Estimation of Diffusional Growth Rate and Reassessing Existing Parameterizations for Monsoon Precipitating Clouds: A Process-Based Approach

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Moumita Bhowmik, Anupam Hazra, Suryachandra A. Rao, Lian-Ping Wang
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Abstract

Quantitative prediction of the intensity of rainfall events (light or heavy) has remained a challenge in Numerical Weather Prediction (NWP) models. For the first time, the mean coefficient of diffusional growth rate (\(c_m\)) is calculated using a Eulerian-Lagrangian particle-based model on in situ airborne measurement data from the Cloud Aerosol Interaction and Precipitation Enhancement Experiment (CAIPEEX) during monsoon over the Indian sub-continent. The results show that \(c_m\) varies in the range of \(\sim 0.25\times 10^{-3} - 1.5\times 10^{-3}\) (cm \(s^{-1}\)). The generic problem of overestimation of light rain in NWP models might be related to the choice of \(c_m\) in the model. It is also shown from a direct numerical simulation (DNS) experiment using small-scale model that relative dispersion (\(\epsilon \)) is constrained with average values in the range of \(\sim \) 0.2\(-\)0.37 (\(\sim \) 0.1\(-\)0.26) in less humid (more humid) conditions. This is in agreement with in situ airborne observation (\(\epsilon \) \(\sim \) 0.36) and previous studies over the Indian sub-continent. The linear relationship between relative dispersion (\(\epsilon \)) and cloud droplet number concentration (NC) is obtained using CAIPEEX. The present study compares different exciting parameterizations for the cloud-to-rain “autoconversion” and effective radius using a sophisticated parcel-DNS model guided by CAIPEEX observation. The dispersion-based ‘autoconversion’ and effective radius parameterization schemes for the Indian region must be useful for the calculation of Indian summer monsoon precipitation in the general circulation model. The present study also provides valuable guidance for parameterizing the effective radius, which is important for the radiation scheme.

季风降水云扩散增长率的估计和现有参数化的重新评估:一个基于过程的方法
在数值天气预报(NWP)模式中,降水事件(轻或重)强度的定量预测一直是一个挑战。本文首次利用基于欧拉-拉格朗日粒子的模型计算了印度次大陆季风期间云气溶胶相互作用和降水增强实验(CAIPEEX)的现场机载测量数据的平均扩散增长率系数(\(c_m\))。结果表明,\(c_m\)在\(\sim 0.25\times 10^{-3} - 1.5\times 10^{-3}\) (cm \(s^{-1}\))范围内变化。NWP模型中小雨估计过高的一般问题可能与模型中\(c_m\)的选择有关。利用小尺度模型进行的直接数值模拟(DNS)实验也表明,相对色散(\(\epsilon \))在较低湿度(较潮湿)条件下的平均值为\(\sim \) 0.2 \(-\) 0.37 (\(\sim \) 0.1 \(-\) 0.26)。这与现场机载观测(\(\epsilon \)\(\sim \) 0.36)和以前对印度次大陆的研究相一致。利用CAIPEEX得到了相对色散(\(\epsilon \))与云滴数浓度(NC)之间的线性关系。在CAIPEEX观测的指导下,本研究使用复杂的包- dns模型比较了云-雨“自动转换”和有效半径的不同激励参数化。印度地区基于弥散的“自转换”和有效的半径参数化方案对于一般环流模式下印度夏季风降水的计算一定是有用的。本研究还为有效半径的参数化提供了有价值的指导,有效半径的参数化对辐射方案具有重要意义。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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