Seismological Gradients in SalvusProject

# Variable used in the notebook to determine which site
# is used to run the simulations.
import os

SALVUS_FLOW_SITE_NAME = os.environ.get("SITE_NAME", "local")
PROJECT_DIR = "project"

import time
import pathlib

import matplotlib.pyplot as plt
import numpy as np
import obspy
import xarray as xr

from salvus import namespace as sn

SALVUS_FLOW_SITE_NAME = os.environ.get("SITE_NAME", "local")
PROJECT_DIR = "project"

# Define a spherical chunk domain.
lat_c, lon_c = -27.5, 135
lat_e, lon_e = 25.5, 42.0

# Uncomment the following line to start from scratch
# !rm -rf project
d = sn.domain.dim3.SphericalChunkDomain(
    lat_center=lat_c,
    lat_extent=lat_e,
    lon_center=lon_c,
    lon_extent=lon_e,
    radius_in_meter=6371e3,
)
p = sn.Project.from_domain(path=PROJECT_DIR, domain=d, load_if_exists=True)

# Add an event by parsing some prepared data.
e = sn.Event(
    sources=sn.simple_config.source.seismology.parse(
        "./event.txt", dimensions=3
    ),
    receivers=sn.simple_config.receiver.seismology.parse(
        obspy.read_inventory("stations.txt"),
        dimensions=3,
        fields=["displacement"],
    ),
)

p += e

lat = np.linspace(lat_c - lat_e / 2.0, lat_c + lat_e / 2.0, 50)
lon = np.linspace(lon_c - lon_e / 2.0, lon_c + lon_e / 2.0, 50)
depth = np.linspace(0, 1000.0, 40)

_, lon_grid, lat_grid = np.meshgrid(depth, lon, lat, indexing="ij")

# Distance from center in degree.
d = ((lon_grid - lon_c) ** 2 + (lat_grid - lat_c) ** 2) ** 0.5

# Apply Gaussian
sigma = 5.0
d = 1.0 / (sigma * np.sqrt(2 * np.pi)) * np.exp(-0.5 * (d / sigma) ** 2)

# Normalize to 10 % deviation
d /= d.max()
d *= 10.0

ds = xr.Dataset(
    data_vars={
        "vs": (["depth", "longitude", "latitude"], d),
        "vp": (["depth", "longitude", "latitude"], d),
    },
    coords={"depth": depth, "latitude": lat, "longitude": lon},
)

ds.vs.attrs["units"] = "%"
ds.vp.attrs["units"] = "%"

# Same for the coordinate axes.
ds.depth.attrs["units"] = "km"
ds.latitude.attrs["units"] = "degrees_north"
ds.longitude.attrs["units"] = "degrees_east"
ds.attrs["geospatial_lat_units"] = "degrees_north"
ds.attrs["geospatial_lon_units"] = "degrees_east"
ds.attrs["geospatial_vertical_units"] = "km"

ds.vs.isel(depth=0).T.plot()
plt.show()

ec = sn.EventConfiguration(
    wavelet=sn.simple_config.stf.GaussianRate(half_duration_in_seconds=100.0),
    waveform_simulation_configuration=sn.WaveformSimulationConfiguration(
        end_time_in_seconds=1800.0
    ),
)

mc = sn.ModelConfiguration(background_model="prem_iso_no_crust")

p += sn.SimulationConfiguration(
    tensor_order=1,
    name="initial_model",
    elements_per_wavelength=1.0,
    min_period_in_seconds=200,
    max_depth_in_meters=500e3,
    model_configuration=sn.ModelConfiguration(
        background_model="prem_iso_no_crust",
    ),
    event_configuration=ec,
)

p += sn.model.volume.seismology.GenericModel(name="vs_blob", data=ds)

p += sn.SimulationConfiguration(
    tensor_order=1,
    name="target_model",
    elements_per_wavelength=1.0,
    min_period_in_seconds=200,
    max_depth_in_meters=500e3,
    model_configuration=sn.ModelConfiguration(
        background_model="prem_iso_no_crust", volume_models=["vs_blob"]
    ),
    event_configuration=ec,
)

p.viz.nb.simulation_setup("target_model", events=p.events.list())

for simulation in ["initial_model", "target_model"]:
    p.simulations.launch(
        ranks_per_job=2,
        site_name=SALVUS_FLOW_SITE_NAME,
        events=p.events.list()[0],
        wall_time_in_seconds_per_job=3600,
        simulation_configuration=simulation,
    )

p.simulations.query(block=True, ping_interval_in_seconds=1.0)

def process(st, inv, receiver, sources):
    # This particular function adds some random noise to
    # the data. To make it reproducible let's create some
    # deterministic seed - the seed is based on the receiver
    # number and the point-to-point amplitude of the first
    # trace.
    np.random.seed(
        int.from_bytes((receiver.name + str(st[0].data.ptp())).encode(), "big")
        % 2 ** 32
    )
    # Add 5% of normal distributed noise.
    for tr in st:
        tr.data += np.random.normal(
            scale=0.05 * tr.data.ptp(), size=tr.data.shape
        )

    # Filter it again to not have really high-frequencies.
    st.filter("lowpass", freq=1.0 / 80.0, zerophase=True)

    return st


p += sn.processing.seismology.SeismologyProcessingConfiguration(
    name="target_model_with_noise",
    data_source_name="SYNTHETIC_DATA:target_model",
    processing_function=process,
)

# ### Pick Windows
#
# Real world applications usually need some form of data selection. In seismology this oftentimes takes the form of picking windows. Salvus offers some utilities to automatically select these.

if not p.entities.has(
    "data_selection_configuration", "initial_model_100_to_300s"
):
    p.actions.seismology.pick_windows(
        data_selection_configuration="initial_model_100_to_300s",
        observed_data_name="PROCESSED_DATA:target_model_with_noise",
        synthetic_data_name="initial_model",
        events=p.events.list(),
        receiver_field="displacement",
        window_taper_width_in_seconds=50.0,
        window_picking_function="built-in",
        window_picking_function_kwargs={
            "minimum_period_in_seconds": 100.0,
            "maximum_period_in_seconds": 300.0,
        },
    )

p.viz.nb.waveforms(
    data=[
        "SYNTHETIC_DATA:initial_model",
        "PROCESSED_DATA:target_model_with_noise",
    ],
    receiver_field="displacement",
    data_selection_configuration="initial_model_100_to_300s",
)