过去2 000年的特征气候时段及其影响因素

黄博津, 余克服, 陈特固. 过去2 000年的特征气候时段及其影响因素[J]. 海洋地质与第四纪地质, 2013, 33(1): 97-108. doi: 10.3724/SP.J.1140.2013.01097
引用本文: 黄博津, 余克服, 陈特固. 过去2 000年的特征气候时段及其影响因素[J]. 海洋地质与第四纪地质, 2013, 33(1): 97-108. doi: 10.3724/SP.J.1140.2013.01097
HUANG Bojin, YU Kefu, CHEN Tegu. RECENT PROGRESS ON SPECIFIC CLIMATIC STAGES AND DRIVING FORCES OVER LAST 2000 YEARS[J]. Marine Geology & Quaternary Geology, 2013, 33(1): 97-108. doi: 10.3724/SP.J.1140.2013.01097
Citation: HUANG Bojin, YU Kefu, CHEN Tegu. RECENT PROGRESS ON SPECIFIC CLIMATIC STAGES AND DRIVING FORCES OVER LAST 2000 YEARS[J]. Marine Geology & Quaternary Geology, 2013, 33(1): 97-108. doi: 10.3724/SP.J.1140.2013.01097

过去2 000年的特征气候时段及其影响因素

  • 基金项目:

    中国科学院战略性先导科技专项(XDA05080301)

    国家自然科学基金项目(40830852、41025007)

    国家重大科学研究规划项目(2010CB950101)

详细信息
    作者简介: 黄博津(1987-),女,研究生,从事珊瑚古气候研究,E-mail:dearjin@126.com
  • 中图分类号: P532

RECENT PROGRESS ON SPECIFIC CLIMATIC STAGES AND DRIVING FORCES OVER LAST 2000 YEARS

  • 清楚认识过去2 000年来特征气候时段的气候特性,对于了解现代气候状况及其变化趋势有重要意义。大量研究显示,过去2 000年来的特征气候时段可概括为相对寒冷的黑暗时代冷期(简称DACP,大体位于400-600AD)、相对温暖的中世纪暖期(简称MWP,大体位于900-1400AD)、相对寒冷的小冰期(简称LIA,大体位于1500-1850AD)和20世纪异常温暖期。DACP的起止时间等目前仍有争议;MWP的争议在于它的全球性以及温暖程度,特别是它是否暖过20世纪后期;LIA是继MWP之后的一个冷期,全球大部分区域都有记录,但不同区域LIA的起始时间和温度变化幅度各不相同;20世纪异常温暖期指的是20世纪初(1920s)以来的气候变暖,目前的争论主要集中于它的驱动机制和影响因素。一般认为,过去2 000年来特征气候时段的形成可能与太阳活动、火山爆发和人类活动、温室气体增多和海气相互作用等因素有关。其中工业化(1860s)以前长时间尺度的气候主要受太阳和火山活动等的影响,工业化后的气候与温室气体的增多有关。未来对过去2 000年气候的研究,需要提高代用资料指示年代和区域气候信息的准确性,增加高分辨率、高精度代用资料,扩展研究区域,关注气候变化的全面性,发展气候模型进一步了解气候变化的规律和机制。
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收稿日期:  2012-08-05
修回日期:  2012-10-11

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