Collaborative Research: Dynamics and Climatic Response of the Taylor Glacier System

合作研究：泰勒冰川系统的动力学和气候响应

• 批准号: 0125579
• 负责人: Kurt Cuffey
• 金额: --
• 依托单位: University of California-Berkeley
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2002
• 资助国家: 美国
• 起止时间: 2002-08-15 至 2007-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0125579&HistoricalAwards=false
• 关键词: Collaborative; Research; Dynamics; Climatic; Response

This award supports a project to significantly improve our understanding of how Taylor Glacier flows and responds to climate changes. Taylor Glacier drains the Taylor Dome region of the East Antarctic Ice Sheet and terminates in Taylor Valley, one of the Dry Valleys of Victoria Land. It provides a crucial and unique link between two intensively studied Antarctic environments: the Taylor Dome, from which a 130 kyr ice core paleoclimate record has recently been extracted, and the Dry Valleys, a pivotal Long-Term Ecological Research (LTER) site and a focus of research on geomorphology and glacial geology. The proposed work will thus make an important contribution to ongoing efforts to exploit the Taylor Dome - Dry Valleys system to build a uniquely comprehensive view of regional long-term environmental changes. The proposed work has two complementary components: field research and numerical modelling. Two field seasons will be used to measure velocity, surface strain rate, mass balance, ice thickness, glacier bed reflectance, and subglacial topography, along a nearly complete longitudinal transect of the Taylor Glacier, and along select cross-valley transects. This information will be used to constrain numerical models of ice and heat flow for the Taylor Dome - Taylor Glacier system. These calibrated models will be used to analyze the time-dependent response of the Taylor Glacier to climate changes. The synthesis of results will be aimed to improve understanding of the glacial geomorphology of Taylor Valley, and to illuminate impacts on the Taylor Valley lakes ecosystem. The project will have a major role in furthering the careers of a doctoral-level graduate student and a post-doctoral researcher.

该奖项支持一个项目，以显著提高我们对泰勒冰川如何流动和应对气候变化的理解。泰勒冰川从南极东部冰盖的泰勒穹窿地区流出，最终到达维多利亚地干谷之一的泰勒谷。它为两个被深入研究的南极环境提供了一个关键而独特的联系：泰勒穹窿（Taylor Dome）和干谷（Dry Valleys），前者最近从其中提取了130凯尔的冰芯古气候记录，后者是一个关键的长期生态研究（ltr）地点，也是地貌学和冰川地质学研究的重点。因此，拟议的工作将对正在进行的利用泰勒穹窿-干谷系统的努力作出重要贡献，以建立对区域长期环境变化的独特全面的看法。提出的工作有两个互补的组成部分：实地研究和数值模拟。两个野外季节将用于测量速度、表面应变率、质量平衡、冰厚、冰川床反射率和冰下地形，沿着泰勒冰川几乎完整的纵向样带，以及沿着选定的跨山谷样带。这些信息将被用来约束泰勒穹窿-泰勒冰川系统的冰和热流的数值模型。这些经过校准的模型将用于分析泰勒冰川对气候变化的随时间变化的响应。综合结果将有助于提高对泰勒谷冰川地貌的认识，并阐明对泰勒谷湖泊生态系统的影响。该项目将对博士级研究生和博士后研究人员的职业发展起到重要作用。