Changes of the North Atlantic sea surface temperature related to the atmospheric circulation in the period 1973 to 1992
Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SS...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
H. Malberg [verfasserIn] G. Frattesi [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1995 |
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| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
In: Meteorologische Zeitschrift - Borntraeger, 2014, 4(1995), 1, Seite 37-42 |
|---|---|
| Übergeordnetes Werk: |
volume:4 ; year:1995 ; number:1 ; pages:37-42 |
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|---|
| DOI / URN: |
10.1127/metz/4/1995/37 |
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DOAJ094748624 |
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| 520 | |a Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SST. At the surface as well as at 500 hPa a significant intensification of the Icelandic low and a strengthening of the frontal zone over the northern Atlantic Ocean correspond to the changes of SST and thus to the air temperature near the surface. | ||
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10.1127/metz/4/1995/37 doi (DE-627)DOAJ094748624 (DE-599)DOAJaa8e226aae9f4db383391d7afc98c822 DE-627 ger DE-627 rakwb eng QC851-999 H. Malberg verfasserin aut Changes of the North Atlantic sea surface temperature related to the atmospheric circulation in the period 1973 to 1992 1995 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SST. At the surface as well as at 500 hPa a significant intensification of the Icelandic low and a strengthening of the frontal zone over the northern Atlantic Ocean correspond to the changes of SST and thus to the air temperature near the surface. subtropical atlantic eastern atlantic meeresoberflächentemperatur Meteorology. Climatology G. Frattesi verfasserin aut In Meteorologische Zeitschrift Borntraeger, 2014 4(1995), 1, Seite 37-42 (DE-627)328187488 (DE-600)2045168-4 16101227 nnns volume:4 year:1995 number:1 pages:37-42 https://doi.org/10.1127/metz/4/1995/37 kostenfrei https://doaj.org/article/aa8e226aae9f4db383391d7afc98c822 kostenfrei http://dx.doi.org/10.1127/metz/4/1995/37 kostenfrei https://doaj.org/toc/0941-2948 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_62 GBV_ILN_70 GBV_ILN_2018 AR 4 1995 1 37-42 |
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10.1127/metz/4/1995/37 doi (DE-627)DOAJ094748624 (DE-599)DOAJaa8e226aae9f4db383391d7afc98c822 DE-627 ger DE-627 rakwb eng QC851-999 H. Malberg verfasserin aut Changes of the North Atlantic sea surface temperature related to the atmospheric circulation in the period 1973 to 1992 1995 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SST. At the surface as well as at 500 hPa a significant intensification of the Icelandic low and a strengthening of the frontal zone over the northern Atlantic Ocean correspond to the changes of SST and thus to the air temperature near the surface. subtropical atlantic eastern atlantic meeresoberflächentemperatur Meteorology. Climatology G. Frattesi verfasserin aut In Meteorologische Zeitschrift Borntraeger, 2014 4(1995), 1, Seite 37-42 (DE-627)328187488 (DE-600)2045168-4 16101227 nnns volume:4 year:1995 number:1 pages:37-42 https://doi.org/10.1127/metz/4/1995/37 kostenfrei https://doaj.org/article/aa8e226aae9f4db383391d7afc98c822 kostenfrei http://dx.doi.org/10.1127/metz/4/1995/37 kostenfrei https://doaj.org/toc/0941-2948 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_62 GBV_ILN_70 GBV_ILN_2018 AR 4 1995 1 37-42 |
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10.1127/metz/4/1995/37 doi (DE-627)DOAJ094748624 (DE-599)DOAJaa8e226aae9f4db383391d7afc98c822 DE-627 ger DE-627 rakwb eng QC851-999 H. Malberg verfasserin aut Changes of the North Atlantic sea surface temperature related to the atmospheric circulation in the period 1973 to 1992 1995 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SST. At the surface as well as at 500 hPa a significant intensification of the Icelandic low and a strengthening of the frontal zone over the northern Atlantic Ocean correspond to the changes of SST and thus to the air temperature near the surface. subtropical atlantic eastern atlantic meeresoberflächentemperatur Meteorology. Climatology G. Frattesi verfasserin aut In Meteorologische Zeitschrift Borntraeger, 2014 4(1995), 1, Seite 37-42 (DE-627)328187488 (DE-600)2045168-4 16101227 nnns volume:4 year:1995 number:1 pages:37-42 https://doi.org/10.1127/metz/4/1995/37 kostenfrei https://doaj.org/article/aa8e226aae9f4db383391d7afc98c822 kostenfrei http://dx.doi.org/10.1127/metz/4/1995/37 kostenfrei https://doaj.org/toc/0941-2948 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_62 GBV_ILN_70 GBV_ILN_2018 AR 4 1995 1 37-42 |
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10.1127/metz/4/1995/37 doi (DE-627)DOAJ094748624 (DE-599)DOAJaa8e226aae9f4db383391d7afc98c822 DE-627 ger DE-627 rakwb eng QC851-999 H. Malberg verfasserin aut Changes of the North Atlantic sea surface temperature related to the atmospheric circulation in the period 1973 to 1992 1995 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SST. At the surface as well as at 500 hPa a significant intensification of the Icelandic low and a strengthening of the frontal zone over the northern Atlantic Ocean correspond to the changes of SST and thus to the air temperature near the surface. subtropical atlantic eastern atlantic meeresoberflächentemperatur Meteorology. Climatology G. Frattesi verfasserin aut In Meteorologische Zeitschrift Borntraeger, 2014 4(1995), 1, Seite 37-42 (DE-627)328187488 (DE-600)2045168-4 16101227 nnns volume:4 year:1995 number:1 pages:37-42 https://doi.org/10.1127/metz/4/1995/37 kostenfrei https://doaj.org/article/aa8e226aae9f4db383391d7afc98c822 kostenfrei http://dx.doi.org/10.1127/metz/4/1995/37 kostenfrei https://doaj.org/toc/0941-2948 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_62 GBV_ILN_70 GBV_ILN_2018 AR 4 1995 1 37-42 |
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Changes of the North Atlantic sea surface temperature related to the atmospheric circulation in the period 1973 to 1992 |
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Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SST. At the surface as well as at 500 hPa a significant intensification of the Icelandic low and a strengthening of the frontal zone over the northern Atlantic Ocean correspond to the changes of SST and thus to the air temperature near the surface. |
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Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SST. At the surface as well as at 500 hPa a significant intensification of the Icelandic low and a strengthening of the frontal zone over the northern Atlantic Ocean correspond to the changes of SST and thus to the air temperature near the surface. |
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Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. This results in changes of the meridional and zonal gradient of the North Atlantic SST. At the surface as well as at 500 hPa a significant intensification of the Icelandic low and a strengthening of the frontal zone over the northern Atlantic Ocean correspond to the changes of SST and thus to the air temperature near the surface. |
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Malberg</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Changes of the North Atlantic sea surface temperature related to the atmospheric circulation in the period 1973 to 1992</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1995</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Between 1973 and 1992 the sea surface temperature (SST) of both the subtropical and the eastern Atlantic has increased by 0.5 to 1 K while other regions, mainly the northwestern Atlantic, show a decrease up to 1 K. 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