The distributions of the global photospheric magnetic fields are usually provided by synoptic maps. Conventional synoptic maps are constructed by remapping the full-disk magnetgrams into the heliographic Carrington coordinate system. Magnetograms taken throughout a Carrington Rotation (CR) are used to construct one single full-CR synoptic map, which represents the full-surface field during the 27.275-day period. To better approximate the photospheric magnetic field at a specific time, synoptic maps can be updated regularly by fresh observations. Such updated synoptic maps are constructed by simply merging new observation into the maps, or by employing a more sophisticated flux transport model (e.g., Worden & Harvey, 2000). The updated synoptic maps are more favorable for the operational space weather forecast, as the time-evolving nature of the photosphere is better reflected, and fresh observational information can constrain the model through synoptic map input (Cash et al., 2015). Photospheric synoptic maps serve as basic observational input for coronal and heliospheric models to specify their boundary conditions (Gombosi et al., 2018; Wiegelmann et al., 2017; Yeates et al., 2018). Modeled results obtained by using synoptic maps of different sources can differ substantially. For example, Riley et al. (2012) compared solar wind solutions of CR 2060 obtained by the WSA-ENLIL Magnetohydrodynamics (MHD) heliospheric model. The solutions are computed using synoptic maps from Wilcox Solar Observatory (WSO), Michelson Doppler Imager (MDI), Synoptic Optical Longterm Investigations of the Sun (SOLIS), and Global Oscillation Network Group (GONG). While a major high-speed stream is captured by WSO and GONG results, it is missed by MDI and SOLIS results. Hayashi et al. (2016) examined coronal magnetic field structures derived with the potential field source surface (PFSS) model at CR 2044, using synoptic maps from GONG, MDI, Helioseismic and Magnetic Imager (HMI) and Huairou Solar Observing Station (HSOS). The HSOS results compared best with the extreme-ultraviolet (EUV) images, and the HMI results achieved the best agreements with near-Earth in situ data. Despite such comparison efforts, there is no consensus on which kind of synoptic map better represents the distribution of the photospheric