Development of the Convective Boundary Layer Capping with a Thick Neutral Layer in Badanjilin： Observations and Simulations
In this study, the development of a convective boundary layer （CBL） in the Badaujilin region was investigated by comparing the observation data of two cases. A deep neutral layer capped a CBL that occurred on 30 August 2009. This case was divided into five sublayers from the surface to higher atmosp...
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| Published in | Advances in atmospheric sciences Vol. 29; no. 1; pp. 177 - 192 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Heidelberg
SP Science Press
2012
Springer Nature B.V Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, No. 320, Donggang West Road, Lanzhou 730000 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0256-1530 1861-9533 |
| DOI | 10.1007/s00376-011-0207-4 |
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| Abstract | In this study, the development of a convective boundary layer （CBL） in the Badaujilin region was investigated by comparing the observation data of two cases. A deep neutral layer capped a CBL that occurred on 30 August 2009. This case was divided into five sublayers from the surface to higher atmospheric elevations： surface layer, mixed layer, inversion layer, neutral layer, and sub-inversion layer. The development process of the CBL was divided into three stages： S1, S2, and S3. This case was quite different from the development of the three-layer CBL observed on 31 August 2009 because the mixed layer of the five-layer CBL （CBL5） eroded the neutral layer during S2. The specific initial structure of the CBL5 was correlated to the synoptic background of atmosphere during nighttime. The three-stage development process of the CBL5 was confirmed by six simulations using National Center for Atmospheric Research （USA） large-eddy simulation （NCAR-LES）, and some of its characteristics are presented in detail. |
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| AbstractList | In this study, the development of a convective boundary layer (CBL) in the Badanjilin region was investigated by comparing the observation data of two cases. A deep neutral layer capped a CBL that occurred on 30 August 2009. This case was divided into five sublayers from the surface to higher atmospheric elevations: surface layer, mixed layer, inversion layer, neutral layer, and sub-inversion layer. The development process of the CBL was divided into three stages: S1, S2, and S3. This case was quite different from the development of the three-layer CBL observed on 31 August 2009 because the mixed layer of the five-layer CBL (CBL5) eroded the neutral layer during S2. The specific initial structure of the CBL5 was correlated to the synoptic background of atmosphere during nighttime. The three-stage development process of the CBL5 was confirmed by six simulations using National Center for Atmospheric Research (USA) large-eddy simulation (NCAR-LES), and some of its characteristics are presented in detail.[PUBLICATION ABSTRACT] In this study, the development of a convective boundary layer (CBL) in the Badanjilin region was investigated by comparing the observation data of two cases. A deep neutral layer capped a CBL that occurred on 30 August 2009. This case was divided into five sublayers from the surface to higher atmospheric elevations: surface layer, mixed layer, inversion layer, neutral layer, and sub-inversion layer. The development process of the CBL was divided into three stages: S1, S2, and S3. This case was quite different from the development of the three-layer CBL observed on 31 August 2009 because the mixed layer of the five-layer CBL (CBL5) eroded the neutral layer during S2. The specific initial structure of the CBL5 was correlated to the synoptic background of atmosphere during nighttime. The three-stage development process of the CBL5 was confirmed by six simulations using National Center for Atmospheric Research (USA) large-eddy simulation (NCAR-LES), and some of its characteristics are presented in detail. P412.292; In this study,the development of a convective boundary layer (CBL) in the Badanjilin region was investigated by comparing the observation data of two cases.A deep neutral layer capped a CBL that occurred on 30 August 2009.This case was divided into five sublayers from the surface to higher atmospheric elevations:surface layer,mixed layer,inversion layer,neutral layer,and sub-inversion layer.The development process of the CBL was divided into three stages:S1,S2,and S3.This case was quite different from the development of the three-layer CBL observed on 31 August 2009 because the mixed layer of the five-layer CBL (CBL5) eroded the neutral layer during S2.The specific initial structure of the CBL5 was correlated to the synoptic background of atmosphere during nighttime.The three-stage development process of the CBL5 was confirmed by six simulations using National Center for Atmospheric Research (USA) large-eddy simulation (NCAR-LES),and some of its characteristics are presented in detail. In this study, the development of a convective boundary layer （CBL） in the Badaujilin region was investigated by comparing the observation data of two cases. A deep neutral layer capped a CBL that occurred on 30 August 2009. This case was divided into five sublayers from the surface to higher atmospheric elevations： surface layer, mixed layer, inversion layer, neutral layer, and sub-inversion layer. The development process of the CBL was divided into three stages： S1, S2, and S3. This case was quite different from the development of the three-layer CBL observed on 31 August 2009 because the mixed layer of the five-layer CBL （CBL5） eroded the neutral layer during S2. The specific initial structure of the CBL5 was correlated to the synoptic background of atmosphere during nighttime. The three-stage development process of the CBL5 was confirmed by six simulations using National Center for Atmospheric Research （USA） large-eddy simulation （NCAR-LES）, and some of its characteristics are presented in detail. |
| Author | 韩博 吕世华 奥银焕 |
| AuthorAffiliation | Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, No. 320, Donggang West Road, Lanzhou 730000 |
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| CitedBy_id | crossref_primary_10_1155_2017_8352461 crossref_primary_10_5194_acp_14_4515_2014 crossref_primary_10_1016_j_atmosres_2024_107252 crossref_primary_10_1175_JAS_D_15_0148_1 crossref_primary_10_1007_s00376_014_4164_6 crossref_primary_10_1007_s00704_016_2014_4 crossref_primary_10_1007_s00704_017_2258_7 crossref_primary_10_1360_TB_2024_1294 crossref_primary_10_5194_acp_24_10947_2024 crossref_primary_10_1007_s13351_018_8001_1 |
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| ClassificationCodes | P412.292 |
| ContentType | Journal Article |
| Copyright | Chinese National Committee for International Association of Meteorology and Atmospheric Sciences, Institute of Atmospheric Physics, Science Press and Springer-Verlag Berlin Heidelberg 2012 Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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| DOI | 10.1007/s00376-011-0207-4 |
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| DocumentTitleAlternate | Development of the Convective Boundary Layer Capping with a Thick Neutral Layer in Badanjilin： Observations and Simulations |
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| Notes | In this study, the development of a convective boundary layer （CBL） in the Badaujilin region was investigated by comparing the observation data of two cases. A deep neutral layer capped a CBL that occurred on 30 August 2009. This case was divided into five sublayers from the surface to higher atmospheric elevations： surface layer, mixed layer, inversion layer, neutral layer, and sub-inversion layer. The development process of the CBL was divided into three stages： S1, S2, and S3. This case was quite different from the development of the three-layer CBL observed on 31 August 2009 because the mixed layer of the five-layer CBL （CBL5） eroded the neutral layer during S2. The specific initial structure of the CBL5 was correlated to the synoptic background of atmosphere during nighttime. The three-stage development process of the CBL5 was confirmed by six simulations using National Center for Atmospheric Research （USA） large-eddy simulation （NCAR-LES）, and some of its characteristics are presented in detail. HAN Bo, LU Shihua, AO Yinhuan Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, No. 320, Donggang West Road, Lanzhou 730000 convective boundary layer, neutral layer, large-scale circulation, large-eddy simulation 11-1925/O4 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14 ObjectType-Article-1 ObjectType-Feature-2 content type line 23 |
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| PublicationTitle | Advances in atmospheric sciences |
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| PublicationYear | 2012 |
| Publisher | SP Science Press Springer Nature B.V Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, No. 320, Donggang West Road, Lanzhou 730000 |
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| Snippet | In this study, the development of a convective boundary layer （CBL） in the Badaujilin region was investigated by comparing the observation data of two cases. A... In this study, the development of a convective boundary layer (CBL) in the Badanjilin region was investigated by comparing the observation data of two cases. A... P412.292; In this study,the development of a convective boundary layer (CBL) in the Badanjilin region was investigated by comparing the observation data of two... |
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| SourceType | Aggregation Database Enrichment Source Index Database Publisher |
| StartPage | 177 |
| SubjectTerms | Atmospheric boundary layer Atmospheric circulation Atmospheric research Atmospheric Sciences Atmospherics Boundary layer Boundary layers Capping Correlation Earth and Environmental Science Earth Sciences Elevation Geophysics/Geodesy Large eddy simulation Marine Mesoscale convective complexes Meteorology Simulation Surface layer 中性层 大涡模拟 天气背景 对流边界层 巴丹吉林 覆盖层 观测数据 边界带 |
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| Title | Development of the Convective Boundary Layer Capping with a Thick Neutral Layer in Badanjilin： Observations and Simulations |
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