New experimental and theoretical investigations on the atmospheric ozone layer

Paetzold, H. K.

doi:10.1016/0021-9169(55)90120-3

Cited by 32 publications

(7 citation statements)

References 15 publications

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“…2, minimal and maximal fluxes and sinks are compiled in Tab Our results are in good agreement with the estimates of PAETZOLD [9], KROENING and NEY [7], JUNGE [6], and BREWER and WILSON [3], which are demonstrated in Tab. 1.…”

Section: Estimate Of the Global Ozone Sinksupporting

confidence: 87%

“…Assuming an average ozone concentration of 40 y OJm 3 he found the global ozone sink ranging from 1.3 to 2.1 9 109 tons of ozone per year. These values basing on the most accurate data obtained so far are much higher than previous results of estimates by D/)TSCH [5], LETTAU [8], PAETZOLD [9], KROENING and NEY [7], JUNGE [6], and BREWER and WILSON [3], which are given in the last column of Tab. 1.…”

Section: Introductionmentioning

confidence: 45%

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Global rate of ozone destruction at the earth's surface

Fabian

Junge

1970

Arch. Met. Geoph. Biokl. A.

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SummaryModel calculations were performed to estimate the vertical ozone transport in the lower troposphere due to turbulence as a function of horizontal wind velocity and surface roughness. Using measured values of the ozone destruction rates the ozone sink strength for various surface types within different latitude belts were calculated. The global ozone sink is likely to range between 4.0 and 7.1.10 s tons/year, which is in good agreement with previous estimates by different methods. Zusammenfassung Globaler Betrag der Ozonzerst6rung an der Erdoberfl~icheMit Hilfe einer Modellrechnung wird der in der unteren Troposphfire im Mittel fiberwiegende vertikale Ozontransport durch turbulente Diffusion abgesch~itzt. Dieser h/ingt fiir die verschiedenen Oberfl/ichentypen der Erde ab yon der Oberfl/ichenwindgeschwindigkeit, der Oberfl/ichenrauhigkeit sowie der spezifischen Ozonzerst6rungsrate. Durch Aufsummierung der Zerst6rungsraten aller Oberfl/ichentypen der Erde ergibt sich eine globale Ozonsenke zwischen 4,0 und 7,1. l0 s Tonnen Ozon pro Jahr, was sich in l]bereinstimmung mit verschiedenen Absch/itzungen nach anderen Methoden befindet.

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Section: Estimate Of the Global Ozone Sinksupporting

confidence: 87%

Section: Introductionmentioning

confidence: 45%

Global rate of ozone destruction at the earth's surface

Fabian

Junge

1970

Arch. Met. Geoph. Biokl. A.

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“…This picture is consistent with the general decrease of ozone mixing ratio from the stratosphere to the ground. Knowledge of the strength of the ozone sink at the ground continuous to attract scientists in that research area for at least the past 30 years [1,2,3,6,7,8,9,10,11,12,13,14,15,18,19,20,21]. Knowledge of the strength of the ozone sink at the ground continuous to attract scientists in that research area for at least the past 30 years [1,2,3,6,7,8,9,10,11,12,13,14,15,18,19,20,21].…”

Section: Introductionmentioning

confidence: 99%

On the strength of the ozone sink at the ground

Ziomas

Zerefos

Bais

et al. 1983

Arch. Met. Geoph. Biocl., Ser. B

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“…Ozone fluxes can then be calculated (northern hemisphere annual averages) (in 10 xø molecules cm -•' s-•): 7.5 [Junge, 1962], 6 [Kroening and Ney, 1962], Copyright ¸ 1977 by the American Geophysical Union. [Paetzold, 1955], and 6.6 [Fabian and Pruchniewicz, 1976].…”

Section: Introductionmentioning

confidence: 99%

Ozone measurements in rural areas

Mohnen¹,

Hogan²,

Coffey³

1977

J. Geophys. Res.

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Analyses of ozone observations obtained at single surface stations usually indicate an afternoon peaking diurnal variation in ozone concentration; several photochemical models have been developed which can accurately predict this trend by adjusting the rate constants of reaction or the concentration of the several precursor gases to ozone. Ozone observations obtained atop isolated hills in rural surroundings rarely show such an afternoon peaking diurnal variation of concentrations; the behavior of ozone concentrations at these sites can be predicted by meteorological analysis, based on the classical hypothesis of a single ozone source in the stratosphere, and subsident transport to the measuring station. Observations at Whiteface Mountain and surrounding surface sites with supporting meteorological analyses show that it is impossible to define variation in ozone concentrations uniquely by either of these analytical techniques. These observations do strongly support an hypothesis that above average ozone concentrations over this area have their source above the 850‐mbar level.

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New experimental and theoretical investigations on the atmospheric ozone layer

Cited by 32 publications

References 15 publications

Global rate of ozone destruction at the earth's surface

Global rate of ozone destruction at the earth's surface

On the strength of the ozone sink at the ground

Ozone measurements in rural areas

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