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Extreme climatic characteristics near the coastline of the southeast region of Brazil in the last 40 years

机译:在过去的40年里,巴西东南地区海岸线附近的极端气候特征

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The southeastern Brazilian coast is a vulnerable region to the development of severe storms, mainly caused by the passage of cold fronts and extratropical cyclones. In the last decades, there has been an increase in the occurrence of subtropical cyclones. This study investigates trends and climatic variations, analyzing surface meteoceanographic series at six grid points from the reanalysis databases of ERA-Interim and ERA5 (European Center for Medium-Range Weather Forecasts (ECMWF)) from 1979 to 2018 over the ocean region bounded, approximately, at 18 degrees S, 25 degrees S, and 37oW, 45oW (between the states of Espirito Santo, Rio de Janeiro, and Sao Paulo). Non-parametric statistical tests and the generalized extreme value distribution are employed for annual, seasonal, and daily maxima/minima. The numbers of occurrence of extreme values, as well as the extremal index, are also estimated in order to better understand the behavior of extremes. Annual maximum sea-surface temperature anomalies of the ERA-Interim databases show very low negative values, mainly at the beginning of measurements (between 1979 and 1982), leading to high positive trend values. The results are compared to the updated data from ERA5 which have anomalies that are more homogeneous with positive trends but without statistical significance. The other meteorological series of the ERA-Interim does not present discrepancies. Only the maximum anomalies of air temperature have significant annual and seasonal positive trends at grid points near the coast of Rio de Janeiro and Sao Paulo. Despite that the analyses for pressure and wind speed anomalies do not indicate significant trends, they present increases in the interdecadal pattern of the numbers of occurrence of extreme percentiles for almost every grid point. Return levels for 10, 25, 50, 75, and 100 years are estimated at each grid point, and many maximum/minimum peaks are close to the return levels for 100-year return periods. The extremal index suggests average cluster sizes associated with no predominance of clustering for the extreme percentiles, which represents weak dependence between the exceedances. These results characterize some independence between extreme meteorological events such as the event that has been taking place in the region. The occurrence of maximum daily wind speed peaks calculated in austral spring, whose values exceeded the previous ones, is identified at three grid points near the southeast Brazilian coast, caused by the passage of the subtropical cyclone "Deni," which occurred in November 2016.
机译:巴西东南部的海岸是一个脆弱的地区,发展严重风暴,主要是由冷锋和潜在旋风的通过引起的。在过去的几十年中,亚热带旋风器的发生是有所增加。本研究调查了趋势和气候变化,分析了来自Era-Interim和Era5的Reanaly分析数据库的六个网格点(欧洲中距离(ECMWF)的六个网格点(Ecmwwf)),从1979年到2018年在海洋地区,大约,在18度S,25度S和37OW,45OW(Espirito Santo,Rio de Janeiro和Sao Paulo之间)。非参数统计测试和广义极值分布用于年度,季节性和日常的最大值/最小值。还估计了极端值的发生次数以及极值指数,以便更好地理解极端的行为。年度最大海面温度异常的时代数据库显示出非常低的负值,主要是在测量开始时(在1979年至1982年之间),导致高正极趋势值。将结果与来自ERA5的更新数据进行比较,其具有更加均匀的积极趋势,但没有统计显着性。 ERA临时的其他气象系列并不存在差异。只有空气温度的最大异常,在里约热内卢和圣保罗海岸附近的网格点存在大幅度和季节性的积极趋势。尽管对压力和风速异常的分析并不表示重大趋势,但它们在几乎每个网格点出现极端百分位数的跨界模式的跨界模式的增加。在每个网格点估计10,25,50,75和100年的返回级别,并且许多最大/最小峰值接近返回级别为100年返回期。极值指数表明,与极端百分位数没有聚类的群集相关联的平均簇大小,这表示超标之间的弱依赖性。这些结果表征了极端气象事件之间的一些独立性,例如在该地区发生的事件。在南部春天计算的最大日常风速峰值的发生,其值超过以前的春天,由2016年11月发生的亚热带气旋“迪尼”的通过引起的三个网格点。

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