Tracing Thermocline Waters to the Ocean Surface to Link Glacial Thermocline Processes and Climate

追踪温跃层水域至海洋表面，将冰川温跃层过程与气候联系起来

• 批准号: 9203866
• 负责人: Niall Slowey
• 金额: $ 10.88万
• 依托单位: Texas A&M Research Foundation
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 1992
• 资助国家: 美国
• 起止时间: 1992-06-01 至 1996-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9203866&HistoricalAwards=false
• 关键词: Tracing; Thermocline; Waters; Ocean; Surface

During the last glacial period temperatures were colder, the thermocline base was shallower, nutrient concentrations were lower and oxygen minimum zone was indistinct. The PI will examine isotopic variations in formaminifera south of the glacial polar front in the North Atlantic to learn more about their relationship to thermocline and its dynamics and the changes in glacial polar front.

在最后的冰川期间温度更冷，热层碱基较浅，养分浓度较低，氧气最小区域不明显。 PI将检查北大西洋冰川极前线以南的Formaminifera的同位素变化，以了解更多有关其与热级别及其动力学的关系以及冰川极前方的变化。