Today I had a short discussion with my officemate Roy, who is a senior PhD student in my program. The topic we discussed was the method of deaggregation. To draw a smooth line connecting the six given points (from USGS data), spline method is preferred. But I had problem on producing a series of smooth lines for each magnitude. There are weird curvature of the curves when the PGA values are within a 0.01g to 0.1g. After the evaluation with Roy, I figured out I need to change my interpolation process to make sure the curve is reasonable. Here is the summary from our meeting. (I write it down here to help me remember.)
- Apply spline once and only once to the total seismic hazard curve.
- Estimate the probability of Mw for six return period, then construct the deaggregation points for each Mw.
- Assume the probability between every two points from original six points (USGS data) is linear relationship.
- Assume the lines are parallel with each other when the PGA is smaller or greater than the smallest or greatest one of the six points (USGS data) separately.
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