MozartV1, PascalFrancis, Corpus, bibRecord, 000133

A set of diagnostics for evaluating chemistry-climate models in the extratropical tropopause region

Identifieur interne : 000133 ( PascalFrancis/Corpus ); précédent : 000132; suivant : 000134

A set of diagnostics for evaluating chemistry-climate models in the extratropical tropopause region

Auteurs : L. L. Pan ; J. C. Wei ; D. E. Kinnison ; R. R. Garcia ; D. J. Wuebbles ; G. P. Brasseur

Source :

Journal of geophysical research [ 0148-0227 ] ; 2007.

RBID : Pascal:07-0290419

Descripteurs français

Pascal (Inist)
- Modèle climat, Tropopause, Phénomène transport, Troposphère, Stratosphère, Transport, In situ, Ozone, Monoxyde carbone, Carbone monoxyde, Vapeur eau, NASA, Composé trace, Altitude, Coordonnée, Traceur, Epaisseur, Couche transition, Indicateur, Dynamique, Champ météorologique.

English descriptors

KwdEn :
- Carbon monoxide, Climate models, Meteorological field, NASA, Trace compound, Transition layer, Transport process, Tropopause, altitude, carbon monoxide, coordinates, dynamics, in situ, indicators, ozone, stratosphere, thickness, tracers, transport, troposphere, water vapor.

Abstract

[1] Three related diagnostics are used to evaluate the representation of chemical transport processes in the extratropical upper troposphere and lower stratosphere (UTLS) by chemistry-transport and chemistry-climate models. The diagnostics are based on in situ observations of ozone, carbon monoxide, water vapor profiles (obtained on board the NASA ER-2 research aircraft, near 65°N and during 1997), and their interrelationships in the UTLS. The first diagnostic compares the observed and modeled UTLS trace gas profiles in a relative altitude coordinate. The second one compares the observed and modeled UTLS tracer relationships. The third one compares the observed and modeled thickness of the tropopause transition layer. Together, they characterize the model's ability to reproduce the observed chemical distribution in the UTLS region and chemical transition across the extratropical tropopause. These are key indicators of whether the contributions of dynamics and chemistry to this region are correctly represented in the models. These diagnostics are used to evaluate the performance of an NCAR chemistry-transport model (CTM), MOZART-3, and a chemistry-climate model (CCM), WACCM3. Results from four model runs with different meteorological fields and grid resolution are examined. Overall, the NCAR models show qualitative agreement with the observations in the location of the chemical transition across the extratropical tropopause. Quantitatively, there are significant differences between the modeled and the observed chemical distributions. Both the meteorological field and grid resolutions are contributing factors to the differences.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A11	`01`	`1`		`@1 PAN (L. L.)`
A11	`02`	`1`		`@1 WEI (J. C.)`
A11	`03`	`1`		`@1 KINNISON (D. E.)`
A11	`04`	`1`		`@1 GARCIA (R. R.)`
A11	`05`	`1`		`@1 WUEBBLES (D. J.)`
A11	`06`	`1`		`@1 BRASSEUR (G. P.)`
A14	`01`			`@1 Atmospheric Chemistry Division, National Center for Atmospheric Research @2 Boulder, Colorado @3 USA @Z 1 aut. @Z 3 aut. @Z 4 aut. @Z 6 aut.`
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C01	`01`		`ENG`	@0 [1] Three related diagnostics are used to evaluate the representation of chemical transport processes in the extratropical upper troposphere and lower stratosphere (UTLS) by chemistry-transport and chemistry-climate models. The diagnostics are based on in situ observations of ozone, carbon monoxide, water vapor profiles (obtained on board the NASA ER-2 research aircraft, near 65°N and during 1997), and their interrelationships in the UTLS. The first diagnostic compares the observed and modeled UTLS trace gas profiles in a relative altitude coordinate. The second one compares the observed and modeled UTLS tracer relationships. The third one compares the observed and modeled thickness of the tropopause transition layer. Together, they characterize the model's ability to reproduce the observed chemical distribution in the UTLS region and chemical transition across the extratropical tropopause. These are key indicators of whether the contributions of dynamics and chemistry to this region are correctly represented in the models. These diagnostics are used to evaluate the performance of an NCAR chemistry-transport model (CTM), MOZART-3, and a chemistry-climate model (CCM), WACCM3. Results from four model runs with different meteorological fields and grid resolution are examined. Overall, the NCAR models show qualitative agreement with the observations in the location of the chemical transition across the extratropical tropopause. Quantitatively, there are significant differences between the modeled and the observed chemical distributions. Both the meteorological field and grid resolutions are contributing factors to the differences.
C02	`01`	`2`		`@0 220`
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C03	`08`	`2`	`FRE`	`@0 Ozone @5 08`
C03	`08`	`2`	`ENG`	`@0 ozone @5 08`
C03	`08`	`2`	`SPA`	`@0 Ozono @5 08`
C03	`09`	`2`	`FRE`	`@0 Monoxyde carbone @5 09`
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C03	`10`	`X`	`FRE`	`@0 Carbone monoxyde @2 NK @2 FX @5 10`
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C03	`14`	`2`	`SPA`	`@0 Altitud @5 14`
C03	`15`	`2`	`FRE`	`@0 Coordonnée @5 15`
C03	`15`	`2`	`ENG`	`@0 coordinates @5 15`
C03	`16`	`2`	`FRE`	`@0 Traceur @5 16`
C03	`16`	`2`	`ENG`	`@0 tracers @5 16`
C03	`16`	`2`	`SPA`	`@0 Trazador @5 16`
C03	`17`	`2`	`FRE`	`@0 Epaisseur @5 17`
C03	`17`	`2`	`ENG`	`@0 thickness @5 17`
C03	`17`	`2`	`SPA`	`@0 Espesor @5 17`
C03	`18`	`X`	`FRE`	`@0 Couche transition @5 18`
C03	`18`	`X`	`ENG`	`@0 Transition layer @5 18`
C03	`18`	`X`	`SPA`	`@0 Capa transición @5 18`
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C03	`20`	`2`	`SPA`	`@0 Dinámica @5 20`
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N44	`01`			`@1 OTO`
N82				`@1 OTO`

Format Inist (serveur)

NO :	PASCAL 07-0290419 INIST
ET :	A set of diagnostics for evaluating chemistry-climate models in the extratropical tropopause region
AU :	PAN (L. L.); WEI (J. C.); KINNISON (D. E.); GARCIA (R. R.); WUEBBLES (D. J.); BRASSEUR (G. P.)
AF :	Atmospheric Chemistry Division, National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (1 aut., 3 aut., 4 aut., 6 aut.); Department of Atmospheric Sciences, University of Illinois at Urbana-Champaign/Urbana, Illinois/Etats-Unis (2 aut., 5 aut.)
DT :	Publication en série; Niveau analytique
SO :	Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 2007; Vol. 112; No. D9; D09316.1-D09316.12; Bibl. 3/4 p.
LA :	Anglais
EA :	[1] Three related diagnostics are used to evaluate the representation of chemical transport processes in the extratropical upper troposphere and lower stratosphere (UTLS) by chemistry-transport and chemistry-climate models. The diagnostics are based on in situ observations of ozone, carbon monoxide, water vapor profiles (obtained on board the NASA ER-2 research aircraft, near 65°N and during 1997), and their interrelationships in the UTLS. The first diagnostic compares the observed and modeled UTLS trace gas profiles in a relative altitude coordinate. The second one compares the observed and modeled UTLS tracer relationships. The third one compares the observed and modeled thickness of the tropopause transition layer. Together, they characterize the model's ability to reproduce the observed chemical distribution in the UTLS region and chemical transition across the extratropical tropopause. These are key indicators of whether the contributions of dynamics and chemistry to this region are correctly represented in the models. These diagnostics are used to evaluate the performance of an NCAR chemistry-transport model (CTM), MOZART-3, and a chemistry-climate model (CCM), WACCM3. Results from four model runs with different meteorological fields and grid resolution are examined. Overall, the NCAR models show qualitative agreement with the observations in the location of the chemical transition across the extratropical tropopause. Quantitatively, there are significant differences between the modeled and the observed chemical distributions. Both the meteorological field and grid resolutions are contributing factors to the differences.
CC :	220; 001E; 001E01
FD :	Modèle climat; Tropopause; Phénomène transport; Troposphère; Stratosphère; Transport; In situ; Ozone; Monoxyde carbone; Carbone monoxyde; Vapeur eau; NASA; Composé trace; Altitude; Coordonnée; Traceur; Epaisseur; Couche transition; Indicateur; Dynamique; Champ météorologique
ED :	Climate models; Tropopause; Transport process; troposphere; stratosphere; transport; in situ; ozone; carbon monoxide; Carbon monoxide; water vapor; NASA; Trace compound; altitude; coordinates; tracers; thickness; Transition layer; indicators; dynamics; Meteorological field
SD :	Tropopausa; Fenómeno transporte; Estratosfera; Transporte; Ozono; Carbono monóxido; Vapor agua; Compuesto huella; Altitud; Trazador; Espesor; Capa transición; Dinámica; Campo meteorológico
LO :	INIST-3144.354000149880920490
ID :	07-0290419

Links to Exploration step

Pascal:07-0290419

Le document en format XML

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<front><div type="abstract" xml:lang="en">[1] Three related diagnostics are used to evaluate the representation of chemical transport processes in the extratropical upper troposphere and lower stratosphere (UTLS) by chemistry-transport and chemistry-climate models. The diagnostics are based on in situ observations of ozone, carbon monoxide, water vapor profiles (obtained on board the NASA ER-2 research aircraft, near 65°N and during 1997), and their interrelationships in the UTLS. The first diagnostic compares the observed and modeled UTLS trace gas profiles in a relative altitude coordinate. The second one compares the observed and modeled UTLS tracer relationships. The third one compares the observed and modeled thickness of the tropopause transition layer. Together, they characterize the model's ability to reproduce the observed chemical distribution in the UTLS region and chemical transition across the extratropical tropopause. These are key indicators of whether the contributions of dynamics and chemistry to this region are correctly represented in the models. These diagnostics are used to evaluate the performance of an NCAR chemistry-transport model (CTM), MOZART-3, and a chemistry-climate model (CCM), WACCM3. Results from four model runs with different meteorological fields and grid resolution are examined. Overall, the NCAR models show qualitative agreement with the observations in the location of the chemical transition across the extratropical tropopause. Quantitatively, there are significant differences between the modeled and the observed chemical distributions. Both the meteorological field and grid resolutions are contributing factors to the differences.</div>
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<fA14 i1="01"><s1>Atmospheric Chemistry Division, National Center for Atmospheric Research</s1>
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<sZ>5 aut.</sZ>
</fA14>
<fA20><s2>D09316.1-D09316.12</s2>
</fA20>
<fA21><s1>2007</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
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<fA43 i1="01"><s1>INIST</s1>
<s2>3144</s2>
<s5>354000149880920490</s5>
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<s1>© 2007 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>3/4 p.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>07-0290419</s0>
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<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Journal of geophysical research</s0>
</fA64>
<fA66 i1="01"><s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>[1] Three related diagnostics are used to evaluate the representation of chemical transport processes in the extratropical upper troposphere and lower stratosphere (UTLS) by chemistry-transport and chemistry-climate models. The diagnostics are based on in situ observations of ozone, carbon monoxide, water vapor profiles (obtained on board the NASA ER-2 research aircraft, near 65°N and during 1997), and their interrelationships in the UTLS. The first diagnostic compares the observed and modeled UTLS trace gas profiles in a relative altitude coordinate. The second one compares the observed and modeled UTLS tracer relationships. The third one compares the observed and modeled thickness of the tropopause transition layer. Together, they characterize the model's ability to reproduce the observed chemical distribution in the UTLS region and chemical transition across the extratropical tropopause. These are key indicators of whether the contributions of dynamics and chemistry to this region are correctly represented in the models. These diagnostics are used to evaluate the performance of an NCAR chemistry-transport model (CTM), MOZART-3, and a chemistry-climate model (CCM), WACCM3. Results from four model runs with different meteorological fields and grid resolution are examined. Overall, the NCAR models show qualitative agreement with the observations in the location of the chemical transition across the extratropical tropopause. Quantitatively, there are significant differences between the modeled and the observed chemical distributions. Both the meteorological field and grid resolutions are contributing factors to the differences.</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="3" l="FRE"><s0>Modèle climat</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="3" l="ENG"><s0>Climate models</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Tropopause</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Tropopause</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Tropopausa</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Phénomène transport</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Transport process</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Fenómeno transporte</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Troposphère</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>troposphere</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Stratosphère</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>stratosphere</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Estratosfera</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Transport</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>transport</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Transporte</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>In situ</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>in situ</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Ozone</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>ozone</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Ozono</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Monoxyde carbone</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>carbon monoxide</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Carbone monoxyde</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Carbon monoxide</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Carbono monóxido</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Vapeur eau</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>water vapor</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Vapor agua</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>NASA</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>NASA</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Composé trace</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Trace compound</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Compuesto huella</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Altitude</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>altitude</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Altitud</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Coordonnée</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>coordinates</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Traceur</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>tracers</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Trazador</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Epaisseur</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>thickness</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Espesor</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="X" l="FRE"><s0>Couche transition</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="X" l="ENG"><s0>Transition layer</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="X" l="SPA"><s0>Capa transición</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Indicateur</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>indicators</s0>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Dynamique</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>dynamics</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Dinámica</s0>
<s5>20</s5>
</fC03>
<fC03 i1="21" i2="X" l="FRE"><s0>Champ météorologique</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="X" l="ENG"><s0>Meteorological field</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="X" l="SPA"><s0>Campo meteorológico</s0>
<s5>21</s5>
</fC03>
<fN21><s1>190</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 07-0290419 INIST</NO>
<ET>A set of diagnostics for evaluating chemistry-climate models in the extratropical tropopause region</ET>
<AU>PAN (L. L.); WEI (J. C.); KINNISON (D. E.); GARCIA (R. R.); WUEBBLES (D. J.); BRASSEUR (G. P.)</AU>
<AF>Atmospheric Chemistry Division, National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (1 aut., 3 aut., 4 aut., 6 aut.); Department of Atmospheric Sciences, University of Illinois at Urbana-Champaign/Urbana, Illinois/Etats-Unis (2 aut., 5 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 2007; Vol. 112; No. D9; D09316.1-D09316.12; Bibl. 3/4 p.</SO>
<LA>Anglais</LA>
<EA>[1] Three related diagnostics are used to evaluate the representation of chemical transport processes in the extratropical upper troposphere and lower stratosphere (UTLS) by chemistry-transport and chemistry-climate models. The diagnostics are based on in situ observations of ozone, carbon monoxide, water vapor profiles (obtained on board the NASA ER-2 research aircraft, near 65°N and during 1997), and their interrelationships in the UTLS. The first diagnostic compares the observed and modeled UTLS trace gas profiles in a relative altitude coordinate. The second one compares the observed and modeled UTLS tracer relationships. The third one compares the observed and modeled thickness of the tropopause transition layer. Together, they characterize the model's ability to reproduce the observed chemical distribution in the UTLS region and chemical transition across the extratropical tropopause. These are key indicators of whether the contributions of dynamics and chemistry to this region are correctly represented in the models. These diagnostics are used to evaluate the performance of an NCAR chemistry-transport model (CTM), MOZART-3, and a chemistry-climate model (CCM), WACCM3. Results from four model runs with different meteorological fields and grid resolution are examined. Overall, the NCAR models show qualitative agreement with the observations in the location of the chemical transition across the extratropical tropopause. Quantitatively, there are significant differences between the modeled and the observed chemical distributions. Both the meteorological field and grid resolutions are contributing factors to the differences.</EA>
<CC>220; 001E; 001E01</CC>
<FD>Modèle climat; Tropopause; Phénomène transport; Troposphère; Stratosphère; Transport; In situ; Ozone; Monoxyde carbone; Carbone monoxyde; Vapeur eau; NASA; Composé trace; Altitude; Coordonnée; Traceur; Epaisseur; Couche transition; Indicateur; Dynamique; Champ météorologique</FD>
<ED>Climate models; Tropopause; Transport process; troposphere; stratosphere; transport; in situ; ozone; carbon monoxide; Carbon monoxide; water vapor; NASA; Trace compound; altitude; coordinates; tracers; thickness; Transition layer; indicators; dynamics; Meteorological field</ED>
<SD>Tropopausa; Fenómeno transporte; Estratosfera; Transporte; Ozono; Carbono monóxido; Vapor agua; Compuesto huella; Altitud; Trazador; Espesor; Capa transición; Dinámica; Campo meteorológico</SD>
<LO>INIST-3144.354000149880920490</LO>
<ID>07-0290419</ID>
</server>
</inist>
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A set of diagnostics for evaluating chemistry-climate models in the extratropical tropopause region

A set of diagnostics for evaluating chemistry-climate models in the extratropical tropopause region

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