P2C2: Detection of Long-term Variability in Storm Tracks Using Seasonally Resolved Tree-ring Isotope Records: Implications for Hydroclimatic Change in the U.S. Pacific Northwest

P2C2：使用季节性解析的树木年轮同位素记录检测风暴路径的长期变化：对美国太平洋西北地区水文气候变化的影响

• 批准号: 1304422
• 负责人: Erika Wise
• 金额: $ 63.99万
• 依托单位: University of North Carolina at Chapel Hill
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2013
• 资助国家: 美国
• 起止时间: 2013-06-01 至 2017-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1304422&HistoricalAwards=false
• 关键词: P2C2; Detection; Long; term; Variability

The trajectory of incoming storms from the Pacific Ocean influences precipitation patterns in the western United States, shaping drought and flood events. Long-term changes in these trajectories may have resulted in North American "megadroughts" and other extreme climate events, but little is known about the range of variability in storm-track patterns, particularly at a seasonal timescale. The isotopic composition of precipitation, which reflects atmospheric circulation patterns, is recorded in tree rings. In this collaborative study, researchers from the University of North Carolina at Chapel Hill, the University of Arizona, and the University of Alaska, Fairbanks, will use seasonally resolved tree-ring data (based on earlywood and latewood widths, δ18O, and δ13C) and weekly precipitation isotope sampling at nearby sites to reconstruct storm-track position and moisture delivery pathways to the U.S. Pacific Northwest. Four major objectives of this project are to: (1) develop a long-term record of storm track using stable isotopes in tree rings; (2) determine the seasonal signal embedded within the tree rings; (3) examine controls on spatial drought patterns through time in the Pacific Northwest; and (4) evaluate implications for future climate change.This project will help characterize the stability of the moisture-delivery system to the Columbia River Basin, with implications for water resources. Given the projected changes in storm track and seasonality in future climate scenarios, understanding past limits in these systems will be important for evaluating the potential impacts of future trends. Data generated through this project will extend spatial coverage of tree-ring isotope records across North America. In addition to providing research opportunities for graduate and undergraduate students, the researchers will collaborate with teachers in the Pacific Northwest through citizen-science partnerships that will involve middle- and high-school students in data collection and enhance science education in public schools.

来自太平洋的传入风暴的轨迹影响了美国西部的降水模式，塑造了干旱和洪水事件。这些轨迹的长期变化可能导致了北美的“巨型”和其他极端气候事件，但对于风暴轨道模式的可变性范围知之甚少，尤其是在季节性的时间表上。 在树环中记录了反映大气循环模式的降水的同位素组成。 在这项合作研究中，来自北卡罗来纳大学教堂山，亚利桑那大学和阿拉斯加大学费尔班克斯大学的研究人员将使用季节性解决的树环数据（基于早期和深木的宽度，以及18o的早期和末日木材宽度，以及18O; 18O，以及附近的降水式水样，并在附近的烟雾供应量，并在附近的水分及其潮流，以便在附近的水样及其潮流及其潮流及其潮流及其潮流的水样，并在潮流中供应风暴及其潮流的水样，并在暴风雨中及其潮流的水样及其潮流的水样及其潮流的水样，太平洋西北。该项目的四个主要目标是：（1）使用树环中稳定的同位素制定风暴轨迹的长期记录； （2）确定嵌入在树环内的季节性信号； （3）检查西北太平洋时期的空间干旱模式的控制； （4）评估对未来气候变化的影响。该项目将有助于表征水分交付系统对哥伦比亚河流域的稳定性，并对水资源产生影响。 考虑到未来气候场景中风暴轨道和季节性的预计变化，了解这些系统的过去限制对于评估未来趋势的潜在影响至关重要。通过该项目生成的数据将扩展北美整个北美树木同位素记录的空间覆盖范围。除了为研究生和本科生提供研究机会外，研究人员还将通过公民科学科学伙伴关系与太平洋西北地区的老师合作，​​这将涉及中学和高中生在数据收集中，并增强公立学校的科学教育。