In:
Journal of Geophysical Research: Planets, American Geophysical Union (AGU), Vol. 126, No. 1 ( 2021-01)
Kurzfassung:
Seismic noise on Mars is polarized horizontally at low frequency (0.03–0.3 Hz) and vertically at high frequency (0.3–1 Hz) Polarization azimuth varies with local hour and season and follows the wind direction during the day Day polarization can partly be explained by pressure or acoustic emission and seismic wavefield may only be identified in the evening
Materialart:
Online-Ressource
ISSN:
2169-9097
,
2169-9100
DOI:
10.1029/2020JE006545
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2021
ZDB Id:
1086497-0
ZDB Id:
3094268-8
ZDB Id:
2016810-X
SSG:
16,13