Advanced Search
Article Contents

A Study on Frontal Motion over Orography


doi: 10.1007/BF02656981

  • In order to study the characteristic features of the frontal motion over mountains, a frontal model is designed in this paper. The analytical solution of the model with the assumption of semigeostrophic approximation and no fric-tion is obtained and compared with numerical solution without the assumption. It assumes that the front is a free sur-face between two fluid layers with different densities. It also assumes that the mountain and the front are indefinitely long. Therefore, the motion of such a front can be determined by the one-dimensional shallow water equation system. By making a series of experiments, we confirm the rule further that front can be retarded when climbing the mountain and accelerated when going down the mountains. We also found some interesting characteristics of frontal structure influenced by topography in addition.
  • [1] Xuwei BAO, Leiming MA, Jianyong LIU, Jie TANG, Jing XU, 2018: Formation and Development of a Mountain-induced Secondary Center inside Typhoon Morakot (2009), ADVANCES IN ATMOSPHERIC SCIENCES, 35, 1160-1176.  doi: 10.1007/s00376-018-7199-2
    [2] Wenshou TIAN, GUO Zhenhai, YU Rucong, 2004: Treatment of LBCs in 2D Simulation of Convection over Hills, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 573-586.  doi: 10.1007/BF02915725
    [3] Peng WEI, Xin XU, Ming XUE, Chenyue ZHANG, Yuan WANG, Kun ZHAO, Ang ZHOU, Shushi ZHANG, Kefeng ZHU, 2023: On the Key Dynamical Processes Supporting the 21.7 Zhengzhou Record-breaking Hourly Rainfall in China, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 337-349.  doi: 10.1007/s00376-022-2061-y
    [4] A. A. Bidokhti, T. Bani-Hashem, 2001: Structure of Thunderstorm Gust Fronts with Topographic Effects, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 1161-1174.  doi: 10.1007/s00376-001-0030-4
    [5] LIU Guimei, WANG Hui, SUN Song, HAN Boping, 2003: Numerical Study on the Velocity Structure around Tidal Fronts in the Yellow Sea, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 453-460.  doi: 10.1007/BF02690803
    [6] Gu Wei, Wu Rongsheng, 1992: The Theory Study of the Influence of the Topography on the Cold Frontal Motion, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 167-172.  doi: 10.1007/BF02657507
    [7] Mengru FENG, Yujing QIN, Chuhan LU, 2021: An Objective Identification Method for Wintertime Cold Fronts in Eurasia, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1695-1705.  doi: 10.1007/s00376-021-0315-8
    [8] Li Yang, Mu Mu, Wu Yonghui, 2000: A Study on the Nonlinear Stability of Fronts in the Ocean on a Sloping Continental Shelf, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 275-284.  doi: 10.1007/s00376-000-0009-6
    [9] XU Zhongfeng, QIAN Yongfu, FU Congbin, 2010: The Role of Land--sea Distribution and Orography in the Asian Monsoon. Part II: Orography, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 528-542.  doi: 10.1007/s00376-009-9045-z
    [10] Ni Yunqi, Bette L. Otto-Bliesner, David D. Houghton, 1987: THE SENSITIVITY OF THE NUMERICAL SIMULATION TO OROGRAPHY SPECIFICATION IN THE LOWRESOLUTION SPECTRAL MODEL-PART II: IMPACT OF THE SMOOTHED OROGRAPHY AND RIPPLES ON SIMULATIONS, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 145-155.  doi: 10.1007/BF02677061
    [11] Li Long, Zhu Baozhen, 1990: The Modified Envelope Orography and the Air Flow over and around Mountains, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 249-260.  doi: 10.1007/BF03179759
    [12] Ni Yunqi, Bette L. Otto-Bliesner, David D. Houghton, 1987: THE SENSITIVITY OF NUMERICAL SIMULATION TO OROGRAPHY SPECIFICATION IN THE LOW RESOLUTION SPECTRAL MODEL-PART I: THE EFFECTS OF OROGRAPHY ON THE ATMOSPHERIC GENERAL CIRCULATION, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 1-12.  doi: 10.1007/BF02663607
    [13] Guidi ZHOU, Xuhua CHENG, 2022: Impacts of Oceanic Fronts and Eddies in the Kuroshio-Oyashio Extension Region on the Atmospheric General Circulation and Storm Track, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 22-54.  doi: 10.1007/s00376-021-0408-4
    [14] REN Shihe, XIE Jiping, ZHU Jiang*, 2014: The Roles of Different Mechanisms Related to the Tide-induced Fronts in the Yellow Sea in Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 1079-1089.  doi: 10.1007/s00376-014-3236-y
    [15] Tian Yongxiang, Luo Zhexian, 1994: Vertical Structure of Beta Gyres and Its Effect on Tropical Cyclone Motion, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 43-50.  doi: 10.1007/BF02656992
    [16] Chen Lianshou, Luo Zhexian, 1995: Effect of the Interaction of Different Scale Vortices on the Structure and Motion of Typhoons, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 207-214.  doi: 10.1007/BF02656833
    [17] FENG Lei, ZHANG Yaocun, 2007: Impacts of the Thermal Effects of Sub-grid Orography on the Heavy Rainfall Events Along the Yangtze River Valley in 1991, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 881-892.  doi: 10.1007/s00376-007-0881-4
    [18] Wu Rongsheng, 1985: THE INFLUENCES OF OROGRAPHY UPON THE FLOW WITHIN EKMAN BOUNDARY LAYER UNDER THE APPROXIMATION OF GEOSTROPHIC MOMENTUM, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 1-7.  doi: 10.1007/BF03179731
    [19] XU Zhongfeng, QIAN Yongfu, FU Congbin, 2010: The Role of Land--sea Distribution and Orography in the Asian Monsoon. Part I: Land--sea Distribution, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 403-420.  doi: 10.1007/s00376-009-9005-7
    [20] Luo Zhexian, 1987: ABRUPT CHANGE OF FLOW PATTERN IN BAROCLINIC ATMOSPHERE FORCED BY JOINT EFFECTS OF DIABATIC HEATING AND OROGRAPHY, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 137-144.  doi: 10.1007/BF02677060

Get Citation+

Export:  

Share Article

Manuscript History

Manuscript received: 10 July 1995
Manuscript revised: 10 July 1995
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

A Study on Frontal Motion over Orography

  • 1. Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093

Abstract: In order to study the characteristic features of the frontal motion over mountains, a frontal model is designed in this paper. The analytical solution of the model with the assumption of semigeostrophic approximation and no fric-tion is obtained and compared with numerical solution without the assumption. It assumes that the front is a free sur-face between two fluid layers with different densities. It also assumes that the mountain and the front are indefinitely long. Therefore, the motion of such a front can be determined by the one-dimensional shallow water equation system. By making a series of experiments, we confirm the rule further that front can be retarded when climbing the mountain and accelerated when going down the mountains. We also found some interesting characteristics of frontal structure influenced by topography in addition.

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return