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    The Upper Atmosphere of Venus in Light of the Mariner 5 Measurements 

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 004:;page 574
    Author(s): McElroy, Michael B.
    Publisher: American Meteorological Society
    Abstract: Models for the Venus atmosphere and ionosphere are presented and compared with data obtained in the S-band occultation experiment on Mariner 5. Good agreement is found between model and experiment if the Venus atmosphere ...
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    Contributions of the Hadley and Ferrel Circulations to the Energetics of the Atmosphere over the Past 32 Years 

    Source: Journal of Climate:;2014:;volume( 027 ):;issue: 007:;page 2656
    Author(s): Huang, Junling; McElroy, Michael B.
    Publisher: American Meteorological Society
    Abstract: he Hadley system provides an example of a thermally direct circulation; the Ferrel system in contrast provides an example of a thermally indirect circulation. In this study, the authors develop an approach to investigate ...
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    Odd Nitrogen in the Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 008:;page 1465
    Author(s): McConnell, John C.; McElroy, Michael B.
    Publisher: American Meteorological Society
    Abstract: Sources and sinks for atmospheric odd nitrogen are discussed and detailed calculations are presented for the altitude range 0?80 km. The mixing ratio of odd nitrogen is approximately 2?10?9 throughout the troposphere and ...
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    Photochemistry of the Venus Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 007:;page 1437
    Author(s): McElroy, Michael B.; Dak Sze, Nien; Ling Yung, Yuk
    Publisher: American Meteorological Society
    Abstract: Carbon monoxide, produced in the Venus atmosphere by photolysis of CO2, is removed mainly by reaction with OH. The radical OH is formed in part by photolysis of H2O2, in part by reaction of 0 with H02. Photolysis of HCl ...
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    Dissociation of CO2 in the Martian Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 006:;page 879
    Author(s): McElroy, Michael B.; McConnell, John C.
    Publisher: American Meteorological Society
    Abstract: Detailed calculations are presented for the production of O and CO in the Martian atmosphere. The diffusion equations are solved and results compared with Mariner observations of O and CO in the upper Marian atmosphere. ...
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    Nitrous Oxide: A Natural Source of Stratospheric NO 

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 006:;page 1095
    Author(s): McElroy, Michael B.; McConnell, John C.
    Publisher: American Meteorological Society
    Abstract: Supersonic transport planes currently under development will cruise in the stratosphere and there is concern about possible environmental effects. In particular, NO emitted by these aircraft may catalytically affect ...
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    Nucleation and Growth of HNO3·3H2O Particles in the Polar Stratosphere 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 016:;page 2004
    Author(s): Wofsy, Steven C.; Gobbi, Gian Paolo; Salawitch, Ross J.; McElroy, Michael B.
    Publisher: American Meteorological Society
    Abstract: Growth of nitric acid trihydrate (NAT) particles on background stratospheric aerosols is examined for an isolated air parcel cooled at a uniform rate. The free energy barrier against nucleation and rates of cooling are ...
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    Atmospheric Ozone: Possible Impact of Stratospheric Aviation 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 001:;page 287
    Author(s): McElroy, Michael B.; Wofsy, Steven C.; Penner, Joyce E.; McConnell, John C.
    Publisher: American Meteorological Society
    Abstract: Models for stratosphere temperature and ozone are developed and shown to give good agreement with observational data. The atmosphere is in local radiative equilibrium at heights above about 35 km, and concentrations of ...
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