“…However, isolating wildfire-driven DOM response is challenging because of natural background sources of DOM, contributed by other hydrological, topographical, physicochemical, and microbiological processes 2,56 . DOM levels monotonically decrease 89 or remain the same 61 with increasing burn severity in some studies, while others report peak DOM concentrations under moderate burn severity conditions 5,26,30,83,90 . Lower DOM concentrations are frequently reported at high burn intensities, likely due to DOM vaporization (transformation of organic material into carbon dioxide and water vapor) at extreme temperatures 6,43,89 .…”