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Volume 7 Issue 3

Jul.  1990

Article Contents

The Modified Envelope Orography and the Air Flow over and around Mountains


doi: 10.1007/BF03179759

  • By use of the two-layer adiabatic globe spectral model and the zonally averaged climatic data of winter season as initial values, 10-day integrations are carried out based on three kinds of model topography (i.e., (1) the averaged to-pography; (2) the envelope topography; (3) the modified envelope topography). The results show that the orography of the Northern Hemisphere plays an important role in the simulation of large-scale weather patterns in winter sea-son. The simulation based on the envelope topography developed by Wallace et al. has some improvements in the Rocky Mountains area. But this scheme causes very serious horizontal expansion around the Tibetan Plateau (hereafter referred to as the TP). A modified envelope topography scheme has been worked out that increases the slope of the TP by decreasing; the horizontal expansion while keeping the maximum altitude. The results show some improve-ments of the scheme around the TP. By analysis of the mechanical effects of the large-scale orography on the currents, the different forcings of the air flow over and around the TP sad the Rocky Mountain (the RM) are investi-gated.
  • [1] Zhao Qiang, Fu Zuntao, Liu Shikuo, 2001: Equatorial Envelope Rossby Solitons in a Shear Flow, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 418-428.  doi: 10.1007/BF02919321
    [2] CHEN Wei, and LU Riyu, 2014: A Decadal Shift of Summer Surface Air Temperature over Northeast Asia around the Mid-1990s, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 735-742.  doi: 10.1007/s00376-013-3154-4
    [3] Yong-Hoon YOUN, 2005: The Climate Variabilities of Air Temperature Around the Korean Peninsula, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 575-584.  doi: 10.1007/BF02918489
    [4] Xiao Qingnong, Wu Rongsheng, 1995: A Study on Frontal Motion over Orography, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 325-334.  doi: 10.1007/BF02656981
    [5] 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
    [6] 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
    [7] CHENG Xueling, HU Fei, 2005: Numerical Studies on Flow Fields Around Buildings in an Urban Street Canyon and Cross-Road, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 290-299.  doi: 10.1007/BF02918518
    [8] Li Shuanglin, Ji Liren, Lin Wantao, 2001: On the Formation and Maintenance of the Persistent Anomalies of Summertime Circulation over the Ural Mountains, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 819-830.
    [9] Wu Rongsheng, 1991: The Surface Friction and the Flow over Mountain, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 272-278.  doi: 10.1007/BF02919609
    [10] Tan Benkui, Yin Dongping, 1995: Propagation of Envelope Solitons in Baroclinic Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 439-448.  doi: 10.1007/BF02657004
    [11] Li Shuanglin, Ji Liren, Lin Wantao, Ni Yunqi, 2001: The Maintenance of the Blocking over the Ural Mountains during the Second Meiyu Period in the Summer of 1998, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 87-105.  doi: 10.1007/s00376-001-0006-4
    [12] Qiwei WANG, Ming XUE, Zhemin TAN, 2016: Convective Initiation by Topographically Induced Convergence Forcing over the Dabie Mountains on 24 June 2010, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 1120-1136.  doi: 10.1007/s00376-016-6024-z
    [13] Zuohao CAO, Huaqing CAI, 2016: Identification of Forcing Mechanisms of Convective Initiation over Mountains through High-Resolution Numerical Simulations, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 1104-1105.  doi: 10.1007/s00376-016-6198-4
    [14] Peiling FU, Kefeng ZHU, Kun ZHAO, Bowen ZHOU, Ming XUE, 2019: Role of the Nocturnal Low-level Jet in the Formation of the Morning Precipitation Peak over the Dabie Mountains, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 15-28.  doi: 10.1007/s00376-018-8095-5
    [15] Ting LEI, Shuanglin LI, 2023: The Role of Underlying Boundary Forcing in Shaping the Recent Decadal Change of Persistent Anomalous Activity over the Ural Mountains, ADVANCES IN ATMOSPHERIC SCIENCES.  doi: 10.1007/s00376-023-2365-6
    [16] LIU Wenhuo, GOU Xiaohua, YANG Meixue, ZHANG Yong, FANG Keyan, YANG Tao, JIN Liya, 2009: Drought Reconstruction in the Qilian Mountains over the Last Two Centuries and Its Implications for Large-Scale Moisture Patterns, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 621-629.  doi: 10.1007/s00376-009-9028-0
    [17] HAN Zhe, LI Shuanglin, MU Mu, 2011: The Role of Warm North Atlantic SST in the Formation of Positive Height Anomalies over the Ural Mountains during January 2008, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 246-256.  doi: 10.1007/s00376-010-0069-1
    [18] Jinling PIAO, Wen CHEN, Ke WEI, Yong LIU, Hans-F. GRAF, Joong-Bae AHN, Alexander POGORELTSEV, 2017: An Abrupt Rainfall Decrease over the Asian Inland Plateau Region around 1999 and the Possible Underlying Mechanism, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 456-468.  doi: 10.1007/s00376-016-6136-5
    [19] Qin SU, Buwen DONG, Fangxing TIAN, Nicholas P. KLINGAMAN, 2024: Anthropogenic Influence on Decadal Changes in Concurrent Hot and Dry Events over China around the Mid-1990s, ADVANCES IN ATMOSPHERIC SCIENCES, 41, 233-246.  doi: 10.1007/s00376-023-2319-z
    [20] LIAO Hong, CHANG Wenyuan, YANG Yang, 2015: Climatic Effects of Air Pollutants over China: A Review, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 115-139.  doi: 10.1007/s00376-014-0013-x

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Manuscript History

Manuscript received: 10 July 1990
Manuscript revised: 10 July 1990
通讯作者: 陈斌, bchen63@163.com
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The Modified Envelope Orography and the Air Flow over and around Mountains

  • 1. Beijing Meteorological Centre, State Meteorological Administration, Beijing 100081,Institute of Atmospheric Physics, Academia Sinica, Beijing, 100080

Abstract: By use of the two-layer adiabatic globe spectral model and the zonally averaged climatic data of winter season as initial values, 10-day integrations are carried out based on three kinds of model topography (i.e., (1) the averaged to-pography; (2) the envelope topography; (3) the modified envelope topography). The results show that the orography of the Northern Hemisphere plays an important role in the simulation of large-scale weather patterns in winter sea-son. The simulation based on the envelope topography developed by Wallace et al. has some improvements in the Rocky Mountains area. But this scheme causes very serious horizontal expansion around the Tibetan Plateau (hereafter referred to as the TP). A modified envelope topography scheme has been worked out that increases the slope of the TP by decreasing; the horizontal expansion while keeping the maximum altitude. The results show some improve-ments of the scheme around the TP. By analysis of the mechanical effects of the large-scale orography on the currents, the different forcings of the air flow over and around the TP sad the Rocky Mountain (the RM) are investi-gated.

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