Comparison of Mesoscale and Large-Eddy Simulation Results with Observational Data in the Atmospheric Boundary Layer

被引：0

作者：

Anisimov, S. V. ^{[1
]}

Mareev, E. A. ^{[2
]}

Galichenko, S. V. ^{[1
]}

Ilin, N. V. ^{[2
]}

Prokhorchuk, A. A. ^{[1
]}

Klimanova, E. V. ^{[1
]}

Kozmina, A. S. ^{[1
]}

Aphinogenov, K. V. ^{[1
]}

Guriev, A. V. ^{[1
]}

机构：

[1] Russian Acad Sci, Inst Phys Earth, Borok Geophys Observ, Branch Schmidt, Yaroslavl oblast 152742, Russia

[2] Russian Acad Sci, Fed Res Ctr, Gaponov Grekhov Inst Appl Phys, Nizhnii Novgorod 603950, Russia

来源：

IZVESTIYA ATMOSPHERIC AND OCEANIC PHYSICS | 2025年 / 61卷 / 02期

基金：

俄罗斯科学基金会;

关键词：

atmospheric boundary layer; mesoscale atmospheric modeling; large-eddy simulation; acoustic and microwave atmospheric sounding; TURBULENT INFLOW GENERATION; WEATHER RESEARCH; MODEL; WRF; APPROXIMATION; SENSITIVITY; CONVECTION;

D O I：

10.1134/S0001433825700239

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

A numerical model of micrometeorology and turbulent dynamics of the daytime atmospheric boundary layer over a complex surface has been developed. The model was built by nesting the large-eddy simulation using the PALM into the mesoscale Weather Research and Forecasting (WRF) model. The modeling results are compared with the data of acoustic and microwave sounding of the atmosphere and ground-based and airborne observations using a tethered balloon with temperature and humidity sensors. Deviations of the main meteorological and turbulent parameters predicted by the model from the measured values are estimated.

引用

页码：111 / 131

页数：21

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