Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation.

• Main Authors: Schilt, Adrian, Brook, Edward J, Bauska, Thomas K, Baggenstos, Daniel, Fischer, Hubertus, Joos, Fortunat, Petrenko, Vasilii V, Schaefer, Hinrich, Schmitt, Jochen, Severinghaus, Jeffrey P, Spahni, Renato, Stocker, Thomas F
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2014
• Subjects: Nitrous Oxide; Nitrogen Isotopes; Oxygen Isotopes; Temperature; Atmosphere; Rain; Ice Cover; Time Factors; History; Ancient; Antarctic Regions; Global Warming; Aquatic Organisms; General Science & Technology; Antarctic; Taylor Glacier; Antarc*; Antarctica
• Online Access: https://escholarship.org/uc/item/70v807md

Nitrous oxide (N2O) is an important greenhouse gas and ozone-depleting substance that has anthropogenic as well as natural marine and terrestrial sources. The tropospheric N2O concentrations have varied substantially in the past in concert with changing climate on glacial-interglacial and millennial...