Stratospheric and Oceanic Contribution to Atlantic Decadal Climate Variability

平流层和海洋对大西洋年代际气候变化的贡献

• 批准号: 0002267
• 负责人: Gavin Schmidt
• 金额: $ 16.91万
• 依托单位: Columbia University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2000
• 资助国家: 美国
• 起止时间: 2000-08-01 至 2002-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0002267&HistoricalAwards=false
• 关键词: Stratospheric; Oceanic; Contribution; Atlantic; Decadal

This project seeks to determine how the impact of stratospheric changes at the earth's surface is affected by model resolution, improvements in model physics and the nature of the ocean model used (dynamical versus mixed layer ocean). The PIs will examine to what extent any cooling in the North Atlantic is a feature of natural variability or forced (including ocean heat transport changes, changes in atmospheric circulation, increasing greenhouse gases and/or aerosol loadings). The PIs will (i) to quantify the importance of including stratospheric dynamics in climate change experiments and the potential for important tropospheric and oceanic feedbacks; (ii) to project (based on given scenarios) future trends in the North Atlantic surface air temperature and examine their dependence on the inclusion of the stratospheric and oceanic components; and (iii) to examine to what extent fingerprints of anthropogenic climate change are robust over all the model configurations used in the study. The NASA GISS model with finer vertical and horizontal resolution will be used. The model will also include on-line ozone chemistry and transport. This will improve the solar cycle heating effects in the stratosphere. Interannual varying SST will be used, this may help generate more realistic summer results than with the low resolution. The work is important because it will increase understanding of the role of the stratosphere in climate.

该项目旨在确定地球表面平流层变化的影响如何受到模型分辨率、模型物理学的改进和所用海洋模型的性质（动力海洋与混合层海洋）的影响。研究所将审查北大西洋的任何冷却在多大程度上是自然变率或强迫变率的特征（包括海洋热传输变化、大气环流变化、温室气体和/或气溶胶负荷增加）。主要研究者将（一）量化将平流层动力学纳入气候变化实验的重要性以及重要的对流层和海洋反馈的潜力;（二）预测（根据给定的设想）北大西洋表面气温的未来趋势，并审查其对纳入平流层和海洋组成部分的依赖性;以及（iii）检查在研究中使用的所有模式配置中，人为气候变化的指纹在多大程度上是稳健的。 将使用具有更高垂直和水平分辨率的NASA GISS模型。该模型还将包括在线臭氧化学和传输。这将改善平流层中太阳循环的加热效应。将使用年际变化的SST，这可能有助于产生比低分辨率更真实的夏季结果。 这项工作很重要，因为它将增加对平流层在气候中作用的理解。