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Rainfall and climate variability: long-term trends in the Metropolitan Area of S?o Paulo in the 20th century

机译:降雨和气候多变性:20世纪圣保罗大都市区的长期趋势

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摘要

We investigated spatial-temporal variability and long-term trends of rainfall over the Metropolitan Area of S?o Paulo (MASP). Due to a lack of continuous and consistent rainfall observations in the MASP, a database for the spatial analysis was created from a composite of 94 stations, with daily rainfall data for 1973-1997, plus data from the University of S?o Paulo's Institute of Geophysics and Astronomy (IAG/USP) station for 1933-2011, as the base of the long-term variability analysis. It is shown that the seasonal and interannual rainfall variability result from underlying local influences and remote large-scale atmospheric dynamics. These effects appear to be more complex during the austral spring and fall seasons, and seem to determine the duration of the rainy period over the MASP. The intraseasonal (30-60 d) oscillation of rainfall does not exhibit any long-term modulation; interannual rainfall variability for 1975-1990 appears modulated by the El Ni?o-Southern Oscillation (ENSO) scale (2-8 yr). Nonetheless, there exists statistical evidence that the rainfall climate over the MASP had an abrupt change at the end of the 1950s, but the global climatic change that occurred in the middle of the 1970s is not evident. The progressive increase in the frequency of rainy days and total daily rainfall throughout the period of analysis are prominent factors in the trend of annual and seasonal rainfall. Furthermore, rainfall variability over the MASP may be modulated by the Southern Annular Mode (SAM), Pacific Decadal Oscillation (PDO) and ENSO at seasonal scales, altering the normal progression of the seasonal rainfall cycle, while at interannual scales, each one of these patterns drives the rainfall variability, mainly when each pattern reaches its extreme value.
机译:我们调查了圣保罗大都会地区(MASP)的时空变化和降雨的长期趋势。由于MASP中缺乏连续和一致的降雨观测结果,因此建立了一个空间分析数据库,该数据库由94个观测站组成,其中包含1973-1997年的每日降雨数据以及圣保罗大学研究所的数据。 1933-2011年的地球物理和天文学(IAG / USP)站,作为长期变异性分析的基础。结果表明,季节和年际降雨的变化是由于潜在的局部影响和偏远的大规模大气动力学造成的。在南方的春季和秋季,这些影响似乎更为复杂,并且似乎决定了MASP上雨季的持续时间。降雨的季节内(30-60 d)振荡没有任何长期的调节; 1975-1990年的年际降雨量变化似乎受到厄尔尼诺-南方涛动(ENSO)尺度(2-8年)的调节。但是,有统计证据表明,MASP上的降雨气候在1950年代末发生了突然变化,但是在1970年代中期发生的全球气候变化并不明显。在整个分析期间,雨天频率和每日总降雨量的逐渐增加是年度和季节性降雨趋势的主要因素。此外,MASP上的降雨变化可能由南环型模式(SAM),太平洋年代际涛动(PDO)和ENSO在季节性尺度上进行调节,从而改变了季节性降雨周期的正常进程,而在年际尺度上,这些因素中的每一种模式驱动降雨变化,主要是当每种模式达到其极值时。

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