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    Analysis of Passive Tracer Transport as Modeled by an Atmospheric General Circulation Model

    Source: Journal of Climate:;1999:;volume( 012 ):;issue: 006::page 1659
    Author:
    Holzer, Mark
    DOI: 10.1175/1520-0442(1999)012<1659:AOPTTA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Tracers without feedback on the atmosphere are used to probe tropospheric transport. Such passive tracers are considered for two important anthropogenic sources, Europe and eastern North America. The linearity of passive tracer continuity allows transport to be formulated in terms of a Green function, G. A coarse-grained Green function is defined that is suitable for numerical investigation with a GCM. An ensemble of independent realizations of the atmosphere is used to obtain the model?s ensemble mean, or ?climate? Green function. With increasing time, the individual realizations of G converge to their climate mean and this convergence is quantified in terms of the decay of ensemble fluctuations. Throughout, G is analyzed with the goal of gaining new insight into the tracer climate that results from constant sources. The climate Green function is used to identify transport timescales, pathways, and mechanisms. The Green function is zonally mixed after about 3 months. The time to mix G to within 10% of its asymptotic value exceeds 1 yr at high-latitude lower levels, while the interhemispheric two-box exchange time is ?7 months. Tracers from Europe and eastern North America follow different pathways with distinct seasonality. Eddies play a key role in transport. Transport in the Southern Hemisphere is dominated by transient eddies resulting from tracer injected ?4 months earlier. These transient eddies extend throughout much of the troposphere, and align to a large degree with contours of zonally averaged mixing ratio. Large seasonal changes of the mean-motion part of the tracer flux are primarily compensated by the standing-eddy transport. Ensemble fluctuations of G decay with an approximate t?3 power law. Eddy conversion provides a source of fluctuations, while dissipation damps ensemble fluctuations with a timescale of ?10 days. In the GCM context, the relative importance of parameterized versus resolved vertical transport is examined.
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      Analysis of Passive Tracer Transport as Modeled by an Atmospheric General Circulation Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4192001
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    contributor authorHolzer, Mark
    date accessioned2017-06-09T15:44:33Z
    date available2017-06-09T15:44:33Z
    date copyright1999/06/01
    date issued1999
    identifier issn0894-8755
    identifier otherams-5224.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4192001
    description abstractTracers without feedback on the atmosphere are used to probe tropospheric transport. Such passive tracers are considered for two important anthropogenic sources, Europe and eastern North America. The linearity of passive tracer continuity allows transport to be formulated in terms of a Green function, G. A coarse-grained Green function is defined that is suitable for numerical investigation with a GCM. An ensemble of independent realizations of the atmosphere is used to obtain the model?s ensemble mean, or ?climate? Green function. With increasing time, the individual realizations of G converge to their climate mean and this convergence is quantified in terms of the decay of ensemble fluctuations. Throughout, G is analyzed with the goal of gaining new insight into the tracer climate that results from constant sources. The climate Green function is used to identify transport timescales, pathways, and mechanisms. The Green function is zonally mixed after about 3 months. The time to mix G to within 10% of its asymptotic value exceeds 1 yr at high-latitude lower levels, while the interhemispheric two-box exchange time is ?7 months. Tracers from Europe and eastern North America follow different pathways with distinct seasonality. Eddies play a key role in transport. Transport in the Southern Hemisphere is dominated by transient eddies resulting from tracer injected ?4 months earlier. These transient eddies extend throughout much of the troposphere, and align to a large degree with contours of zonally averaged mixing ratio. Large seasonal changes of the mean-motion part of the tracer flux are primarily compensated by the standing-eddy transport. Ensemble fluctuations of G decay with an approximate t?3 power law. Eddy conversion provides a source of fluctuations, while dissipation damps ensemble fluctuations with a timescale of ?10 days. In the GCM context, the relative importance of parameterized versus resolved vertical transport is examined.
    publisherAmerican Meteorological Society
    titleAnalysis of Passive Tracer Transport as Modeled by an Atmospheric General Circulation Model
    typeJournal Paper
    journal volume12
    journal issue6
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(1999)012<1659:AOPTTA>2.0.CO;2
    journal fristpage1659
    journal lastpage1684
    treeJournal of Climate:;1999:;volume( 012 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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