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Oxygen isotopic composition of fogs and rains from the North Atlantic

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Riassunto

È stata determinata la composizione isotopica dell'ossigeno in campioni di nebbia e di pioggia raccolti principalmente nell'Atlantico nord-occidentale. I risultati mostrano che la nebbia deriva, almeno in buona parte dei casi, da condensazioni parziali di vapor d'acqua in equilibrio con l'acqua oceanica. Il contenuto in O18 delle piogge misurate varia in relazione alla durata ed alla latitudine.

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Authors and Affiliations

  1. Laboratorio di Geologia Nucleare, Contratto EURATOM-ULB-CNEN, Pisa, Italy

    R. Gonfiantini & A. Longinelli

Authors
  1. R. Gonfiantini
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  2. A. Longinelli
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Gonfiantini, R., Longinelli, A. Oxygen isotopic composition of fogs and rains from the North Atlantic. Experientia 18, 222–223 (1962). https://doi.org/10.1007/BF02148311

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