A tsunami wave recorded near a glacier front Natural Hazards and Earth System Sciences DOI 10.5194/nhess-12-415-2012 27 February 2012 We observed a tsunami wave near the glacier front in the Temple Fjord (Spitsbergen). Two temperature and pressure recorders were deployed on a wire from the ice approximately 300 m from the glacier front. The measurements allowed us to estimate the wave number of these waves and the Young’s modulus of the ice. Read more
Revisiting “Narrow Bipolar Event” intracloud lightning using the FORTE satellite Annales Geophysicae DOI 10.5194/angeo-30-389-2012 24 February 2012 The lightning stroke called a “Narrow Bipolar Event”, or NBE, is an intracloud discharge responsible for significant charge redistribution. The NBE occurs within 10–20 μs, and some associated process emits irregular bursts of intense radio noise, fading at shorter timescales, sporadically during the charge transfer. Read more
Tomography of the 2011 Iwaki earthquake (M 7.0) and Fukushima nuclear power plant area Solid Earth DOI 10.5194/se-3-43-2012 14 February 2012 High-resolution tomographic images of the crust and upper mantle in and around the area of the 2011 Iwaki earthquake (M 7.0) and the Fukushima nuclear power plant are determined by inverting a large number of high-quality arrival times with both the finite-frequency and ray tomography methods. The similar structures under the Iwaki source area and the Fukushima nuclear power plant suggest that the security of the nuclear power plant site should be strengthened to withstand potential large earthquakes in the future. Read more
Magnetopause displacements: the possible role of dust Annales Geophysicae DOI 10.5194/angeo-29-2219-2011 1 December 2011 Large compressions of the magnetopause are proposed to occasionally result from temporary encounters of the magnetosphere with dust streams in interplanetary space. Such streams may have their origin in cometary dust tails or asteroids which cross the inner heliosphere or in meteoroids in Earth’s vicinity. Read more
