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On-The-Fly (OTF) is a technique to perform mapping observations: the antenna is driven continuously in a mapping region and the data are taken in short interval (tdump: in case of 45-m system, it can be set to be 0.1 or 0.04 times N [s]). OTF is effective in particular when a wide area is surveyed in relatively short integrations. The OTF observations have advantages over usual position-switch observations as follows.
For details, please refer to Sawada et al. 2008, PASJ, 60, 445 . Please read the page Status Report on the details of the receivers and spectromaters that can be used for OTF obsrevations.
Schematic illustration of an OTF scan pattern is shown in Fig. 1-1. The behavior of the antenna is similar to those in raster-scan mapping of continuum observations. The "on-source" part of the figure stands for the main-run of a scan (hereafter simply "scan"), during which the antenna is driven at a constant speed and the data are taken at every tdump seconds. The "approach-run" is inserted before every scan to let the antenna move stably during the scan. If there is no OFF (integration on emission-free reference position) between two scans (Fig. 1-1 middle), a "transit-run" (from the end point of the first scan to the start point of the second approach run) is inserted.
Like usual position switch ("step-and-integrate") observations, the "chopper-wheel" calibration (R-SKY) data should be obtained during the observation in an appropriate interval. OFF points are taken before every scan or several scans.
Fig. 1-1: Schematic illustration of an OTF scan pattern. (top) in case of a sequence pattern of "1*" (OFF-ON); (middle) in case of a sequence pattern of "1**" (OFF-ON-ON). (bottom) A sample scan for the FOREST receiver. About the beam rotation angle, please see this page.
As a result of the observations, the mapped region is filled with (spectrum) data points with spacings smaller than the Nyquist sampling rate. Since the data points do not align on any regular grid, the data should be regridded onto a regular grid using a convolution funciton. Convolution functions are listed in this page.
You need specify the following parameters for the OTF observations.
The resultant map has so-called scanning effects if scans along only one direction are coadded. The scanning effect will be significantly reduced by combining orthogonal scans. The so-called PLAIT algorithm described by Emerson & Gräve (1988) is implemented in the data reduction software. Please refer to the Data Reduction section.
The observation time and the sensitivity can be estimated by
* Parameters : 1.Receiver = FOREST 2.Pol = Double 3.Frequency = 115 GHz 4.Max Elevation [deg] = 60 5.Length along the scans [arcsec] = 1200 6.Length perp. to the scans [arcsec] = 1200 7.Time for scan [sec] = 20 8.Num. of ONs per OFF = 1 9.Separation between scans [arcsec] = 5 10.Map grid [arcsec] = 6 12.OFF-point separation [arcmin] = 40 12.Tsys_inp [K] = 300.0 13.Resolution - Frequency resolution (kHz) = 100 - Velocity resolution (km/s) = 14.Convolution function = Bessel*Gauss * Results : 1.theta [deg] = 0.0 2.Beam overlapped area = 1150.0 ["] * 1150.0 ["] 3.vscan is 60.0 ["/sec] (6.0 per 0.1s sample) 4.Nrow = 231 5.tapp [sec] = 7, ttran [sec] = 8, ttranoff [sec] = 12 6.tOFF = 4.7 [sec] -> 5 [sec] 7.tOH = 31.0 [sec] 8.ttot(ON) [min] = 77.0 9.ttot(OBS) [min]/[hour] = 230.0 / 3.83 10.eta(ON/OBS) = 0.33 11.tcell(ON) [sec] = 4.13 12.tcell(OFF) [sec] = 48.00 13.Tsys_inp [K] = 300.0 14.Tsys_obs_sa[K] = 306.0 15.dTa*_sa [K] = 0.5641 16.Tsys_obs_sb[K] = 422.8 17.dTa*_sb [K] = 0.7794 18.Version = 2.0170721
The optimal OFF-integration is 5 seconds. This table will take about 80 minutes to run and ΔTA*=0.56 [K] is obtained. About 1150" × 1150" region is covered with all the 4 beams. Effective spatial resolution becomes about 17" (if the telescope beam is 15"). About the effective resolution, please see Miscellaneous Information: Convolution in "Make Map" .
Please use "nobs" to make observig scripts. The usage of nobs is described in this page. Please select OTF mode in "Scan Tab". The scan pattern made by nobs can be checked with obspoint. About the FOREST beam rotation angle, please refer to this page.
For data download, please refer to this page, which can be accessed only inside NAOJ and via NRO VPN.
Please use " NOSTAR" to reduce the OTF data. The usage of NOSTAR is described in this page.
Derivation of sensitivity, effective angluar resoultion, notice for projection and others are summarised in Miscellaneous Information page.Scroll back to the Top