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A 28-year climatological analysis of size parameters for Northwestern Pacific tropical cyclones

机译:西北太平洋热带气旋大小参数的28年气候分析

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A 28-year best track dataset containing size parameters that include the radii of the 15.4 m s?1 winds (R15) and the 25.7 m s?1 winds (R26) of tropical cyclones (TCs) in the Northwestern Pacific, the NCEP/NCAR reanalysis dataset and the Extended Reconstructed Sea Surface Temperature (ERSST) dataset are employed in this study. The climatology of size parameters for the tropical cyclones in the Northwestern Pacific from 1977 to 2004 is investigated in terms of the spatial and temporal distributions. The results show that the major activity of TCs in the Northwestern Pacific is from July to October. A majority of TCs lie over the ocean west of 150°E, and a few TCs can intensify to the Saffir-Simpson (S-S) categories 4, 5. Both R15 and R26 tend to increase as the tropical cyclones intensify. The values of R15 and R26 are larger for intense TCs in the Northwestern Pacific than in the North Atlantic generally. Both R15 and R26 peak in October, and before and after October, R15 and R26 decrease, which is different from the case in the North Atlantic. The smaller R15s and R26s occur in a large range over the Northwestern Pacific, while the larger R15s and R26s mainly lie in the eastern ocean from Taiwan Island to the Philippine Islands where many tropical cyclones develop in intense systems. The tropical cyclones with size parameters of R15 or R26 on average take a longer time to intensify than to weaken, and the weak tropical cyclones have faster weakening rates than intensification rates. From 1977 to 2004, the annual mean values of R15 increase basically with year; during the 28-year period, the value of R15 increases by 52.7 km, but R26 does not change with year obviously.
机译:包含大小参数的28年最佳航迹数据集,其中包括热带气旋(TC)的15.4 ms?1 风的半径(R15)和25.7 ms?1 风的半径(R26)。在这项研究中,采用了西北太平洋,NCEP / NCAR再分析数据集和扩展的重建海面温度(ERSST)数据集。根据空间和时间分布,研究了西北太平洋从1977年到2004年的热带气旋大小参数的气候学。结果表明,西北太平洋地区TC的主要活动是从7月到10月。大部分TC位于150°E以西的海洋上,少数TC可以增强到Saffir-Simpson(S-S)4、5类。随着热带气旋的加剧,R15和R26都趋于增加。对于西北太平洋的强TC,R15和R26的值通常比北大西洋的大。 R15和R26均在10月达到峰值,而在10月前后,R15和R26下降,这与北大西洋的情况不同。较小的R15和R26分布在西北太平洋,分布范围较大,而较大的R15和R26主要位于从台湾岛到菲律宾群岛的东部海洋,那里有许多热带气旋在密集的系统中生长。强度参数平均为R15或R26的热带气旋的强化时间要比减弱的时间长,而弱热带气旋的减弱速度要比强度大。从1977年到2004年,R15的年均值基本上随年份增加;在28年的时间里,R15的值增加了52.7 km,但是R26并没有明显的随年变化。

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