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Time-resolved carbon and water isotope signatures of coastal fog on the Southern California Coast
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DOI：10.1016/j.atmosenv.2026.122209.png)
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Abstract
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• Time-resolved water isotope of dissolved organic carbon (δ13CDOC) in coastal fog water. • δ13CDOC consistently decreased during individual fog events. • Total organic content varied with liquid water content but not with δ13CDOC. • Fog water δ2H and δ18O tracked meteorological and air mass changes. • Carbon and water isotopes provide constraints on fog scavenging and processing.
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