MozartV1, PascalFrancis, Corpus, bibRecord, 000181

Elevated ozone in the troposphere over the Atlantic and Pacific oceans in the Northern Hemisphere

Identifieur interne : 000181 ( PascalFrancis/Corpus ); précédent : 000180; suivant : 000182

Elevated ozone in the troposphere over the Atlantic and Pacific oceans in the Northern Hemisphere

Auteurs : S. Chandra ; J. R. Ziemke ; XUEXI TIE ; Guy Brasseur

Source :

Geophysical research letters [ 0094-8276 ] ; 2004.

RBID : Pascal:05-0078873

Descripteurs français

Pascal (Inist)
- Ozone, Troposphère, Atlantique(Holocène), Océan Pacifique, Hémisphère Nord, Contenu total ozone, Variété applications, Stratosphère, Hyperfréquence, Instrumentation, Satellite UARS, Source, Printemps, Eté, Moyenne latitude, Continent, Amérique du Nord, Europe, Asie, Haute altitude, Massif montagneux, Biomasse, Facteur biogène, Mesure satellite.

English descriptors

KwdEn :
- Asia, Atlantic, Biogenic factor, Europe, High altitude, Mapping manifolds, Mid latitude, North America, Northern Hemisphere, Pacific Ocean, Spring(season), Summer, Total ozone content, UARS satellite, biomass, continents, instruments, microwaves, mountains, ozone, satellite measurements, springs, stratosphere, troposphere.

Abstract

Tropospheric column ozone (TCO) is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone (SCO) from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). It is shown that TCO during late spring and summer months over the Atlantic and Pacific oceans at northern mid-latitudes is about 50-60 Dobson Units (DU) which is about the same as over the continents of North America, Europe and Asia (except high altitude mountain regions), where surface emissions of NO_x from industrial sources, biomass and biofuel burning, and biogenic emissions are significantly larger. The zonal characteristics of TCO derived from satellite measurements are generally simulated by a global chemical transport model called MOZART-2, but some discrepancies are also shown. The model results are analyzed to delineate the relative importance of surface NO_x emission, lightning NO_x and stratospheric flux.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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C01	`01`		`ENG`	@0 Tropospheric column ozone (TCO) is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone (SCO) from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). It is shown that TCO during late spring and summer months over the Atlantic and Pacific oceans at northern mid-latitudes is about 50-60 Dobson Units (DU) which is about the same as over the continents of North America, Europe and Asia (except high altitude mountain regions), where surface emissions of NO_x from industrial sources, biomass and biofuel burning, and biogenic emissions are significantly larger. The zonal characteristics of TCO derived from satellite measurements are generally simulated by a global chemical transport model called MOZART-2, but some discrepancies are also shown. The model results are analyzed to delineate the relative importance of surface NO_x emission, lightning NO_x and stratospheric flux.
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C03	`03`	`2`	`ENG`	`@0 Atlantic @2 NX @5 08`
C03	`04`	`2`	`FRE`	`@0 Océan Pacifique @5 09`
C03	`04`	`2`	`ENG`	`@0 Pacific Ocean @5 09`
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C03	`11`	`X`	`ENG`	`@0 UARS satellite @5 16`
C03	`11`	`X`	`SPA`	`@0 Satélite UARS @5 16`
C03	`12`	`2`	`FRE`	`@0 Source @5 17`
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C03	`15`	`X`	`SPA`	`@0 Latitud media @5 20`
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C03	`17`	`2`	`FRE`	`@0 Amérique du Nord @5 22`
C03	`17`	`2`	`ENG`	`@0 North America @5 22`
C03	`17`	`2`	`SPA`	`@0 America del norte @5 22`
C03	`18`	`2`	`FRE`	`@0 Europe @5 23`
C03	`18`	`2`	`ENG`	`@0 Europe @5 23`
C03	`18`	`2`	`SPA`	`@0 Europa @5 23`
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C03	`19`	`2`	`SPA`	`@0 Asia @5 24`
C03	`20`	`X`	`FRE`	`@0 Haute altitude @5 25`
C03	`20`	`X`	`ENG`	`@0 High altitude @5 25`
C03	`20`	`X`	`SPA`	`@0 Gran altura @5 25`
C03	`21`	`2`	`FRE`	`@0 Massif montagneux @5 61`
C03	`21`	`2`	`ENG`	`@0 mountains @5 61`
C03	`21`	`2`	`SPA`	`@0 Macizo montañoso @5 61`
C03	`22`	`2`	`FRE`	`@0 Biomasse @5 63`
C03	`22`	`2`	`ENG`	`@0 biomass @5 63`
C03	`22`	`2`	`SPA`	`@0 Biomasa @5 63`
C03	`23`	`X`	`FRE`	`@0 Facteur biogène @5 64`
C03	`23`	`X`	`ENG`	`@0 Biogenic factor @5 64`
C03	`23`	`X`	`SPA`	`@0 Factor biógeno @5 64`
C03	`24`	`2`	`FRE`	`@0 Mesure satellite @5 65`
C03	`24`	`2`	`ENG`	`@0 satellite measurements @5 65`
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Format Inist (serveur)

NO :	PASCAL 05-0078873 INIST
ET :	Elevated ozone in the troposphere over the Atlantic and Pacific oceans in the Northern Hemisphere
AU :	CHANDRA (S.); ZIEMKE (J. R.); XUEXI TIE; BRASSEUR (Guy)
AF :	University of Maryland Baltimore County (UMBC) Goddard Earth Sciences and Technology (GEST)/Baltimore, Maryland/Etats-Unis (1 aut., 2 aut.); NASA Goddard Space Flight Center, Code 916/Greenbelt, Maryland/Etats-Unis (1 aut., 2 aut.); National Center of Atmospheric Research/Boulder, Colorado/Etats-Unis (3 aut., 4 aut.)
DT :	Publication en série; Niveau analytique
SO :	Geophysical research letters; ISSN 0094-8276; Coden GPRLAJ; Etats-Unis; Da. 2004; Vol. 31; No. 23; L23102.1-L23102.4; Bibl. 16 ref.
LA :	Anglais
EA :	Tropospheric column ozone (TCO) is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone (SCO) from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). It is shown that TCO during late spring and summer months over the Atlantic and Pacific oceans at northern mid-latitudes is about 50-60 Dobson Units (DU) which is about the same as over the continents of North America, Europe and Asia (except high altitude mountain regions), where surface emissions of NO_x from industrial sources, biomass and biofuel burning, and biogenic emissions are significantly larger. The zonal characteristics of TCO derived from satellite measurements are generally simulated by a global chemical transport model called MOZART-2, but some discrepancies are also shown. The model results are analyzed to delineate the relative importance of surface NO_x emission, lightning NO_x and stratospheric flux.
CC :	220; 001E; 001E01
FD :	Ozone; Troposphère; Atlantique(Holocène); Océan Pacifique; Hémisphère Nord; Contenu total ozone; Variété applications; Stratosphère; Hyperfréquence; Instrumentation; Satellite UARS; Source; Printemps; Eté; Moyenne latitude; Continent; Amérique du Nord; Europe; Asie; Haute altitude; Massif montagneux; Biomasse; Facteur biogène; Mesure satellite
FG :	Holocène; Quaternaire sup; Quaternaire; Cénozoïque; Phanérozoïque
ED :	ozone; troposphere; Atlantic; Pacific Ocean; Northern Hemisphere; Total ozone content; Mapping manifolds; stratosphere; microwaves; instruments; UARS satellite; springs; Spring(season); Summer; Mid latitude; continents; North America; Europe; Asia; High altitude; mountains; biomass; Biogenic factor; satellite measurements
EG :	Holocene; upper Quaternary; Quaternary; Cenozoic; Phanerozoic
SD :	Ozono; Océano Pacífico; Hemisferio norte; Contenido total ozono; Estratosfera; Instrumentación; Satélite UARS; Fuente; Primavera; Verano; Latitud media; America del norte; Europa; Asia; Gran altura; Macizo montañoso; Biomasa; Factor biógeno
LO :	INIST-16687.354000126129830020
ID :	05-0078873

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Pascal:05-0078873

Le document en format XML

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<term>Océan Pacifique</term>
<term>Hémisphère Nord</term>
<term>Contenu total ozone</term>
<term>Variété applications</term>
<term>Stratosphère</term>
<term>Hyperfréquence</term>
<term>Instrumentation</term>
<term>Satellite UARS</term>
<term>Source</term>
<term>Printemps</term>
<term>Eté</term>
<term>Moyenne latitude</term>
<term>Continent</term>
<term>Amérique du Nord</term>
<term>Europe</term>
<term>Asie</term>
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<front><div type="abstract" xml:lang="en">Tropospheric column ozone (TCO) is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone (SCO) from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). It is shown that TCO during late spring and summer months over the Atlantic and Pacific oceans at northern mid-latitudes is about 50-60 Dobson Units (DU) which is about the same as over the continents of North America, Europe and Asia (except high altitude mountain regions), where surface emissions of NO<sub>x</sub>
 from industrial sources, biomass and biofuel burning, and biogenic emissions are significantly larger. The zonal characteristics of TCO derived from satellite measurements are generally simulated by a global chemical transport model called MOZART-2, but some discrepancies are also shown. The model results are analyzed to delineate the relative importance of surface NO<sub>x</sub>
 emission, lightning NO<sub>x</sub>
 and stratospheric flux.</div>
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<fA14 i1="01"><s1>University of Maryland Baltimore County (UMBC) Goddard Earth Sciences and Technology (GEST)</s1>
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<fA14 i1="02"><s1>NASA Goddard Space Flight Center, Code 916</s1>
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</fA14>
<fA14 i1="03"><s1>National Center of Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
</fA14>
<fA20><s2>L23102.1-L23102.4</s2>
</fA20>
<fA21><s1>2004</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>16687</s2>
<s5>354000126129830020</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2005 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>16 ref.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>05-0078873</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Geophysical research letters</s0>
</fA64>
<fA66 i1="01"><s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>Tropospheric column ozone (TCO) is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone (SCO) from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). It is shown that TCO during late spring and summer months over the Atlantic and Pacific oceans at northern mid-latitudes is about 50-60 Dobson Units (DU) which is about the same as over the continents of North America, Europe and Asia (except high altitude mountain regions), where surface emissions of NO<sub>x</sub>
 from industrial sources, biomass and biofuel burning, and biogenic emissions are significantly larger. The zonal characteristics of TCO derived from satellite measurements are generally simulated by a global chemical transport model called MOZART-2, but some discrepancies are also shown. The model results are analyzed to delineate the relative importance of surface NO<sub>x</sub>
 emission, lightning NO<sub>x</sub>
 and stratospheric flux.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>220</s0>
</fC02>
<fC02 i1="02" i2="3"><s0>001E</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>001E01</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Ozone</s0>
<s5>06</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>ozone</s0>
<s5>06</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Ozono</s0>
<s5>06</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Troposphère</s0>
<s5>07</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>troposphere</s0>
<s5>07</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Atlantique(Holocène)</s0>
<s2>NX</s2>
<s5>08</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>Atlantic</s0>
<s2>NX</s2>
<s5>08</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Océan Pacifique</s0>
<s5>09</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>Pacific Ocean</s0>
<s5>09</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Océano Pacífico</s0>
<s5>09</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Hémisphère Nord</s0>
<s5>10</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>Northern Hemisphere</s0>
<s5>10</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Hemisferio norte</s0>
<s5>10</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Contenu total ozone</s0>
<s5>11</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Total ozone content</s0>
<s5>11</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Contenido total ozono</s0>
<s5>11</s5>
</fC03>
<fC03 i1="07" i2="3" l="FRE"><s0>Variété applications</s0>
<s5>12</s5>
</fC03>
<fC03 i1="07" i2="3" l="ENG"><s0>Mapping manifolds</s0>
<s5>12</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Stratosphère</s0>
<s5>13</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>stratosphere</s0>
<s5>13</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Estratosfera</s0>
<s5>13</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Hyperfréquence</s0>
<s5>14</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>microwaves</s0>
<s5>14</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Instrumentation</s0>
<s5>15</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>instruments</s0>
<s5>15</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Instrumentación</s0>
<s5>15</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Satellite UARS</s0>
<s5>16</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>UARS satellite</s0>
<s5>16</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Satélite UARS</s0>
<s5>16</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Source</s0>
<s5>17</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>springs</s0>
<s5>17</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Fuente</s0>
<s5>17</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Printemps</s0>
<s5>18</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Spring(season)</s0>
<s5>18</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Primavera</s0>
<s5>18</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Eté</s0>
<s5>19</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Summer</s0>
<s5>19</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Verano</s0>
<s5>19</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE"><s0>Moyenne latitude</s0>
<s5>20</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG"><s0>Mid latitude</s0>
<s5>20</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA"><s0>Latitud media</s0>
<s5>20</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Continent</s0>
<s5>21</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>continents</s0>
<s5>21</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Amérique du Nord</s0>
<s5>22</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>North America</s0>
<s5>22</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>America del norte</s0>
<s5>22</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Europe</s0>
<s5>23</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>Europe</s0>
<s5>23</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Europa</s0>
<s5>23</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Asie</s0>
<s5>24</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>Asia</s0>
<s5>24</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Asia</s0>
<s5>24</s5>
</fC03>
<fC03 i1="20" i2="X" l="FRE"><s0>Haute altitude</s0>
<s5>25</s5>
</fC03>
<fC03 i1="20" i2="X" l="ENG"><s0>High altitude</s0>
<s5>25</s5>
</fC03>
<fC03 i1="20" i2="X" l="SPA"><s0>Gran altura</s0>
<s5>25</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Massif montagneux</s0>
<s5>61</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>mountains</s0>
<s5>61</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>Macizo montañoso</s0>
<s5>61</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Biomasse</s0>
<s5>63</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>biomass</s0>
<s5>63</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Biomasa</s0>
<s5>63</s5>
</fC03>
<fC03 i1="23" i2="X" l="FRE"><s0>Facteur biogène</s0>
<s5>64</s5>
</fC03>
<fC03 i1="23" i2="X" l="ENG"><s0>Biogenic factor</s0>
<s5>64</s5>
</fC03>
<fC03 i1="23" i2="X" l="SPA"><s0>Factor biógeno</s0>
<s5>64</s5>
</fC03>
<fC03 i1="24" i2="2" l="FRE"><s0>Mesure satellite</s0>
<s5>65</s5>
</fC03>
<fC03 i1="24" i2="2" l="ENG"><s0>satellite measurements</s0>
<s5>65</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Holocène</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Holocene</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Holoceno</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Quaternaire sup</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>upper Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Cuaternario sup</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Quaternaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Cuaternario</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Phanérozoïque</s0>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>Phanerozoic</s0>
</fC07>
<fC07 i1="05" i2="2" l="SPA"><s0>Fanerozoico</s0>
</fC07>
<fN21><s1>045</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 05-0078873 INIST</NO>
<ET>Elevated ozone in the troposphere over the Atlantic and Pacific oceans in the Northern Hemisphere</ET>
<AU>CHANDRA (S.); ZIEMKE (J. R.); XUEXI TIE; BRASSEUR (Guy)</AU>
<AF>University of Maryland Baltimore County (UMBC) Goddard Earth Sciences and Technology (GEST)/Baltimore, Maryland/Etats-Unis (1 aut., 2 aut.); NASA Goddard Space Flight Center, Code 916/Greenbelt, Maryland/Etats-Unis (1 aut., 2 aut.); National Center of Atmospheric Research/Boulder, Colorado/Etats-Unis (3 aut., 4 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Geophysical research letters; ISSN 0094-8276; Coden GPRLAJ; Etats-Unis; Da. 2004; Vol. 31; No. 23; L23102.1-L23102.4; Bibl. 16 ref.</SO>
<LA>Anglais</LA>
<EA>Tropospheric column ozone (TCO) is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone (SCO) from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). It is shown that TCO during late spring and summer months over the Atlantic and Pacific oceans at northern mid-latitudes is about 50-60 Dobson Units (DU) which is about the same as over the continents of North America, Europe and Asia (except high altitude mountain regions), where surface emissions of NO<sub>x</sub>
 from industrial sources, biomass and biofuel burning, and biogenic emissions are significantly larger. The zonal characteristics of TCO derived from satellite measurements are generally simulated by a global chemical transport model called MOZART-2, but some discrepancies are also shown. The model results are analyzed to delineate the relative importance of surface NO<sub>x</sub>
 emission, lightning NO<sub>x</sub>
 and stratospheric flux.</EA>
<CC>220; 001E; 001E01</CC>
<FD>Ozone; Troposphère; Atlantique(Holocène); Océan Pacifique; Hémisphère Nord; Contenu total ozone; Variété applications; Stratosphère; Hyperfréquence; Instrumentation; Satellite UARS; Source; Printemps; Eté; Moyenne latitude; Continent; Amérique du Nord; Europe; Asie; Haute altitude; Massif montagneux; Biomasse; Facteur biogène; Mesure satellite</FD>
<FG>Holocène; Quaternaire sup; Quaternaire; Cénozoïque; Phanérozoïque</FG>
<ED>ozone; troposphere; Atlantic; Pacific Ocean; Northern Hemisphere; Total ozone content; Mapping manifolds; stratosphere; microwaves; instruments; UARS satellite; springs; Spring(season); Summer; Mid latitude; continents; North America; Europe; Asia; High altitude; mountains; biomass; Biogenic factor; satellite measurements</ED>
<EG>Holocene; upper Quaternary; Quaternary; Cenozoic; Phanerozoic</EG>
<SD>Ozono; Océano Pacífico; Hemisferio norte; Contenido total ozono; Estratosfera; Instrumentación; Satélite UARS; Fuente; Primavera; Verano; Latitud media; America del norte; Europa; Asia; Gran altura; Macizo montañoso; Biomasa; Factor biógeno</SD>
<LO>INIST-16687.354000126129830020</LO>
<ID>05-0078873</ID>
</server>
</inist>
</record>

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Elevated ozone in the troposphere over the Atlantic and Pacific oceans in the Northern Hemisphere

Elevated ozone in the troposphere over the Atlantic and Pacific oceans in the Northern Hemisphere

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