巴西亚马逊地区的降雨分布:变异图函数在时间序列中的应用

Darwich, A.J., Aprile, F., Siqueira, G.W.
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引用次数: 0

摘要

亚马逊地区幅员辽阔,气候多样,有多个气候带,直接影响着相关的生态系统。本研究分析了 1991-2022 年间巴西亚马逊(北部地区)的年度(水文年)和季节(干旱和潮湿)气候模式。在数值数据中应用了不完全伽马分布模型、克里格法和克里格法插值检验、等值线法估算平均降水量和等值线法估算降水量。数据归一化技术和图像插值也有助于确定巴西北部地区的降水模式和趋势。使用了按最小方差进行分层分组的方法,并辅以频率直方图的构建和显著性检验。结果表明,降雨具有很强的季节性。最高降水率出现在西北轴,最低降水率出现在南赤道地区。活跃的大气系统在降雨量的年度和季节分布中发挥了重要作用。四个不同的气候带已经形成:南部、中部、西北部和东北部。根据 10%至 90%概率水平确定的降雨频率,结果表明南部和中部大部分地区降水量在 25%至 50%之间的天数呈上升趋势,北部地区降水量在 50%至 75%之间的天数呈上升趋势。普通克里金检验和球形半变量图模型显示出最佳的数据插值结果,对气候变量的行为和历史序列的时空不连续性有更好的响应。结果表明存在各向同性气候现象的趋势,特别是在风分布模型中。结果表明,它们有助于了解亚马逊地区的降雨分布情况。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Rainfall Distribution in the Brazilian Amazon: Application of the Variogram Function to Time Series
The Amazon area is vast and diversified, with several climatic zones that influence directly in the associated ecosystems. This research analyzed the annual (hydrological year) and seasonal (drought and wet) climatological patterns of the Brazilian Amazon (North Region) between 1991–2022. The incomplete Gamma distribution model, kriging and cokriging interpolation tests, estimates of mean precipitation by the isohyet method, and of precipitated volume by the contour method were applied to numerical data. Data normalization techniques and image interpolation also contributed to identify precipitation patterns and trends in the northern region of Brazil. The method of hierarchical grouping by minimum variance was used, aided by the construction of frequency histograms and tests of significance. The results indicated a strong seasonality of rainfall. The highest precipitation rates occurred in the N-NW axis and the lowest in the south equatorial zone. The active atmospheric systems played an important role in the distribution of rainfall, both annual and seasonal. Four distinct climatic zones were established: southern, central, northwestern and northeastern. Based on the frequency of rainfall determined at levels of 10 to 90% probability, the results suggested a trend in the number of days with precipitation between 25 and 50% in most of the southern and central zones and an increase in precipitation from 50 to 75 % in the northern region. The ordinary kriging test and the spherical semivariogram model showed the best results for data interpolation, with better responses to the behavior of climatic variables and solutions for the spatial-temporal discontinuity of historical series. The results indicated a tendency towards the presence of isotropic climatic phenomena, especially in the wind distribution model. The results showed that they could support the understanding of the distribution of rainfall in the Amazon region.
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