Study of Seasonal Radiocarbon Variability in the Eastern Tropical Pacific During Periods of Decadal and Interannual Climate Shifts

年代际和年际气候变化期间热带东太平洋季节性放射性碳变化研究

• 批准号: 0551940
• 负责人: Ellen Druffel
• 金额: $ 51.29万
• 依托单位: University of California-Irvine
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2006
• 资助国家: 美国
• 起止时间: 2006-01-01 至 2010-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0551940&HistoricalAwards=false
• 关键词: Study; Seasonal; Radiocarbon; Variability; Eastern

In this project, investigators at the University of California at Irvine will determine the detailed changes of radiocarbon in the surface of the eastern tropical Pacific during distinctive climatic periods in the past 400 years. The researchers expect that these studies will aid in our understanding of how natural variability in climate can influence the ability of the ocean to absorb excess CO2 produced from fossil fuel and biomass burning. High-precision AMS (accelerator mass spectrometry) 14C measurements on seasonal coral bands from the eastern tropical Pacific, located in the "center of action" with respect to El Nino, will be made to determine the variability of the low 14C component of the source waters (presumably Sub-Antarctic Mode Water) from the South Pacific. Three hypotheses will be tested: 1) Wintertime 14C values in Galapagos corals are an indicator for the phase of the PDO; 2) Prolonged periods of winter-time upwelling were present at in the eastern tropical Pacific during the early 1600s and early 1800s, which were likely caused by prolonged entrainment of Sub-Antarctic Mode Water into the Equatorial Under Current; and 3) Wintertime 14C values at Galapagos reveal interannual-to-decadal variability in climate.To test these hypotheses, the following studies will be done: 1) Seasonal 14C and, in collaboration with colleagues at Stanford University, 18O will be measured in Galapagos coral bands that grew from 1900-1996 to determine if the winter-time 14C was significantly lower during recorded periods when the PDO was known to have been in a negative phase (1915-1925 and 1945-1955). A calibration experiment will be performed to demonstrate that the coral species used in this study is indeed recording the entire seasonal signal. 2) Seasonal 14C and 18O measurements of coral bands that grew from 1598-1611 and from 1804-1825 will be made to determine if the winter-time 14C was significantly lower and/or persisted for a longer period of time during these unusual climatic periods. 3) Seasonal 14C measurements will be made of coral bands from time periods that display clear interannual variability in climate (ENSO) and those that are dominated by distinct decadal variability. Collaboration with colleagues at Princeton University is planned to utilize the seasonal 14C records in his ocean circulation modeling experiments designed to calculate variability of past pCO2 and CO2 out-gassing fluxes in the equatorial Pacific.In terms of broader impacts, the project will support the work of one graduate student and two undergraduate students and provide hands-on experience that will prepare them for careers as scientists and educators. The PI is involved with developing outreach activities in conjunction with middle and high school youths. She is also on the advisory board for FCOSEE (Florida Center for Ocean Science Education Excellence COSEE) to assist in developing web-based educational classes at the college level, and participates in teaching a short course on Radiocarbon and the Carbon Cycle every summer.

在这个项目中，位于欧文的加州大学的研究人员将确定过去400年中不同气候时期热带太平洋东部表面放射性碳的详细变化。 研究人员预计，这些研究将有助于我们了解气候的自然变化如何影响海洋吸收化石燃料和生物质燃烧产生的过量二氧化碳的能力。 高精度AMS（加速器质谱） 将对位于厄尔尼诺“作用中心”的热带太平洋东部的季节性珊瑚带进行14 C测量，以确定南太平洋源沃茨（推测为亚南极模式水）的低14 C成分的变化。 本研究将检验三个假设：1）冬季加拉帕戈斯珊瑚中的~（14）C值是PDO相态的一个指标; 2）17世纪初至19世纪初，热带东太平洋冬季上升流持续时间较长，这可能是由于亚南极模态水长期卷入赤道潜流所致;加拉帕戈斯冬季14 C值揭示了气候的年际至年代际变化。为了验证这些假设，将进行以下研究：1）季节性14 C，并与斯坦福大学的同事合作，将在1900-1996年生长的加拉帕戈斯珊瑚带中测量18 O，以确定在PDO处于负相的记录期间，冬季14 C是否明显较低（1915-1925和1945-1955）。 将进行校准实验，以证明本研究中使用的珊瑚物种确实记录了整个季节信号。 2)对1598-1611年和1804-1825年生长的珊瑚带进行季节性的14 C和18 O测量，以确定在这些不寻常的气候时期，冬季的14 C是否显著降低和/或持续更长的时间。 3)季节性14 C测量将由珊瑚带从时间段，显示明显的年际变化的气候（厄尔尼诺/南方涛动）和那些由明显的十年变化为主。 计划与普林斯顿大学的同事合作，在他的海洋环流模拟实验中利用季节性14 C记录，该实验旨在计算赤道太平洋过去pCO 2和CO2出气通量的变化。该项目将支持一名研究生和两名本科生的工作，并提供人手-经验将为他们成为科学家和教育家的职业做好准备。 PI参与与初中和高中青年一起开展外联活动。 她也是FCOSEE（佛罗里达中心海洋科学教育卓越COSEE）的顾问委员会，以协助开发基于网络的教育课程在大学水平，并参与教学放射性碳和碳循环的短期课程，每年夏天。