MARAJóARCHIPÉLAGO气象干旱的遥感评价:CPC变形技术数据的空间解释

IF 0.1 Q4 GEOGRAPHY Boletin Goiano de Geografia Pub Date : 2019-12-31 DOI:10.5216/bgg.v39i0.55910
Jefferson Souto, Norma Ely Santos Beltrão, R. L. D. S. Oliveira
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引用次数: 2

摘要

亚马逊地区极易受到严重干旱的影响,这些干旱对水文、生物多样性和社会经济制度的动态产生了深远影响。在这项研究中,我们分析了CPC形态技术,该技术基于极端气候指标和标准化降水指数,用于诊断马拉戈群岛的干旱事件。重新分析的数据用于确定2004年至2016年的大气模式。对计算的空间序列的分析表明,干旱事件是Bol。戈亚。地理。2019年,诉39:555910 SOUTO,J.I.DE.O。;贝尔特罗。;奥利维拉。https://revistas.ufg.br/bgghttps://doi.org/10.5216/bgg.v39.55910B G G 2-25受到太平洋和北热带大西洋正异常的强烈影响,导致降雨量不足。与降水量相关的指数显示,年累积降雨量有所减少,可以分别观察到CWD和CDD的较小值和较高值。观察到SPI频率为中度(-1.0至-1.49)和重度(-1.49至-1.99)干旱,导致水文流量延迟。总之,CPC形态数据可用于短期气象干旱的可靠监测,因为较长时间尺度存在时间限制。
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AVALIAÇÃO DE SECAS METEOROLÓGICAS POR DETECÇÃO REMOTA NO ARQUIPÉLAGO DO MARAJÓ: UMA INTERPRETAÇÃO ESPACIAL DOS DADOS DA CPC MORPHING TECNIQUE
The Amazon region is highly susceptible to severe droughts that cause profound impacts on the dynamics of the hydrological, biodiversity and socioeconomic regimes. In this study, we analize CPC MORPHing tecnique was utilized to diagnose drought events in the Marajó Archipelago, based on indicators of climatic extremes and the Standardized Precipitation Index. Data from the Reanalysis was used to identify the atmospheric patterns between the years 2004 to 2016. The analysis of the calculated spatial series suggests that drought events are Bol.Goia. Geogr. 2019, v. 39: 55910 SOUTO, J. I. DE. O.; BELTRÃO, N. E. S.; OLIVEIRA, R. M. E. S. DE. https://revistas.ufg.br/bgg https://doi.org/10.5216/bgg.v39.55910 B G G 2-25 strongly influenced by the positive anomalies of the Pacific Ocean and North Tropical Atlantic, leading a deficit rainfall. Indices related to precipitation show a decrease in the annual rainfall accumulations, being possible to observe smaller and higher values in the CWD and CDD, respectively. SPI frequencies were observed with moderate (-1.0 to -1.49) and severe (-1.49 to -1.99) drought categories, causing a delay in hydrological flow. In summary, CPC MORPHing data can be used for reliable monitoring of short-term meteorological droughts, as there are temporal limitations for longer time scales.
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