Calibration and Reconstruction of Temperature and Precipitation Change in Arctic Lakes

主要研究人员将根据北极湖泊中的有机生物标志物校准新的温度和降水替代指标。他们将测量独立的温度和陆地径流指数从一类新的四醚生物标志物在一个密集的空间网络的表面湖泊样本从巴芬岛地区。他们将校准这些生物标志物指数，以适应巴芬岛的陡峭温度和降水梯度，并延伸到冰岛、拉布拉多和S。格陵兰岛以及北方加拿大群岛。这个表层沉积物网络将使他们能够开发一个低温的湖泊温度代理，并提供第一次校准的径流指数降水数据。来自冰岛和巴芬岛的长沉积物岩心将作为整个全新世及以后高分辨率古气候记录的目标，以量化最后一次冰消期和全新世最热期的变暖程度。他们还将量化末次间冰期的温度变化。这些时间间隔代表了更温暖的时间段，这些时间段在定量温度方面受到很大的限制，但对于估计未来温暖对北极环境的影响至关重要。北极在气候方面是一个具有全球重要性的区域，全球气候变化的影响可能在北极地区可以发现，然后才能在其他地方发现，正如近年来整个北极环境的大规模和快速变化所表明的那样。除了对全球气候变化表现出敏感性外，北极还可能迫使广泛的气候变化，因此，北极气候变化的详细记录对于构建全球系统的综合图景至关重要。北极是区分自然和人为气候强迫的重要区域，这与近几个世纪以来的快速变暖特别相关，因为古气候记录表明，人类活动对近期变暖的贡献超过了自然强迫机制。准确的校准气候代理是至关重要的，以解决区域汇编之间的差异，并得出可靠的估计，目前变暖的幅度，以及量化变暖在过去的间隔时，北极可能一直free.Broader影响：这项研究将提供研究机会和培训的一名女博士后学者和一名女研究助理。这些科学家将受益于学习尖端有机地球化学分析技术的直接经验，并将有机会旅行，与不同的研究小组互动，并在国际会议上展示他们的成果。主要调查员积极与公众和决策者联系。具体活动包括为科学记者和美国国会代表举办讲座，以及接受电视台和国内外新闻机构的采访。这项研究将调查利用有机生物标志物重建北极湖泊沉积物的湖泊温度和降水记录。他们将使用多种平行化合物和分析技术，以最大限度地从沉积物中提取信息。利用沉积物中的有机生物标志物研究古气候过程仍然是一个年轻的领域，他们预计，从拟议的分析中产生的丰富数据将导致新的见解和新的生物标志物为基础的环境代理的发展。

ABSTRACT OPP-0520266HughenThe Principal Investigators will calibrate new proxies for temperature and precipitation basedon organic biomarkers in Arctic lakes. They will measure independent temperature and terrestrial runoff indices from a new class of tetraether biomarkers within a dense spatial network of surface lake samples from the Baffin Island region. They will calibrate these biomarker indices to steep temperature and precipitation gradients across Baffin Island and extending to Iceland, Labrador and S. Greenland as well as the northern Canadian Archipelago. This surface sediment network will allow them to develop a lake temperature proxy for low-temperatures, and provide the first calibration of a runoff index to precipitation data. Long sediment cores from Iceland and Baffin Island will be targeted for high-resolution paleoclimate records throughout the Holocene and beyond, to quantify the degree of warming during the last deglaciation and Holocene Thermal Maximum. They will also quantify temperature changes during the Last Interglaciation. These intervals represent time periods of greater warmth that are poorly constrained in quantitative temperature, but are critical for estimating the impacts of future warmth on Arctic environments.Intellectual MeritAccurate records of the pattern and timing of climate change in the Arctic are important tounderstanding how the global climate system functions. The Arctic is a globally significant region with respect to climate, and the effects of global climate change might be identifiable in the Arctic before they can be found elsewhere, as suggested by the large and rapid changes documented throughout the Arctic environment in recent years. In addition to showing sensitivity to global changes in climate, the Arctic may also be capable of forcing widespread climate shifts, and detailed records of Arctic climate change are thus critical to the construction of an integrated picture of the global system. The Arctic is an important region for discriminating between natural and anthropogenic forcing of climate, which is particularly relevant for the rapid warming during recent centuries when paleoclimate records have implicated an anthropogenic contribution to recent warming, above and beyond the contribution from natural forcing mechanisms. Accurate calibrations of climate proxies are crucial to resolving differences between regional compilations and deriving reliable estimates of the magnitude of current warming, as well as quantifying warming during past intervals when the Arctic may have been ice-free.Broader Impacts: This study will provide research opportunities and training for one female Postdoctoral Scholar and one female Research Associate. These scientists will benefit from direct experience learning cutting-edge organic geochemical analytical techniques, and will have opportunities to travel, interact with different research groups, and present their results at international meetings. The Principal Investigators are active in outreach to the public and policy-makers. Specific activities include lectures to science journalists and Representatives to the U.S. Congress, as well as interviews for TV and domestic and international news organizations. The study will investigate the use of organic biomarkers to reconstruct lake temperature and precipitation records from Arctic Lacustrine sediments. They will use multiple parallel compounds and analytical techniques to maximize the information extracted from the sediments. The use of organic biomarkers in sediments for the study of paleoclimate processes is still a young field, and they anticipate that the wealth of data arising from the proposed analyses will lead to new insights and the development of new biomarkerbased environmental proxies.