Stabilized Criegee intermediates (SCIs) and organic peroxy radicals (ROinline-formula2) are critical in atmospheric oxidation processes and secondary organic aerosol (SOA) formation. However, the influence of temperature on their corresponding reaction mechanisms in SOA formation is unclear. Through utilizing formic acid as a SCI scavenger and regulating the ratio of hydroperoxyl radials (HOinline-formula2) to ROinline-formula2 ([HOinline-formula
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]) from inline-formula∼ 0.3 to inline-formula∼ 1.9 using different concentrations of CO, the roles of ROinline-formula2 and SCIs in SOA formation were investigated from 248 to 298 K, particularly for dimer formation in inline-formulaβ-pinene ozonolysis. The SOA yield increased by 21 % from 298 to 273 K, while it decreased by 40 % from 273 to 248 K. Both changing [HOinline-formula
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] and scavenging SCIs significantly affect SOA yield and composition. SCI reactions accounted for more than 40 % of dimer and SOA mass formation for all temperatures. Increasing [HOinline-formula
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] inhibited dimer and SOA formation, and this inhibition became larger with decreasing temperature. Compared to low [HOinline-formula
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] (0.30–0.34), the dimer abundance at high [HOinline-formula
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] (1.53–1.88) decreased by about 31 % at 298 K and 70 % at 248 K. [HOinline-formula
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] has a specific impact on SCI-controlled dimers at lower temperatures by especially influencing the Cinline-formula9–SCI reactions with ROinline-formula2. The dimers formed from Cinline-formula9–SCI reactions with ROinline-formula2 were estimated to decrease by 61 % at high [HOinline-formula
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] compared to low [HOinline-formula
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] at 248 K. The high reactivity and substantial contribution to SOA of inline-formulaβ-pinene-derived SCIs at lower temperatures observed in this study suggest that monoterpene-derived SCI reactions should be accounted for in describing colder regions of the atmosphere.