On-Land Detecting a Motionally Induced Electric Field: Test Measurements in Northern Finland.

N. Palshin, P. Kaikkonen, L. Vanyan, J. Tiikkainen, V. H. Rukol
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引用次数: 4

Abstract

Test measurements of the electric voltage in Kilpisjarvi, northern Finland during September 9-October 12, 1995 were made with the aim of studying the possibility of detecting a motionally induced electric field by means of a horizontal electric dipole 3800 meters in length located at a distance of about 50 km from the nearest fjord of the Norwegian Sea. In addition to the electric voltage we measured at Kilpisjarvi, the water level, magnetic field and meteorological data from Tromso, Norway, the meteorological data from Kilpisjarvi and the magnetic field data from Sodankyla, Finland were used in analysis. Raw data were preprocessed to eliminate non-stationarities (remove outliers) and to remove solar daily variations, and were then smoothed. No significant influence of the local temperature, humidity and rainfall on the smoothed voltages was found. Probably due to a source effect the voltage was not coherent with the magnetic field from Tromso and Sodankyla. The long-period anomaly with the period of about 16 days was observed in the smoothed voltage, water level and air pressure. More data are necessary to derive a definite conclusion about the nature of the observed phenomenon, which is probably associated with direct atmospheric forcing on the coastal zone of the Norwegian Sea.
陆上感应电场探测:芬兰北部的测试测量。
1995年9月9日至10月12日,在芬兰北部基尔皮斯jarvi进行了电压测试测量,目的是研究利用距离挪威海最近的峡湾约50公里的3800米长的水平电偶极子探测动感应电场的可能性。除了我们在基尔皮斯jarvi测量的电压外,还使用了挪威特罗姆瑟的水位、磁场和气象数据,基尔皮斯jarvi的气象数据和芬兰索丹凯拉的磁场数据进行分析。对原始数据进行预处理,以消除非平稳性(去除异常值)和太阳日变化,然后进行平滑处理。局部温度、湿度和降雨量对平滑电压无显著影响。可能是由于源效应,电压与来自特罗姆瑟和索丹基拉的磁场不一致。平滑后的电压、水位和气压均存在周期约为16 d的长周期异常。要对观测到的现象的性质得出明确的结论,还需要更多的资料,这可能与挪威海沿岸地区的直接大气强迫有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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