Selective intensity estimates of the power radiated by a facade subject to random excitation also appear to be feasible.
The use of measured coherence functions in predicting the random errors of sound intensity estimates is discussed.
Thus, the energy intensity estimates reported here are similar to other estimates and appear to be valid.
Approximately 85% of intensity estimates have some form of associated uncertainty, ranging from almost 0 μT to approximately 33 μT, with a median of 3.7 μT (Figure 3).
These provide the basis for the sensitivity analyses for each field and the affect of boundary definition is assessed using exploratory methods (summary statistics) and spatial intensity estimates.
To assess the reasonableness of our baseline water intensity estimates, we compared these results with values published in the literature [20, 33].
The intensity was based on satellite intensity estimates.
Based on the development of rainbands, satellite intensity estimates indicated winds of.
Despite this, intensity estimates from the JMA note that Betty did not intensify any further.
Intensity estimates around that time indicated sustained wind speeds of 70 mph (110 km/h).
Satellite intensity estimates reached as high as 160 mph, or a Category 5 hurricane.
