台风威马逊(1409)强度与降水变化的相互作用

覃皓; 郑凤琴; 伍丽泉

doi:10.11898/1001-7313.20220408

台风威马逊(1409)强度与降水变化的相互作用

DOI: 10.11898/1001-7313.20220408

覃皓¹,
郑凤琴^2, ,,
伍丽泉^{2, 3}

1.
广西壮族自治区气象台，南宁 530022
2.
广西壮族自治区气候中心，南宁 530022
3.
广西壮族自治区气象灾害防御技术中心，南宁 530022

资助项目:

广西重点研发计划项目桂科AB20159013

广西气象科研计划项目桂气科2022QN08

广西科技计划项目桂科AB21075008

详细信息

通信作者:
郑凤琴，邮箱：zhengfengq@sohu.com

计量
- 摘要浏览量: 1663
- HTML全文浏览量: 94
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- 被引次数: 0
出版历程
- 收稿日期: 2022-02-23
- 修回日期: 2022-04-11
- 刊出日期: 2022-07-13

The Interaction Between Intensity and Rainfall of Typhoon Rammasun(1409)

Qin Hao¹,
Zheng Fengqin^{2
, ,},
Wu Liquan^{2, 3}

1.
Guangxi Meteorological Observatory, Nanning 530022
2.
Guangxi Climate Center, Nanning 530022
3.
Guangxi Meteorological Disaster Prevention Technology Center, Nanning 530022

摘要

摘要: 利用2014年7月10日00:00—19日18:00(世界时)热带降水测量(TRMM)卫星3B42降水估测数据以及ERA5再分析数据，结合傅里叶变换以及Liang-Kleeman信息流等方法，分析台风威马逊(1409)强度与降水变化的相互作用。结果表明：台风威马逊(1409)降水具有明显的非对称性，降水主要位于台风中心偏西一侧，在该区域台风强度与降水相互影响。相较于台风强度对降水的影响，由降水到台风强度的信息流减小接近1个量级，表明在两者的相互作用中，台风强度变化的影响占主导。在水汽条件上，台风强度的增强(减弱)导致台风中心西南侧水汽通量辐合(辐散)的增强，进而与该区域的降水建立联系。此外，台风威马逊(1409)移动过程中随着强度变化，南海以及西太平洋水汽通道均存在明显响应。在动力条件上，中低层垂直螺旋度强值中心主要位于台风中心西侧，台风强度的增强(减弱)，导致台风中心西侧的垂直螺旋度绝对值增大(减小)，一定程度促进(抑制)了该区域上升运动的发展，造成更多(更少)的水汽凝结致雨。
- 台风强度;
- 降水;
- 信息流;
- 相互作用;
- 非对称
Abstract: Based on the methods of Fourier decomposition, correlation analysis and Liang-Kleeman information flow, the interaction between intensity and rainfall of Typhoon Rammasun (1409) is studied using the best track data of Shanghai Typhoon Institute (STI) of China Meteorological Administration (CMA), Tropical Rainfall Measuring Mission (TRMM) satellite 3B42 rainfall estimation data of National Aeronautics and Space Administration (NASA) and ERA5 reanalysis data of European Centre for Medium-Range Weather Forecasts (ECMWF) with 0.25°×0.25° grids. The results show that the rainfall of Typhoon Rammasun (1409) has obvious characteristics of asymmetry, and it is mainly located in the west side of the typhoon center. The rainfall of Typhoon Rammasun (1409) increases significantly twice during the whole life cycle, which corresponds to the intensification period. The information flow analysis shows that the rainfall of Typhoon Rammasun (1409) is affected by the intensity of typhoon itself, whereas the rainfall can also feedback on the latter. Compared with the influence of typhoon intensity on rainfall, the information flow from rainfall to typhoon intensity decreases by nearly an order of magnitude, indicating that the typhoon intensity plays a dominant role in the interaction relationship. The possible mechanism by which the typhoon intensity affects rainfall are analyzed by diagnosing the water vapor and dynamic conditions respectively. In terms of water vapor conditions, the convergence area of vertical integral of moisture flux corresponds well to the rainfall. The intensification (reduction) of Typhoon Rammasun (1409) partly results in the enhanced convergence (divergence) of vertical integral of moisture flux in the southwest of the typhoon center, which brings more (less) rainfall in this region. In addition, the South China Sea and the Western Pacific water vapor transport channel have obvious response to the changes of Typhoon Rammasun (1409) intensity. In terms of dynamic conditions, the strong center of vertical helicity in the middle and lower layers is mainly located in the west side of the typhoon center, indicating the rainfall area. The intensification (reduction) of Typhoon Rammasun (1409) leads to the increase (decrease) of absolute vertical helicity on the west side of the typhoon center, thus promotes (inhibits) the development of upward movement to a certain extent, resulting in more (less) water vapor condensation and rainfall.
- typhoon intensity;
- rainfall;
- information flow;
- interaction;
- asymmetry

HTML全文

图 1 2014年7月10日00:00—19日18:00台风威马逊实况路径(实线) 及累积降水量(填色)

Fig. 1 The best track (the solid line) of Typhoon Rammasun and accumulated precipitation (the shaded) from 0000 UTC 10 Jul to 1800 UTC 19 Jul in 2014

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图 2 2014年7月11日00:00—19日18:00台风威马逊环状平均(a)和1波降水率(b)的径向-时间剖面

Fig. 2 Radius-time cross-sections of azimuthally averaged precipitation rate(a) and wavenumber 1 precipitation rate(b) from 0000 UTC 11 Jul to 1800 UTC 19 Jul in 2014

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图 3 台风中心附近降水率

(a)2014年7月14日12:00，(b)2014年7月15日12:00，(c)2014年7月18日18:00

Fig. 3 Rain rate near the typhoon center

(a)1200 UTC 14 Jul 2014,(b)1200 UTC 15 Jul 2014,(c)1800 UTC 18 Jul 2014

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图 4 台风强度到降水率(a)及降水率到台风强度(b)的信息流(填色)

(打点区域表示达到0.05显著性水平；等值线为降水率过程平均值，单位：mm·h^-1)

Fig. 4 Information flows (the shaded) from typhoon intensity to precipitation rate(a) and from precipitation rate to typhoon intensity(b)

(dotted areas denote passing the test of 0.05 level;the contour denotes the averaged rain rate, unit:mm·h^-1)

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图 5 台风中心附近平均整层水汽通量散度

(a)2014年7月14日06:00—12:00，(b)2014年7月15日06:00—12:00，(c)2014年7月18日12:00—18:00

Fig. 5 Averaged moisture flux divergence of vertical integral near the typhoon center

(a)from 0600 UTC to 1200 UTC on 14 Jul 2014,(b)from 0600 UTC to 1200 UTC on 15 Jul 2014, (c)from 1200 UTC to 1800 UTC on 18 Jul 2014

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图 6 台风强度到整层水汽通量散度(a)和潜热能(b)的信息流(填色)(打点区域表示达到0.05显著性水平，图 6a中等值线为整层水汽通量散度的过程平均值，单位：g·m^-2·s^-1；图 6b中等值线为整层潜热能的过程平均值，单位：J·m^-2)

Fig. 6 Information flows (the shaded) from typhoon intensity to moisture flux divergence of vertical integral(a) and from typhoon intensity to latent energy of vertical integral(b)(dotted areas denote passing the test of 0.05 level, the contour in Fig. 6a denotes the averaged moisture flux diveragence of vertical integral, unit:g·m^-2·s^-1; the contour in Fig. 6b denotes the averaged latent energy of vertical integral, unit:J·m^-2)

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图 7 2014年7月15日12:00(a)和7月18日12:00(b)整层水汽通量(矢量)、通量值(填色) 及台风强度到整层水汽通量值的信息流(打点区域表示达到0.05显著性水平) (c)

Fig. 7 Moisture flux of vertical integral (the arrow) and its value (the shaded) at 1200 UTC 15 Jul 2014(a) and 1200 UTC 18 Jul 2014(b) with information flow from typhoon intensity to precipitation rate (dotted areas denote passing the test of 0.05 level) (c)

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图 8 台风强度到700 hPa垂直螺旋度的信息流(填色)

(等值线为700 hPa垂直螺旋度的过程平均值，单位：10^-3 Pa·s^-2)

Fig. 8 Information flow from typhoon intensity to 700 hPa vertical helicity (the shaded)

(the contour denotes the averaged 700 hPa vertical helicity, unit:10^-3 Pa·s^-2)

下载: 全尺寸图片幻灯片

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台风威马逊(1409)强度与降水变化的相互作用

DOI: 10.11898/1001-7313.20220408

通信作者:
郑凤琴，邮箱：zhengfengq@sohu.com

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The Interaction Between Intensity and Rainfall of Typhoon Rammasun(1409)

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台风威马逊(1409)强度与降水变化的相互作用

DOI: 10.11898/1001-7313.20220408

通信作者: 郑凤琴，邮箱：zhengfengq@sohu.com

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The Interaction Between Intensity and Rainfall of Typhoon Rammasun(1409)

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出版历程

目录

通信作者:
郑凤琴，邮箱：zhengfengq@sohu.com