Hazard Comparisons with NSHM18

This report compares hazard between the NSHM23 and NSHM18 WUS ERFs, attempting to tease apart the contributions from the fault and gridded seismicity models to overall hazard changes.

All comparisons are done with a branch-averaged mean ERF model (as is used in the final NSHM), and a single ground motion model, ASK (2014), using uniform and default site conditions. All maps are for 1s SA, 10% in 50 year. The Cascadia subduction zone implementation is excluded in these comparisons.

Table Of Contents

Fault-Based Hazard Comparisons

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This section compares NSHM23 with NSHM18, but holding the gridded seismicity model constant in order to focus on fault-based changes (due both to ingredient and methodological changes) in areas where hazard is dominated by modeled faults.

NSHM23NSHM18 w/ NSHM23 Gridded
MapMap

Ratio

Difference

MapMap

Hazard Comparison Statistics:

Within 1%

Within 5%

Within 10%

% Range

Average % Change

14.49%56.36%80.43%[-37.43%, 459.48%]5.74%

Within 0.05g

Within 0.1g

Within 0.2g

Diff Range (g)

Average Diff (g)

98.50%99.62%99.95%[-0.11, 0.27]0.00

Fault and Deformation Model Moment Changes

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This section shows how fault-based deformation model moment changed between NSHM23 and NSHM18. We will use this map to mask hazard changes, highlighting only areas where changes are primarily due to methdological differences. In the ratio map, areas where moment exists in NSHM23 but not in NSHM18 are shown in yellow (i.e., a fault was added), and those with moment in NSHM18 but not in NSHM23 are shown in green (i.e., a fault was removed).

To smooth out minor geometry changes between the two models, moment is distributed around faults using a linear ramp in (3-D) up to 12 km; this is the same ramp used to carve out gridded seismicity near faults when constructing the NSHM23 gridded seismicity model.

RatioDifference
MapMap

Fault-Based Hazard Comparisons, Moment Chage Masked

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This section masks hazard changes, only showing them near faults where NSHM23 fault-moment is within a given factor of NSHM18 fault-moment. Hazard changes in areas that remain may still be largely due to moment changes, but this helps to narrow the search space for identification of areas where methodological changes may dominate hazard changes.

Various thresholds are used, starting with one that only includes areas with faults in both models, and then the threshold decreases to only show areas where moment is similar in the two models. Areas where the sign of the hazard change differs from the sign of moment change are shown regardless of the threshold value.

RatioDifference
MapMap
MapMap
MapMap
MapMap

Near-Fault Hazard Comparison Statistics:

Threshold

% Locs Within Moment Threshold

Within 1%

Within 5%

Within 10%

% Range

Average % Change

Areas w/ Moment in Both Models22.23%9.41%43.13%71.90%[-37.43%, 459.48%]4.03%
<100% Moment Change Threshold19.24%10.08%43.90%72.44%[-37.43%, 119.97%]1.62%
<50% Moment Change Threshold16.23%10.45%45.30%73.02%[-35.23%, 109.34%]2.03%
<20% Moment Change Threshold11.83%11.07%47.35%72.95%[-35.23%, 109.34%]3.30%
Threshold

% Locs Within Moment Threshold

Within 0.05g

Within 0.1g

Within 0.2g

Diff Range (g)

Average Diff (g)

Areas w/ Moment in Both Models22.23%93.75%98.37%99.76%[-0.11, 0.27]0.01
<100% Moment Change Threshold19.24%93.91%98.86%99.93%[-0.11, 0.25]0.00
<50% Moment Change Threshold16.23%93.76%98.74%99.91%[-0.11, 0.25]0.01
<20% Moment Change Threshold11.83%93.05%98.53%99.88%[-0.11, 0.25]0.01

NSHM18 Special Cases

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NSHM18 includes a number of special cases that are not carried forward. These also affect hazard comparisons beyond the moment changes shown above, and are plotted below.

Special Cases

NSHM18 Ingredient Runs vs NSHM18

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We also ran inversions using NSHM18 deformation models as input, but using updated methodologies. This helps to isolate regions where methodological changes (the inversion, as well as elmination of the special cases above) dominate hazard change. All comparisons hold the NSHM23 gridded seismicity model constant.

We ran this test both using updated scaling relationships, as well as using Wells and Coppersmith (94); for the latter, results are masked in California as UCERF3 used their own scaling relationships. We also show results using the classic segmentation branches only, which should be most similar to NSHM18 outside of California.

NSHM18 Ingredients, NSHM23 Methodology (new scaling)

MapMap

NSHM18 Ingredients, NSHM23 Methodology (W-C '94)

MapMap

NSHM18 Ingredients, NSHM23 Methodology (new scaling, classic only)

MapMap

NSHM18 Ingredients, NSHM23 Methodology (W-C '94, classic only

MapMap

Gridded Seismicity Model Hazard Changes

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These plots compare the gridded seismicity components of the models. For the ratio and difference maps, the contributions of NSHM23 fault sources are held constant (added to both models).

NSHM23, Gridded OnlyNSHM18, Gridded Only
MapMap

Ratio

Difference

MapMap

Hazard Comparison Statistics:

Within 1%

Within 5%

Within 10%

% Range

Average % Change

3.20%16.26%33.65%[-63.34%, 555.73%]11.26%

Within 0.05g

Within 0.1g

Within 0.2g

Diff Range (g)

Average Diff (g)

97.06%99.28%99.91%[-0.12, 0.39]0.01

Complete Model Hazard Changes

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These plots compare the full models, including both fault and gridded seismicity changes (both ingredients and methodology).

Full NSHM23Full NSHM18
MapMap

Full Ratio

Full Difference

MapMap

Fault-Only Ratio

Fault-Only Difference

MapMap

Gridded-Only Ratio

Gridded-Only Difference

MapMap

Hazard Comparison Statistics:

Within 1%

Within 5%

Within 10%

% Range

Average % Change

Full Models3.20%16.26%33.65%[-63.34%, 555.73%]11.26%
Faults Only14.49%56.36%80.43%[-37.43%, 459.48%]5.74%
Gridded Only3.20%16.26%33.65%[-63.34%, 555.73%]11.26%

Within 0.05g

Within 0.1g

Within 0.2g

Diff Range (g)

Average Diff (g)

Full Models97.06%99.28%99.91%[-0.12, 0.39]0.01
Faults Only98.50%99.62%99.95%[-0.11, 0.27]0.00
Gridded Only97.06%99.28%99.91%[-0.12, 0.39]0.01

Fault vs Gridded, Hazard Change Attribution

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This section shows hazard changes, colored by the primary contributor to hazard change (faults or gridded seismicity) rather than the sign of that change. Small changes are masked out.

Ratio AttributionDifference Attribution
MapMap
Attributed to FaultsAttributed to GriddedSum
Full Map18.41%81.59%100.00%
> 10% Change8.49%57.86%66.35%
> 0.05g Change1.64%1.30%2.94%

Full Model Rate and Moment Rate Comparisons

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Full Model Rate Comparisons

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NSHM23, M≥5

NSHM18, M≥5

MapMap

Ratio

Difference

MapMap

NSHM23, M≥6.5

NSHM18, M≥6.5

MapMap

Ratio

Difference

MapMap

NSHM23, M≥7.5

NSHM18, M≥7.5

MapMap

Ratio

Difference

MapMap

Full Model Moment Rate Comparison

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NSHM23

NSHM18

MapMap

Ratio

Difference

MapMap

Smoothed Moment Rate Hazard vs Model Hazard Change Comparisons

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Here, we calculate simple hazard maps by placing point sources at every grid location with a G-R b=1 MFD with magnitudes in the range [6,7.5] that satisfies each cell's moment rate. We then compare hazard changes from this simple model to the actual model hazard change. Areas where simplified model hazard change is similar to full model hazard change are likely dominated by ingredient (moment rate) changes, and those that differ may be affected by methodological changes (although this simplified comparison is not definitive).

Note that these comparisons use final model moment rate maps, as opposed to the prior moment comparisons that used deformation model moment rates directly. Thus, any slip rate misfits will be incorporated into these comparisons.

Simplified Full Model Moment Rate Hazard RatioFull Model Hazard Ratio
MapMap

Scatter Plot

Hazard Change Comparison

scatter plotmap plot
Simplified Fault Moment Rate Hazard RatioFault Hazard Ratio
MapMap

Scatter Plot

Hazard Change Comparison

scatter plotmap plot
Simplified Gridded Moment Rate Hazard RatioGridded Hazard Ratio
MapMap

Scatter Plot

Hazard Change Comparison

scatter plotmap plot

Smoothed M5 Rate Hazard vs Model Hazard Change Comparisons

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Here, we calculate simple hazard maps by placing point sources at every grid location with a G-R b=1 MFD with magnitudes in the range [5,7.5] that matches the total nucleation M5 rate in each cell. We then compare hazard changes from this simple model to the actual model hazard change. Areas where simplified model hazard change is similar to full model hazard change are likely dominated by ingredient (total rate) changes, and those that differ may be affected by methodological changes (although this simplified comparison is not definitive).

Simplified Full Model M5 Rate Hazard RatioFull Model Hazard Ratio
MapMap

Scatter Plot

Hazard Change Comparison

scatter plotmap plot
Simplified Gridded M5 Rate Hazard RatioGridded Hazard Ratio
MapMap

Scatter Plot

Hazard Change Comparison

scatter plotmap plot