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As the number of hops in HRP is mainly influenced by the depth of source and target nodes, the node will choose its parent based on the depth along with LQ in the proposed routing optimization algorithm.
The magma for such a volcano must originate at a depth where diamonds can be formed —150 km or more (three times or more the depth of source magma for most volcanoes).
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The reflector located at a depth of about 3 km corresponds to the horizontal location of the source B. The depth of this source was estimated to be 4 km and, therefore, there is a difference of 1 km between the depths of the source and the reflector.
The depth of the source was calculated using one of the following equations: Here, Z is the distance of the source from the P surface; JPP, JPN, JNN, and JNP, are the spatial integral intensities of the PP, PN, NN, and NP images, respectively.
They have different sensitivities to the depth of the source.
The width of the displacement area is a function of the depth of the source.
This characteristic implies that the depth of deformation source is quite shallow.
b Ray model outputs where the depth of the source (moving boat) was set to 0.5 m.
The depth of the source is estimated to be shallower than the magma chamber that produced most of the effusive material during the eruptions of Shinmoe-dake.
The earthquake hypocenter locations (Kato et al. 2015) are 1 2 km deeper than the depth of the source of the phreatic eruption estimated from other methods.
If the depth of the source was similar for the two events, the amount of inflation in the shallow region would not be very different.
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