“…Snow, soil, vegetation, water, and deposited atmospheric particles are some of the possible secondary sources in remote areas when significant correlations involving higher atmospheric concentrations at higher temperature are observed. Temperature trends similar to those reported in this study were attributed to volatilization of chlorinated OPEs from water bodies in the Canadian Arctic (Sühring et al, 2016a), by secondary emissions and gas-particle partitioning of TCEP, TCIPP, and TDCIPP in China (Wang et al, 2020a), and secondary TBP emissions from soil and water bodies in the Great Lakes (Ma et al, 2021). However, the high-mountain areas in the Pyrenees are covered with snow most of the year and, therefore, snow is a preliminary source to consider.…”