对流边界层湍流通量及逆梯度输送参数化分析
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

国家自然科学基金资助项目(41075113;41175093);南京信息工程大学引进人才启动资助项目(20110304)


A case study of turbulent flux and counter gradient transport in the convective boundary layer
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 文章评论
  • |
  • 资源附件
    摘要:

    "K"理论是众多气象预报模式中运用最广泛的湍流参数化方案之一,但无法解释"逆梯度"的输送,必须进行修正。最具代表性的修正方案有三种:方案Ⅰ(Deardroff方案)、方案Ⅱ(Holtslag和Moeng方案)和方案Ⅲ(刘烽方案)。本文利用香河的边界层观测资料对上述三种方案进行验证和比较,发现方案Ⅰ的结果在整个对流边界层(Convective Boundary Layer,CBL)呈系统性偏低,与观测不符;方案Ⅱ在CBL中上部能够再现逆梯度输送现象,基本能给出合理的湍流通量垂直分布,但在CBL的下部和上部与观测不符;方案Ⅲ的逆梯度项与高度有关,并在CBL中部达到最大,而其他两个方案中逆梯度项随高度不变。该方案不但在CBL中上部与方案Ⅱ的结果一致,并能合理表达整个CBL内的湍流通量分布,更接近观测结果。

    Abstract:

    K-theory is one of the most extensive turbulent closure revision schemes using weather patterns.However,because it cannot explain the counter-gradient transportation phenomenon,it must be corrected.There are three turbulent closure revision schemes representative of the convective boundary layer(CBL):the first was developed by Deardorff(1972),the second scheme by Holtslag and Moeng(1991),and the third by Liu Feng(2001).Because these schemes are based on different physical assumptions,they present different parameterizations and interpretations of counter-gradient transportation within the CBL.In the present work,using part of the published database obtained from the WL-ARPDD94 Experiment in Xianghe,the three schemes were tested and compared.The results showed that the first scheme systematically underestimates the heat flux within the entire CBL,and is inconsistent with the observations of the Xianghe CBL Experiment.The second scheme can reproduce inverse gradient transportation phenomena in most of the CBL,and can basically depict the vertical distribution of turbulent flux.However,it is not in agreement with observations in the lower and upper CBL.The third scheme's counter-gradient item is related to height,reaching a maximum in the central CBL,while the other two schemes' counter-gradient items remain constant with changes in height.The third scheme's results are not only consistent with the second scheme in most of the CBL,but can also reasonably describe the turbulent flux distribution within the entire CBL.Liu's parameterization exhibits good agreement with observations in the whole CBL.The analysis suggests that Liu's scheme,first used to determine heat flux based on field experiment data,is able to represent the heat flux profile for the CBL.On the basis of reviewing the physical interpretation of counter-gradient transport phenomena by the different closure schemes,a universal scheme for the planetary boundary layer,suitable for numerical weather forecasting models,is urgently needed.

    参考文献
    相似文献
    引证文献
引用本文

韩永翔,宋昊冬,刘烽,赵天良,2016.对流边界层湍流通量及逆梯度输送参数化分析[J].大气科学学报,39(3):417-425. HAN Yongxiang, SONG Haodong, LIU Feng, ZHAO Tianliang,2016. A case study of turbulent flux and counter gradient transport in the convective boundary layer[J]. Trans Atmos Sci,39(3):417-425. DOI:10.13878/j. cnki. dqkxxb.20130510001

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2013-05-10
  • 最后修改日期:2015-06-11
  • 录用日期:
  • 在线发布日期: 2016-05-27
  • 出版日期:

地址:江苏南京宁六路219号南京信息工程大学    邮编:210044

联系电话:025-58731158    E-mail:xbbjb@nuist.edu.cn    QQ交流群号:344646895

大气科学学报 ® 2024 版权所有  技术支持:北京勤云科技发展有限公司