Sea state information is needed for many applications, ranging from safety at sea and on the
coast, for which real time data are essential, to planning and design needs for infrastructure …

Noise with periods 3 to 10 s, ubiquitous in seismic records, is expected to be mostly
generated by pairs of ocean wave trains of opposing propagation directions with half the …

SUMMARY Between 0.1 and 0.5 Hz, infrasound signals recorded in the atmosphere are
dominated by ocean-generated noise called microbaroms. Microbaroms propagate through …

Long‐term changes in ocean surface waves are relevant to society and climate research.
Significant wave height climatologies and trends over 1992–2017 are intercompared in four …

The Hawaii‐2 Observatory (H2O) is an excellent site for studying the source regions and
propagation of microseisms since it is located far from shorelines and shallow water. During …

Using NCEP–NCAR reanalysis and in situ data, evidence of important changes in the winter
(December–March) cyclone climatology of the North Pacific Ocean over the past 50 years is …

Comparison of the ambient noise data recorded at near‐coastal ocean bottom and inland
seismic stations at the Oregon coast with both offshore and nearshore buoy data shows that …

Sea waves constitute a natural phenomenon with a great impact on human activities, and
their monitoring is essential for meteorology, coastal safety, navigation, and renewable …

Broad-band urban seismic noise (USN) must be considered as a temporally and spatially
non-stationary random process. Due to the high variability of USN a single measure like the …

Ocean waves excite continuous globally observable seismic signals. We use data from 52
globally distributed seismographs to analyze the vertical component primary microseism …