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131.
Modulation of Twin Tropical Cyclogenesis by the MJO Westerly Wind Burst during the Onset Period of 1997/98 ENSO 总被引:1,自引:0,他引:1
The modulation of twin tropical cyclogenesis in the Indian-western Pacific Oceans by the Madden-Julian Oscillation (MJO) during the onset period of 1997/98 ENSO is explored for the period of September 1996 to June 1997 based on daily OLR, NCEP/NCAR wind vector, and JTWC best track datasets. The MJO westerly wind burst associated with its eastward propagation can result in a series of tropical cyclogeneses in a multi-day interval. Only in the transition seasons are pairs of tropical cyclones observed in both the tropical sectors of the Indian-western Pacific Oceans. Two remarkable twin tropical cyclogeneses probably modulated by the MJO westerly wind burst are found: one is observed in the Indian Ocean in the middle of October 1996, and the other is observed in the Western Pacific Ocean in late May 1997. The twin tropical cyclogenesis in mid-October 1996 is observed when the super cloud cluster separates into two isolated clusters by the enhanced westerly wind, which is accompanied by two independent vortices in the equatorial tropical sectors. The other one, in late-May 1997, however, is characterized by one cyclonic flow that later results in another cyclonic cell in its opposite equatorial sector. Thus, there are two very important conditions for twin cyclogenesis: one is the MJO westerly wind straddling the equator, and the other is the integral super cloud cluster, which later splits into two cloud convective clusters with independent vortices. 相似文献
132.
本文引入湿静力温度物理量和运用能量天气学方法,对9405号热带风暴登陆前后我省中部和南部出现的一次暴雨过程进行综合分析,了解夏季暴雨落区和单站暴雨产生的能量特征,提出一些具有参考价值的结论。1湿较大温度含义1.1湿份力温度单位质量空气的湿静力能量是湿热能、位能、潜热能之和巴一C。T+gZ+LqE.称为湿静力能量。为了能用观测资料直接简便地计算能量,引入与能量相当的温度——湿静力温度T.一E。/C。。T+gZ/C。-+L。/C。由于T。综合表示了压、温、湿各要素,故分析其局地演变对于掌握气团属性的演变和本地天气的关… 相似文献
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“0112”海南岛大暴雨的分析和暴雨落区预报的讨论 总被引:1,自引:0,他引:1
2001年12月,受到热带风暴外围环流和冷空气的共同影响,在南海北部生成一支低空东风急流,同时,在海南岛东南部生成一个θse高值区,低空东风急流轴与θse高值区有很好的对应关系,使得在θse平流高值区内发生了一次强降水过程。 相似文献
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138.
Diagnosis of the Secondary Circulation of Tropical Storm Bilis
(2006) and the Effects of Convective Systems on Its Track 下载免费PDF全文
We diagnose characteristics of the quasi-balanced flow and secondary circulation(SC) of tropical storm Bilis(2006) using the potential vorticity(PV)-ω inversion method.We further analyze how secondary steering flows associated with mesoscale convective systems affected the track of tropical storm Bilis after it made landfall.The quasi-balanced asymmetric and axisymmetric circulation structures of tropical storm Bilis are represented well by the PV-w inversion.The magnitude of the nonlinear quasi-balanced vertical velocity is approximately 75%of the magnitude simulated using the Weather Research and Forecasting(WRF) model.The SC of Bilis(2006) contained two strong regions of ascending motion,both of which were located in the southwest quadrant of the storm.The first(150-200 km southwest of the storm center) corresponded to the eyewall region,while the second(approximately 400 km southwest of the storm center) corresponded to latent heat release associated with strong precipitation in major spiral rainbands.The SC was very weak in the northeast quadrant(the upshear direction).Dynamical processes related to the environmental vertical wind shear produced an SC that partially offset the destructive effects of the environmental vertical wind shear(by 20%-25%).This SC consisted of upward motion in the southwest quadrant and subsidence in the northeast quadrant,with airflow oriented from southwest to northeast at high altitudes and from northeast to southwest at lower levels.The inverted secondary zonal and meridional steering flows associated with continuous asymmetric mesoscale convective systems were about-2.14 and-0.7 m s~(-1),respectively.These steering flows contributed substantially to the zonal(66.15%) and meridional(33.98%) motion of the storm at 0000 UTC15 July 2006.The secondary steering flow had a significant influence on changing the track of Bilis from southward to northward.The direction of the large-scale meridional steering flow(3.02 m s~(-1)) was 相似文献
139.
12月,全国平均气温为-3.2℃,比常年同期(-3.9℃)偏高0.7℃;全国平均降水量为7.6mm,较常年同期(10.0mm)偏少。月内,我国中东部地区多发生大雾天气;青海部分地区发生雪灾,广西遭受冻害;热带风暴尤特袭击西沙群岛;华北干旱缓和,云南干旱持续。 相似文献
140.