MozartV1, PascalFrancis, Corpus, bibRecord, 000177

Analysis of seasonal and interannual variability in transpacific transport

Identifieur interne : 000177 ( PascalFrancis/Corpus ); précédent : 000176; suivant : 000178

Analysis of seasonal and interannual variability in transpacific transport

Auteurs : JUNFENG LIU ; Denise L. Mauzerall ; Larry W. Horowitz

Source :

Journal of geophysical research [ 0148-0227 ] ; 2005.

RBID : Pascal:05-0166150

Descripteurs français

Pascal (Inist)
- Océan Pacifique Nord, Variation interannuelle, Transport, Traceur, Durée vie, Monde, Modèle, Ozone, Météorologie, Moyenne latitude, Source, Printemps, Hiver, Haute latitude, Eté, El Nino, Amérique du Nord, Oscillation australe, Interaction atmosphère océan.

English descriptors

KwdEn :
- El Nino, High latitude, Interannual variation, Lifetime, Mid latitude, North America, North Pacific, Southern oscillation, Spring(season), Summer, Winter, global, meteorology, models, ocean-atmosphere interaction, ozone, springs, tracers, transport.

Abstract

[1] The purpose of our analysis is both to evaluate the meteorological component of the seasonal and interannual variability of transpacific transport and to identify meteorological features that can be used to estimate transpacific transport. To accomplish this goal, we simulate the transport of nine continental tracers with uniform emissions and two-week lifetimes using the global Model of Ozone and Related Tracers Version 2 (MOZART-2) driven with NCEP reanalysis meteorology from 1991-2001. In addition, we define a transpacific "transport potential," a measure of the quantity of a tracer transported from a particular region normalized by its total emissions from that region, across a meridional plane in the eastern Pacific at 130°W. We find that at midlatitudes, the east Asian and Indian tracers have the largest transport potentials, particularly in spring. The interannual variability of the transpacific transport potentials of most tracers is relatively high in winter and fall (particularly in February and September) but is low from April to August. At high latitudes the former Soviet Union, east Asian, and European tracers have the largest transpacific transport potentials, especially in late summer and fall, when the lowest interannual variability is observed. We find that El Niño winters are associated with stronger eastward transport of east Asian emissions in the subtropical eastern Pacific. Transport of the east Asian tracer in the central North Pacific is well correlated with the North Pacific Index. However, we find that the interannual variability of transport across the west coast of North America is mostly driven by local meteorology. We therefore created a new index based on meteorology over the eastern Pacific, which we call the Eastern Pacific Index (EPI). The EPI captures most of the interannual variability of transpacific transport at both middle- and high-latitude regions across the west coast of North America.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A03		`1`		`@0 J. geophys. res.`
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A08	`01`	`1`	`ENG`	`@1 Analysis of seasonal and interannual variability in transpacific transport`
A11	`01`	`1`		`@1 JUNFENG LIU`
A11	`02`	`1`		`@1 MAUZERALL (Denise L.)`
A11	`03`	`1`		`@1 HOROWITZ (Larry W.)`
A14	`01`			`@1 Woodrow Wilson School of Public and Intemational Affairs, Princeton University @2 Princeton, New Jersey @3 USA @Z 1 aut. @Z 2 aut.`
A14	`02`			`@1 Geophysical Fluid Dynamics Laboratory @2 Princeton, New Jersey @3 USA @Z 3 aut.`
A20				`@2 D04302.1-D04302.17`
A21				`@1 2005`
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A43	`01`			`@1 INIST @2 3144 @5 354000126883480140`
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C01	`01`		`ENG`	@0 [1] The purpose of our analysis is both to evaluate the meteorological component of the seasonal and interannual variability of transpacific transport and to identify meteorological features that can be used to estimate transpacific transport. To accomplish this goal, we simulate the transport of nine continental tracers with uniform emissions and two-week lifetimes using the global Model of Ozone and Related Tracers Version 2 (MOZART-2) driven with NCEP reanalysis meteorology from 1991-2001. In addition, we define a transpacific "transport potential," a measure of the quantity of a tracer transported from a particular region normalized by its total emissions from that region, across a meridional plane in the eastern Pacific at 130°W. We find that at midlatitudes, the east Asian and Indian tracers have the largest transport potentials, particularly in spring. The interannual variability of the transpacific transport potentials of most tracers is relatively high in winter and fall (particularly in February and September) but is low from April to August. At high latitudes the former Soviet Union, east Asian, and European tracers have the largest transpacific transport potentials, especially in late summer and fall, when the lowest interannual variability is observed. We find that El Niño winters are associated with stronger eastward transport of east Asian emissions in the subtropical eastern Pacific. Transport of the east Asian tracer in the central North Pacific is well correlated with the North Pacific Index. However, we find that the interannual variability of transport across the west coast of North America is mostly driven by local meteorology. We therefore created a new index based on meteorology over the eastern Pacific, which we call the Eastern Pacific Index (EPI). The EPI captures most of the interannual variability of transpacific transport at both middle- and high-latitude regions across the west coast of North America.
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C02	`03`	`2`		`@0 001E01`
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C03	`01`	`2`	`ENG`	`@0 North Pacific @2 NG @5 01`
C03	`02`	`X`	`FRE`	`@0 Variation interannuelle @5 06`
C03	`02`	`X`	`ENG`	`@0 Interannual variation @5 06`
C03	`02`	`X`	`SPA`	`@0 Variación interanual @5 06`
C03	`03`	`2`	`FRE`	`@0 Transport @5 07`
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C03	`03`	`2`	`SPA`	`@0 Transporte @5 07`
C03	`04`	`2`	`FRE`	`@0 Traceur @5 08`
C03	`04`	`2`	`ENG`	`@0 tracers @5 08`
C03	`04`	`2`	`SPA`	`@0 Trazador @5 08`
C03	`05`	`X`	`FRE`	`@0 Durée vie @5 09`
C03	`05`	`X`	`ENG`	`@0 Lifetime @5 09`
C03	`05`	`X`	`SPA`	`@0 Tiempo vida @5 09`
C03	`06`	`2`	`FRE`	`@0 Monde @5 10`
C03	`06`	`2`	`ENG`	`@0 global @5 10`
C03	`06`	`2`	`SPA`	`@0 Mundo @5 10`
C03	`07`	`2`	`FRE`	`@0 Modèle @5 11`
C03	`07`	`2`	`ENG`	`@0 models @5 11`
C03	`07`	`2`	`SPA`	`@0 Modelo @5 11`
C03	`08`	`2`	`FRE`	`@0 Ozone @5 12`
C03	`08`	`2`	`ENG`	`@0 ozone @5 12`
C03	`08`	`2`	`SPA`	`@0 Ozono @5 12`
C03	`09`	`2`	`FRE`	`@0 Météorologie @5 13`
C03	`09`	`2`	`ENG`	`@0 meteorology @5 13`
C03	`09`	`2`	`SPA`	`@0 Meteorología @5 13`
C03	`10`	`X`	`FRE`	`@0 Moyenne latitude @5 14`
C03	`10`	`X`	`ENG`	`@0 Mid latitude @5 14`
C03	`10`	`X`	`SPA`	`@0 Latitud media @5 14`
C03	`11`	`2`	`FRE`	`@0 Source @5 15`
C03	`11`	`2`	`ENG`	`@0 springs @5 15`
C03	`11`	`2`	`SPA`	`@0 Fuente @5 15`
C03	`12`	`X`	`FRE`	`@0 Printemps @5 16`
C03	`12`	`X`	`ENG`	`@0 Spring(season) @5 16`
C03	`12`	`X`	`SPA`	`@0 Primavera @5 16`
C03	`13`	`X`	`FRE`	`@0 Hiver @5 17`
C03	`13`	`X`	`ENG`	`@0 Winter @5 17`
C03	`13`	`X`	`SPA`	`@0 Invierno @5 17`
C03	`14`	`X`	`FRE`	`@0 Haute latitude @5 18`
C03	`14`	`X`	`ENG`	`@0 High latitude @5 18`
C03	`14`	`X`	`SPA`	`@0 Alta latitud @5 18`
C03	`15`	`X`	`FRE`	`@0 Eté @5 19`
C03	`15`	`X`	`ENG`	`@0 Summer @5 19`
C03	`15`	`X`	`SPA`	`@0 Verano @5 19`
C03	`16`	`2`	`FRE`	`@0 El Nino @5 20`
C03	`16`	`2`	`ENG`	`@0 El Nino @5 20`
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`	`X`	`FRE`	`@0 Oscillation australe @5 23`
C03	`18`	`X`	`ENG`	`@0 Southern oscillation @5 23`
C03	`18`	`X`	`SPA`	`@0 Oscilación austral @5 23`
C03	`19`	`2`	`FRE`	`@0 Interaction atmosphère océan @5 24`
C03	`19`	`2`	`ENG`	`@0 ocean-atmosphere interaction @5 24`
C07	`01`	`2`	`FRE`	`@0 Océan Pacifique`
C07	`01`	`2`	`ENG`	`@0 Pacific Ocean`
C07	`01`	`2`	`SPA`	`@0 Océano Pacífico`
N21				`@1 108`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

Format Inist (serveur)

NO :	PASCAL 05-0166150 INIST
ET :	Analysis of seasonal and interannual variability in transpacific transport
AU :	JUNFENG LIU; MAUZERALL (Denise L.); HOROWITZ (Larry W.)
AF :	Woodrow Wilson School of Public and Intemational Affairs, Princeton University/Princeton, New Jersey/Etats-Unis (1 aut., 2 aut.); Geophysical Fluid Dynamics Laboratory/Princeton, New Jersey/Etats-Unis (3 aut.)
DT :	Publication en série; Niveau analytique
SO :	Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 2005; Vol. 110; No. D4; D04302.1-D04302.17; Bibl. 38 ref.
LA :	Anglais
EA :	[1] The purpose of our analysis is both to evaluate the meteorological component of the seasonal and interannual variability of transpacific transport and to identify meteorological features that can be used to estimate transpacific transport. To accomplish this goal, we simulate the transport of nine continental tracers with uniform emissions and two-week lifetimes using the global Model of Ozone and Related Tracers Version 2 (MOZART-2) driven with NCEP reanalysis meteorology from 1991-2001. In addition, we define a transpacific "transport potential," a measure of the quantity of a tracer transported from a particular region normalized by its total emissions from that region, across a meridional plane in the eastern Pacific at 130°W. We find that at midlatitudes, the east Asian and Indian tracers have the largest transport potentials, particularly in spring. The interannual variability of the transpacific transport potentials of most tracers is relatively high in winter and fall (particularly in February and September) but is low from April to August. At high latitudes the former Soviet Union, east Asian, and European tracers have the largest transpacific transport potentials, especially in late summer and fall, when the lowest interannual variability is observed. We find that El Niño winters are associated with stronger eastward transport of east Asian emissions in the subtropical eastern Pacific. Transport of the east Asian tracer in the central North Pacific is well correlated with the North Pacific Index. However, we find that the interannual variability of transport across the west coast of North America is mostly driven by local meteorology. We therefore created a new index based on meteorology over the eastern Pacific, which we call the Eastern Pacific Index (EPI). The EPI captures most of the interannual variability of transpacific transport at both middle- and high-latitude regions across the west coast of North America.
CC :	220; 001E; 001E01
FD :	Océan Pacifique Nord; Variation interannuelle; Transport; Traceur; Durée vie; Monde; Modèle; Ozone; Météorologie; Moyenne latitude; Source; Printemps; Hiver; Haute latitude; Eté; El Nino; Amérique du Nord; Oscillation australe; Interaction atmosphère océan
FG :	Océan Pacifique
ED :	North Pacific; Interannual variation; transport; tracers; Lifetime; global; models; ozone; meteorology; Mid latitude; springs; Spring(season); Winter; High latitude; Summer; El Nino; North America; Southern oscillation; ocean-atmosphere interaction
EG :	Pacific Ocean
SD :	Variación interanual; Transporte; Trazador; Tiempo vida; Mundo; Modelo; Ozono; Meteorología; Latitud media; Fuente; Primavera; Invierno; Alta latitud; Verano; America del norte; Oscilación austral
LO :	INIST-3144.354000126883480140
ID :	05-0166150

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Pascal:05-0166150

Le document en format XML

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<term>North Pacific</term>
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<term>Spring(season)</term>
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<front><div type="abstract" xml:lang="en">[1] The purpose of our analysis is both to evaluate the meteorological component of the seasonal and interannual variability of transpacific transport and to identify meteorological features that can be used to estimate transpacific transport. To accomplish this goal, we simulate the transport of nine continental tracers with uniform emissions and two-week lifetimes using the global Model of Ozone and Related Tracers Version 2 (MOZART-2) driven with NCEP reanalysis meteorology from 1991-2001. In addition, we define a transpacific "transport potential," a measure of the quantity of a tracer transported from a particular region normalized by its total emissions from that region, across a meridional plane in the eastern Pacific at 130°W. We find that at midlatitudes, the east Asian and Indian tracers have the largest transport potentials, particularly in spring. The interannual variability of the transpacific transport potentials of most tracers is relatively high in winter and fall (particularly in February and September) but is low from April to August. At high latitudes the former Soviet Union, east Asian, and European tracers have the largest transpacific transport potentials, especially in late summer and fall, when the lowest interannual variability is observed. We find that El Niño winters are associated with stronger eastward transport of east Asian emissions in the subtropical eastern Pacific. Transport of the east Asian tracer in the central North Pacific is well correlated with the North Pacific Index. However, we find that the interannual variability of transport across the west coast of North America is mostly driven by local meteorology. We therefore created a new index based on meteorology over the eastern Pacific, which we call the Eastern Pacific Index (EPI). The EPI captures most of the interannual variability of transpacific transport at both middle- and high-latitude regions across the west coast of North America.</div>
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<fC01 i1="01" l="ENG"><s0>[1] The purpose of our analysis is both to evaluate the meteorological component of the seasonal and interannual variability of transpacific transport and to identify meteorological features that can be used to estimate transpacific transport. To accomplish this goal, we simulate the transport of nine continental tracers with uniform emissions and two-week lifetimes using the global Model of Ozone and Related Tracers Version 2 (MOZART-2) driven with NCEP reanalysis meteorology from 1991-2001. In addition, we define a transpacific "transport potential," a measure of the quantity of a tracer transported from a particular region normalized by its total emissions from that region, across a meridional plane in the eastern Pacific at 130°W. We find that at midlatitudes, the east Asian and Indian tracers have the largest transport potentials, particularly in spring. The interannual variability of the transpacific transport potentials of most tracers is relatively high in winter and fall (particularly in February and September) but is low from April to August. At high latitudes the former Soviet Union, east Asian, and European tracers have the largest transpacific transport potentials, especially in late summer and fall, when the lowest interannual variability is observed. We find that El Niño winters are associated with stronger eastward transport of east Asian emissions in the subtropical eastern Pacific. Transport of the east Asian tracer in the central North Pacific is well correlated with the North Pacific Index. However, we find that the interannual variability of transport across the west coast of North America is mostly driven by local meteorology. We therefore created a new index based on meteorology over the eastern Pacific, which we call the Eastern Pacific Index (EPI). The EPI captures most of the interannual variability of transpacific transport at both middle- and high-latitude regions across the west coast of North America.</s0>
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<s5>07</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Traceur</s0>
<s5>08</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>tracers</s0>
<s5>08</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Trazador</s0>
<s5>08</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Durée vie</s0>
<s5>09</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Lifetime</s0>
<s5>09</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Tiempo vida</s0>
<s5>09</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Monde</s0>
<s5>10</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>global</s0>
<s5>10</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Mundo</s0>
<s5>10</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Modèle</s0>
<s5>11</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>models</s0>
<s5>11</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Modelo</s0>
<s5>11</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Ozone</s0>
<s5>12</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>ozone</s0>
<s5>12</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Ozono</s0>
<s5>12</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Météorologie</s0>
<s5>13</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>meteorology</s0>
<s5>13</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Meteorología</s0>
<s5>13</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Moyenne latitude</s0>
<s5>14</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Mid latitude</s0>
<s5>14</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Latitud media</s0>
<s5>14</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Source</s0>
<s5>15</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>springs</s0>
<s5>15</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Fuente</s0>
<s5>15</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE"><s0>Printemps</s0>
<s5>16</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>Spring(season)</s0>
<s5>16</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>Primavera</s0>
<s5>16</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Hiver</s0>
<s5>17</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Winter</s0>
<s5>17</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Invierno</s0>
<s5>17</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Haute latitude</s0>
<s5>18</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>High latitude</s0>
<s5>18</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Alta latitud</s0>
<s5>18</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE"><s0>Eté</s0>
<s5>19</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG"><s0>Summer</s0>
<s5>19</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA"><s0>Verano</s0>
<s5>19</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>El Nino</s0>
<s5>20</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>El Nino</s0>
<s5>20</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="X" l="FRE"><s0>Oscillation australe</s0>
<s5>23</s5>
</fC03>
<fC03 i1="18" i2="X" l="ENG"><s0>Southern oscillation</s0>
<s5>23</s5>
</fC03>
<fC03 i1="18" i2="X" l="SPA"><s0>Oscilación austral</s0>
<s5>23</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Interaction atmosphère océan</s0>
<s5>24</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>ocean-atmosphere interaction</s0>
<s5>24</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Océan Pacifique</s0>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Pacific Ocean</s0>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Océano Pacífico</s0>
</fC07>
<fN21><s1>108</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 05-0166150 INIST</NO>
<ET>Analysis of seasonal and interannual variability in transpacific transport</ET>
<AU>JUNFENG LIU; MAUZERALL (Denise L.); HOROWITZ (Larry W.)</AU>
<AF>Woodrow Wilson School of Public and Intemational Affairs, Princeton University/Princeton, New Jersey/Etats-Unis (1 aut., 2 aut.); Geophysical Fluid Dynamics Laboratory/Princeton, New Jersey/Etats-Unis (3 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 2005; Vol. 110; No. D4; D04302.1-D04302.17; Bibl. 38 ref.</SO>
<LA>Anglais</LA>
<EA>[1] The purpose of our analysis is both to evaluate the meteorological component of the seasonal and interannual variability of transpacific transport and to identify meteorological features that can be used to estimate transpacific transport. To accomplish this goal, we simulate the transport of nine continental tracers with uniform emissions and two-week lifetimes using the global Model of Ozone and Related Tracers Version 2 (MOZART-2) driven with NCEP reanalysis meteorology from 1991-2001. In addition, we define a transpacific "transport potential," a measure of the quantity of a tracer transported from a particular region normalized by its total emissions from that region, across a meridional plane in the eastern Pacific at 130°W. We find that at midlatitudes, the east Asian and Indian tracers have the largest transport potentials, particularly in spring. The interannual variability of the transpacific transport potentials of most tracers is relatively high in winter and fall (particularly in February and September) but is low from April to August. At high latitudes the former Soviet Union, east Asian, and European tracers have the largest transpacific transport potentials, especially in late summer and fall, when the lowest interannual variability is observed. We find that El Niño winters are associated with stronger eastward transport of east Asian emissions in the subtropical eastern Pacific. Transport of the east Asian tracer in the central North Pacific is well correlated with the North Pacific Index. However, we find that the interannual variability of transport across the west coast of North America is mostly driven by local meteorology. We therefore created a new index based on meteorology over the eastern Pacific, which we call the Eastern Pacific Index (EPI). The EPI captures most of the interannual variability of transpacific transport at both middle- and high-latitude regions across the west coast of North America.</EA>
<CC>220; 001E; 001E01</CC>
<FD>Océan Pacifique Nord; Variation interannuelle; Transport; Traceur; Durée vie; Monde; Modèle; Ozone; Météorologie; Moyenne latitude; Source; Printemps; Hiver; Haute latitude; Eté; El Nino; Amérique du Nord; Oscillation australe; Interaction atmosphère océan</FD>
<FG>Océan Pacifique</FG>
<ED>North Pacific; Interannual variation; transport; tracers; Lifetime; global; models; ozone; meteorology; Mid latitude; springs; Spring(season); Winter; High latitude; Summer; El Nino; North America; Southern oscillation; ocean-atmosphere interaction</ED>
<EG>Pacific Ocean</EG>
<SD>Variación interanual; Transporte; Trazador; Tiempo vida; Mundo; Modelo; Ozono; Meteorología; Latitud media; Fuente; Primavera; Invierno; Alta latitud; Verano; America del norte; Oscilación austral</SD>
<LO>INIST-3144.354000126883480140</LO>
<ID>05-0166150</ID>
</server>
</inist>
</record>

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Analysis of seasonal and interannual variability in transpacific transport

Analysis of seasonal and interannual variability in transpacific transport

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