To further understand the relations between volumetric weight and the EastAsian monsoon evolution, we established volumetric weight sequences of loesspaleosols at the Luochuan section since 250 ka BP and Baicaoyuan section since 140 ka BP, respectively. Comparison between volumetric weight, magnetic susceptibility, particle size and deepsea oxygen isotope show that loesspaleosols volumetric weight in different climate regions east and west of the Liupanshan indicates different paleoclimate significance mainly controlled by different climate factors. Loesspaleosols volumetric weight is controlled by EastAsian summer monsoon in semihumid and semiarid region lying in east to the Liupanshan, whose values are influenced by pedogenesis, and by EastAsian winter monsoon in semiarid region west of the Liupanshan, whose values are influenced by particle size, and can be employed as a proxy indicator of summer monsoon evolution and winter monsoon evolution in the abovementioned two climate regions, respectively. Compared with sections in Baicaoyuan, Luochuan, Lingtai and Sanmenxia, volumetric weight values increase spatially from northwest to southeast in China, further indicating different influences of summer and winter monsoon on volumetric weight values of different climate region.