FURTHER RESEARCH ON MECHANISM OF TBO IN SOUTH ASIAN MONSOON REGION
The results of this study prove that there is significant troposphere biennial oscillation (TBO) in the South Asian climate, especially with the Indian summer monsoon rainfall. In order to explore the mechanism of TBO in the South Asian region, we defined a unified South Asian monsoon index to depic...
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Published in | Journal of Tropical Meteorology Vol. 20; no. 3; pp. 202 - 207 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Guangzhou
Guangzhou Institute of Tropical & Marine Meteorology
01.09.2014
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Subjects | |
Online Access | Get full text |
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Abstract | The results of this study prove that there is significant troposphere biennial oscillation (TBO) in the South Asian climate, especially with the Indian summer monsoon rainfall. In order to explore the mechanism of TBO in the South Asian region, we defined a unified South Asian monsoon index to depict South Asian summer monsoon (SASM) and South Asian winter monsoon (SAWM) and the transition features between SASM and SAWM. Through further analysis, the connection between the abnormity of SASM and SAWM was discovered. Normally, a strong SAWM is beneficial for a weak SASM later, while a weak SAWM favors a strong SASM. Meanwhile, a strong SASM is favorable for a weak SAWM and a weak SAWM always happens after a weak SASM. Such results suggest the evolution of the South Asian monsoon, which may be an important mechanism to excite TBO in South Asia. |
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AbstractList | The results of this study prove that there is significant troposphere biennial oscillation (TBO) in the South Asian climate, especially with the Indian summer monsoon rainfall. In order to explore the mechanism of TBO in the South Asian region, we defined a unified South Asian monsoon index to depict South Asian summer monsoon (SASM) and South Asian winter monsoon (SAWM) and the transition features between SASM and SAWM. Through further analysis, the connection between the abnormity of SASM and SAWM was discovered. Normally, a strong SAWM is beneficial for a weak SASM later, while a weak SAWM favors a strong SASM. Meanwhile, a strong SASM is favorable for a weak SAWM and a weak SAWM always happens after a weak SASM. Such results suggest the evolution of the South Asian monsoon, which may be an important mechanism to excite TBO in South Asia. The results of this study prove that, there is significant troposphere biennial oscillation (TBO) in the South Asian climate, especially with the Indian summer monsoon rainfall. In order to explore the mechanism of TBO in the South Asian region, the authors have defined a unified South Asian monsoon index to depict South Asian summer monsoon (SASM) and South Asian winter monsoon (SAWM) and the transition features between SASM and SAWM. Through further analysis, the connection between the abnormity of SASM and SAWM was discovered. Normally, a strong SAWM is beneficial for a weak SASM later, while a weak SAWM favors a strong SASM. Meanwhile, a strong SASM is favorable for a weak SAWM and a weak SAWM always happens after a weak SASM. Such results suggest the evolution of the South Asian monsoon, which may be an important mechanism to excite TBO in South Asia. |
Author | 李崇银 李琳 阙志萍 |
AuthorAffiliation | Institute of Meteorology and Oceanography, PLA University of Science and Technology, Nanjing211101 China Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 China Beijing Institute of Applied Meteorology, Beijing 100029 China Graduate University of the Chinese Academy of Sciences, Beijing 100049 China |
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Notes | South Asia; troposphere biennial oscillation (TBO); monsoon The results of this study prove that there is significant troposphere biennial oscillation (TBO) in the South Asian climate, especially with the Indian summer monsoon rainfall. In order to explore the mechanism of TBO in the South Asian region, we defined a unified South Asian monsoon index to depict South Asian summer monsoon (SASM) and South Asian winter monsoon (SAWM) and the transition features between SASM and SAWM. Through further analysis, the connection between the abnormity of SASM and SAWM was discovered. Normally, a strong SAWM is beneficial for a weak SASM later, while a weak SAWM favors a strong SASM. Meanwhile, a strong SASM is favorable for a weak SAWM and a weak SAWM always happens after a weak SASM. Such results suggest the evolution of the South Asian monsoon, which may be an important mechanism to excite TBO in South Asia. 44-1409/P 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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Snippet | The results of this study prove that there is significant troposphere biennial oscillation (TBO) in the South Asian climate, especially with the Indian summer... The results of this study prove that, there is significant troposphere biennial oscillation (TBO) in the South Asian climate, especially with the Indian summer... |
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SubjectTerms | Precipitation TBO Time series Wind 南亚地区 南亚季风 季风区 季风指数 季风降水 机制 过渡特征 |
Title | FURTHER RESEARCH ON MECHANISM OF TBO IN SOUTH ASIAN MONSOON REGION |
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