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cso:instruments:heterodyne:obstime [2013-12-01 07:19]
sradford
cso:instruments:heterodyne:obstime [2014-04-15 00:05] (current)
sradford
Line 1: Line 1:
 +====== Observing Time ======
  
 +
 +For heterodyne observations,​ estimate the sensitivity with the radiometer equation: ​
 +  * //​T//<​sub>​rms</​sub>​ = //K// //​T//<​sub>​sys</​sub>​ (//t ∆f //​)<​sup>​-1/​2</​sup>, ​
 +where //​T//<​sub>​sys</​sub>​ is the system temperature,​ //t// is the integration time, //∆f// is the channel width, and //K// ≈ 2, depending on the switching scheme and observing strategy. Invert this equation to estimate the necessary observing time. Do not neglect to add overhead for setup, pointing, calibration,​ etc.  ​
 +
 +
 +===== System Temperature =====
 +
 +
 +Estimate system temperature on the //​T//<​sub>​A</​sub><​sup>​*</​sup>​ scale with: 
 +
 +  * //​T//<​sub>​sys</​sub>​ [SSB, //​T//<​sub>​A</​sub><​sup>​*</​sup>​] = [exp(//​τA//​ ) / //α//] × 2 × (//​T//<​sub>​rx</​sub>​ [DSB] + //α// [1 - exp(-//​τA//​ )] //​T//<​sub>​atm</​sub>​ + (1 - //α// ) //​T//<​sub>​spill</​sub>​ ) ,
 +
 +where
 +  * //τ// is the atmospheric optical depth at the observing frequency, see [[http://​cso.caltech.edu/​atm|model atmospheric spectra]],
 +  * //A// is the airmass = secant (zenith angle),
 +  * //α// is the hot spillover efficiency = 1 - (fraction of power falling on ground, etc.), ≈ 93%,
 +  * //​T//<​sub>​atm</​sub>​ is the atmospheric temperature,​ ≈ 280 K,
 +  * //​T//<​sub>​spill</​sub>​ is the warm spillover temperature,​ ≈ 280 K, and
 +  * the Cosmic (Microwave) Background Radiation has been ignored.
 +
 +For the above parameters and //​T//<​sub>​Rx</​sub>​ = 40 K [DSB], the approximate SSB system temperature at 230 GHz is:\\
 +{{tsys-230.png?​600}}
 +
 +
 +If you're observing small sources, further adjust for the main beam efficiency.
 +
 +If the atmospheric optical depth in the two sidebands is different, please review the discussion of [[calibration#​sideband correction]].
 
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