author_facet Zheng, J.
Hua, Z.
Liu, Y.
Hao, Z.
Zheng, J.
Hua, Z.
Liu, Y.
Hao, Z.
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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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