Historical earthquakes: a real ShakeMap over your places
The model lab's openquake-shakemap lane answers one question: what would the shaking of a real earthquake do to your places today? It takes the USGS ShakeMap of one of ten historical earthquakes, the map of how hard the ground shook, built from that earthquake's seismic recordings and felt reports, and runs it through the OpenQuake engine over your schedule. Every lab model is an open model, run as its authors published it on fixed inputs. Craton has not validated it. How to reach the lab is in the agent walk; what each figure means is in lab metrics.
On this page
The earthquakes
The lane runs a closed list. Each earthquake's ShakeMap is the one the USGS catalog (ComCat) marks preferred, pinned by its product address and its sha256, so a run always reads the same map. GET https://lab.oncraton.com/models lists them with the same fields.
event |
Earthquake | Date (local) | Magnitude | Region |
|---|---|---|---|---|
northridge-1994 |
Northridge | 1994-01-17 | 6.7 | San Fernando Valley, Los Angeles, California |
loma-prieta-1989 |
Loma Prieta | 1989-10-17 | 6.9 | Santa Cruz Mountains, San Francisco Bay Area, California |
nisqually-2001 |
Nisqually | 2001-02-28 | 6.8 | Puget Sound, Washington |
south-napa-2014 |
South Napa | 2014-08-24 | 6.0 | Napa Valley, California |
ridgecrest-2019 |
Ridgecrest | 2019-07-05 | 7.1 | Searles Valley near Ridgecrest, California |
anchorage-2018 |
Anchorage | 2018-11-30 | 7.1 | Anchorage, Alaska |
puerto-rico-2020 |
Puerto Rico | 2020-01-07 | 6.4 | Southwest Puerto Rico |
kaikoura-2016 |
Kaikoura | 2016-11-14 | 7.8 | Canterbury and Marlborough, New Zealand |
kahramanmaras-2023 |
Kahramanmaras | 2023-02-06 | 7.8 | Southern Turkey and northern Syria |
tohoku-2011 |
Tohoku | 2011-03-11 | 9.1 | Off the Pacific coast of Tohoku, Japan |
Ridgecrest is the M7.1 mainshock alone, without the M6.4 foreshock of the day before; Kahramanmaras is the M7.8 mainshock alone, without the M7.5 earthquake about nine hours later. Tohoku's figures are shaking damage only: its tsunami, which caused most of the deaths and much of the damage, is not modeled. Each of these results says so in a warning.
Run one
Send the spec to https://lab.oncraton.com/runs (or as arguments.spec on a run_climate_model call over MCP), with your key:
{
"model": "openquake-shakemap",
"event": "northridge-1994",
"vulnerability": "hazus_c1m_moderate_code",
"exposure": {"points": [
{"lat": 34.1511, "lon": -118.449, "value": 5000000},
{"lat": 34.0195, "lon": -118.4912, "value": 5000000}
]}
}event is required and must be one of the ids above; there is no rupture to describe and no USGS id to pass. vulnerability is optional and takes the same five curves as the earthquake scenario lane, with the same default: hazus_c1m_moderate_code, hazus_c1m_high_code and hazus_c1m_pre_code (HAZUS 5.1 mid-rise concrete frames), or the engine's Nepal demonstration curves demo_nonengineered_concrete and demo_wood. Up to 500 places, or exposure: {"object_id": ...} for a stored object's own schedule. The same spec is the same content-addressed run, replayed from the store.
What comes back
The result keeps the earthquake scenario lane's shape, so a reader of one reads the other. For the spec above (Sherman Oaks and Santa Monica, $5 million each, stored under version openquake-3.26.2-shakemap-r1):
total_mean_lossandmetrics.loss_mean: $3,490,880, the mean loss over 100 shaking patterns.metrics.loss_ratio: a mean of 34.9% of the value, 19.6% in the mildest tenth of patterns (p10) and 49.3% in the worst tenth (p90).metrics.per_point, for each place:loss_mean,loss_ratioand its spread across the patterns (loss_ratio_p10,loss_ratio_p50,loss_ratio_p90); the shaking as peak ground acceleration in g, both aspga_geometric_mean_g(the engine's own average) andpga_arithmetic_mean_g, which is higher; and the ShakeMap's own value at that place,pga_shakemap_gandmmi_shakemap(Modified Mercalli intensity), with the USGS words for it inshaking. Sherman Oaks: the ShakeMap reads 0.53 g, intensity 8.4, "severe"; the patterns average 0.52 g; the mean loss is $1,818,690 (36.4%), from 18.0% to 55.9% across the patterns.metrics.vulnerability_sensitivity: the same patterns through every curve. Here: 19.3% for high-code concrete, 34.9% moderate code, 66.3% pre-code.metrics.eventandresult.event: which earthquake, and the ShakeMap product, its addresses and digests.assumptionsandwarnings, as plain sentences.
There is no average annual loss and no return period: one earthquake has no frequency attached. metrics.basis is scenario, like the scenario lane; the run document's basis says "observed history".
Two more of the lab's own runs: Ridgecrest over one $10 million building in Ridgecrest, 0.38 g and intensity 7.2 on the ShakeMap, a mean loss of $2,325,370 (23.3%); Tohoku over one $10 million building in Sendai, 0.67 g and intensity 7.8, a mean loss of $4,295,960 (43.0%).
How the lab computes it
- The ShakeMap. Each ShakeMap is two grids from the USGS: the shaking at every node (
grid.xml) and its uncertainty (uncertainty.xml), which is smallest near the recording stations. The lab checks both files against their pinned sha256 before every run and reads them from disk; it never fetches a ShakeMap at run time. - 100 shaking patterns. The OpenQuake engine samples 100 ground-motion fields around the ShakeMap's values, spread by its uncertainty and correlated in space (Jayaram and Baker 2009), so neighbors shake alike. The sampling is seeded, single-process and truncated at three standard deviations. Local ground conditions are the ShakeMap's own.
- Loss. Each pattern's peak ground acceleration at each place goes through the chosen curve. The curves read only peak ground acceleration, so the ShakeMap's spectral accelerations are not used.
The lab's figures carry the engine's six significant digits.
Where it applies
Each ShakeMap covers a rectangle around its epicenter, from about 330 km across (South Napa) to about 1,600 km (Tohoku); /models gives each rectangle as grid. A place outside the chosen earthquake's rectangle is never sent to the engine and comes back modeled: false, counted in locations.unmodeled and named in an unmodeled_points warning. Kaikoura's rectangle crosses the 180th meridian, and the lab handles that. If no place is inside, the run still succeeds, every place is unmodeled, and there is no metrics block: nothing was measured, so there is no figure to show.
What it leaves out
Ground-up losses only, to buildings only. Shaking only: fire following, liquefaction, landslide and tsunami are not modeled. One curve for every place. No demand surge. The figures are what that day's shaking would do to the values you send, not what the earthquake cost when it happened. Every result lists these as assumptions.
Replaying a result
The ten earthquakes and the digests of their twenty ShakeMap files live in one pinned manifest, recorded with its own digest in every run id (the events input). The OpenQuake engine and the curves are the scenario lane's, pinned the same way. Repeat runs of the same spec give the same bytes, on either kind of machine the lab rents.