“…Recent update of MRMS incorporated the specific attenuation (AH) and KDP to enhance the ZH-based algorithm (Wang et al, 2019) and such an update can benefit from (i) the insensitivity of AH to raindrop size distribution (DSD) variability ( Ryzhkov et al, 2014); (ii) KDP is a better indicator of rain rate and liquid water content (LWC, g‧m -3 ) than ZH since KDP is more tightly connected to the precipitation particle size distribution; (iii) R(KDP) and R(AH) inherit the immunity of ФDP to miscalibration, attenuation, partial beam blockage, and wet radome effects (Park et al, 2005;Ryzhkov et al 2014), which is hard to address when using ZH for QPE, especially at higher frequencies such as C-and X-bands (Park et al, 2005;Matrosov.2010;Frasier et al, 2013). Multi-parameter radar QPE algorithms further integrates ZDR with ZH, KDP or AH to infer more information about raindrop shape, such as the double-measurement algorithm R(ZH, ZDR), R(KDP, ZDR), R(AH, ZDR) and the triple-measurement radar QPE algorithm as R(ZH, ZDR, KDP) (Matrosov,2010;Gosset et al, 2010;Schneebeli andBerne, 2012, Keenan et al, 2001;Chen et al, 2017;Gou et al,2019), but these algorithms usually assume that ZDR measurements are well calibrated and attenuation-corrected (Ryzhkov et al, 2005;Bringi et al, 2010).…”