AustralieFrV1, PascalFrancis, Curation, bibRecord, 003387

Trends in North Atlantic sea-surface fC02 from 1990 to 2006

Identifieur interne : 003387 ( PascalFrancis/Curation ); précédent : 003386; suivant : 003388

Trends in North Atlantic sea-surface fC02 from 1990 to 2006

Auteurs : U. Schuster [Royaume-Uni] ; A. J. Watson [Royaume-Uni] ; N. R. Bates ; A. Corbiere [France] ; M. Gonzalez-Davila [Espagne] ; N. Metzl [France] ; D. Pierrot [États-Unis] ; M. Santana-Casiano [Espagne]

Source :

Deep-sea research. Part 2. Topical studies in oceanography [ 0967-0645 ] ; 2009.

RBID : Pascal:09-0358081

Descripteurs français

Pascal (Inist)
- Analyse tendance, Surface marine, Série temporelle, Variation annuelle, Zone subtropicale, Atmosphère, Air, Latitude, Basse fréquence, Oscillation Atlantique Nord, Plomb, Température surface marine, Circulation, Mixage, Mélangeage, Océan Atlantique Nord, Mer du Nord.
Wicri :
- topic : Zone subtropicale, Atmosphère, Plomb, Mer du Nord.

English descriptors

KwdEn :
- Mixing, North Atlantic, North Atlantic oscillation, North Sea, Sea surface, Sea surface temperature, Time series, air, annual variations, atmosphere, circulation, latitude, lead, low frequency, mixing, subtropical zone, trend-surface analysis.

Abstract

We examine observations from 1990 to 2006 from four voluntary observing ships and two time-series stations in the North Atlantic, fitting a sinusoidal annual cycle and linear year-on-year trend at all locations where there are sufficient data. Results show that in the subtropical regions, sea-surface fCO₂ has closely followed the increasing trend in atmospheric fCO₂. In contrast, farther north, sea-surface fCO₂ has increased faster than fCO₂ in the atmosphere. The resulting ΔfCO₂, driving air-sea flux of CO₂, has therefore decreased in the North Atlantic, particularly at higher latitudes, as has the annual mean air-sea flux. Several underlying causes may have led to the observed changes in sea-surface fCO₂. Low-frequency modes, such as the North Atlantic Oscillation, lead to changes in the sea-surface temperature, in sea-surface circulation and in vertical mixing, affecting sea-surface fCO₂ through biogeochemical processes. A comparison with measurements covering a longer time period shows that the sea-surface fCO₂ rise has accelerated since 1990 in the northern North Atlantic.

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N. R. Bates

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Le document en format XML

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<front><div type="abstract" xml:lang="en">We examine observations from 1990 to 2006 from four voluntary observing ships and two time-series stations in the North Atlantic, fitting a sinusoidal annual cycle and linear year-on-year trend at all locations where there are sufficient data. Results show that in the subtropical regions, sea-surface fCO<sub>2</sub>
 has closely followed the increasing trend in atmospheric fCO<sub>2</sub>
. In contrast, farther north, sea-surface fCO<sub>2</sub>
 has increased faster than fCO<sub>2</sub>
 in the atmosphere. The resulting ΔfCO<sub>2</sub>
, driving air-sea flux of CO<sub>2</sub>
, has therefore decreased in the North Atlantic, particularly at higher latitudes, as has the annual mean air-sea flux. Several underlying causes may have led to the observed changes in sea-surface fCO<sub>2</sub>
. Low-frequency modes, such as the North Atlantic Oscillation, lead to changes in the sea-surface temperature, in sea-surface circulation and in vertical mixing, affecting sea-surface fCO<sub>2</sub>
 through biogeochemical processes. A comparison with measurements covering a longer time period shows that the sea-surface fCO<sub>2</sub>
 rise has accelerated since 1990 in the northern North Atlantic.</div>
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<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0967-0645</s0>
</fA01>
<fA03 i2="1"><s0>Deep-sea res., Part 2, Top. stud. oceanogr.</s0>
</fA03>
<fA05><s2>56</s2>
</fA05>
<fA06><s2>8-10</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Trends in North Atlantic sea-surface fC0<sub>2</sub>
 from 1990 to 2006</s1>
</fA08>
<fA09 i1="01" i2="1" l="ENG"><s1>Surface Ocean CO<sub>2</sub>
 Variabilities and Vulnerabilities</s1>
</fA09>
<fA11 i1="01" i2="1"><s1>SCHUSTER (U.)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>WATSON (A. J.)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>BATES (N. R.)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>CORBIERE (A.)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>GONZALEZ-DAVILA (M.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>METZL (N.)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>PIERROT (D.)</s1>
</fA11>
<fA11 i1="08" i2="1"><s1>SANTANA-CASIANO (M.)</s1>
</fA11>
<fA12 i1="01" i2="1"><s1>ROY (Sylvie)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="02" i2="1"><s1>METZL (Nicolas)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="03" i2="1"><s1>TILBROOK (Bronte)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="04" i2="1"><s1>DONEY (Scott C.)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="05" i2="1"><s1>FEELY (Richard A.)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="06" i2="1"><s1>BAKKER (Dorothee)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="07" i2="1"><s1>LE QUERE (Corinne)</s1>
<s9>ed.</s9>
</fA12>
<fA14 i1="01"><s1>School of Environmental Science, University of East Anglia</s1>
<s2>Norwich</s2>
<s3>GBR</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Bermuda Institute of Ocean Sciences</s1>
<s2>Ferry Reach, GE01</s2>
<s3>BMU</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Laboratoire d'Océanographie et du Climat, LOCEAN/IPSL, CNRS, Université Pierre, et Marie Curie</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>4 aut.</sZ>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Department of Marine Chemistry, Universidad de Las Palmas de Gran Canaria, 35017 Las Palmas de</s1>
<s2>Gran Canaria</s2>
<s3>ESP</s3>
<sZ>5 aut.</sZ>
<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration</s1>
<s2>Miami, FL</s2>
<s3>USA</s3>
<sZ>7 aut.</sZ>
</fA14>
<fA15 i1="01"><s1>Institut Universitaire Européenne de la Mer, IMBER International Project Office, Technopôle Brest-Iroise, Place Nicolas Copernic</s1>
<s2>Plouzané 29280</s2>
<s3>FRA</s3>
<sZ>1 aut.</sZ>
</fA15>
<fA15 i1="02"><s1>LOCEAN/IPSL, CNRS, Univ. P.M. Curie, Case 100, 4 pl. Jussieu</s1>
<s2>75252 Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
</fA15>
<fA15 i1="03"><s1>CSIRO Marine and Atmospheric Research, Castray Esplanade</s1>
<s2>Hobart TAS 7000</s2>
<s3>AUS</s3>
<sZ>3 aut.</sZ>
</fA15>
<fA20><s1>620-629</s1>
</fA20>
<fA21><s1>2009</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>7679A2</s2>
<s5>354000187106900100</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2009 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>3/4 p.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>09-0358081</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Deep-sea research. Part 2. Topical studies in oceanography</s0>
</fA64>
<fA66 i1="01"><s0>GBR</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>We examine observations from 1990 to 2006 from four voluntary observing ships and two time-series stations in the North Atlantic, fitting a sinusoidal annual cycle and linear year-on-year trend at all locations where there are sufficient data. Results show that in the subtropical regions, sea-surface fCO<sub>2</sub>
 has closely followed the increasing trend in atmospheric fCO<sub>2</sub>
. In contrast, farther north, sea-surface fCO<sub>2</sub>
 has increased faster than fCO<sub>2</sub>
 in the atmosphere. The resulting ΔfCO<sub>2</sub>
, driving air-sea flux of CO<sub>2</sub>
, has therefore decreased in the North Atlantic, particularly at higher latitudes, as has the annual mean air-sea flux. Several underlying causes may have led to the observed changes in sea-surface fCO<sub>2</sub>
. Low-frequency modes, such as the North Atlantic Oscillation, lead to changes in the sea-surface temperature, in sea-surface circulation and in vertical mixing, affecting sea-surface fCO<sub>2</sub>
 through biogeochemical processes. A comparison with measurements covering a longer time period shows that the sea-surface fCO<sub>2</sub>
 rise has accelerated since 1990 in the northern North Atlantic.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>001E02B</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>001E01P02</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>001E01H</s0>
</fC02>
<fC02 i1="04" i2="2"><s0>226C02</s0>
</fC02>
<fC02 i1="05" i2="2"><s0>223B</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Analyse tendance</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>trend-surface analysis</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Análisis tendencia</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Surface marine</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Sea surface</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Superficie marina</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Série temporelle</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Time series</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Serie temporal</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Variation annuelle</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>annual variations</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Variación anual</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Zone subtropicale</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>subtropical zone</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Zona subtropical</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Atmosphère</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>atmosphere</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Atmósfera</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Air</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>air</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Latitude</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>latitude</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Basse fréquence</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>low frequency</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Oscillation Atlantique Nord</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>North Atlantic oscillation</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Oscilación Atlántico Norte</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Plomb</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>lead</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Plomo</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE"><s0>Température surface marine</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>Sea surface temperature</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>Temperature superficie marina</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Circulation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>circulation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Mixage</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>mixing</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Mezcla</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE"><s0>Mélangeage</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG"><s0>Mixing</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA"><s0>Mezclado</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Océan Atlantique Nord</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>North Atlantic</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Océano Atlántico Norte</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Mer du Nord</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>North Sea</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Mar del Norte</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Océan Atlantique</s0>
<s2>564</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Atlantic Ocean</s0>
<s2>564</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Océano Atlántico</s0>
<s2>564</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Océan Atlantique Nord Est</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Northeast Atlantic</s0>
<s2>NG</s2>
</fC07>
<fN21><s1>257</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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	Serveur d'exploration sur les relations entre la France et l'Australie
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Trends in North Atlantic sea-surface fC02 from 1990 to 2006

Trends in North Atlantic sea-surface fC02 from 1990 to 2006

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