The mantle electromagnetic and tomography (MELT) experiment on the east Pac
ific rise near 17 degrees S was the first large teleseismic experiment on a
midocean ridge. During the six-month deployment, no compressional arrivals
were well recorded above 0.5 Hz. In comparison, the ICEMELT experiment in
Iceland recorded compressional arrivals at 1-2 Hz from about 2 earthquakes
per month. We compare noise spectra from the two experiments and show that
this difference in detection is at least in part a result of noise. Near 1
Hz, seismic noise in the oceans is produced locally by wind-generated waves
. At both experiment sites, 1-Hz noise levels are well correlated with loca
l sea-surface-wind speeds derived from satellite observations. For a given
wind speed, 1-Hz noise levels are about 10-20 dB lower in Iceland. At the M
ELT site, cross-correlations of wind speed with the logarithm of noise in a
narrow-frequency band yield correlation coefficients exceeding 0.7 at freq
uencies between 0.4 Hz and 2 Hz. Noise levels at 1 Hz increase with wind by
1.3-1.4 dB per m/sec for wind speeds less than 10 m/sec. For the ICEMELT e
xperiment, high correlation coefficients extend to markedly higher frequenc
ies for coastal stations, and there is a 10-dB drop in 1-Hz noise levels 10
0-km inland. Noise levels increase by about 0.8 dB per m/sec. The strong co
rrelation between wind speed and 1-Hz seismic noise provides justification
for using satellite wind speed data to search for locations on the global s
preading system where there is a better probability of recording high-frequ
ency arrivals. The calmest sites are found on the northern east Pacific ris
e, near the equator in all oceans, and near 34 degrees N and 22 degrees S o
n the mid-Atlantic ridge.