Mountain-Wave Evolution and Orographic Precipitation

山波演化与地形降水

• 批准号: 1545927
• 负责人: Dale Durran
• 金额: $ 73.35万
• 依托单位: University of Washington
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2016
• 资助国家: 美国
• 起止时间: 2016-01-01 至 2019-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1545927&HistoricalAwards=false
• 关键词: Mountain; Wave; Evolution; Orographic; Precipitation

Mountains form natural barriers to wind flow. As winds in general, and storms in particular, approach mountain ranges, mountain waves develop above and downstream of the barrier. At the same time, low-level flow may become blocked and diverted around the periphery of the mountains. These flows are often too small in scale to be accurately captured by global weather and climate models, but produce drag on the large-scale flow that must be parameterized. This research includes the training and professional development of two graduate students, including one under-represented minority. Results will be shared through journal articles and conference presentations, including webinars organized by the Mountain Meteorology Committee of the American Meteorological Society (AMS). The results of this research will also benefit water resource managers, hydrologists and those studying the current state of our climate and potential future shifts in mid-latitude storms.This study attempts to place parameterization on a firmer theoretical foundation. The large-scale responses to orographic drag will be studied through the analysis of high-resolution numerical simulations. Heavy precipitation over mountains is largely driven by the passage of large-scale weather systems. Prototypical theoretical studies of the interactions of these weather systems with idealized mountain ranges have not previously been undertaken due to the complexity of modeling large- and small-scale flows. This research builds on prior studies of multi-scale interactions in dry air flow by the inclusion of moist flow as a result of the combination of mid-latitude cyclones and more localized ascent forced by topography into vigorous updrafts and enhanced precipitation.

山形成了自然障碍风流。 随着风的一般风暴，尤其是暴风雨，接近山脉，山脉在障碍物的上方和下游发展。 同时，低水平的流程可能会被阻塞并在山区的周围转移。 这些流的规模通常太小，无法被全球天气和气候模型准确捕获，但是在必须被参数化的大规模流程上产生阻力。 这项研究包括对两名研究生的培训和专业发展，其中包括一个代表性不足的少数民族。 结果将通过期刊文章和会议演讲共享，包括美国气象学会山气象委员会（AMS）组织的网络研讨会。 这项研究的结果还将使水资源经理，水文学家以及研究我们气候状态的当前状态以及中纬度风暴中潜在的未来转变的结果受益。这项研究试图将参数化置于更坚定的理论基础上。 通过分析高分辨率数值模拟，将研究对地形阻力的大规模响应。 大型天气系统通过大量造成的山脉降水。 这些天气系统与理想化的山脉相互作用的典型理论研究以前没有进行，这是由于对大型和小规模流量进行建模的复杂性。 这项研究是基于对干燥空气流中多尺度相互作用的先前研究，这是由于中纬度旋风旋风的结合和更具局部化的升高而被形态强迫到剧烈的上升气流和增强的降水而导致的。

项目成果

The Influence of Gravity Waves on the Slope of the Kinetic Energy Spectrum in Simulations of Idealized Midlatitude Cyclones

• DOI: 10.1175/jas-d-18-0329.1
• 发表时间: 2019-06
• 期刊: Journal of the Atmospheric Sciences
• 影响因子: 3.1
• 作者: M. Menchaca;D. Durran

Mountain Waves, Downslope Winds, and Low-Level Blocking Forced by a Midlatitude Cyclone Encountering an Isolated Ridge

中纬度气旋遇到孤立山脊所造成的山浪、下坡风和低空阻挡

• DOI: 10.1175/jas-d-16-0092.1
• 发表时间: 2017
• 期刊: Journal of the Atmospheric Sciences
• 影响因子: 3.1
• 作者: Menchaca, Maximo Q.;Durran, Dale R.
• 通讯作者: Durran, Dale R.

Can Mountain Waves Contribute to Damaging Winds Far Away from the Lee Slope?

远离李坡的山浪会带来破坏性的风吗？

• DOI: 10.1175/waf-d-18-0207.1
• 发表时间: 2019
• 期刊: Weather and Forecasting
• 影响因子: 2.9
• 作者: Kelley, Jeffrey D.;Schultz, David M.;Schumacher, Russ S.;Durran, Dale R.
• 通讯作者: Durran, Dale R.

Unusual Trapped Mountain Lee Waves with Deep Vertical Penetration and Significant Stratospheric Amplitude

具有深垂直穿透和平流层振幅的异常困山背风波

• DOI: 10.1175/jas-d-19-0093.1
• 发表时间: 2020
• 期刊: Journal of the Atmospheric Sciences
• 影响因子: 3.1
• 作者: Metz, Johnathan J.;Durran, Dale R.;Blossey, Peter N.
• 通讯作者: Blossey, Peter N.

The Influence of Vertical Wind Shear on the Evolution of Mountain-Wave Momentum Flux

垂直风切变对山波动量通量演化的影响

• DOI: 10.1175/jas-d-18-0231.1
• 发表时间: 2019
• 期刊: Journal of the Atmospheric Sciences
• 影响因子: 3.1
• 作者: Durran, Dale R.;Menchaca, Maximo Q.
• 通讯作者: Menchaca, Maximo Q.