Heinrich-Scale Events in Western North America and the Northeastern Pacific? Testing Possible Mechanisms

北美西部和东北太平洋发生海因里希规模的事件？

• 批准号: 9615822
• 负责人: Cathy Whitlock
• 金额: $ 23.84万
• 依托单位: University of Oregon Eugene
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 1996
• 资助国家: 美国
• 起止时间: 1996-09-01 至 2001-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9615822&HistoricalAwards=false
• 关键词: Heinrich; Scale; Events; Western; North

9615822 Whitlock This award supports a collaborative research effort to test hypotheses regarding the occurrence of millennial-scale climate fluctuations now recognized in western North America and the northeastern Pacific Ocean. Preliminary data from marine sediments off California and Oregon, pollen records from Pacific Northwest lakes, and glacial records from western North America reveal climate events that appear to be related to the Heinrich events of the North Atlantic. This study will test two hypotheses: 1) that climate events originating in the North Atlantic are transmitted to the North Pacific Ocean and western North America via thermohaline circulation and its influence on surface ocean characteristics and circulation of the atmosphere, and 2) that climates of the North Atlantic, North America, and the northeast Pacific depend jointly on the elevation of the Laurentide Ice Sheet and its influence on atmospheric circulation. These hypotheses will be constrained by analyzing the paleoclimate record in a geographic array of sites in the northeastern Pacific Ocean and in western North America. Focus of this study will include: constraints on oceanic upwelling and near-surface advection, deep ocean properties and vegetation on land, and comparing these data with model output. A significant advance will come from linking the records from land and sea with a well- constrained chronology, and with stratigraphic links of pollen and terrigenous sediment in marine cores.

9615822 Whitlock该奖项支持一项合作研究工作，以检验有关现在在北美西部和东北太平洋中认可的千禧年气候波动的假设。 来自加利福尼亚和俄勒冈州海洋沉积物的初步数据，太平洋西北湖泊的花粉记录以及北美西部的冰川记录揭示了与北大西洋海因里希事件有关的气候事件。 这项研究将检验两个假设：1）源自北大西洋的气候事件通过热盐循环传播到北太平洋和北美西部，及其对大气层的表面海洋特征和循环的影响，以及2）北美大西洋，北美，北美，北美，北部太平洋，以及东北的联合依赖于Laurentide Icepertic Icepertic Iclection Iclection and Icterction Icecruattion and Cipercy Iclecript and Icteric Iclection Cipertic Iclectix Iclectic and Icteric Iclectic Iclectic and Ictercient coptict。 这些假设将通过分析东北太平洋和北美西部地理地理地理地理地理阵列中的古气候记录来限制。 这项研究的重点将包括：对海洋上升流和近地面对流的限制，陆地上的深海特性和植被，并将这些数据与模型输出进行比较。 将陆地和海洋的记录与良好的时间顺序连接在一起，以及在海洋核心中花粉和陆源沉积物的地层环节，将带来重大进展。