| 大洋环流型式转换在冰期旋回中的作用及经典第四纪冰期理论质疑(续) |
| |
| 引用本文： | 汉景泰.大洋环流型式转换在冰期旋回中的作用及经典第四纪冰期理论质疑(续)[J].第四纪研究,1996,16(2):176-180. |
| |
| 作者姓名： | 汉景泰 |
| |
| 作者单位： | 加拿大西安大略大学地质系 |
| |
| 摘 要： | 大洋环流型式转换在冰期旋回中的作用及经典第四纪冰期理论质疑(续)汉景泰Ｗ．Ｓ．Ｆｙｆｅ(加拿大西安大略大学地质系)４问题及讨论大洋环流－气候学说认为从冰期到间冰期海洋－大气系统全球性巨型再组合导致了末次冰期的终止。
|
| 关 键 词： | 大洋环流 更新世 第四纪 冰期旋回 |
OCEAN RESPONSE TO THE LAST DEGLACIATION:CONVENTIONAL PALEOCLIMATE MODELS AND CONTROVERSY |
| |
| Han Jingtai,W. S. Fyfe.OCEAN RESPONSE TO THE LAST DEGLACIATION:CONVENTIONAL PALEOCLIMATE MODELS AND CONTROVERSY[J].Quaternary Sciences,1996,16(2):176-180. |
| |
| Authors: | Han Jingtai W S Fyfe |
| |
| Institution: | Department of Geology, University of Western Ontario, Canada |
| |
| Abstract: | Geological evidence, obtained from oxygen-isotopic analysis of deep sea sediments, continental ice sheets, mountain glaciers and polar ice cores in the both hemispheres shows that the last glaciation terminated at about 14000 aB. P. It occurred prior to the insolation maximum as expected by the Milankovitch astronomical theory. The evidence also shows that the glacial-interglacial cycles are dominated by the 100 000a periodicity with asymmetrical shape. Long-term ice build-up ends abruptly with rapid wasting. The insolation perturbations induced by the earth's orbital parameters have greater powers only at 41000a, and 23000a/19000a cycles. Thus the characteristics of geological records deny direct simple response of the climatic changes to the solar radiation forcing. While summarizing the leading hypothesis for explanation of the ice ages and the ice sheet-size-climate linkage, this paper centres on the ocean-operation-climate model. This model stresses the impact of the Atlantic conveyor belt of the oceanic circulation on the northern hemispheric climate with the analyses of energy, water mass and salinity balance. Based on geological evidence from deep sea sediments, the model suggests that the ocean circulation pattern was different during glacial time than today. The Younger Dryas cold event probably exemplifies the influence of the ocean reorganization on climate. Here we also discuss some basic problems regarding climate theories of the ice ages. |
| |
| Keywords: | hypothesis of ice sheet explanation climate ocean circulationclimate model climatic forcing termination of glacial ocean circulation pattern |
| 本文献已被 CNKI 维普 等数据库收录！ |
| 点击此处可从《第四纪研究》浏览原始摘要信息 |
| 点击此处可从《第四纪研究》下载免费的PDF全文 |
