Collaborative Research: Climate Variability and Change in the U.S. GLOBEC Regions as Simulated by the IPCC Climate Models: Ecosystem Implications

合作研究：IPCC 气候模型模拟的美国 GLOBEC 地区的气候变率和变化：生态系统影响

• 批准号: 0814578
• 负责人: Nicholas Bond
• 金额: $ 3.42万
• 依托单位: University of Washington
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2008
• 资助国家: 美国
• 起止时间: 2008-09-01 至 2011-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0814578&HistoricalAwards=false
• 关键词: Collaborative; Research; Climate; Variability; Change

A large body of literature has shown that ecosystem dynamics is strongly influenced by large scale climate variations. A primary way by which climate can affect marine biological processes is through wind-driven changes of the ocean circulation, which are influenced by both natural and anthropogenically-induced variability. Simulations performed with 23 state-of-the-art climate models in support of the Intergovermental Panel for Climate Change (IPCC) Assessment Report 4 (AR4) are the principle means for examining climate change. The IPCC-AR4 simulations include runs with fixed external (solar, volcanoes, greenhouse gases) forcing (control simulations), as well as simulations where external forcing is prescribed according to the observed 20th century record (20th century simulations) or according to different climate change scenarios. These climate integrations are global and provide complete information on a large number of variables, including those relevant for marine ecosystems, at each model grid point. The output from the IPCC-AR4 simulations will be used to examine climate variability and change in the three GLOBEC regions (northeast Pacific, northwest Atlantic, and Southern Ocean) focusing on the following questions:1. Does the present generation of climate models show connections between large-scale low-frequency wind forcing variations and ocean circulation changes in the three GLOBEC study areas similar to those that are believed to exist in nature? Can the IPCC-AR4 multi-model ensembles be used to extend the observational record and test hypotheses on the climate-circulation links with a larger statistical confidence?2. Based on the most reliable climate models, to what extent will the influence of climate upon regional processes change over the 21st and 22nd centuries?3. Can statistical downscaling methods be developed and used for relating variations at the regional (ecosystem) scale to large-scale climate forcing? Can specific parameters be identified that are more amenable to statistical downscaling?The first question will be addressed by analyzing the control and 20th century simulations, while projections of the influence of climate on regional processes in the next century will be examined using the scenario simulations. Available data, as well as output from a regional model at different resolutions will be used to assess the feasibility of statistical downscaling.This study will improve understanding of the links between large-scale climate forcing and physical processes important for ecosystem dynamics in different regions. The global nature of climate models enables a consistent means of establishing connections within and between different geographical regions. Thus, results from this study support the pan-regional synthesis phase of the GLOBEC program.The present study has the potential to enhance the ability to predict ecosystem changes due to natural and/or anthropogenically induced climate variations. Results from this project can support regional ecosystem studies by providing a perspective of the large-scale forcing and its evolution in a changing climate, as well as boundary condition and forcing fields for regional models. Specifically, a key aspect of this project will be to provide output from the IPPC model simulations and guidance in how to use the output to other researchers funded through this phase of the GLOBEC program. Results from this study will also be presented to middle and high school students through the outreach programs at NOAA and at the investigators' Universities.

大量文献表明，生态系统动力学受到大尺度气候变化的强烈影响。气候可以影响海洋生物过程的一个主要方式是通过风驱动的海洋环流变化，这种变化受到自然和人为引起的变率的影响。为支持政府间气候变化专门委员会（IPCC）第4次评估报告（AR4），利用23个最先进的气候模式进行的模拟是审查气候变化的主要手段。IPCC-AR4模拟包括具有固定外部强迫（太阳、火山、温室气体）的运行（控制模拟），以及根据观测到的20世纪记录（20世纪模拟）或根据不同气候变化情景规定外部强迫的模拟。这些气候综合是全球性的，在每个模式网格点提供了大量变量的完整信息，包括与海洋生态系统有关的变量。IPCC-AR4模拟的结果将用于检查三个GLOBEC区域（东北太平洋、西北大西洋和南大洋）的气候变率和变化，重点关注以下问题：当前这一代的气候模式是否表明，在三个GLOBEC研究区域中，大尺度低频风强迫变化与海洋环流变化之间的联系与那些被认为存在于自然界的联系相似？IPCC-AR4多模式组合能否以更高的统计置信度扩展观测记录和检验关于气候环流联系的假设？基于最可靠的气候模式，在21世纪和22世纪，气候对区域过程的影响将在多大程度上发生变化？能否开发和使用统计降尺度方法将区域（生态系统）尺度上的变化与大尺度气候强迫联系起来？是否可以确定更适合统计缩尺的具体参数？第一个问题将通过分析控制和20世纪的模拟来解决，而下个世纪气候对区域过程影响的预估将使用情景模拟来研究。现有数据以及不同分辨率的区域模式产出将用于评估统计降尺度的可行性。这项研究将提高对大尺度气候强迫与不同区域生态系统动力学重要物理过程之间联系的认识。气候模式的全球性使其能够在不同地理区域内部和区域之间建立一致的联系。因此，本研究的结果支持GLOBEC项目的泛区域综合阶段。本研究有可能提高对自然和/或人为气候变化引起的生态系统变化的预测能力。本项目的研究结果可以为区域生态系统研究提供一个视角，揭示气候变化中的大尺度强迫及其演化，以及区域模式的边界条件和强迫场。具体而言，该项目的一个关键方面将是提供国际植物保护公约模式模拟的结果，并指导如何将这些结果用于GLOBEC计划这一阶段资助的其他研究人员。这项研究的结果也将通过国家海洋和大气管理局和调查人员所在大学的外展项目向初高中学生展示。