与厄瓜多尔通古拉瓦火山喷发过程相关的安巴托河流域降水模式的变化

I. García, A. Solera
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引用次数: 2

摘要

通古拉瓦火山位于安第斯山脉,是厄瓜多尔目前喷发最频繁的火山。1993年记录了火山爆发的初始过程,1999年8月,经过近80年的沉寂,火山开始了爆发期。本研究考察了火山喷发过程对水文流域短期降水变化模式的影响。他们的研究结果旨在为在当地和全球水平上了解天气及其变化的影响因素的研究作出贡献。它还旨在为有关人工火山试验和人工影响天气的辩论提供技术数据。分析表明,在火山喷发过程中,降雨量呈现再分配的过程,从12月的42.25%显著增加到9月的40.03%显著减少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variations in the Patterns of Precipitation in the Watershed of the Ambato River Associated with the Eruptive Process of the Tungurahua Volcano in Ecuador
The Tungurahua, located in the Cordillera de los Andes, is the volcano with the most eruptive activity in Ecuador nowadays. 1993 records the eruptive initial process and in August of 1999, after almost 80 years of rest, the volcano begins an explosive eruptive period. This research examines the effects of the eruptive process of the volcano in the patterns of change in precipitation in the short term in a hydrographic watershed. Their results are intended to contribute to the studies carried out to understand the weather and the factors influencing its variability at local and global level. It aims also to contribute with technical data in the debate about experimenting with artificial volcanoes to weather modification. The analysis demonstrates a process of redistribution of rainfall, with significant increases in rainfall from 42.25% on December, and significant decreases of 40.03% on September, during the presence of the eruptive process.
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