Monitoring atmospheric water vapour at ESO’s Paranal observatory Florian Kerber (ESO) Calibration and Standardization of Large Surveys and Missions in.

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Presentation transcript:

Monitoring atmospheric water vapour at ESO’s Paranal observatory Florian Kerber (ESO) Calibration and Standardization of Large Surveys and Missions in Astronomy and Astrophysics Apr th, 2012 Fermilab

Presentation title | xx.yy.2012 Water vapour monitor installed and commissioned on Paranal (Oct/Nov 2011) Performance validated: Instrument fully compliant with SoW and Technical specifications Data will be part of VISIR science header information Precipitable water vapour (PWV) as user-provided constraint for service mode observing Tool for characterizing atmospheric properties VISIR upgrade: PWV Monitor

Presentation title | xx.yy.2012 Atmospheric Model: PWV (Univ. Lethbridge) All other constituents: CO 2, O 2 H 2 O only, PWV = 1 mm

Presentation title | xx.yy.2012 Querel et al UVES: high resolution echelle optical spectra

Presentation title | xx.yy.2012 E-ELT site characterisation (2009)

Presentation title | xx.yy.2012 E-ELT site characterisation

Presentation title | xx.yy.2012 E-ELT site characterisation

Presentation title | xx.yy.2012 Radiosondes In-situ measurements: T, p, relative humidity 2 sec time resolution trajectory follows wind duration 1.5 h up to 25 km

Presentation title | xx.yy T06:00:00

Presentation title | xx.yy.2012 Comparison with other instruments UVES IRMACRIRES VISIR Kerber et al & in preparation

Presentation title | xx.yy.2012 Comparison with other instruments Satellite Data: fine for site testing, but not adequate for observatory science operations

Presentation title | xx.yy.2012 Lessons learned n E-ELT site characterisation: La Silla, Paranal, Armazones (in collaboration with TMT)  Spectroscopy plus atmospheric model works  10 year history of Paranal reconstructed from archival data  Remote sensing data only for statistical purposes n Dedicated PWV campaigns  Validation of methods with respect to radiosondes (standard in atmospheric research)  Visible/IR instruments: precision 15-20%  Radiometer: precision 5%

Presentation title | xx.yy.2012 PWV Monitor: requirements n VISIR upgrade  mid-IR instrument, N (10  m) and Q (20  m) band  Optimise use of periods with low PWV  Real-time support of science operations n PWV Monitor  High precision,  real-time,  High time-resolution,  low maintenance,  absolute calibration,  stand-alone instrument

Presentation title | xx.yy.2012 PWV Monitor: options n Remote sensing  Lack of precision, time resolution  Spatial resolution n Radiosondes  Expensive, operational load prohibitive  Cadence n VLT instruments  Precision, Time resolution and coverage, expensive use of 8 m telescope n GPS  Precision, real-time

Presentation title | xx.yy.2012 PWV Monitor: options n Radiometers:  IRMA 20  m  22 GHz: range > 3 mm PWV  183 GHz: range 0-5 mm PWV  Paranal median: 2.5 mm n Selected: 183 GHz profiling radiometer (LHATPRO) built by Radiometer Physics GmbH (RPG)

Presentation title | xx.yy.2012 LHATPRO n Instrument (commercial product):  183 GHz, 6 channels (H 2 O line, humidity profile)  58 GHz, 7 channels (O 2 line, temperature profile)  IR camera 10  m (sky brightness, cloud detection)  All-sky pointing capability  Boundary layer scan n Observing strategy  Zenith, staring mode  2-D sky map every 6 h (ELEV degrees)  Cone (Hovmoeller) scan (ELEV 30 degrees)

Presentation title | xx.yy.2012 Atmospheric Spectra at Different Altitudes LHATPRO WVL disappears Modelled atmospheric attenuation up to 300 GHz for various altitudes (courtesy of Feist, Univ. of Bern). IWV = 70 kg / m^2 Courtesy: RPG

Presentation title | xx.yy.2012 Freq. Channels: Humidity Profiling: GHz (6 channels) Temp. Profiling: GHz Band (7 channels) How does the Profiling work? RPG-HATPRO 31.4 GHz Courtesy: RPG

Presentation title | xx.yy.2012 LHATPRO Instrument Configuration Scanning parabola mirror Beam combiner 6 channel 183 GHz WV Radiometer Ambient temp. target GHz temp. profiler Courtesy: RPG

Presentation title | xx.yy.2012 Thermal Receiver Stabilisation Two stage thermal stabilisation system: Receiver stabilisation: <30 mK over full operating temperature range (-50°C to + 45°C) Courtesy: RPG

Presentation title | xx.yy.2012 Test at UF Schneefernerhaus n Very valuable test period under variable conditions (2650 m); Sep 2011

Presentation title | xx.yy.2012 Commissioning on Paranal n 2-week period in Oct/Nov, 2011, 2635 m n Location: NE part of telescope platform n Th. Rose (RPG) on site for set-up and tests n Dedicated campaign with radiosonde balloons (U. Valparaiso) – 22 balloons launched n IR radiometer (Lethbridge, loan from GMT) n VLT instruments (CRIRES, UVES, VISIR, XSH)

Presentation title | xx.yy.2012 Commissioning on Paranal n Excellent support from Paranal staff

Presentation title | xx.yy.2012 Commissioning on Paranal

Presentation title | xx.yy.2012 Commissioning on Paranal

Presentation title | xx.yy.2012 Atmospheric Data from Dome C Humidity profile time series and IWV for the period to (courtesy of P.Ricaud, Laboratoire d'Aerologie, Observatoire Midi-Pyrenees). Absolute humidity profile map IWV variation (summer): 0.5 – 1.5 mm Courtesy: RPG

Presentation title | xx.yy.2012 First Atmospheric Data from ESO Paranal Observatory IWV Temporal Variability IWV Spatial Variability IRT Temporal Variability

Presentation title | xx.yy.2012 Example of Cirrus Detection (Measured at RPG) IWV Temporal Variability IWV Spatial Variability IRT Temporal Variability

Presentation title | xx.yy.2012 First Atmospheric Data from ESO Paranal Observatory Temperature Profile Comparison with Paranal Radio Sounding ( , 12:00 UTC) Blue: Radiometer Red: Radio Sonde

Presentation title | xx.yy.2012 Potential of Temperatur Profiling: Inversion Development and Decay

Presentation title | xx.yy.2012 Tool on Paranal

Presentation title | xx.yy.2012 Commissioning: Results n WVR meets all specifications  PWV range mm validated  PWV precision: ca 30  m  PWV accuracy: ca 0.1 mm  All sky pointing, 2-D scanning capability  High time-resolution (sec)  Autonomous operation  Remote data access and control option  Absolute calibration (LN2)  Integrated into Paranal meteo-information  New header keywords (VISIR)

Presentation title | xx.yy.2012 Early operations: Results n WVR reliable  About 3% downtime n Learning how to best use it n PWV homogeneity 5-20% n Saturation limit: ca 20 mm n IR channel: powerful tool for cloud detection  need to characterise quantitatively n Ready to support science operations for VISIR n Other VLT instruments will also use it

Presentation title | xx.yy.2012 PWV as an Observing Constraint n Implemented in observation preparation software p2pp n Scheduled for full release for Phase 2 P90 (period starting Oct 1, 2012 n Simultaneous release of new VISIR ETC with PWV as user-defined constraint n Update user manual with new observing strategy

Presentation title | xx.yy.2012 Paranal PWV Statistics Paranal median PWV: 2.4 mm (vs 1.5 mm for Mauna Kea)

Presentation title | xx.yy.2012 PWV in Fits headers TEL AMBI START/END (being implemented)  Type: double  Value Format: %.2f  Content Field: integrated water vapour (WVR)  Description: integrated water vapour at zenith in mm at Start/End of exposure PWV variation over 2-min interval

Presentation title | xx.yy.2012 Water vapour monitor (profiling radiometer) operational on Paranal Performance validated:  Range: 0-9 mm (saturation limit: 20 mm),  Precision: 30  m, accuracy ca 0.1 mm PWV as user-provided constraint for service mode observing PWV for real-time decisions at telescope PWV in FITS headers VISIR upgrade: PWV Monitor

Presentation title | xx.yy.2012 Humidity profiles Temperature profiles Atmospheric modeling – telluric standard stars Quality control tool for survey work Meso-scale models for forecasting ? Routine characterisation of atmosphere Combination with other techniques of atmospheric sensing … PWV profiling radiometer

Presentation title | xx.yy.2012 PWV radiometer on Paranal Tool for real-time support of science operations Commercial product (standardisation) Absolute calibration (LN2) Characterisation of impact of atmospheric properties on science  Optimisation of science time  Data quality of survey Summary