Not exact matches
An OBS was placed at the ocean floor at 400 - meter
water depth offshore Western Svalbard, and
recorded every sound from the seabed and ocean for a full year.
In this case, the researchers combined
records of ancient lake levels, location and extent of glaciation, variations in the composition of stalagmites in caves, and evidence for changes in vegetation and subsurface soil deposits associated with
water table
depth.
Despite their violence, very little is known about silicic eruptions and most knowledge about them comes from ancient rock
records, which lack details such as the timing, duration, source, and
water depth of the events.
Sequential pairs of images (2.5 ms apart in time) were
recorded and cross-correlated to study the flow physics in the illumination plane, which was parametrically varied along the
depth of the
water tunnel, see Figure 3.
Failure to identify contamination of the sedimentary
record by allochtonous foram tests, will lead to false
water depth estimations for the sediments that host the forams.
For such empirical forecasts regionally
depth - dependent damping rates \ (\ lambda (x, y, z) \) could be derived from the lag - 1 autocorrelation of long term observational
records of
water storage and soil moisture.
As a weather man with a great track
record... I would say Joe can see through the maze and tell us with great
depth of knowledge his opinions... and to me they hold
water!
For the
record, more than half (52 %) of ocean
waters lie below the 2000 meter
depth, so calling the 500 - 2,000 meter layer the «deep ocean» is still quite relative.