贡献率 | 特征向量 | |||||||
1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | |
方差贡献率/% | 57.2 | 9.2 | 5.4 | 3.2 | 2.5 | 1.6 | 1.4 | 1.1 |
累计方差贡献率/% | 57.2 | 66.4 | 71.8 | 75.0 | 77.5 | 79.1 | 80.5 | 81.6 |
Citation: | Gao Shuanzhu, Zhang Shengjun, Lü Xinyan, et al. Circulation characteristics and thermal and dynamic conditions 48 hours before typhoon formation in South China Sea. J Appl Meteor Sci, 2021, 32(3): 272-288. DOI: 10.11898/1001-7313.20210302. |
Fig. 2 The infrared cloud image of geostationary satellite GMS at 0800 BT 23 Sep 2002 for Typhoon Mekkhala(a) and the infrared cloud image of geostationary satellite GOE at 0200 BT 9 Jun 2004 for Typhoon Chanthu(b) in the South China Sea 48 hours before typhoon formation
( denotes the center of tropical disturbance, the circle with diameter 1.5 degree denotes the area of vast deep convection closest to the disturbance center)
Fig. 4 The sea surface temperature(the contour, unit:℃, the red one is 26.5℃) and the convective potential energy(the shaded) 48 hours before typhoon formation for Typhoon Haima in 2011(a) and Typhoon Haitang in 2011(b) in the South China Sea
(the solid circle and red connector denotes the disturbance track inner 48 hours prior to typhoon formation, the black solid circle denotes the position of disturbance center at 48 hours before typhoon formation, the typhoon symbol is the location for typhoon formation)
Fig. 5 The box diagram for the time evolution of the sea surface temperature(a) and convective potential energy(b) of the disturbance center inner 48 hours prior to typhoon formation with the box diagram for the water vapor content of the disturbance center from sea-level surface to 300 hPa along the track of the disturbance 48 hours before typhoon formation(c) and at the time of typhoon formation(d)
Fig. 6 The atmospheric precipitable water(the shaded) and relative humidity at 600 hPa(the contour, unit:%) 48 hours before typhoon formation(a) and the time of typhoon formation(b) for Typhoon Haima in 2011(the others same as in Fig. 4)
Fig. 7 The streamline at 850 hPa(the black) and 200 hPa(the green) 48 hours before typhoon formation for Typhoon Haima in 2011(a), the streamline of the wind vertical shear and the wind shear amplitude(the shaded) between 200 hPa and 850 hPa 48 hours before typhoon formation for Typhoon Haima in 2011(b), the streamline of the wind vertical shear(black line) and the wind shear amplitude(the shaded) between 200 hPa and 850 hPa 48 hours before typhoon formation for Typhoon Herbert in 1980(c)
(the others same as in Fig. 4)
Fig. 10 The box diagram for the time evolution of OW index of the disturbance center at 850 hPa(a) and 500 hPa(b) inner 48 hours prior to typhoon formation with the change of OW index of the disturbance center along the track of the disturbance 48 hours before typhoon formation at 850 hPa(c) and 500 hPa(d)
Table 1 The variance contribution and the cumulative variance contribution of the first 8 eigenvectors of combined EOF analysis of u and v at 850 hPa and 200 hPa 48 hours before typhoon formation in the South China Sea
贡献率 | 特征向量 | |||||||
1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | |
方差贡献率/% | 57.2 | 9.2 | 5.4 | 3.2 | 2.5 | 1.6 | 1.4 | 1.1 |
累计方差贡献率/% | 57.2 | 66.4 | 71.8 | 75.0 | 77.5 | 79.1 | 80.5 | 81.6 |
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