Nitrous oxide concentration from South Pole Ice (SPICE) core for the last 11 thousand years

Nitrous oxide (N2O) is an important greenhouse gas which destroys the ozone in the stratosphere. Primary sources of atmospheric N2O are nitrification and denitrification in terrestrial soils and the ocean, and the main sink is photolysis in the stratosphere. Studies have mostly focused on the climat...

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Bibliographic Details
Main Authors: Azharuddin, Syed, Ahn, Jinho, Ryu, Yeongjun, Brook, Edward J, Salehnia, Nasrin
Format: Dataset
Language:English
Published: PANGAEA 2023
Subjects:
AGE
N2O
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.964081
https://doi.org/10.1594/PANGAEA.964081
Description
Summary:Nitrous oxide (N2O) is an important greenhouse gas which destroys the ozone in the stratosphere. Primary sources of atmospheric N2O are nitrification and denitrification in terrestrial soils and the ocean, and the main sink is photolysis in the stratosphere. Studies have mostly focused on the climate-related response of N2O during glacial-interglacial periods. However, its mechanism of variation during the Holocene remains unclear. We present a high-resolution N2O record from the South Pole Ice (SPICE) core covering the Holocene epoch.