Refinement of Historical Variability and the Baseline for Hydroclimatic Conditions within the Walker Basin: A Multi-Elevational Dendrochronological and Ecohydrological Approach

沃克盆地历史变率和水文气候条件基线的完善：多海拔树木年代学和生态水文学方法

• 批准号: 1230329
• 负责人: Franco Biondi
• 金额: $ 34.5万
• 依托单位: Board of Regents, NSHE, obo University of Nevada, Reno
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-09-01 至 2017-02-28
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1230329&HistoricalAwards=false
• 关键词: Refinement; Historical; Variability; Baseline; Hydroclimatic

Hydroclimatic variability is an increasingly important aspect of water supply planning in arid and semi-arid regions of the United States and the world. Our understanding of past processes at relevant timescales (i.e. decadal to centennial) is often derived from high resolution palaeorecords such as tree rings. This research project will use tree-ring records to quantify wet and dry episodes within the Walker River watershed in western Nevada/eastern California. Along with the collection of long tree-ring chronologies that will stretch from the present back over 1000 years, this project will establish baseline conditions at multiple study sites with respect to climate and ecology. To capture tree-ring responses to individual hydroclimatic variables, such as summertime temperatures and wintertime precipitation, the researchers will target four tree species across a range of elevations as well as multiple topographic aspects. Baseline ecological surveys will be conducted at each study site to allow for comparison of conditions among a wide range of other surveyed locations across the Great Basin region. The researchers will use in-situ, free-air temperature sensors to better interpret microsite conditions relative to modeled and regional climate data. A climate monitoring station will be installed at high elevation in an isolated portion of the watershed, which will capture not only temperature and precipitation, but also solar radiation, wind patterns, and soil conditions. Both the ecological and sensory data will aid interpretation of palaeoclimate records, as existing data for most of the conifer zones in the watershed are limited to modeling products. A primary goal of this project is to reconstruct seasonal climate variables which would serve as inputs to water balance modeling over the last 1200 years, a time period which has seen tremendous variability based on previous tree-ring and lake sediment studies. Evaluation of watershed behavior during past time periods that exceed the envelope of our modern observations will aid water managers and users in decision making and planning as we move into an uncertain future. Records of past processes show how landscapes respond to variations in climatic and energy input, and regardless of the cause of future changes in conditions, it is critical to understand watershed dynamics in arid and semi-arid environments. This research approach will bolster knowledge in tree-ring science, increase our understanding of climatic variability at the watershed scale, and clarify relationships between tree-ring records and water budgets. Reconstruction results from the project will be of immediate use to scientists, water managers, and water users within the Walker Basin and adjacent watersheds. Climatic and ecological data acquired as a result of the project's surveys and installations will be available to a wide range of public users, with sensor data provided in real-time. By bringing together Federal, University, and Community College researchers, this project provides a unique opportunity for collaboration and outreach across diverse levels. Educational opportunities will be provided to graduate, undergraduate, and Community College students, who will be able to participate in field and laboratory work as well as scientific conferences.

在美国和世界的干旱和半干旱地区，水文气候变率是供水规划的一个日益重要的方面。我们对相关时间尺度（即十年至百年）的过去过程的理解通常来自高分辨率的古记录，如树木年轮。该研究项目将使用树木年轮记录来量化内华达州西部/加利福尼亚州东部沃克河流域的干湿事件。随着树木年轮年表的收集，将从现在追溯到1000多年前，该项目将在多个研究地点建立关于气候和生态的基线条件。为了捕捉树木年轮对单个水文气候变量（如夏季温度和冬季降水）的响应，研究人员将以不同海拔高度和多个地形方面的四种树种为目标。基线生态调查将在每个研究地点进行，以便与大盆地地区范围广泛的其他调查地点进行条件比较。研究人员将使用原位、自由空气温度传感器来更好地解释与模型和区域气候数据相关的微站点条件。气候监测站将安装在分水岭的一个孤立部分的高海拔地区，不仅可以捕捉温度和降水，还可以捕捉太阳辐射、风型和土壤状况。生态和感官数据都将有助于解释古气候记录，因为该流域大多数针叶树带的现有数据仅限于建模产品。该项目的一个主要目标是重建季节性气候变量，这些变量将作为过去1200年水平衡模型的输入，这一时期基于以前的树木年轮和湖泊沉积物研究已经出现了巨大的变化。在我们进入一个不确定的未来时，对过去时间段内超出我们现代观察范围的流域行为进行评估，将有助于水资源管理者和使用者做出决策和规划。过去过程的记录显示了景观如何响应气候和能量输入的变化，无论未来条件变化的原因如何，了解干旱和半干旱环境中的流域动态至关重要。这一研究方法将增强树木年轮科学的知识，增加我们对流域尺度气候变化的理解，并阐明树木年轮记录与水收支之间的关系。该项目的重建结果将立即用于沃克盆地和邻近流域的科学家、水管理人员和用水者。通过该项目的调查和安装获得的气候和生态数据将提供给广泛的公共用户，并实时提供传感器数据。通过将联邦、大学和社区学院的研究人员聚集在一起，该项目为不同层次的合作和推广提供了独特的机会。教育机会将提供给研究生、本科生和社区学院的学生，他们将能够参加实地和实验室工作以及科学会议。