Supercooled Liquid Water at the Top of a Snow-Producing Nimbostratus Cloud and Its Association With Gravity Wave Breaking and Turbulence: An IMPACTS Case Study

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Mei Han, Scott A. Braun, Timothy Lang, Matthew L. Walker Mclinden, Gerald M. Heymsfield, Lihua Li, Kenneth L. Thornhill
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Abstract

Supercooled liquid water (SLW) at the top of a snow-producing nimbostratus cloud was thoroughly characterized with remote-sensing and in situ measurements during the NASA Investigation of Microphysics and Precipitation for Atlantic Coast-Threatening Snowstorms (IMPACTS) field campaign on 30 January 2022. With three coordinated flight legs, airborne downward-looking cloud radar and lidar and in situ microphysics and wind probes provided a comprehensive depiction of the cloud system over a one-hour period. NASA Cloud Physics Lidar (CPL) measurements suggest that the SLW layer was greater than several hundred meters thick and ∼100 km long within the sampling window. The in situ cloud probes measured a maximum liquid water content (LWC) of 0.58 g m−3. NASA Cloud Radar System (CRS) reflectivity and Doppler data revealed gravity waves within the nimbostratus below a strong temperature inversion that was caused by warm air advection near an occluded front in an extratropical cyclone. The enhanced CRS Doppler spectrum width indicated turbulence that was likely generated by gravity wave breaking while propagating upward. Analyses of the Brunt–Väisälä frequency and the Richardson number with NOAA High Resolution Rapid Refresh (HRRR) model supported the observed gravity wave activity. The eddy dissipation rate (EDR) was calculated from both the CRS spectrum width and the in situ wind measured by the Turbulent Air Motion Measurement Systems (TAMMS) to quantify the magnitudes of turbulence and to provide a promising intercomparison between the remote-sensing and in situ turbulence data. A moderate correlation between in situ EDR and LWC suggests that the turbulence likely contributed to the SLW cloud top.

产生雪的雨层云顶部的过冷液态水及其与重力波破裂和湍流的关系:一个影响案例研究
在2022年1月30日NASA“大西洋沿岸威胁暴风雪(影响)的微物理和降水调查”野外活动期间,通过遥感和现场测量,对产生雪的nimbostratus云顶部的过冷液态水(SLW)进行了全面表征。通过三个协调的飞行腿,机载向下看云雷达和激光雷达以及现场微物理和风探测器在一小时内提供了云系统的全面描述。NASA云物理激光雷达(CPL)的测量结果表明,在采样窗口内,SLW层的厚度大于数百米,长度约为100公里。原位云探针测得的最大液态水含量(LWC)为0.58 g m−3。美国国家航空航天局云雷达系统(CRS)的反射率和多普勒数据显示,在一个强逆温区下面的气平流层中存在重力波,该逆温区是由温带气旋中一个阻塞锋附近的暖空气平流引起的。增强的CRS多普勒频谱宽度表明湍流可能是由重力波在向上传播过程中破裂产生的。利用NOAA高分辨率快速刷新(HRRR)模式对Brunt-Väisälä频率和Richardson数的分析支持观测到的重力波活动。涡流耗散率(EDR)由CRS频谱宽度和湍流空气运动测量系统(TAMMS)测量的现场风计算得到,以量化湍流的强度,并为遥感和现场湍流数据之间的比较提供了一个有希望的方法。原位EDR和LWC之间的中等相关性表明湍流可能对SLW云顶有贡献。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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