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应用WRF（v3.4）模式输出资料，揭示双台风条件下水汽的输送与收支特征及其对台风强度的影响.分析表明，菲特台风与副热带高压、中高纬地区槽脊、西面大陆高压及其东南面尾随台风丹娜丝存在周边系统相互作用，这种相互作用使得菲特台风背景风场改变，从而影响其水汽输送通道的调整.水汽输送特征分析表明，周边系统相互作用，特别是尾随丹娜丝台风作为水汽收集-输送站的作用，对菲特台风在近海强度的维持及后期偏北强降水有重要影响.水汽通量辐合带的分布和演变与台风强对流带的分布和演变具有一致性，即水汽的输送对台风内核区强对流带的强度和结构具有重要影响.水汽收支诊断分析表明，水汽输送对两类台风强度的变化具有重要影响，即总的水汽通量与台风强度随时间的变化均具有较好的一致性.东边界是台风的主要水汽输送来源，南、北边界次之，西边界为负贡献；各边界水汽输送主要分布在对流层底层，西边界的对流层中低层为负贡献.水汽的垂直输送对台风内部水汽的再分配起着重要作用，同时水汽垂直输送大值带的持续时间与台风研究区域内强对流大值带的持续时间一致，说明水汽的垂直输送对U型和V型台风区域的强对流也具有重要的影响.In this paper, we simulate a process of binary typhoon and the budget diagnoses of water vapor in this process to analyze the transportation characteristics of water vapor and their influences on the variation of typhoon intensity. The results show that the interactions between typhoon Fitow and surrounding systems, including subtropical high, mid-latitude trough, west of the continent high and Southeast trailing typhoon Danas, change the background wind fields of Fitow, and then adjust the transport channels of moisture. Those surrounding systems, especially the trailing typhoon Danas which can be called the collection-transfer station of water vapor, have important effects on the intensity maintenance and the northern strong precipitation in the offshore and landing period of Fitow. The distribution and evolution of water vapor flux convergence band are consistent with those of strong convection band, revealing that the water vapor transport has important influences on the structure and intensity of the inner-core convection band in typhoon. The budget results show that the time series of total water vapor flux and typhoon intensity change synchronously. And the eastern boundary is the main source of water vapor transport, and the southern and northern boundary are also important, while the western boundary makes a negative contribution. The inflow transport channel is mainly located at the bottom of the troposphere, while the outflow transport area of water vapor is located at middle- and low-level troposphere of western boundary. The vertical transportation of water vapor plays an important role in redistributing the internal moisture of typhoon. The duration of sever convection band in typhoon is accompanied by the strong vertical transport of water vapor, which indicates that the vertical transport of water vapor is important for developing the strong convection in U and V type typhoon.
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Keywords:
- double typhoon condition /
- water vapor transport and budget /
- meso-scale convective zone /
- typhoon intensity change
[1] Wang Y Q, Zhu Y T 1989 J. CAMS 21 232 (in Chinese) [王玉清, 朱永禔 1989 气象科学研究院院刊 21 232]
[2] Wang Y Q, Zhu Y T 1992 Chin. J. Atmos. Sci. 16 659 (in Chinese) [王玉清, 朱永禔 1992 大气科学 16 659]
[3] Wang Y Q, Zhu Y T 1992 Chin. J. Atmos. Sci. 16 573 (in Chinese) [王玉清, 朱永禔 1992 大气科学 16 573]
[4] Zeng Z H, Chen L S, Wang Y Q 2008 Mon. Wea. Rev. 136 3307
[5] Ying Y, Zhang Q H 2012 J. Meteor. Soc. Jpn. 90 755
[6] Wang Y Q 2002 J. Atmos. Sci. 59 1213
[7] Wang Y Q 2002 J. Atmos. Sci. 59 1239
[8] Zhang Q H, Chen S J, Kuo Y H 2005 Mon. Wea. Rev. 133 725
[9] Houze Jr R A, Chen S S, Smull B F 2007 Science 315 1235
[10] Qiu X, Tan Z M, Xiao Q N 2010 Mon. Wea. Rev. 138 2092
[11] Sun Y, Zhong Z, Lu W 2014 Mon. Wea. Rev. 142 240
[12] Sun Y, Zhong Z, Lu W 2015 J. Atmos. Sci. 72 1346
[13] Sun Y, Zhong Z, Dong H 2015 Mon. Wea. Rev. 143 3478
[14] Li Y, Chen L S, Xu X D 2005 Chin. J. Atmos. Sci. 29 93 (in Chinese) [李英, 陈联寿, 徐样德 2005 大气科学 29 93]
[15] Shou S W, Yao X P 1995 Chin. J. Atmos. Sci. 19 488 (in Chinese) [寿绍文, 姚秀萍 1995 大气科学 19 488]
[16] Hu C M, Duan Y H, Yu H 2005 J. Trop. Meteor. 21 378 (in Chinese) [胡春梅, 端义宏, 余焊 2005 热带气象学报 21 378]
[17] Ding Y H, Liu Y Z 2003 Acta Oceanol. Sin. 25 142 (in Chinese) [丁一汇, 刘月贞 2003 海洋学报 25 142]
[18] Fujiwhara S 1921 Quart. J. Roy. Meteor. Soc. 47 287
[19] Fujiwhara S 1923 Quart. J. Roy. Meteor. Soc. 49 287
[20] Fujiwhara S 1931 Quart. J. Roy. Meteor. Soc. 49 75
[21] Carr L E, Boothe M A, Elsberry R L 1997 Mon. Wea. Rev. 125 2094
[22] Carr L E, Elsberry R L 1998 Mon. Wea. Rev. 126 1734
[23] Xu H X, Xu X D, Chen B, Chen L S, Zhu F C 2013 Acta Meteor. Sin. 71 825 (in Chinese) [徐洪雄, 徐祥德, 陈斌, 陈联寿, 朱复成 2013 气象学报 71 825]
[24] Wu X, Fei J, Huang X, Zhang X, Cheng X, Ren J 2012 Adv. Atmos. Sci. 29 561
[25] Liang L, Wu Z W, Yan G H 1995 J. Trop. Meteor. 21 232 (in Chinese) [梁力, 吴志伟, 严光华 1995 热带气象学报 21 232]
[26] Ding Y H 1989 Diagnostic Analysis Method in Weather Dynamics (Beijing: Science Press) 第293页 (in Chinese) [丁一汇 1989 天气动力学中的诊断分析方法 (北京: 科学出版社) 第293页]
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[1] Wang Y Q, Zhu Y T 1989 J. CAMS 21 232 (in Chinese) [王玉清, 朱永禔 1989 气象科学研究院院刊 21 232]
[2] Wang Y Q, Zhu Y T 1992 Chin. J. Atmos. Sci. 16 659 (in Chinese) [王玉清, 朱永禔 1992 大气科学 16 659]
[3] Wang Y Q, Zhu Y T 1992 Chin. J. Atmos. Sci. 16 573 (in Chinese) [王玉清, 朱永禔 1992 大气科学 16 573]
[4] Zeng Z H, Chen L S, Wang Y Q 2008 Mon. Wea. Rev. 136 3307
[5] Ying Y, Zhang Q H 2012 J. Meteor. Soc. Jpn. 90 755
[6] Wang Y Q 2002 J. Atmos. Sci. 59 1213
[7] Wang Y Q 2002 J. Atmos. Sci. 59 1239
[8] Zhang Q H, Chen S J, Kuo Y H 2005 Mon. Wea. Rev. 133 725
[9] Houze Jr R A, Chen S S, Smull B F 2007 Science 315 1235
[10] Qiu X, Tan Z M, Xiao Q N 2010 Mon. Wea. Rev. 138 2092
[11] Sun Y, Zhong Z, Lu W 2014 Mon. Wea. Rev. 142 240
[12] Sun Y, Zhong Z, Lu W 2015 J. Atmos. Sci. 72 1346
[13] Sun Y, Zhong Z, Dong H 2015 Mon. Wea. Rev. 143 3478
[14] Li Y, Chen L S, Xu X D 2005 Chin. J. Atmos. Sci. 29 93 (in Chinese) [李英, 陈联寿, 徐样德 2005 大气科学 29 93]
[15] Shou S W, Yao X P 1995 Chin. J. Atmos. Sci. 19 488 (in Chinese) [寿绍文, 姚秀萍 1995 大气科学 19 488]
[16] Hu C M, Duan Y H, Yu H 2005 J. Trop. Meteor. 21 378 (in Chinese) [胡春梅, 端义宏, 余焊 2005 热带气象学报 21 378]
[17] Ding Y H, Liu Y Z 2003 Acta Oceanol. Sin. 25 142 (in Chinese) [丁一汇, 刘月贞 2003 海洋学报 25 142]
[18] Fujiwhara S 1921 Quart. J. Roy. Meteor. Soc. 47 287
[19] Fujiwhara S 1923 Quart. J. Roy. Meteor. Soc. 49 287
[20] Fujiwhara S 1931 Quart. J. Roy. Meteor. Soc. 49 75
[21] Carr L E, Boothe M A, Elsberry R L 1997 Mon. Wea. Rev. 125 2094
[22] Carr L E, Elsberry R L 1998 Mon. Wea. Rev. 126 1734
[23] Xu H X, Xu X D, Chen B, Chen L S, Zhu F C 2013 Acta Meteor. Sin. 71 825 (in Chinese) [徐洪雄, 徐祥德, 陈斌, 陈联寿, 朱复成 2013 气象学报 71 825]
[24] Wu X, Fei J, Huang X, Zhang X, Cheng X, Ren J 2012 Adv. Atmos. Sci. 29 561
[25] Liang L, Wu Z W, Yan G H 1995 J. Trop. Meteor. 21 232 (in Chinese) [梁力, 吴志伟, 严光华 1995 热带气象学报 21 232]
[26] Ding Y H 1989 Diagnostic Analysis Method in Weather Dynamics (Beijing: Science Press) 第293页 (in Chinese) [丁一汇 1989 天气动力学中的诊断分析方法 (北京: 科学出版社) 第293页]
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