High-Resolution Paleoclimatic Record of a Closed-Basin Lake in the Northern Great Plains

北部大平原封闭盆地湖泊的高分辨率古气候记录

• 批准号: 9414381
• 负责人: Sherilyn Fritz
• 金额: $ 4.01万
• 依托单位: University of Minnesota-Twin Cities
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 1995
• 资助国家: 美国
• 起止时间: 1995-04-01 至 1996-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9414381&HistoricalAwards=false
• 关键词: Resolution; Paleoclimatic; Record; Closed; Basin

Abstract ATM-9414381 Fritz, Sherilyn C. University of Minnesota This award supports the study of fossil diatom assemblages as paleohydrological/paleoclimatic indicators in Moon Lake,a closed- basin lake in the northern Great Plains. This study will attempt to reconstruct changes ineffective moisture (precipitation minus evapotranspiration. The historical relationship between diatom- inferred salinity and climate will be used to calculate a transfer function for effective moisture and hydrological drought (Palmer Hydrological Drought Index) which will then be extended to the entire post-glacial record. Climatic conditions will be assessed at century-scale resolution through the entire Holocene and at decadal-scale resolution during three periods: the last glaciation- deglaciation period, the early-Holocene forest/prairie transition, and past 2000 years. Paleoclimatic records from climatically sensitive agricultural regions such as the Great Plains, where little is known of past climate, and what is known is of a coarse resolution, will provide a valuable contribution to the understanding of climatic variability on local, regional, and global scales. Understanding drought characteristics through the analysis of long-term trends in the paleoclimatic record will provide valuable information for planning and managing water shortages that may accompany future drought events.

摘要ATM-9414381 Fritz，Sherilyn C. 明尼苏达大学 该奖项支持化石硅藻组合作为月亮湖古水文/古气候指标的研究，月亮湖是北方大平原的一个封闭盆地湖泊。 这项研究将试图重建变化无效水分（降水减去蒸散。 硅藻推断的盐度和气候之间的历史关系将用于计算有效水分和水文干旱（帕尔默水文干旱指数）的传递函数，然后将其扩展到整个冰后期记录。 气候条件将在整个全新世以世纪尺度的分辨率进行评估，并在三个时期以十年尺度的分辨率进行评估：末次冰期-冰消期、早全新世森林/草原过渡期和过去2000年。 来自气候敏感的农业区（如大平原）的古气候记录，对过去的气候知之甚少，所知的是一个粗略的分辨率，将为理解局部，区域和全球尺度的气候变化提供有价值的贡献。 通过分析古气候记录中的长期趋势来了解干旱特征，将为规划和管理可能伴随未来干旱事件的水资源短缺提供宝贵的信息。