Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau
Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend,...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Ninglian [verfasserIn] |
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| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2006 |
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| Schlagwörter: |
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| Anmerkung: |
© Science in China Press 2006 |
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| Übergeordnetes Werk: |
Enthalten in: Science in China / D - Science in China Press, 1996, 49(2006), 10 vom: Okt., Seite 1079-1089 |
|---|---|
| Übergeordnetes Werk: |
volume:49 ; year:2006 ; number:10 ; month:10 ; pages:1079-1089 |
| Links: |
|---|
| DOI / URN: |
10.1007/s11430-006-1079-9 |
|---|
| Katalog-ID: |
OLC2063780226 |
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| 520 | |a Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. | ||
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10.1007/s11430-006-1079-9 doi (DE-627)OLC2063780226 (DE-He213)s11430-006-1079-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2006 Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. the Tibetan Plateau the Malan ice core climate changes dust event frequency Yao, Tandong aut Pu, Jianchen aut Zhang, Yongliang aut Sun, Weizhen aut Enthalten in Science in China / D Science in China Press, 1996 49(2006), 10 vom: Okt., Seite 1079-1089 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:49 year:2006 number:10 month:10 pages:1079-1089 https://doi.org/10.1007/s11430-006-1079-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 GBV_ILN_4082 AR 49 2006 10 10 1079-1089 |
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10.1007/s11430-006-1079-9 doi (DE-627)OLC2063780226 (DE-He213)s11430-006-1079-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2006 Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. the Tibetan Plateau the Malan ice core climate changes dust event frequency Yao, Tandong aut Pu, Jianchen aut Zhang, Yongliang aut Sun, Weizhen aut Enthalten in Science in China / D Science in China Press, 1996 49(2006), 10 vom: Okt., Seite 1079-1089 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:49 year:2006 number:10 month:10 pages:1079-1089 https://doi.org/10.1007/s11430-006-1079-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 GBV_ILN_4082 AR 49 2006 10 10 1079-1089 |
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10.1007/s11430-006-1079-9 doi (DE-627)OLC2063780226 (DE-He213)s11430-006-1079-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2006 Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. the Tibetan Plateau the Malan ice core climate changes dust event frequency Yao, Tandong aut Pu, Jianchen aut Zhang, Yongliang aut Sun, Weizhen aut Enthalten in Science in China / D Science in China Press, 1996 49(2006), 10 vom: Okt., Seite 1079-1089 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:49 year:2006 number:10 month:10 pages:1079-1089 https://doi.org/10.1007/s11430-006-1079-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 GBV_ILN_4082 AR 49 2006 10 10 1079-1089 |
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10.1007/s11430-006-1079-9 doi (DE-627)OLC2063780226 (DE-He213)s11430-006-1079-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2006 Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. the Tibetan Plateau the Malan ice core climate changes dust event frequency Yao, Tandong aut Pu, Jianchen aut Zhang, Yongliang aut Sun, Weizhen aut Enthalten in Science in China / D Science in China Press, 1996 49(2006), 10 vom: Okt., Seite 1079-1089 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:49 year:2006 number:10 month:10 pages:1079-1089 https://doi.org/10.1007/s11430-006-1079-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 GBV_ILN_4082 AR 49 2006 10 10 1079-1089 |
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10.1007/s11430-006-1079-9 doi (DE-627)OLC2063780226 (DE-He213)s11430-006-1079-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Ninglian verfasserin aut Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2006 Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. the Tibetan Plateau the Malan ice core climate changes dust event frequency Yao, Tandong aut Pu, Jianchen aut Zhang, Yongliang aut Sun, Weizhen aut Enthalten in Science in China / D Science in China Press, 1996 49(2006), 10 vom: Okt., Seite 1079-1089 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:49 year:2006 number:10 month:10 pages:1079-1089 https://doi.org/10.1007/s11430-006-1079-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 GBV_ILN_4082 AR 49 2006 10 10 1079-1089 |
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climatic and environmental changes over the last millennium recorded in the malan ice core from the northern tibetan plateau |
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Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau |
| abstract |
Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. © Science in China Press 2006 |
| abstractGer |
Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. © Science in China Press 2006 |
| abstract_unstemmed |
Abstract In this paper, climatic and environmental changes were reconstructed since 1129A.D. based on the Malan ice core from Hol Xil, the northern Tibetan Plateau. The record of δ18O in the Malan ice core indicated that the warm-season air temperature variations displayed a general increase trend, the 20th-century warming was within the range of natural climate variability, and the warmest century was the 17th century while the warmest decade was the 1610s, over the entire study period. The “Medieval Warm Epoch” and “Little Ice Age” were also reflected by the ice core record. The dust ratio in the Malan ice core is a good proxy for dust event frequency. The 870-year record of the dust ratio showed that dust events occurred much frequently in the 19th century. Comparing the variations of δ18O and the dust ratio, it is found that there was a strong negative correlation between them on the time scales of $ 10^{1} $–$ 10^{2} $ years. By analyses of all the climatic records of ice cores and tree rings from the northern Tibetan Plateau, it was revealed that dust events were more frequent in the cold and dry periods than in the warm and wet periods. © Science in China Press 2006 |
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Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau |
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