OBSERVATIONAL AND THEORETICAL STUDIES OF THE MOIST BAROCLINIC ATMOSPHERE

Xie Yibing

doi:10.1007/BF02678127

Impact Factor: 5.8

Volume 1 Issue 2

Jul. 1984

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1984 > 1(2): 141-164

OBSERVATIONAL AND THEORETICAL STUDIES OF THE MOIST BAROCLINIC ATMOSPHERE

Xie Yibing

1.
DepartmentofGeophysics,PekingUniversity,Beijing

Xie Yibing

doi: 10.1007/BF02678127

Abstract
References
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Abstract:
In this paper, the main scientific conclusions of a national wide project of heavy summer rainstorms are presented. The active role of the moisture in the large scale motion of the atmosphere is stressed when the water vapour is saturated. The concept of moist baroclinity is introduced, and moist baroclinic processes are studied. Theoretical results, i. e., moist solenoid, moist available potential energy, moist jet, moist baroclinic instability, etc. are presented. Some observational and numerically experimental results are also shown.
References

[1]	Na LI, Lingkun RAN, Shouting GAO, 2016: The Impact of Deformation on Vortex Development in a Baroclinic Moist Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 233-246. doi: 10.1007/s00376-015-5082-y
[2]	Tan Benkui, Yin Dongping, 1995: Propagation of Envelope Solitons in Baroclinic Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 439-448. doi: 10.1007/BF02657004
[3]	BEI Naifang, Fuqing ZHANG, 2014: Mesoscale Predictability of Moist Baroclinic Waves: Variable and Scale-dependent Error Growth, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 995-1008. doi: 10.1007/s00376-014-3191-7
[4]	LIU Qinyu, WU Shu, YANG Jianling, HU Haibo, HU Ruijin, LI Lijuan, 2006: A Review of Ocean-Atmosphere Interaction Studies in China, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 982-991. doi: 10.1007/s00376-006-0982-5
[5]	Xu Yinlong, Qian Fenlan, Chen Zhi, Li Shiming, Zhou Mingyu, 2002: Observational Analyses of Baroclinic Boundary Layer Characteristics during One Frontal Winter Snowstorm, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 153-168. doi: 10.1007/s00376-002-0041-9
[6]	LU Daren, YI Fan, XU Jiyao, 2004: Advances in Studies of the Middle and Upper Atmosphere and Their Coupling with the Lower Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 361-368. doi: 10.1007/BF02915564
[7]	Yong-Sang CHOI, Chang-Hoi HO, Sang-Woo KIM, Richard S. LINDZEN, 2010: Observational Diagnosis of Cloud Phase in the Winter Antarctic Atmosphere for Parameterizations in Climate Models, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 1233-1245. doi: 10.1007/s00376-010-9175-3
[8]	Yang Guoxiang, Lu Hancheng, He Qiqiang, 1987: A MESO-α SCALE STUDY OF MEIYU FRONT HEAVY RAIN－PART I: OBSERVATIONAL STUDIES, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 264-277. doi: 10.1007/BF02915593
[9]	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
[10]	Gang LI, Daoyong YANG, Xiaohua JIANG, Jing PAN, Yanke TAN, 2017: Diagnosis of Moist Vorticity and Moist Divergence for a Heavy Precipitation Event in Southwestern China, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 88-100. doi: 10.1007/s00376-016-6124-9
[11]	T. S. Spassova, 1992: A Theoretical Test of the Geostrophic Momentum Approximation, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 251-255. doi: 10.1007/BF02657516
[12]	YUE Caijun, SHOU Shaowen, 2008: A Modified Moist Ageostrophic Q Vector, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 1053-1061. doi: 10.1007/s00376-008-1053-x
[13]	Zhang Xuehong, Zeng Qingcun, Bao Ning, 1986: NONLINEAR BAROCLINIC HAURWITZ WAVES, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 330-340. doi: 10.1007/BF02678653
[14]	YAO Xiuping, YU Yubin, SHOU Shaowen, 2004: Diagnostic Analyses and Application of the Moist Ageostrophic Vector Q, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 96-102. doi: 10.1007/BF02915683
[15]	Zuohao CAO, Da-Lin ZHANG, 2004: Tracking Surface Cyclones with Moist Potential Vorticity, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 830-835. doi: 10.1007/BF02916379
[16]	Liu Shida, Liu Shikuo, Xin Guojun, Liang Fuming, 1994: The Theoretical Model of Atmospheric Turbulence Spectrum in Surface Layer, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 408-414. doi: 10.1007/BF02658160
[17]	SUN Guodong, MU Mu, 2011: Response of a Grassland Ecosystem to Climate Change in a Theoretical Model, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1266-1278. doi: 10.1007/s00376-011-0169-6
[18]	Ding Yuguo, Jiang Zhihong, 1998: Theoretical Relationship between SSA and MESA with Both Application, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 541-552. doi: 10.1007/s00376-998-0031-7
[19]	Jai-Ho Oh, Won-Tae Kwon, Sang-Boom Ryoo, 1997: Review of the Researches on Changma and Future Observational Study (KORMEX), ADVANCES IN ATMOSPHERIC SCIENCES, 14, 207-222. doi: 10.1007/s00376-997-0020-2
[20]	HU Yongyun, ZHOU Chen, LIU Jiping, 2011: Observational Evidence for Poleward Expansion of the Hadley Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 33-44. doi: 10.1007/s00376-010-0032-1

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Manuscript History

Manuscript received: 10 July 1984

Manuscript revised: 10 July 1984

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

OBSERVATIONAL AND THEORETICAL STUDIES OF THE MOIST BAROCLINIC ATMOSPHERE

Xie Yibing

1. DepartmentofGeophysics,PekingUniversity,Beijing

Manuscript received: 1984-07-10
Manuscript revised: 1984-07-10

Abstract: In this paper, the main scientific conclusions of a national wide project of heavy summer rainstorms are presented. The active role of the moisture in the large scale motion of the atmosphere is stressed when the water vapour is saturated. The concept of moist baroclinity is introduced, and moist baroclinic processes are studied. Theoretical results, i. e., moist solenoid, moist available potential energy, moist jet, moist baroclinic instability, etc. are presented. Some observational and numerically experimental results are also shown.