Atmospheric distribution of 85 Kr simulated with a general circulation model

A three-dimensional chemical tracer model for the troposphere is used to simulate the global distribution of 85Kr, a long-lived radioisotope released at northern mid-latitudes by nuclear industry. Simulated distributions for the period 1980–1983 are in excellent agreement with data from six latitudi...

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Published in:Journal of Geophysical Research
Main Authors: Jacob, Daniel J, Prather, Michael J, Wofsy, Steven C, McElroy, Michael B
Format: Article in Journal/Newspaper
Language:English
Published: eScholarship, University of California 1987
Subjects:
Online Access:http://www.escholarship.org/uc/item/7bh4q444
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spelling ftcdlib:qt7bh4q444 2023-05-15T15:04:39+02:00 Atmospheric distribution of 85 Kr simulated with a general circulation model Jacob, Daniel J Prather, Michael J Wofsy, Steven C McElroy, Michael B 6614 1987-01-01 application/pdf http://www.escholarship.org/uc/item/7bh4q444 english eng eScholarship, University of California qt7bh4q444 http://www.escholarship.org/uc/item/7bh4q444 Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Jacob, Daniel J; Prather, Michael J; Wofsy, Steven C; & McElroy, Michael B. (1987). Atmospheric distribution of 85 Kr simulated with a general circulation model. Journal of Geophysical Research, 92(D6), 6614. doi:10.1029/JD092iD06p06614. UC Irvine: Department of Earth System Science, UCI. Retrieved from: http://www.escholarship.org/uc/item/7bh4q444 Physical Sciences and Mathematics krypton atmosphere geochemical cycles meteorology and atmospheric dynamics general circulation article 1987 ftcdlib https://doi.org/10.1029/JD092iD06p06614 2016-04-02T18:19:26Z A three-dimensional chemical tracer model for the troposphere is used to simulate the global distribution of 85Kr, a long-lived radioisotope released at northern mid-latitudes by nuclear industry. Simulated distributions for the period 1980–1983 are in excellent agreement with data from six latitudinal profiles measured over the Atlantic. High concentrations of 85Kr are predicted over the Arctic in winter, advected from European sources, and somewhat smaller enhancements arising from the same sources are predicted over the tropical Atlantic in summer. Latitudinal gradients are steepest in the northern tropics, with distinctly different seasonal variations over the Pacific, as compared to the Atlantic. The global inventory of 85Kr is reconstructed for the period 1980–1983 by combining the concentrations measured over the Atlantic with the global distributions predicted by the model. The magnitude of the Soviet source is derived. The interhemispheric exchange time is calculated as 1.1 years, with little seasonal dependence. Article in Journal/Newspaper Arctic University of California: eScholarship Arctic Pacific Journal of Geophysical Research 92 D6 6614
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language English
topic Physical Sciences and Mathematics
krypton
atmosphere
geochemical cycles
meteorology and atmospheric dynamics
general circulation
spellingShingle Physical Sciences and Mathematics
krypton
atmosphere
geochemical cycles
meteorology and atmospheric dynamics
general circulation
Jacob, Daniel J
Prather, Michael J
Wofsy, Steven C
McElroy, Michael B
Atmospheric distribution of 85 Kr simulated with a general circulation model
topic_facet Physical Sciences and Mathematics
krypton
atmosphere
geochemical cycles
meteorology and atmospheric dynamics
general circulation
description A three-dimensional chemical tracer model for the troposphere is used to simulate the global distribution of 85Kr, a long-lived radioisotope released at northern mid-latitudes by nuclear industry. Simulated distributions for the period 1980–1983 are in excellent agreement with data from six latitudinal profiles measured over the Atlantic. High concentrations of 85Kr are predicted over the Arctic in winter, advected from European sources, and somewhat smaller enhancements arising from the same sources are predicted over the tropical Atlantic in summer. Latitudinal gradients are steepest in the northern tropics, with distinctly different seasonal variations over the Pacific, as compared to the Atlantic. The global inventory of 85Kr is reconstructed for the period 1980–1983 by combining the concentrations measured over the Atlantic with the global distributions predicted by the model. The magnitude of the Soviet source is derived. The interhemispheric exchange time is calculated as 1.1 years, with little seasonal dependence.
format Article in Journal/Newspaper
author Jacob, Daniel J
Prather, Michael J
Wofsy, Steven C
McElroy, Michael B
author_facet Jacob, Daniel J
Prather, Michael J
Wofsy, Steven C
McElroy, Michael B
author_sort Jacob, Daniel J
title Atmospheric distribution of 85 Kr simulated with a general circulation model
title_short Atmospheric distribution of 85 Kr simulated with a general circulation model
title_full Atmospheric distribution of 85 Kr simulated with a general circulation model
title_fullStr Atmospheric distribution of 85 Kr simulated with a general circulation model
title_full_unstemmed Atmospheric distribution of 85 Kr simulated with a general circulation model
title_sort atmospheric distribution of 85 kr simulated with a general circulation model
publisher eScholarship, University of California
publishDate 1987
url http://www.escholarship.org/uc/item/7bh4q444
op_coverage 6614
geographic Arctic
Pacific
geographic_facet Arctic
Pacific
genre Arctic
genre_facet Arctic
op_source Jacob, Daniel J; Prather, Michael J; Wofsy, Steven C; & McElroy, Michael B. (1987). Atmospheric distribution of 85 Kr simulated with a general circulation model. Journal of Geophysical Research, 92(D6), 6614. doi:10.1029/JD092iD06p06614. UC Irvine: Department of Earth System Science, UCI. Retrieved from: http://www.escholarship.org/uc/item/7bh4q444
op_relation qt7bh4q444
http://www.escholarship.org/uc/item/7bh4q444
op_rights Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1029/JD092iD06p06614
container_title Journal of Geophysical Research
container_volume 92
container_issue D6
container_start_page 6614
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