Figure 4.14 A plot comparing atmospheric quality on the two candidate sites in the submillimeter band. The dark line shows that Chajnantor has two to three times better transparency than Maunakea (dashed line) for the best observing conditions.

Credit: Simon Radford; NRAO/AUI/NSF, CC BY 3.0.
Figure 14

Figure 4.15 Left to right: Eduardo Hardy, President Eduardo Frei, Martha Haynes, who was interim AUI president at the time. The framed map was constructed from satellite images by a group at Cornell University.

Credit: Paul Vanden Bout; NRAO/AUI/NSF, CC BY 3.0.

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