Abstract
The absolute brightness temperature of the Sun at millimeter wavelengths is an important diagnostic of the solar chromosphere. Because the Sun is so bright, measurement of this property usually involves the operation of telescopes under extreme conditions and requires a rigorous performance assessment of the telescope. In this study, we establish solar observation and calibration techniques at 2.6 mm wavelength for the Nobeyama 45 m telescope and accurately derive the absolute solar brightness temperature. We tune the superconductor–insulator–superconductor (SIS) receiver by inducing different bias voltages onto the SIS mixer to prevent saturation. Then, we examine the linearity of the receiver system by comparing outputs derived from different tuning conditions. Furthermore, we measure the lunar filled beam efficiency of the telescope using the New Moon, and then derive the absolute brightness temperature of the Sun. The derived solar brightness temperature is 7700 pm 310~mbox{K} at 115 GHz. The telescope beam pattern is modeled as a summation of three Gaussian functions and derived using the solar limb. The real shape of the Sun is determined via deconvolution of the beam pattern from the observed map. Such well-calibrated single-dish observations are important for high-resolution chromospheric studies because they provide the absolute temperature scale that is lacking from interferometer observations.
Highlights
The brightness temperature of the Sun constitutes a basic property of the solar atmosphere
2.1 Observation The Nobeyama 45-m-diameter radio telescope is a ground-based, millimeter-wavelength radio telescope operated by the Nobeyama Radio Observatory (NRO), which is part of the National Astronomical Observatory of Japan (NAOJ)
1 Brightness Temperature of the Sun We assume that the observed radio emission is pure thermal free–free emission which, at 100 GHz, is dominated by opacity from free electrons colliding with ions (e.g. Wedemeyer et al, 2016)
Summary
The brightness temperature of the Sun constitutes a basic property of the solar atmosphere. The main emission mechanism of the Sun at millimeter and sub-millimeter wavelengths is thermal free–free emission from the chromosphere, which is an atmospheric layer with temperature ranging between 6000 and 20,000 K. Many new discoveries relating to the chromosphere have been reported based on data from the Hinode and Interface Region Imaging Spectrograph (IRIS) spacecraft, especially as regards chromospheric fine structures and dynamics (e.g., Okamoto and De Pontieu, 2011; De Pontieu et al, 2014). These high-resolution observations have led to the identification of complex chromospheric structures. The single-dish observations allow us to measure the absolute brightness temperature accurately, and they can be used to supply the absolute temperature information missing from interferometer observations of smaller spatial scales
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