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

DOI

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.

Identifier
DOI https://doi.org/10.1594/PANGAEA.964081
Related Identifier IsSupplementTo https://doi.org/10.1029/2023EA002840
Related Identifier References https://doi.org/10.1594/PANGAEA.964085
Related Identifier References https://doi.org/10.5194/cp-16-2431-2020
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.964081
Provenance
Creator Azharuddin, Syed ORCID logo; Ahn, Jinho; Ryu, Yeongjun; Brook, Edward J; Salehnia, Nasrin (ORCID: 0000-0002-0395-581X)
Publisher PANGAEA
Publication Year 2023
Funding Reference National Research Foundation of Korea https://doi.org/10.13039/501100003725 Crossref Funder ID 2018R1A2B3003256
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 365 data points
Discipline Earth System Research
Spatial Coverage (-98.160 LON, -89.990 LAT)
Temporal Coverage Begin 2014-11-01T00:00:00Z
Temporal Coverage End 2015-02-28T00:00:00Z