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On the Latitude Variation of Ammonia, Acetylene, and Phosphine Altitude Profiles on Jupiter from HST Faint Object Spectrograph Observations

Identifieur interne : 002626 ( Istex/Corpus ); précédent : 002625; suivant : 002627

On the Latitude Variation of Ammonia, Acetylene, and Phosphine Altitude Profiles on Jupiter from HST Faint Object Spectrograph Observations

Auteurs : S. G. Edgington ; S. K. Atreya ; L. M. Trafton ; J. J. Caldwell ; R. F. Beebe ; A. A. Simon ; R. A. West ; C. Barnet

Source :

RBID : ISTEX:5CF2D76DE67CFA0351443AF354FB9B2F0AC05D64

Abstract

Ultraviolet spectra in the spectral region from 160 to 230 nm were taken with the Hubble Space Telescope Faint Object Spectrograph in May 1992. We analyze these data to obtain the altitude distribution of ammonia and its variation with latitude from 6°N to 25°N. Ammonia condenses below the 150-mbar level, above which it departs from saturation due to photolysis. Using a photochemical model, we also derive the value of atmospheric eddy mixing coefficients at the observed latitudes. It is found that the eddy diffusion coefficient varies from 1.5 × 104cm2s−1at 450 mbar to 4.9 × 102cm2s−1at 120 mbar. The vertical distribution of ammonia and the eddy diffusion coefficient do not show a large variation with latitude. We also determine an acetylene mixing ratio of (10–30) × 10−9near 80 mbar and an upper limit of 1.5 × 10−7for the phosphine mixing ratio, if PH3is mixed uniformly below the 140 mbar level. The existence of particulate haze at low and high latitudes is also investigated.

Url:
DOI: 10.1006/icar.1998.5925

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ISTEX:5CF2D76DE67CFA0351443AF354FB9B2F0AC05D64

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<ce:textfn>Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, Michigan, 48109-2143</ce:textfn>
</ce:affiliation>
<ce:affiliation id="IS985925A2">
<ce:label>b</ce:label>
<ce:textfn>McDonald Observatory, University of Texas, Austin, Texas, 78712</ce:textfn>
</ce:affiliation>
<ce:affiliation id="IS985925A3">
<ce:label>c</ce:label>
<ce:textfn>Department of Physics and Astronomy, York University, North York, Ontario, M35 1P3, Canada</ce:textfn>
</ce:affiliation>
<ce:affiliation id="IS985925A4">
<ce:label>d</ce:label>
<ce:textfn>Astronomy Department, New Mexico State University, Las Cruces, New Mexico, 88033</ce:textfn>
</ce:affiliation>
<ce:affiliation id="IS985925A5">
<ce:label>e</ce:label>
<ce:textfn>Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, California, 91109</ce:textfn>
</ce:affiliation>
<ce:affiliation id="IS985925A6">
<ce:label>f</ce:label>
<ce:textfn>NASA Goddard Space Flight Center, Greenbelt, Maryland, 20771</ce:textfn>
</ce:affiliation>
</ce:author-group>
<ce:date-received day="9" month="7" year="1997"></ce:date-received>
<ce:date-revised day="5" month="2" year="1998"></ce:date-revised>
<ce:abstract>
<ce:section-title>Abstract</ce:section-title>
<ce:abstract-sec>
<ce:simple-para>Ultraviolet spectra in the spectral region from 160 to 230 nm were taken with the Hubble Space Telescope Faint Object Spectrograph in May 1992. We analyze these data to obtain the altitude distribution of ammonia and its variation with latitude from 6°N to 25°N. Ammonia condenses below the 150-mbar level, above which it departs from saturation due to photolysis. Using a photochemical model, we also derive the value of atmospheric eddy mixing coefficients at the observed latitudes. It is found that the eddy diffusion coefficient varies from 1.5 × 10
<ce:sup>4</ce:sup>
cm
<ce:sup>2</ce:sup>
s
<ce:sup>−1</ce:sup>
at 450 mbar to 4.9 × 10
<ce:sup>2</ce:sup>
cm
<ce:sup>2</ce:sup>
s
<ce:sup>−1</ce:sup>
at 120 mbar. The vertical distribution of ammonia and the eddy diffusion coefficient do not show a large variation with latitude. We also determine an acetylene mixing ratio of (10–30) × 10
<ce:sup>−9</ce:sup>
near 80 mbar and an upper limit of 1.5 × 10
<ce:sup>−7</ce:sup>
for the phosphine mixing ratio, if PH
<ce:inf>3</ce:inf>
is mixed uniformly below the 140 mbar level. The existence of particulate haze at low and high latitudes is also investigated.</ce:simple-para>
</ce:abstract-sec>
</ce:abstract>
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<title>On the Latitude Variation of Ammonia, Acetylene, and Phosphine Altitude Profiles on Jupiter from HST Faint Object Spectrograph Observations</title>
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<title>On the Latitude Variation of Ammonia, Acetylene, and Phosphine Altitude Profiles on Jupiter from HST Faint Object Spectrograph Observations</title>
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<namePart type="given">S.G.</namePart>
<namePart type="family">Edgington</namePart>
<affiliation>Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, Michigan, 48109-2143</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">S.K.</namePart>
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<affiliation>Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, Michigan, 48109-2143</affiliation>
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<roleTerm type="text">author</roleTerm>
</role>
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<name type="personal">
<namePart type="given">L.M.</namePart>
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<affiliation>McDonald Observatory, University of Texas, Austin, Texas, 78712</affiliation>
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<name type="personal">
<namePart type="given">J.J.</namePart>
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<affiliation>Department of Physics and Astronomy, York University, North York, Ontario, M35 1P3, Canada</affiliation>
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<name type="personal">
<namePart type="given">R.F.</namePart>
<namePart type="family">Beebe</namePart>
<affiliation>Astronomy Department, New Mexico State University, Las Cruces, New Mexico, 88033</affiliation>
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<name type="personal">
<namePart type="given">A.A.</namePart>
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<affiliation>Astronomy Department, New Mexico State University, Las Cruces, New Mexico, 88033</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">R.A.</namePart>
<namePart type="family">West</namePart>
<affiliation>Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, California, 91109</affiliation>
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<roleTerm type="text">author</roleTerm>
</role>
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<name type="personal">
<namePart type="given">C.</namePart>
<namePart type="family">Barnet</namePart>
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<abstract lang="en">Ultraviolet spectra in the spectral region from 160 to 230 nm were taken with the Hubble Space Telescope Faint Object Spectrograph in May 1992. We analyze these data to obtain the altitude distribution of ammonia and its variation with latitude from 6°N to 25°N. Ammonia condenses below the 150-mbar level, above which it departs from saturation due to photolysis. Using a photochemical model, we also derive the value of atmospheric eddy mixing coefficients at the observed latitudes. It is found that the eddy diffusion coefficient varies from 1.5 × 104cm2s−1at 450 mbar to 4.9 × 102cm2s−1at 120 mbar. The vertical distribution of ammonia and the eddy diffusion coefficient do not show a large variation with latitude. We also determine an acetylene mixing ratio of (10–30) × 10−9near 80 mbar and an upper limit of 1.5 × 10−7for the phosphine mixing ratio, if PH3is mixed uniformly below the 140 mbar level. The existence of particulate haze at low and high latitudes is also investigated.</abstract>
<note>G. E. Hunt</note>
<note type="content">Section title: Regular Article</note>
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<dateIssued encoding="w3cdtf">199806</dateIssued>
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<identifier type="ISSN">0019-1035</identifier>
<identifier type="PII">S0019-1035(00)X0044-9</identifier>
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<date>199806</date>
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<accessCondition type="use and reproduction" contentType="copyright">©1998 Academic Press</accessCondition>
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