Abstract. Broadband seismic data recorded 2.3 km from the active vent of Arenal Volcano, Costa Rica, provide new constraints on tremor source processes. Arenal's tremor contains as many as seven harmonics, whose frequencies vary temporally by up to 75 percent, from initial values of 1.9 Hz for the first peak immediately following explosive eruptions to 3.2-3.5 Hz several minutes later. We infer that gas bubble concentration is variable within the conduit and also changes as a function of time, thereby changing the acoustic velocity. We infer that the source is a shallow, 200-660 m-long, vertically oriented 1-D resonator with matched boundary conditions, radiating seismic energy from a dis-placement antinode. Polarization analyses show ...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
Broadband seismic data recorded 2.3 km from the active vent of Arenal Volcano, Costa Rica, provide n...
Broadband seismic data recorded 2.3 km from the active vent of Arenal Volcano, Costa Rica, provide n...
Broadband seismic data recorded 2.3 km from the active vent of Arenal Volcano, Costa Rica, provide n...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
Broadband seismic data recorded 2.3 km from the active vent of Arenal Volcano, Costa Rica, provide n...
Broadband seismic data recorded 2.3 km from the active vent of Arenal Volcano, Costa Rica, provide n...
Broadband seismic data recorded 2.3 km from the active vent of Arenal Volcano, Costa Rica, provide n...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceTypical records of volcanic tremor and explosion quakes at Arenal volcano are ...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...
International audienceWe use wavefield decomposition methods (time-domain crosscorrelationand freque...