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Variations in the Summer Monsoon Rainbands Across


doi: 10.1007/s00376-009-8011-0

  • Based on reconstructions of precipitation events from the rain and snowfall archives of the Qing Dynasty (1736--1911), the drought/flood index data mainly derived from Chinese local gazettes from 1736--2000, and the observational data gathered since 1951, the spatial patterns of monsoon rainbands are analyzed at different time scales. Findings indicate that monsoon rainfall in northern China and the middle-lower reaches of the Yangtze River have significant inter-annual (e.g., 5--7-yr and 2--4-yr) as well as inter-decadal (e.g., 20--30-yr and quasi-10-yr) fluctuation signals. The spatial patterns in these areas also show significant cycles, such as on a 60--80-yr time scale, a reversal phase predominates the entire period from 1736--2000; on a quasi-30-yr time scale, a consistent phase was prevalent from 1736 to 2000; and on a 20-yr time scale, the summer monsoon rains show different spatial patterns before and after 1870.
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Manuscript History

Manuscript received: 10 July 2009
Manuscript revised: 10 July 2009
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Variations in the Summer Monsoon Rainbands Across

  • 1. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101,Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101 and Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101

Abstract: Based on reconstructions of precipitation events from the rain and snowfall archives of the Qing Dynasty (1736--1911), the drought/flood index data mainly derived from Chinese local gazettes from 1736--2000, and the observational data gathered since 1951, the spatial patterns of monsoon rainbands are analyzed at different time scales. Findings indicate that monsoon rainfall in northern China and the middle-lower reaches of the Yangtze River have significant inter-annual (e.g., 5--7-yr and 2--4-yr) as well as inter-decadal (e.g., 20--30-yr and quasi-10-yr) fluctuation signals. The spatial patterns in these areas also show significant cycles, such as on a 60--80-yr time scale, a reversal phase predominates the entire period from 1736--2000; on a quasi-30-yr time scale, a consistent phase was prevalent from 1736 to 2000; and on a 20-yr time scale, the summer monsoon rains show different spatial patterns before and after 1870.

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