On the magnitude of temperature decrease in the equatorial regions during the Last Glacial Maximum
Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Ninglian [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1999 |
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| Schlagwörter: |
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| Anmerkung: |
© Science in China Press 1999 |
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| Übergeordnetes Werk: |
Enthalten in: Science in China / D - Science in China Press, 1996, 42(1999), Suppl 1 vom: Aug., Seite 80-90 |
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| Übergeordnetes Werk: |
volume:42 ; year:1999 ; number:Suppl 1 ; month:08 ; pages:80-90 |
| Links: |
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| DOI / URN: |
10.1007/BF02878856 |
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| Katalog-ID: |
OLC2063771278 |
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| 520 | |a Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum | ||
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| 700 | 1 | |a Cole-Dai, J. |4 aut | |
| 700 | 1 | |a Lin, P. -N. |4 aut | |
| 700 | 1 | |a Davis, M. E. |4 aut | |
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10.1007/BF02878856 doi (DE-627)OLC2063771278 (DE-He213)BF02878856-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut On the magnitude of temperature decrease in the equatorial regions during the Last Glacial Maximum 1999 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 1999 Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum eqastorial regions Last Glacial Maximum temperature variation Yao, Tandong aut Shi, Yafeng aut Thompson, L. G. aut Cole-Dai, J. aut Lin, P. -N. aut Davis, M. E. aut Enthalten in Science in China / D Science in China Press, 1996 42(1999), Suppl 1 vom: Aug., Seite 80-90 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:42 year:1999 number:Suppl 1 month:08 pages:80-90 https://doi.org/10.1007/BF02878856 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 42 1999 Suppl 1 08 80-90 |
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10.1007/BF02878856 doi (DE-627)OLC2063771278 (DE-He213)BF02878856-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut On the magnitude of temperature decrease in the equatorial regions during the Last Glacial Maximum 1999 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 1999 Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum eqastorial regions Last Glacial Maximum temperature variation Yao, Tandong aut Shi, Yafeng aut Thompson, L. G. aut Cole-Dai, J. aut Lin, P. -N. aut Davis, M. E. aut Enthalten in Science in China / D Science in China Press, 1996 42(1999), Suppl 1 vom: Aug., Seite 80-90 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:42 year:1999 number:Suppl 1 month:08 pages:80-90 https://doi.org/10.1007/BF02878856 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 42 1999 Suppl 1 08 80-90 |
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10.1007/BF02878856 doi (DE-627)OLC2063771278 (DE-He213)BF02878856-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut On the magnitude of temperature decrease in the equatorial regions during the Last Glacial Maximum 1999 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 1999 Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum eqastorial regions Last Glacial Maximum temperature variation Yao, Tandong aut Shi, Yafeng aut Thompson, L. G. aut Cole-Dai, J. aut Lin, P. -N. aut Davis, M. E. aut Enthalten in Science in China / D Science in China Press, 1996 42(1999), Suppl 1 vom: Aug., Seite 80-90 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:42 year:1999 number:Suppl 1 month:08 pages:80-90 https://doi.org/10.1007/BF02878856 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 42 1999 Suppl 1 08 80-90 |
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10.1007/BF02878856 doi (DE-627)OLC2063771278 (DE-He213)BF02878856-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut On the magnitude of temperature decrease in the equatorial regions during the Last Glacial Maximum 1999 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 1999 Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum eqastorial regions Last Glacial Maximum temperature variation Yao, Tandong aut Shi, Yafeng aut Thompson, L. G. aut Cole-Dai, J. aut Lin, P. -N. aut Davis, M. E. aut Enthalten in Science in China / D Science in China Press, 1996 42(1999), Suppl 1 vom: Aug., Seite 80-90 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:42 year:1999 number:Suppl 1 month:08 pages:80-90 https://doi.org/10.1007/BF02878856 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 42 1999 Suppl 1 08 80-90 |
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10.1007/BF02878856 doi (DE-627)OLC2063771278 (DE-He213)BF02878856-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut On the magnitude of temperature decrease in the equatorial regions during the Last Glacial Maximum 1999 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 1999 Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum eqastorial regions Last Glacial Maximum temperature variation Yao, Tandong aut Shi, Yafeng aut Thompson, L. G. aut Cole-Dai, J. aut Lin, P. -N. aut Davis, M. E. aut Enthalten in Science in China / D Science in China Press, 1996 42(1999), Suppl 1 vom: Aug., Seite 80-90 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:42 year:1999 number:Suppl 1 month:08 pages:80-90 https://doi.org/10.1007/BF02878856 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_4082 AR 42 1999 Suppl 1 08 80-90 |
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Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum © Science in China Press 1999 |
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Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum © Science in China Press 1999 |
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Abstract Based on the data of temperature changes revealed by means of various paldennometric proxy indices, it ie found that the magnitude of temperature decrease became large with altitude in the equatorial regions during the Last Glacial Maximum. The direct cauw of this phenomenon was the change in temperature lapee rate, which was about (0.1 ±0.05)°C/100 m larger in the equator during the Last Glacial Maximum than at present. Moreover, the analyses show that CLIMAP possibly underestimated the sea surface temperature decrease in the equatorial regions during the Last Glacial Maximum © Science in China Press 1999 |
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Yao, Tandong Shi, Yafeng Thompson, L. G. Cole-Dai, J. Lin, P. -N. Davis, M. E. |
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Yao, Tandong Shi, Yafeng Thompson, L. G. Cole-Dai, J. Lin, P. -N. Davis, M. E. |
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193118238 |
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n |
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false |
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| doi_str |
10.1007/BF02878856 |
| up_date |
2024-07-03T20:12:50.171Z |
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1803590115180675072 |
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