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Description of Infrared Water Vapour Monitor (IWVM)

Figure 2 is an image of the unit in operation at the JCMT. The computer and electronics are seen in the foreground, the IWVM in the background. The IWVM uses a plane steering mirror which directs light onto a fast off-axis parabolic mirror at whose focus is an infrared photoconductor detector. A cold bandpass filter located immediately ahead of the detector defines the spectral bandwidth. A cold aperture in front of the filter defines the detector field of view. A reflective chopper produces a 200Hz modulated signal of the atmosphere which is calibrated by pointing the steering mirror to 2 blackbody sources. The detector and parabolic mirror define the field of view on the sky which is chosen such that it samples a patch of atmosphere of similar size as a submm telescope at the scale height altitude of water vapour ($\sim$10 m @ 1 km).
In the current design a standard, compact, LN2 dewar cools the detector. For installation and long term operation on a submm antenna, a closed cycle cooler would be used (eg. Cryotiger) and the IWVM mounted on the outer rim of the antenna (much like a finding scope). The cold space required is rather small ($\sim$ 18 cm3). The Moon provides an ample signal to align the IWVM (in the Dec 99 run the moon was about first quarter and was easily detected). Once the submm telescope is centred on the Moon it is expected that the IWVM can be aligned to an accuracy of a few arcminutes.
The IWVM can operate in sky-dip or stare modes. In the sky-dip mode the system steps in 0.18$^{\circ}$ increments from the zenith to $\sim$70$^{\circ}$ (corresponding to a range of 1 - 3 airmasses). In the stare mode the system can be fixed at a given zenith angle.
Key components of the IWVM are:
next up previous
Next: Theoretical calculation of radiant Up: An Infrared Water Vapour Previous: Features of an infrared
Al Wootten
2000-04-04