A possible origin of 26 s microseisms

Details A possible origin of 26 s microseisms A possible origin of 26 s microseisms

Publishing date

Oct 1990

URL

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990pepi...63..229b&link_type=abstract

Journals

Physics of the Earth and Planetary Interiors, Volume 63, Issue 3-4, p. 229-231.

Science

Physics

Additional info 2

1

Type

Scientific paper

Abstract

The observations by Oliver and Holcomb of 26-27 s microseisms are compared with a rare occurrence of 12-13 s secondary microseisms, implying a swell period of 26 s. Moreover, at the time of each 26 s world-wide microseismic storm, atmospheric lows are centred on the Falklands continental shelf and it is suggested that primary microseisms are set in these shallow oceanic parts.

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