Tropospheric Ozone During the Last Interglacial
The history of tropospheric O3, an important atmospheric oxidant, is poorly constrained because of uncertainties in its historical budget and a dearth of independent records. Here, we estimate the mean tropospheric O3 burden during the Last Interglacial period (LIG; 115 to 130 thousand years ago) us...
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ftriceuniv:oai:scholarship.rice.edu:1911/114256 2023-05-15T13:44:55+02:00 Tropospheric Ozone During the Last Interglacial Yan, Yuzhen Banerjee, Asmita Murray, Lee T. Tie, Xin Yeung, Laurence Y. 2022 application/pdf https://hdl.handle.net/1911/114256 https://doi.org/10.1029/2022GL101113 eng eng Wiley Yan, Yuzhen, Banerjee, Asmita, Murray, Lee T., et al. "Tropospheric Ozone During the Last Interglacial." Geophysical Research Letters, 49, no. 23 (2022) Wiley: https://doi.org/10.1029/2022GL101113. https://hdl.handle.net/1911/114256 2022-Yan https://doi.org/10.1029/2022GL101113 This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. https://creativecommons.org/licenses/by/4.0/ CC-BY Journal article Text publisher version 2022 ftriceuniv https://doi.org/10.1029/2022GL101113 2023-01-28T23:30:19Z The history of tropospheric O3, an important atmospheric oxidant, is poorly constrained because of uncertainties in its historical budget and a dearth of independent records. Here, we estimate the mean tropospheric O3 burden during the Last Interglacial period (LIG; 115 to 130 thousand years ago) using a record of the clumped isotopic composition of O2 (i.e., Δ36 values) preserved in Antarctic ice. The measured LIG Δ36 value is 0.03 ± 0.02‰ (95% CI) higher than the late pre-industrial Holocene (PI; 1,590–1,850 CE) value and corresponds to a modeled 9% reduction in LIG tropospheric O3 burden (95% CI: 3%–15%), caused in part by a substantial reduction in biomass burning emissions during the LIG relative to the PI. These results are consistent with the hypothesis that late-Pleistocene megafaunal extinctions caused woody and grassy fuels to accumulate on land, leading to enhanced biomass burning in the preindustrial Holocene. Article in Journal/Newspaper Antarc* Antarctic Rice University: Digital Scholarship Archive Antarctic Geophysical Research Letters 49 23 |
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Rice University: Digital Scholarship Archive |
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ftriceuniv |
language |
English |
description |
The history of tropospheric O3, an important atmospheric oxidant, is poorly constrained because of uncertainties in its historical budget and a dearth of independent records. Here, we estimate the mean tropospheric O3 burden during the Last Interglacial period (LIG; 115 to 130 thousand years ago) using a record of the clumped isotopic composition of O2 (i.e., Δ36 values) preserved in Antarctic ice. The measured LIG Δ36 value is 0.03 ± 0.02‰ (95% CI) higher than the late pre-industrial Holocene (PI; 1,590–1,850 CE) value and corresponds to a modeled 9% reduction in LIG tropospheric O3 burden (95% CI: 3%–15%), caused in part by a substantial reduction in biomass burning emissions during the LIG relative to the PI. These results are consistent with the hypothesis that late-Pleistocene megafaunal extinctions caused woody and grassy fuels to accumulate on land, leading to enhanced biomass burning in the preindustrial Holocene. |
format |
Article in Journal/Newspaper |
author |
Yan, Yuzhen Banerjee, Asmita Murray, Lee T. Tie, Xin Yeung, Laurence Y. |
spellingShingle |
Yan, Yuzhen Banerjee, Asmita Murray, Lee T. Tie, Xin Yeung, Laurence Y. Tropospheric Ozone During the Last Interglacial |
author_facet |
Yan, Yuzhen Banerjee, Asmita Murray, Lee T. Tie, Xin Yeung, Laurence Y. |
author_sort |
Yan, Yuzhen |
title |
Tropospheric Ozone During the Last Interglacial |
title_short |
Tropospheric Ozone During the Last Interglacial |
title_full |
Tropospheric Ozone During the Last Interglacial |
title_fullStr |
Tropospheric Ozone During the Last Interglacial |
title_full_unstemmed |
Tropospheric Ozone During the Last Interglacial |
title_sort |
tropospheric ozone during the last interglacial |
publisher |
Wiley |
publishDate |
2022 |
url |
https://hdl.handle.net/1911/114256 https://doi.org/10.1029/2022GL101113 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
Yan, Yuzhen, Banerjee, Asmita, Murray, Lee T., et al. "Tropospheric Ozone During the Last Interglacial." Geophysical Research Letters, 49, no. 23 (2022) Wiley: https://doi.org/10.1029/2022GL101113. https://hdl.handle.net/1911/114256 2022-Yan https://doi.org/10.1029/2022GL101113 |
op_rights |
This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. https://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1029/2022GL101113 |
container_title |
Geophysical Research Letters |
container_volume |
49 |
container_issue |
23 |
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1766208557287473152 |