中国热带第四纪气候波动特征
中国热带早更新世气候波动以高频率小幅度为特征。“中更新世革命”发生在MIS20／MIS21之交。中更新世气候波动一般为三大旋回。晚更新世为两大旋回，但有变暖事件D／01～21及变冷事件H1～H6的表现。可以识别末次间冰期MISS及其阶段5a～5e。末次亚间冰期有4～7次冷暖波动。末次冰期温度一般比今低1～2℃或3～5℃。终止点Ⅰ为15000～13670aB．P．。终止点Ⅱ为0．135～0．130MaB．P．。新冰期Ⅰ、Ⅱ、Ⅲ都有表现。历史时期出现南北朝冷期、北宋冷期、明清小冰期。近200a的气候，前百年升温，后百年降温。...
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| Veröffentlicht in: | Di li yu di li xin xi ke xue = Geography and Geo-information science = GAGIS 2005-08, Vol.21 (4), p.65-70 |
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| container_title | Di li yu di li xin xi ke xue = Geography and Geo-information science = GAGIS |
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| creator | 黄镇国 张伟强 江璐明 |
| description | 中国热带早更新世气候波动以高频率小幅度为特征。“中更新世革命”发生在MIS20／MIS21之交。中更新世气候波动一般为三大旋回。晚更新世为两大旋回，但有变暖事件D／01～21及变冷事件H1～H6的表现。可以识别末次间冰期MISS及其阶段5a～5e。末次亚间冰期有4～7次冷暖波动。末次冰期温度一般比今低1～2℃或3～5℃。终止点Ⅰ为15000～13670aB．P．。终止点Ⅱ为0．135～0．130MaB．P．。新冰期Ⅰ、Ⅱ、Ⅲ都有表现。历史时期出现南北朝冷期、北宋冷期、明清小冰期。近200a的气候，前百年升温，后百年降温。 |
| doi_str_mv | 10.3969/j.issn.1672-0504.2005.04.015 |
| format | Article |
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| fulltext | fulltext |
| identifier | ISSN: 1672-0504 |
| ispartof | Di li yu di li xin xi ke xue = Geography and Geo-information science = GAGIS, 2005-08, Vol.21 (4), p.65-70 |
| issn | 1672-0504 |
| language | chi |
| recordid | cdi_wanfang_journals_dlxygtyj200504015 |
| source | 国家哲学社会科学学术期刊数据库 (National Social Sciences Database) |
| subjects | 中国热带 气候波动 第四纪 |
| title | 中国热带第四纪气候波动特征 |
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