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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Thunderstorm climatology of Brazil: ENSO and Tropical Atlantic connections
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Thunderstorm climatology of Brazil: ENSO and Tropical Atlantic connections

机译:巴西的雷暴气候:ENSO和热带大西洋的联系

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摘要

In this report monthly thunderstorm days (TD) in 14 large cities of Brazil from 1951 to 2010 are compared with data obtained in the first part of the 20th century in the same cities and correlated with sea surface temperature (SST) of the equatorial Pacific Ocean and Tropical Atlantic Ocean. On average over all cities, 77 TD are reported each year after 1951, against 43 TD in the first part of the 20th century, an increase of 79%. The increase seems to be related to increase in the urbanization in these cities, and not to global warming. A comparative analysis of TD for the whole country with El Nino-Southern Oscillation (ENSO) events suggests that the tendency for El Nino to increase the thunderstorm activity is evident in the South (only in the Spring/Summer), Southeast, Northeast and North (only in the Fall/Winter) regions. Regarding the Tropical Atlantic Ocean SST, a similar analysis using the Tropical South Atlantic (TSA) and Tropical North Atlantic (TNA) indices suggests that no significant differences exist between the thunderstorm activity for the two extreme positive and negative TSA conditions in the South and Southeast regions, while in the Northeast and North regions there is a significant increase in the thunderstorm activity during extreme positive TSA. Differently, only in the Northeast region there is a significant influence of TNA on thunderstorm activity. The influence is such that the thunderstorm activity is larger for the extreme negative TNA than for extreme positive TNA. All significant changes were quantified and significant variations were observed. For all parameters investigated (ENSO, TSA and TNA) the Northeast region showed the most significant changes.
机译:在此报告中,将1951年至2010年巴西14个大城市的月雷暴天数(TD)与20世纪上半叶在同一城市中获得的数据进行了比较,并与赤道太平洋的海表温度(SST)相关和热带大西洋。在所有城市中,1951年以后平均每年报告77 TD,而20世纪上半叶则为43 TD,增长了79%。增长似乎与这些城市中城市化的增长有关,与全球变暖无关。通过厄尔尼诺-南方涛动(ENSO)事件对整个国家的TD进行比较分析表明,厄尔尼诺现象增加了雷暴活动的趋势在南部(仅在春季/夏季),东南部,东北部和北部明显(仅在秋季/冬季)区域。关于热带大西洋海表温度,使用热带南大西洋(TSA)和热带北大西洋(TNA)指数进行的类似分析表明,对于南部和东南部两个极端正负TSA条件,雷暴活动之间没有显着差异。 TSA期间,在东北和北部地区,雷暴活动显着增加。不同的是,仅东北地区的TNA对雷暴活动有重大影响。这样的影响使得极端负TNA的雷暴活动大于极端正TNA的雷暴活动。量化所有显着变化并观察到显着变化。对于所调查的所有参数(ENSO,TSA和TNA),东北地区表现出最显着的变化。

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