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Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008
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Zeitschriftentitel: | Climate of the Past |
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Personen und Körperschaften: | , , , |
In: | Climate of the Past, 11, 2015, 11, S. 1553-1561 |
Format: | E-Article |
Sprache: | Englisch |
veröffentlicht: |
Copernicus GmbH
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Schlagwörter: |
author_facet |
Zheng, J. Hua, Z. Liu, Y. Hao, Z. Zheng, J. Hua, Z. Liu, Y. Hao, Z. |
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author |
Zheng, J. Hua, Z. Liu, Y. Hao, Z. |
spellingShingle |
Zheng, J. Hua, Z. Liu, Y. Hao, Z. Climate of the Past Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 Paleontology Stratigraphy Global and Planetary Change |
author_sort |
zheng, j. |
spelling |
Zheng, J. Hua, Z. Liu, Y. Hao, Z. 1814-9332 Copernicus GmbH Paleontology Stratigraphy Global and Planetary Change http://dx.doi.org/10.5194/cp-11-1553-2015 <jats:p>Abstract. Annual temperature anomalies in South Central China from 1850 to 2008 are reconstructed by synthesizing three types of proxies: spring phenodates of plants recorded in historical personal diaries and observations, snowfall days extracted from historical archives and observed at meteorological stations, and five tree-ring width chronologies. Instrumental observation data and the leave-one-out method are used for calibration and validation. The results show that the temperature series in South Central China exhibits interannual and decadal fluctuations since 1850. The first three cold decades were the 1860s, 1890s, and 1950s, while 1893 was very likely the coldest year. Except for the three warm decades that occurred around 1850, 1870, and 1960, along with the 1920s to the 1940s, the recent warm decades of the 1990s and 2000s represent unprecedented warming since 1850. </jats:p> Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 Climate of the Past |
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10.5194/cp-11-1553-2015 |
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Physik Geographie Geologie und Paläontologie |
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title |
Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_unstemmed |
Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_full |
Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_fullStr |
Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_full_unstemmed |
Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_short |
Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_sort |
temperature changes derived from phenological and natural evidence in south central china from 1850 to 2008 |
topic |
Paleontology Stratigraphy Global and Planetary Change |
url |
http://dx.doi.org/10.5194/cp-11-1553-2015 |
publishDate |
2015 |
physical |
1553-1561 |
description |
<jats:p>Abstract. Annual temperature anomalies in South Central China from 1850 to 2008 are reconstructed by synthesizing three types of proxies: spring phenodates of plants recorded in historical personal diaries and observations, snowfall days extracted from historical archives and observed at meteorological stations, and five tree-ring width chronologies. Instrumental observation data and the leave-one-out method are used for calibration and validation. The results show that the temperature series in South Central China exhibits interannual and decadal fluctuations since 1850. The first three cold decades were the 1860s, 1890s, and 1950s, while 1893 was very likely the coldest year. Except for the three warm decades that occurred around 1850, 1870, and 1960, along with the 1920s to the 1940s, the recent warm decades of the 1990s and 2000s represent unprecedented warming since 1850.
</jats:p> |
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author | Zheng, J., Hua, Z., Liu, Y., Hao, Z. |
author_facet | Zheng, J., Hua, Z., Liu, Y., Hao, Z., Zheng, J., Hua, Z., Liu, Y., Hao, Z. |
author_sort | zheng, j. |
container_issue | 11 |
container_start_page | 1553 |
container_title | Climate of the Past |
container_volume | 11 |
description | <jats:p>Abstract. Annual temperature anomalies in South Central China from 1850 to 2008 are reconstructed by synthesizing three types of proxies: spring phenodates of plants recorded in historical personal diaries and observations, snowfall days extracted from historical archives and observed at meteorological stations, and five tree-ring width chronologies. Instrumental observation data and the leave-one-out method are used for calibration and validation. The results show that the temperature series in South Central China exhibits interannual and decadal fluctuations since 1850. The first three cold decades were the 1860s, 1890s, and 1950s, while 1893 was very likely the coldest year. Except for the three warm decades that occurred around 1850, 1870, and 1960, along with the 1920s to the 1940s, the recent warm decades of the 1990s and 2000s represent unprecedented warming since 1850. </jats:p> |
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spelling | Zheng, J. Hua, Z. Liu, Y. Hao, Z. 1814-9332 Copernicus GmbH Paleontology Stratigraphy Global and Planetary Change http://dx.doi.org/10.5194/cp-11-1553-2015 <jats:p>Abstract. Annual temperature anomalies in South Central China from 1850 to 2008 are reconstructed by synthesizing three types of proxies: spring phenodates of plants recorded in historical personal diaries and observations, snowfall days extracted from historical archives and observed at meteorological stations, and five tree-ring width chronologies. Instrumental observation data and the leave-one-out method are used for calibration and validation. The results show that the temperature series in South Central China exhibits interannual and decadal fluctuations since 1850. The first three cold decades were the 1860s, 1890s, and 1950s, while 1893 was very likely the coldest year. Except for the three warm decades that occurred around 1850, 1870, and 1960, along with the 1920s to the 1940s, the recent warm decades of the 1990s and 2000s represent unprecedented warming since 1850. </jats:p> Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 Climate of the Past |
spellingShingle | Zheng, J., Hua, Z., Liu, Y., Hao, Z., Climate of the Past, Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008, Paleontology, Stratigraphy, Global and Planetary Change |
title | Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_full | Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_fullStr | Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_full_unstemmed | Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_short | Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
title_sort | temperature changes derived from phenological and natural evidence in south central china from 1850 to 2008 |
title_unstemmed | Temperature changes derived from phenological and natural evidence in South Central China from 1850 to 2008 |
topic | Paleontology, Stratigraphy, Global and Planetary Change |
url | http://dx.doi.org/10.5194/cp-11-1553-2015 |