COLLABORATIVE PROPOSAL: An Investigation of Wave Dynamics in the Arctic Mesosphere and Coupling Between the Lower and Upper Polar Atmosphere

合作提案：北极中间层波浪动力学以及下层和上层极地大气之间的耦合研究

• 批准号: 1023265
• 负责人: Michael Taylor
• 金额: $ 8.28万
• 依托单位: Utah State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2010
• 资助国家: 美国
• 起止时间: 2010-09-01 至 2014-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1023265&HistoricalAwards=false
• 关键词: COLLABORATIVE; PROPOSAL; Investigation; Wave; Dynamics

The research objective is to utilize a suite of instruments, includingan airglow imager, to investigate short-periodgravity waves in the Arctic atmosphere over Alaska. Short-periodgravity waves are an important component of the larger atmosphericcirculation as these waves are believed to transport a large amount ofvertical moment flux into the mesosphere and lower thermosphere (MLT)region. While the propagation nature and sources of these waves havebeen studied extensively at low- and mid-latitudes, little is known about their behavior at high latitudes. Recent efforts havebegun to characterize the waves over the Antarctic continent, whilethe project proposed here will focus on the Arctic. Specifically, theproposed research will establish a long-term winter time series ofshort-period gravity waves in the Arctic, including their dominantsource regions, and influences of large-scale tidal and planetary wavemotion. The co-located Rayleigh lidar will provide essential highvertical resolution temperature measurements to help elucidate thevertical wave propagation, individual wave contribution to theEliassen-Palm (EP) flux, and coupling between the lower and upperatmosphere during stratospheric warming events.

研究的目的是利用一套仪器，包括airglow成像仪，调查阿拉斯加上空北极大气中的短周期重力波。短周期重力波是大尺度大气环流的重要组成部分，因为这些重力波被认为将大量的垂直矩通量输送到中层和低热层（MLT）区域。虽然这些波的传播性质和来源已经在低纬度和中纬度进行了广泛的研究，但对它们在高纬度的行为知之甚少。最近的努力已经开始描述南极大陆上的波浪，而这里提出的项目将集中在北极。具体来说，拟议的研究将建立北极短期重力波的长期冬季时间序列，包括其主要来源区域以及大规模潮汐和行星波情感的影响。协同定位的瑞利激光雷达将提供必要的高垂直分辨率温度测量，以帮助阐明垂直波传播，个别波对Eliassen-Palm（EP）通量的贡献，以及平流层变暖事件期间低层和高层大气之间的耦合。