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MJO Anomalies relationship with Volcanic Eruption in Indonesian Archipelago

机译:MJO异常与印度尼西亚群岛火山爆发的关系

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Madden-Julian Oscillation(MJO)is a large-scale atmospheric phenomenon that crosses the equator with a propagation area ranging from 15° North to 15° South,and moves from west to east,precisely from the Indian Ocean to the Pacific.MJO propagation is usually characterized by the rising of Sea Surface Temperature(SST)in Indian Ocean respectively.MJO anomaly is closely related to the variability of weather in the area it passes,including the Indonesian Archipelago.The impact of MJO anomaly in Indonesian Archipelago itself is suspected to cause not only excessive rainfall,but also a very long consecutive No Rain Days(NRD),with in the end can also trigger massive crop failures.In addition to SST,there are also external events that can affect the duration of the MJO,i.e.volcanic eruptions.Therefore,the study aims to determine the effect of volcanic eruption events on MJO anomalies,through the SST variable as an MJO anomaly parameter and also the occurrence of volcanic eruptions in the same time span.Data from both variables were taken over a period of 35 years,from 1982 to 2016.The SST data is a daily average data,obtained from ESRL NOAA,which is then filtered by the Bandpass Filter method to reinforce the oscillation of data.The MJO anomaly that seen from the SST fluctuations is then matched with time data and the duration of volcanic eruption events over the same time span.It found out that there are three MJO anomalies occurred during the time span of 35 years,and it is hypothesized that they were clearly in correspondence between the duration of volcanic eruption events with the incidence of MJO anomalies in Indonesian Archipellago.
机译:Madden-julian振荡(MJO)是一种大型大气现象,将赤道交叉,传播区域从北到15°南到15°的繁殖区域,从西到东部移动,精确地从印度洋到Pacific.mjo传播通常是在印度洋海面温度(SST)上升的特点.MJO异常与它通过的地区的天气变化密切相关,包括印度尼西亚群岛。MJO异常在印度尼西亚群岛本身的影响是怀疑不仅导致过度降雨量过多,而且连续长期没有下雨的日子(NRD),最终也可以触发大规模的作物失败。除了SST,还有外部事件可能会影响MJO的持续时间, ievolcanic爆发。因此,该研究旨在通过SST变量作为MJO异常参数来确定火山喷发事件对MJO异常的影响以及同一TI中的火山爆发的发生来自两个变量的ME SPANDATA在1982年至2016年的35年中拍摄了35年。SST数据是从ESRL NOAA获得的每日平均数据,然后通过带通滤波器方法过滤以增强数据的振荡从SST波动中看到的MJO异常与时间数据和波浪爆发事件的持续时间相匹配,在相同的时间范围内发现有三个MJO异常发生在35年的时间范围内,它是假设它们在印度尼西亚群岛MJO异常发生率之间的持续时间与印度尼西亚群岛发生率之间的对应关系。

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