Extreme sea ice events in the Chinese marginal seas during the past 2000 years

Extreme sea ice events in the Chinese marginal seas during the past 2000 years
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近2000年中国边缘海极端海冰事件

DOI:
10.3354/cr01174
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发表时间:
2013-08
期刊:
影响因子:
1.1
通讯作者:
费杰
费杰
中科院分区:
地球科学4区
文献类型:
--
作者:
费杰

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利用中国历史文献资料,分析了近2000年来中国边缘海海冰事件的极端记录。在北纬35度以南海域共发现6次海冰事件。这些极端事件发生在公元821/822、903/904、1453/1454、1493/1494、1654/1655和1670/1671年的冬天。根据历史记载,中国边缘海海冰的南限应在杭州湾(北纬30-31度),最可能在浙江省海盐县附近(北纬30.5度)。1453/1454和1654/1655年海冰事件与太湖封冻事件同步,1670/1671年海冰事件与长江下游封冻事件同步。然而,没有一个海冰事件与日本的Suwa湖的异常早冻结日期或意大利的威尼斯泻湖的极端冻结事件同步。尽管所有海冰事件都发生在30年时间尺度的寒冷气候中,但它们与北方半球其他地点的极端寒冷冬季并不同步。1453/1454年的海冰事件可能与该事件有关。1453年的火山爆发。我们的研究结果增加了我们对中国边缘海区域环境变化和全球气候变化的区域性的理解。
We used Chinese historical literature to examine extreme records of sea ice events in the Chinese marginal seas during the past 2000 yr. We identified a total of 6 sea ice events that occurred in the sea areas to the south of 35 degrees N. These extreme events occurred in the winters of AD 821/822, 903/904, 1453/1454, 1493/1494, 1654/1655 and 1670/1671. According to the historical records, the southern limit of sea ice in the Chinese marginal seas should be in Hangzhou Bay (30-31 degrees N), and most probably near Haiyan County in Zhejiang Province (30.5 degrees N). The sea ice events of 1453/1454 and 1654/1655 were synchronous with the freezing events of Taihu Lake, and the sea ice event of 1670/1671 was synchronous with the freezing event of the lower reaches of the Yangtze River. However, none of the sea ice events was synchronous with the abnormally early freezing dates of Suwa Lake in Japan or the extreme freezing events of Venice Lagoon in Italy. Although all of the sea ice events occurred in a cold climate on a 30 yr timescale, they were not synchronous with the extreme cold winters of other sites in the northern hemisphere. However, the sea ice event of 1453/1454 may have been related to the ca. 1453 Kuwae eruption. Our findings increase our understanding of both regional environmental change in the Chinese marginal seas and the regional nature of global climate change.
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