Stable carbon isotopic composition of atmospheric methane: A comparison of surface level and free tropospheric air

We report CH4 mixing ratios and δ13C of CH4 values for remote air at two ground-based atmospheric sampling sites for the period December 1994 to August 1998 and similar data from aircraft sampling of air masses from near sea level to near tropopause in September and October of 1996 during the Global...

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Main Authors: Tyler, SC, Ajie, HO, Gupta, ML, Cicerone, RJ, Blake, DR, Dlugokencky, EJ
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 1999
Subjects:
Online Access:https://escholarship.org/uc/item/7d04g34m
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spelling ftcdlib:oai:escholarship.org/ark:/13030/qt7d04g34m 2023-05-15T18:23:10+02:00 Stable carbon isotopic composition of atmospheric methane: A comparison of surface level and free tropospheric air Tyler, SC Ajie, HO Gupta, ML Cicerone, RJ Blake, DR Dlugokencky, EJ 13895 - 13910 1999-06-20 application/pdf https://escholarship.org/uc/item/7d04g34m unknown eScholarship, University of California qt7d04g34m https://escholarship.org/uc/item/7d04g34m CC-BY CC-BY Journal of Geophysical Research Atmospheres, vol 104, iss D11 Meteorology & Atmospheric Sciences article 1999 ftcdlib 2021-06-20T14:23:05Z We report CH4 mixing ratios and δ13C of CH4 values for remote air at two ground-based atmospheric sampling sites for the period December 1994 to August 1998 and similar data from aircraft sampling of air masses from near sea level to near tropopause in September and October of 1996 during the Global Tropospheric Experiment Pacific Exploratory Mission (PEM)-Tropics A. Surface values of δ13C-CH4 ranged from -47.02 to -47.52‰ at Niwot Ridge, Colorado (40° N, 105° W), and from -46.81 to -47.64‰ at Montaña de Oro, California (35° N, 121° W). Samples for isotopic analysis were taken from 2° to 27° S latitude and 81° to 158° W longitude and from sea level to 11.3 km in altitude during the PEM-Tropics A mission. They represent the first study of 13CH4 in the tropical free troposphere. At ∼11 km, δ13C-CH4 was ∼1‰ greater than surface level values. Methane was generally enriched in 13C as altitude increased and as latitude increased (toward the South Pole). Using criteria to filter out stratospheric subsidence and convective events on the basis of other trace gases present in the samples, we find evidence of a vertical gradient in δ13C-CH4 in the tropical troposphere. The magnitude of the isotopic shifts in atmospheric CH4 with altitude are examined with a two-dimensional tropospheric photochemical model and experimentally determined values for carbon kinetic isotope effects in chemical loss processes of CH4 Model-calculated values for δ13C-CH4 in both the troposphere and lower stratosphere significantly underpredict the enrichment in 13CH4 with altitude observed in our measurement data and data of other research groups. Copyright 1999 by the American Geophysical Union. Article in Journal/Newspaper South pole University of California: eScholarship Pacific South Pole
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Meteorology & Atmospheric Sciences
spellingShingle Meteorology & Atmospheric Sciences
Tyler, SC
Ajie, HO
Gupta, ML
Cicerone, RJ
Blake, DR
Dlugokencky, EJ
Stable carbon isotopic composition of atmospheric methane: A comparison of surface level and free tropospheric air
topic_facet Meteorology & Atmospheric Sciences
description We report CH4 mixing ratios and δ13C of CH4 values for remote air at two ground-based atmospheric sampling sites for the period December 1994 to August 1998 and similar data from aircraft sampling of air masses from near sea level to near tropopause in September and October of 1996 during the Global Tropospheric Experiment Pacific Exploratory Mission (PEM)-Tropics A. Surface values of δ13C-CH4 ranged from -47.02 to -47.52‰ at Niwot Ridge, Colorado (40° N, 105° W), and from -46.81 to -47.64‰ at Montaña de Oro, California (35° N, 121° W). Samples for isotopic analysis were taken from 2° to 27° S latitude and 81° to 158° W longitude and from sea level to 11.3 km in altitude during the PEM-Tropics A mission. They represent the first study of 13CH4 in the tropical free troposphere. At ∼11 km, δ13C-CH4 was ∼1‰ greater than surface level values. Methane was generally enriched in 13C as altitude increased and as latitude increased (toward the South Pole). Using criteria to filter out stratospheric subsidence and convective events on the basis of other trace gases present in the samples, we find evidence of a vertical gradient in δ13C-CH4 in the tropical troposphere. The magnitude of the isotopic shifts in atmospheric CH4 with altitude are examined with a two-dimensional tropospheric photochemical model and experimentally determined values for carbon kinetic isotope effects in chemical loss processes of CH4 Model-calculated values for δ13C-CH4 in both the troposphere and lower stratosphere significantly underpredict the enrichment in 13CH4 with altitude observed in our measurement data and data of other research groups. Copyright 1999 by the American Geophysical Union.
format Article in Journal/Newspaper
author Tyler, SC
Ajie, HO
Gupta, ML
Cicerone, RJ
Blake, DR
Dlugokencky, EJ
author_facet Tyler, SC
Ajie, HO
Gupta, ML
Cicerone, RJ
Blake, DR
Dlugokencky, EJ
author_sort Tyler, SC
title Stable carbon isotopic composition of atmospheric methane: A comparison of surface level and free tropospheric air
title_short Stable carbon isotopic composition of atmospheric methane: A comparison of surface level and free tropospheric air
title_full Stable carbon isotopic composition of atmospheric methane: A comparison of surface level and free tropospheric air
title_fullStr Stable carbon isotopic composition of atmospheric methane: A comparison of surface level and free tropospheric air
title_full_unstemmed Stable carbon isotopic composition of atmospheric methane: A comparison of surface level and free tropospheric air
title_sort stable carbon isotopic composition of atmospheric methane: a comparison of surface level and free tropospheric air
publisher eScholarship, University of California
publishDate 1999
url https://escholarship.org/uc/item/7d04g34m
op_coverage 13895 - 13910
geographic Pacific
South Pole
geographic_facet Pacific
South Pole
genre South pole
genre_facet South pole
op_source Journal of Geophysical Research Atmospheres, vol 104, iss D11
op_relation qt7d04g34m
https://escholarship.org/uc/item/7d04g34m
op_rights CC-BY
op_rightsnorm CC-BY
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