A Low Humidity and Temperature Profiling (LHATPRO) microwave radiometer is used to monitor sky conditions over ESO’s Paranal observatory. It provides measurements of precipitable water vapour (PWV) at 183 GHz, which are being used in Service Mode for scheduling observations that can take advantage of favourable conditions for infrared (IR) observations. The instrument also contains an IR camera measuring sky brightness temperature at 10.5 μm. It is capable of detecting cold and thin, even sub-visual, cirrus clouds. We present a diagnostic diagram that, based on a sophisticated time series analysis of these IR sky brightness data, allows for the automatic and quantitative classification of photometric observing conditions over Paranal. The method is highly sensitive to the presence of even very thin clouds but robust against other causes of sky brightness variations. The diagram has been validated across the complete range of conditions that occur over Paranal and we find that the automated process provides correct classification at the 95% level. We plan to develop our method into an operational tool for routine use in support of ESO Science Operations.
A Low Humidity and Temperature Profiling (LHATPRO) microwave radiometer, manufactured by Radiometer Physics GmbH (RPG), is used to monitor sky conditions over ESO’s Paranal observatory in support of VLT science operations. In addition to measuring precipitable water vapour (PWV) the instrument also contains an IR camera measuring sky brightness temperature at 10.5 μm. Due to its extended operating range down to -100 °C it is capable of detecting very cold and very thin, even sub-visual, cirrus clouds. We present a set of instrument flux calibration values as compared with a detrended fluctuation analysis (DFA) of the IR camera zenith-looking sky brightness data measured above Paranal taken over the past two years. We show that it is possible to quantify photometric observing conditions and that the method is highly sensitive to the presence of even very thin clouds but robust against variations of sky brightness caused by effects other than clouds such as variations of precipitable water vapour. Hence it can be used to determine photometric conditions for science operations. About 60 % of nights are free of clouds on Paranal. More work will be required to classify the clouds using this technique. For the future this approach might become part of VLT science operations for evaluating nightly sky conditions.
A Low Humidity and Temperature Profiling (LHATPRO) microwave radiometer, manufactured by Radiometer Physics
GmbH (RPG), is used to monitor sky conditions over ESO’s Paranal observatory in support of VLT science operations.
The unit measures several channels across the strong water vapour emission line at 183 GHz, necessary for resolving the
low levels of precipitable water vapour (PWV) that are prevalent on Paranal (median ~2.4 mm). The instrument consists
of a humidity profiler (183-191 GHz), a temperature profiler (51-58 GHz), and an infrared camera (~10 μm) for cloud
detection. We present, for the first time, a statistical analysis of the homogeneity of all-sky PWV using 21 months of
periodic (every 6 hours) all-sky scans from the radiometer. These data provide unique insight into the spatial and
temporal variation of atmospheric conditions relevant for astronomical observations, particularly in the infrared. We find
the PWV over Paranal to be remarkably homogeneous across the sky down to 27.5° elevation with a median variation of
0.32 mm (peak to valley) or 0.07 mm (rms). The homogeneity is a function of the absolute PWV but the relative
variation is fairly constant at 10-15% (peak to valley) and 3% (rms). Such variations will not be a significant issue for
analysis of astronomical data. Users at ESO can specify PWV – measured at zenith – as an ambient constraint in service
mode to enable, for instance, very demanding observations in the infrared that can only be conducted during periods of
very good atmospheric transmission and hence low PWV. We conclude that in general it will not be necessary to add
another observing constraint for PWV homogeneity to ensure integrity of observations. For demanding observations
requiring very low PWV, where the relative variation is higher, the optimum support could be provided by observing
with the LHATPRO in the same line-of-sight simultaneously. Such a mode of operations has already been tested but will
have to be justified in terms of scientific gain before implementation can be considered. This will be explored further in
the future.
We present the performance characteristics of a water vapour monitor that has been permanently deployed at ESO’s
Paranal observatory as a part of the VISIR upgrade project. After a careful analysis of the requirements and an open call for tender, the Low Humidity and Temperature Profiling microwave radiometer (LHATPRO), manufactured by
Radiometer Physics GmbH (RPG), has been selected. The unit measures several channels across the strong water vapour emission line at 183 GHz, necessary for resolving the low levels of precipitable water vapour (PWV) that are prevalent on Paranal (median ~2.5 mm). The unit comprises the above humidity profiler (183-191 GHz), a temperature profiler (51-58 GHz), and an infrared radiometer (~10 μm) for cloud detection. The instrument has been commissioned during a 2.5 week period in Oct/Nov 2011, by comparing its measurements of PWV and atmospheric profiles with the ones obtained by 22 radiosonde balloons. In parallel an IR radiometer (Univ. Lethbridge) has been operated, and various observations with ESO facility spectrographs have been taken. The RPG radiometer has been validated across the range 0.5 – 9 mm demonstrating an accuracy of better than 0.1 mm. The saturation limit of the radiometer is about 20 mm. Currently, the radiometer is being integrated into the Paranal infrastructure to serve as a high time-resolution monitor in support of VLT science operations. The water vapour radiometer’s ability to provide high precision, high time resolution information on this important aspect of the atmosphere will be most useful for conducting IR observations with the VLT under optimal conditions.
Our group has designed, sourced and constructed a radiosonde/ground-station pair using inexpensive opensource
hardware. Based on the Arduino platform, the easy to build radiosonde allows the atmospheric science
community to test and deploy instrumentation packages that can be fully customized to their individual sensing
requirements. This sensing/transmitter package has been successfully deployed on a tethered-balloon, a weather
balloon, a UAV airplane, and is currently being integrated into a UAV quadcopter and a student-built rocket.
In this paper, the system, field measurements and potential applications will be described. As will the science
drivers of having full control and open access to a measurement system in an age when commercial solutions
have become popular but are restrictive in terms of proprietary sensor specifications, “black-box” calibration
operations or data handling routines, etc. The ability to modify and experiment with both the hardware and
software tools is an essential part of the scientific process. Without an understanding of the intrinsic biases or
limitations in your instruments and system, it becomes difficult to improve them or advance the knowledge in
any given field.
The European Southern Observatory (ESO), the Institute for Space Imaging Science (ISIS) and the AstroMeteorology
group at the Universidad de Valparaiso collaborated on a project to understand the precipitable water
vapour (PWV) over the La Silla Paranal Observatory. Both La Silla and Paranal were studied with the goal of
using them as reference sites to evaluate potential E-ELT sites. As ground-based infrared astronomy matures,
our understanding of the atmospheric conditions over the observatories becomes paramount, specifically water
vapour since it is the principle source of atmospheric opacity at infrared wavelengths. Several years of archival
optical spectra (FEROS) have been analysed to reconstruct the PWV history above La Silla using an atmospheric
radiative transfer model (BTRAM) developed by ISIS. In order to better understand the systematics involved, a
dedicated atmospheric water vapour measurement campaign was conducted in May 2009 in close collaboration
with Las Campanas observatory and the GMT site testing team. Several methods of determining the water column
were employed, including radiosonde launches, continuous measurements by infrared radiometers (IRMA),
a compact echelle spectrograph (BACHES) and several high-resolution optical echelle spectrographs (FEROS,
HARPS and MIKE). All available observations were compared to concurrent satellite estimates of water vapour
in an attempt to ground-truth the satellite data. We present a comparison of the methods used, and results
from the archival study and measurement campaign. A mean PWV of 3.4 ± 2.4 mm is found for La Silla using
FEROS data covering the period 2005-2009. Important lessons on the strengths and limitations of satellite data
are presented. The value of a stand-alone high time resolution PWV monitor has been demonstrated in the
context of parallel observations from Las Campanas and La Silla.
Cerro Las Campanas located at Las Campanas Observatory (LCO) in Chile has been selected as the site for the Giant
Magellan Telescope. We report results obtained since the commencement, in 2005, of a systematic site testing survey of
potential GMT sites at LCO. Atmospheric precipitable water vapor (PWV) adversely impacts mid-IR astronomy
through reduced transparency and increased background. Prior to the GMT site testing effort, little was known regarding
the PWV characteristics at LCO and therefore, a multi-pronged approach was used to ensure the determination of the
fraction of the time suitable for mid-IR observations. High time resolution monitoring was achieved with an Infrared
Radiometer for Millimeter Astronomy (IRMA) from the University of Lethbridge deployed at LCO since September of
2007. Absolute calibrations via the robust Brault method (described in Thomas-Osip et al.1) are provided by the
Magellan Inamori Kyocera Echelle (MIKE), mounted on the Clay 6.5-m telescope on a timescale of several per month.
We find that conditions suitable for mid-IR astronomy (PWV < 1.5 mm) are concentrated in the southern winter and
spring months. Nearly 40% of clear time during these seasons have PWV < 1.5mm. Approximately 10% of these nights
meet our PWV requirement for the entire night.
The content of precipitable water vapor (PWV) in the atmosphere is very important for astronomy in the infrared and
radio (sub-millimeter) spectral regions. Therefore, the astrometeorology group has developed different methods to derive
this value from measurements and making forecasts using a meteorological model. The goal is use that model to predict
the atmospheric conditions and support the scheduling of astronomical observations. At ESO, several means to
determine PWV over the observatories have been used, such as IR-radiometers (IRMA), optical and infrared
spectrographs as well as estimates using data from GOES-12 satellite. Using all of these remote sensing methods a study
undertaken to compare the accuracy of these PWV measurements to the simultaneous in-situ measurements provided by
radiosondes. Four dedicated campaigns were conducted during the months of May, July, August and November of 2009
at the La Silla, APEX and Paranal observatory sites. In addition, the astrometeorological group employs the WRF
meteorological model with the goal of simulating the state of the atmosphere (every 6 hours) and forecasting the PWV.
With these simulations, plus satellite images, radiosonde campaign data can be classified synoptically and at the same
time the model can be validated with respect to PWV.
In support of characterization of potential sites for the European Extremely Large Telescope (E-ELT) the European
Southern Observatory (ESO), the Institute for Space Imaging Science (ISIS) and the astrometeorology group of the
Universidad Valparaiso have jointly established an improved understanding of atmospheric precipitable water vapour
(PWV) above ESO's La Silla Paranal Observatory. In a first step, 8 years worth of high resolution near-IR spectra taken
with VLT-UVES have been statistically analysed to reconstruct the PWV history above Paranal. To this end a radiative
transfer model of Earth's atmosphere (BTRAM) developed by ISIS has been used. A median PWV of 2.1 mm is found
for Paranal based on UVES data covering the period 2001-2008. Furthermore we conclude that Paranal can serve as a
reference site for Northern Chile due to the stable atmospheric conditions in the region. The median offset between
Paranal and Armazones is derived to be 0.3 mm, but local arbitrary variations of a few tenths of a mm between the sites
have been found by measurement. In order to better understand the systematics involved two dedicated campaigns were
conducted in August and November 2009. Several methods for determining the water column were employed, including
radiosonde launches, continuous measurements by infrared radiometer, and VLT instruments operating at various
wavelengths: CRIRES, UVES, VISIR and X-shooter. In a first for astronomical instruments all methods have been
evaluated with respect to the radiosondes, the established standard in atmospheric research. Agreement between the
radiosondes and the IR radiometer (IRMA) is excellent while all other astronomical methods covering a wavelength
range from 700 - 20000 nm have also been successfully validated in a quantitative manner. All available observations
were compared to satellite estimates of water vapour above the observatory in an attempt to ground-truth the satellite
data. GOES can successfully be used for site evaluation in a purely statistical approach since agreement with the
radiosondes is very good on average. For use as an operational tool at an observatory GOES data are much less suited
because of significant deviations depending on atmospheric conditions. We propose to routinely monitor PWV at the
VLT and to use it as an operational constraint to guide scheduling of IR observations at Paranal. For the E-ELT we find
that a stand-alone high time resolution PWV monitor will be essential for optimizing the scientific output.
We present simultaneous precipitable water vapour (PWV) measurements made at the Las Campanas Observatory
in late 2007 using an Infrared Radiometer for Millimetre Astronomy (IRMA) and the Magellan Inamori
Kyocera Echelle (MIKE) optical spectrograph. Opacity due to water vapour is the primary concern for ground
based infrared astronomy. IRMA has been developed to measure the emission of rotational transitions of water
vapour across a narrow spectral region centred around 20 μm, using a 0.1 m off-axis parabolic mirror and a
sophisticated atmospheric model to retrieve PWV. In contrast, the MIKE instrument is used in conjunction
with the 6.5 m Magellan Clay telescope, and determines the PWV through absorption measurements of water
vapour lines in the spectra of telluric standard stars. With its high spectral resolution, MIKE is able to measure
absorption from optically thin water vapour lines and can derive PWV values using a simple, single layer
atmospheric model. In an attempt to improve the MIKE derived PWV measurements, we explore the potential
of fitting a series of MIKE water vapour line measurements, having different opacities.
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