hfpytrace.model¶
Package
Model-level pure-Python ray tracing helpers.
Key Classes¶
Class AppletonHartreeDispersion
Class SenWyllerDispersion
Class RT1DProfile
Class RT1D
Class RT2DProfile
Class RT2D
Class RT2DConfig
Class RT3DProfile
Class RT3D
API¶
hfpytrace.model
¶
hfpytrace.model — ionospheric ray-tracing model classes.
This sub-package contains the core ray-tracing and dispersion models:
RT1D
1-D vertical-incidence tracer using a simple ODE integrator.
RT2D / RT2DProfile / RT2DConfig
2-D great-circle ray-tracing with a configurable ionospheric profile
(IRI, SAMI3, GEMINI, etc.).
RT3D / RT3DProfile
3-D oblique ray-tracing via PHaRLAP (raytrace_3d or
raytrace_3d_sp).
DispersionResult
Container for refractive index, absorption, and related propagation metrics.
AppletonHartreeDispersion
Appleton-Hartree magneto-ionic dispersion relation.
SenWyllerDispersion
Sen-Wyller generalized dispersion relation (includes electron collision
frequency via a non-Maxwellian velocity distribution).
RT1DProfile
dataclass
¶
Single-point altitude profile for ray/ionosphere workflows.
Notes¶
alt_kmis required and must be strictly increasing.- Electron density is stored in both m^-3 and cm^-3 (when available).
- MSIS and geomagnetic outputs are attached as namespaces.
Source code in hfpytrace/model/rt1d.py
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compute_collision(Te=None, Ti=None, edens=None, O2p=None, Op=None)
¶
Compute collision frequencies using the already-fetched MSIS neutral data.
Requires self.msise (call fetch_msise() first) and electron
density (call fetch_iri() or set_electron_density() first).
Parameters¶
Te, Ti : array-like or float, optional Electron/ion temperature [K]. Defaults to MSIS neutral temperature Tn.
array-like, optional
Electron density [cm^-3]. Defaults to self.ne_cm3.
O2p, Op : array-like, optional O2+ and O+ ion densities [cm^-3]. Defaults to 10% / 90% of edens (typical F-region mix).
Returns¶
ComputeCollision
The collision object is also stored on self.collision for
subsequent retrieval by :meth:RT1D.NVIS_tracer via
collision_type.
Notes¶
Supported collision types for NVIS_tracer(collision_type=...):
+-----------+-----------------------------------------------+
| Key | Source array |
+===========+===============================================+
| FT | Friedrich-Tonker (nu_ft, a=1.0) |
| FT_cc | Friedrich-Tonker (nu_av_cc, a=2.5) |
| FT_mb | Friedrich-Tonker (nu_av_mb, a=1.5) |
| SN_en | Schunk-Nagy electron-neutral total |
| SN_ei | Schunk-Nagy electron-ion total |
| SN | Schunk-Nagy full total (en + ei) |
| atm | Atmospheric ion-neutral approximation |
+-----------+-----------------------------------------------+
Source code in hfpytrace/model/rt1d.py
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RT2DProfile
dataclass
¶
Container for a 2D ionospheric slice sampled on altitude and path axes.
Conventions:
- vertical axis: alt_km (length nz)
- route axis: x_km / lats / lons (length nx)
- any 2D physical field uses shape (nz, nx)
Source code in hfpytrace/model/rt2d.py
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__post_init__()
¶
Normalize input arrays and run structural validation.
Source code in hfpytrace/model/rt2d.py
validate()
¶
Validate grid monotonicity and attached field shapes.
Source code in hfpytrace/model/rt2d.py
from_cfg(cfg, time=None, lats=None, lons=None, alt_km=None, fetch_iri=True, fetch_msise=False, fetch_geomag=False, workers=1)
classmethod
¶
Build an RT2DProfile from route/height settings in config.
Source code in hfpytrace/model/rt2d.py
set_electron_density(ne_m3=None, ne_cm3=None, source='iri')
¶
Attach user-supplied electron density and keep unit pairs synced.
Source code in hfpytrace/model/rt2d.py
force_zero_density_below(min_alt_km)
¶
Force electron density to zero below a specified altitude threshold.
Parameters¶
min_alt_km
Altitude floor in km. Any row with alt_km < min_alt_km is zeroed.
Returns¶
int Number of altitude rows modified.
Source code in hfpytrace/model/rt2d.py
fetch_iri(cfg, workers=1)
¶
Populate electron density from IRI2d on the profile grid.
Source code in hfpytrace/model/rt2d.py
fetch_msise(workers=1, update_spaceweather=False, suppress_spaceweather_warning=True)
¶
Populate neutral species and neutral temperature from NRLMSISE.
Source code in hfpytrace/model/rt2d.py
fetch_geomag(coord_input='GEO', coeff_dir=None)
¶
Populate geomagnetic vectors and angles along the 2D route grid.
Source code in hfpytrace/model/rt2d.py
compute_collision(Te=None, Ti=None, edens=None, O2p=None, Op=None)
¶
Compute collision frequencies using the already-fetched MSIS neutral data.
Requires self.msise (call fetch_msise() first) and electron
density (call fetch_iri() or set_electron_density() first).
Parameters¶
Te, Ti : array-like or float, optional Electron/ion temperature [K], shape (nz, nx) or broadcastable. Defaults to MSIS neutral temperature Tn.
array-like, optional
Electron density [cm^-3], shape (nz, nx). Defaults to self.ne_cm3.
O2p, Op : array-like, optional O2+ and O+ densities [cm^-3]. Defaults to 10%/90% of edens.
Returns¶
ComputeCollision
Also stored on self.collision for retrieval via
collision_type in :meth:RT2D.build_refractive_index_interpolators.
Notes¶
Supported collision_type keys for :meth:RT2D.oblique_trace:
+-------------+--------------------------------------------------+
| Key | Model |
+=============+==================================================+
| "FT" | Friedrich-Tonker (ν_ft, a=1.0) |
| "FT_cc" | Friedrich-Tonker (ν_av_cc, a=2.5) |
| "FT_mb" | Friedrich-Tonker (ν_av_mb, a=1.5) |
| "SN_en" | Schunk-Nagy electron-neutral total |
| "SN_ei" | Schunk-Nagy electron-ion total |
| "SN" | Schunk-Nagy full (en + ei) |
| "atm" | Atmospheric ion-neutral approximation |
+-------------+--------------------------------------------------+
Source code in hfpytrace/model/rt2d.py
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RT3DProfile
dataclass
¶
3D gridded ionosphere/background container.
Axis convention:
- lats: latitude axis, shape (nlat,)
- lons: longitude axis, shape (nlon,)
- alts_km: altitude axis, shape (nalt,)
- 3D fields use shape (nlat, nlon, nalt)
Source code in hfpytrace/model/rt3d.py
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from_cfg(cfg, time=None, lats=None, lons=None, alts_km=None, fetch_iri=True, fetch_msise=False, fetch_geomag=False, workers=1)
classmethod
¶
Build a profile from explicit axes or config-driven 3D grid settings.
Grid source priority:
1) explicit lats/lons/alts_km
2) cfg.iono_grid fields
3) fallback from global 2D-style height settings and coarse CONUS-like lat/lon grid
Source code in hfpytrace/model/rt3d.py
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force_zero_density_below(min_alt_km)
¶
Set all density values to zero for alt < min_alt_km.
Source code in hfpytrace/model/rt3d.py
compute_collision(Te=None, Ti=None, edens=None, O2p=None, Op=None)
¶
Compute collision frequencies using the already-fetched MSIS neutral data.
Requires self.msise (call fetch_msise() first) and electron
density (call fetch_iri() or set_electron_density() first).
Parameters¶
Te, Ti : array-like or float, optional Electron/ion temperature [K], shape (nlat, nlon, nalt) or broadcastable. Defaults to MSIS neutral temperature Tn.
array-like, optional
Electron density [cm^-3], shape (nlat, nlon, nalt).
Defaults to self.ne_cm3.
O2p, Op : array-like, optional O2+ and O+ densities [cm^-3]. Defaults to 10%/90% of edens.
Returns¶
ComputeCollision
Also stored on self.collision for retrieval via
collision_type in :class:RT3D.
Notes¶
Supported collision_type keys:
+-------------+--------------------------------------------------+
| Key | Model |
+=============+==================================================+
| "FT" | Friedrich-Tonker (ν_ft, a=1.0) |
| "FT_cc" | Friedrich-Tonker (ν_av_cc, a=2.5) |
| "FT_mb" | Friedrich-Tonker (ν_av_mb, a=1.5) |
| "SN_en" | Schunk-Nagy electron-neutral total |
| "SN_ei" | Schunk-Nagy electron-ion total |
| "SN" | Schunk-Nagy full (en + ei) |
| "atm" | Atmospheric ion-neutral approximation |
+-------------+--------------------------------------------------+
Source code in hfpytrace/model/rt3d.py
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DispersionResult
dataclass
¶
Container for derived propagation metrics.
Attributes¶
np.ndarray
Complex refractive index (same shape as broadcasted input fields).
np.ndarray
Absorption coefficient in dB/km.
np.ndarray
Phase constant in rad/km.
np.ndarray
Phase constant in deg/km.
Source code in hfpytrace/model/dispersion.py
AppletonHartreeDispersion
¶
Bases: DispersionBase
Appleton-Hartree style magneto-ionic formulation.
Supported modes¶
- "N"/"NO"/"ISO": isotropic-like branch
- "O": ordinary
- "X": extraordinary
- "R": right-hand circular
- "L": left-hand circular
Source code in hfpytrace/model/dispersion.py
refractive_index(mode='O')
¶
Compute Appleton-Hartree refractive index for the selected mode.
Source code in hfpytrace/model/dispersion.py
SenWyllerDispersion
¶
Bases: DispersionBase
Sen-Wyller generalized formulation.
Notes¶
This implementation follows the structure used in the existing project
absorption workflow and evaluates C(p,y) numerically with scipy.integrate.quad.
Source code in hfpytrace/model/dispersion.py
refractive_index(mode='O')
¶
Compute Sen-Wyller refractive index for the selected mode.
Supported modes: "N"/"NO"/"ISO", "O", "X", "R", "L".
Source code in hfpytrace/model/dispersion.py
RT1D
¶
1D model entry-point that owns a single :class:RT1DProfile.
This initializer is intentionally flexible so callers can construct the profile from:
- a pre-built
RT1DProfileobject, or - a TRACE cfg object (
config1D-style namespace), or - explicit scalar/array user inputs.
Parameters¶
RT1DProfile, optional
Existing profile instance. When provided, this takes precedence and is validated directly.
object, optional
Config namespace used by :meth:RT1DProfile.from_cfg. Can also be used
only for defaults (event/lat/lon/heights) when explicit values are
partially provided.
datetime | str, optional
Profile timestamp. If omitted and cfg has event, cfg event is
used. Otherwise current UTC time is used.
lat, lon : float, optional
Profile location. If omitted, inferred from cfg.origin or
cfg.route.start.
array-like, optional
Altitude grid [km]. If omitted and cfg is provided, built from
start_height_km/end_height_km/height_incriment_km.
ne_m3, ne_cm3 : array-like, optional User-provided electron density. Provide exactly one if overriding model fetch.
str, optional
Density source label when user density is supplied.
fetch_iri, fetch_msise, fetch_geomag : bool, optional If True, populate those profile components during initialization.
int, optional
Worker hint passed to MSIS/cfg-based constructor where supported.
coord_input, coeff_dir : str, optional
Geomagnetic options passed to fetch_geomag when requested and not
provided by cfg.
Notes¶
- This class currently provides initialization/validation orchestration.
- Frequency conversions remain exposed as static compatibility methods.
Source code in hfpytrace/model/rt1d.py
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fetch_collision(Te=None, Ti=None, edens=None, O2p=None, Op=None)
¶
Compute and attach collision frequencies to the profile.
Convenience wrapper around :meth:RT1DProfile.compute_collision.
Requires that fetch_msise() has been called. Plasma defaults
(Te=Ti=Tn, Op=0.9·Ne, O2p=0.1·Ne) are applied when arguments
are omitted.
After calling this, pass collision_type to
:meth:NVIS_tracer to select which model to use, e.g.::
rt.fetch_collision()
result = rt.NVIS_tracer(freq_mhz=freqs, collision_type="SN")
Returns¶
ComputeCollision
Source code in hfpytrace/model/rt1d.py
NVIS_tracer(freq_mhz, mode='O', formulation='appleton', collision_hz=None, collision_type=None, b_t=None, theta_deg=None, n_floor=1e-08, use_nonuniform_grid=True, nonuniform_points=240, nonuniform_sharpness=10.0, compute_absorption_phase=False, round_trip=False)
¶
Vertical-forward-operator style NVIS tracer for a 1D profile.
Parameters¶
array-like or float
Sounding frequencies in MHz.
str, optional
Dispersion mode selector. Supported values are inherited directly
from the selected dispersion formulation in dispersion.py:
- Appleton-Hartree: N/NO/ISO, O, X, R, L
- Sen-Wyller: N/NO/ISO, O, X, R, L
{"appleton", "senwyller"}, optional
Dispersion backend.
array-like or scalar, optional
Collision frequency [Hz] as a direct 1D array. Mutually exclusive
with collision_type.
str, optional
Named collision model. Requires rt.fetch_collision() to have
been called first. Mutually exclusive with collision_hz.
Valid values: "FT", "FT_cc", "FT_mb", "SN_en",
"SN_ei", "SN", "atm" (case-insensitive).
b_t, theta_deg : array-like or scalar, optional Overrides for magnetic field magnitude [T] and wave-normal angle [deg].
float, optional
Minimum refractive index used to identify valid propagation layers.
bool, optional
If True, remap each frequency profile onto a stretched vertical grid with denser sampling near the turning altitude.
int, optional
Number of regridded altitude points used when
use_nonuniform_grid=True.
float, optional
Stretching strength for nonuniform grid. Larger values concentrate more points near the turning altitude.
bool, optional
If True, call dispersion.evaluate() for each frequency and
integrate absorption and phase along the propagation path.
Adds absorption_db, phase_rad, absorption_profile,
and phase_profile to the returned namespace.
bool, optional
If True (and compute_absorption_phase=True), multiply the
integrated absorption and phase by 2 for a two-way (round-trip)
path. Has no effect when compute_absorption_phase=False.
Returns¶
SimpleNamespace
- freq_mhz : frequency array [MHz]
- vh_km : virtual-height estimate [km]
- turning_height_km : turning heights [km]
- n_profile : refractive-index profiles [nfreq, nz]
- reason : per-frequency status strings
- absorption_db : height-integrated absorption [dB, nfreq]
(only when compute_absorption_phase=True)
- phase_rad : height-integrated phase [rad, nfreq]
(only when compute_absorption_phase=True)
- absorption_profile: absorption coefficient [dB/km] on the
altitude grid [nfreq, nz]
(only when compute_absorption_phase=True)
- phase_profile : phase constant [rad/km] on the altitude
grid [nfreq, nz]
(only when compute_absorption_phase=True)
Notes¶
This method intentionally mirrors a vertical forward operator:
it integrates an approximate group index mu' ~= 1 / n from the
bottom altitude up to the turning point for each frequency.
Collision workflow — two ways to supply collision frequency:
- Direct array: pass
collision_hzas a 1D array [Hz]. - Named model: call
rt.fetch_collision()first, then passcollision_typewith one of the keys below.collision_hzmust beNonewhencollision_typeis used.
+-------------+--------------------------------------------------+
| Key | Model |
+=============+==================================================+
| "FT" | Friedrich-Tonker (ν_ft, scaling a=1.0) |
| "FT_cc" | Friedrich-Tonker (ν_av_cc, scaling a=2.5) |
| "FT_mb" | Friedrich-Tonker (ν_av_mb, scaling a=1.5) |
| "SN_en" | Schunk-Nagy electron-neutral total |
| "SN_ei" | Schunk-Nagy electron-ion total |
| "SN" | Schunk-Nagy full (en + ei) |
| "atm" | Atmospheric ion-neutral approximation |
+-------------+--------------------------------------------------+
Source code in hfpytrace/model/rt1d.py
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RT2DConfig
dataclass
¶
Integration controls for :class:RT2D.
Source code in hfpytrace/model/rt2d.py
RT3D
¶
Minimal RT3D container for downstream 3D tracing implementations.
This class currently focuses on profile management and data integrity checks.
Source code in hfpytrace/model/rt3d.py
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fetch_collision(Te=None, Ti=None, edens=None, O2p=None, Op=None)
¶
Compute and attach collision frequencies to the profile.
Convenience wrapper around :meth:RT3DProfile.compute_collision.
Requires that fetch_msise() has been called on the profile.
Returns¶
ComputeCollision
Source code in hfpytrace/model/rt3d.py
trace_cartesian_hamiltonian(freq_hz, elevation_deg, azimuth_deg=0.0, x0_km=0.0, y0_km=0.0, z0_km=0.0, s_max_km=6000.0, mode='O', collision_hz=None, b_abs_t=None, b_psi_deg=None, formulation='appleton-hartree', h0_km=2.0, h_min_km=0.25, h_max_km=8.0, max_step_km=None, local_err_tol_km=0.005, max_steps=20000, boundary_eps_km=0.001)
¶
Adaptive 3D Cartesian Hamiltonian solver for isotropic n(x).
Hamiltonian
H(x, p) = 0.5 (|p|^2 - n(x)^2) = 0
Equations
dx/dtau = p dp/dtau = 0.5 * grad(n^2) = n * grad(n)
Source code in hfpytrace/model/rt3d.py
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oblique_trace(freq_hz, elevation_deg, *, coordinate_system='cartesian', solver='gradient', nhops=1, **kwargs)
¶
Unified 3-D oblique ray-trace entry point.
Parameters¶
coordinate_system : "cartesian" or "spherical".
solver : "gradient" (default) or "hamiltonian" (cartesian only).
int, optional
Number of ionospheric hops (default 1). For nhops > 1 each ground hit is reflected specularly (vz → −vz for cartesian, vr → −vr for spherical) and the ODE restarts from the domain left edge with x/y shifted by the accumulated ground-hit offset (horizontal-homogeneity assumption). All hop segments are concatenated in the returned namespace.
Source code in hfpytrace/model/rt3d.py
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RT2D
¶
Main 2D tracing interface for profile-based and legacy workflows.
Accepted initialization patterns:
1) direct grids: RT2D(x_km, z_km, ne_m3)
2) profile object: RT2D(profile=RT2DProfile(...))
3) config-driven: RT2D(cfg=..., fetch_iri=True, ...)
Source code in hfpytrace/model/rt2d.py
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__init__(x_km=None, z_km=None, ne_m3=None, *, profile=None, cfg=None, time=None, lats=None, lons=None, alt_km=None, ne_cm3=None, source='iri', fetch_iri=False, fetch_msise=False, fetch_geomag=False, workers=1)
¶
Create an RT2D solver instance and prepare interpolation kernels.
Source code in hfpytrace/model/rt2d.py
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fetch_collision(Te=None, Ti=None, edens=None, O2p=None, Op=None)
¶
Compute and attach collision frequencies to the profile.
Convenience wrapper around :meth:RT2DProfile.compute_collision.
Requires fetch_msise() to have been called on the profile first.
After calling this, pass collision_type to
:meth:oblique_trace to select which model to use, e.g.::
rt = RT2D(profile=prof)
rt.fetch_collision()
ray = rt.oblique_trace(freq_hz=10.5e6, elevation_deg=25,
collision_type="SN")
Returns¶
ComputeCollision
Source code in hfpytrace/model/rt2d.py
build_refractive_index_interpolators(freq_hz, b_abs_t=None, b_psi_deg=None, mode='O', formulation='appleton', collision_hz=None, collision_type=None)
¶
Build refractive-index and gradient interpolators on the RT2D grid.
The returned namespace includes:
- n: phase refractive index
- mup: group refractive index proxy (1/n)
- dn_dx, dn_dz: Cartesian gradients of n
Parameters¶
array-like or float, optional
Collision frequency [Hz], shape (nz, nx) or scalar. Mutually
exclusive with collision_type.
str, optional
Named collision model key. Requires fetch_collision() to have
been called first. Mutually exclusive with collision_hz.
Valid values: "FT", "FT_cc", "FT_mb", "SN_en",
"SN_ei", "SN", "atm" (case-insensitive).
Source code in hfpytrace/model/rt2d.py
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trace_cartesian_gradient(freq_hz, elevation_deg, x0_km=0.0, z0_km=0.0, s_max_km=5000.0, mode='O', b_abs_t=None, b_psi_deg=None, formulation='appleton', collision_hz=None, collision_type=None, rtol=1e-07, atol=1e-09, max_step_km=None)
¶
Integrate one oblique ray in Cartesian coordinates using gradient ODEs.
Returns path coordinates, ray direction history, and derived path metrics.
Parameters¶
array-like or float, optional
Collision frequency [Hz], shape (nz, nx) or scalar. Mutually
exclusive with collision_type.
str, optional
Named collision model. Requires fetch_collision() first.
Valid values: "FT", "FT_cc", "FT_mb", "SN_en",
"SN_ei", "SN", "atm" (case-insensitive).
Source code in hfpytrace/model/rt2d.py
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trace_spherical_gradient(freq_hz, elevation_deg, x0_km=0.0, z0_km=0.0, s_max_km=5000.0, mode='O', b_abs_t=None, b_psi_deg=None, formulation='appleton', collision_hz=None, collision_type=None, r_earth_km=6371.0, rtol=1e-07, atol=1e-09, max_step_km=None)
¶
Integrate one oblique ray in spherical geometry over the same n-field.
The n-field is sampled from the internal x-z grid; geometry terms are handled in (r, phi) coordinates for better long-range behavior.
Parameters¶
array-like or float, optional
Collision frequency [Hz]. Mutually exclusive with collision_type.
str, optional
Named collision model key. Requires fetch_collision() first.
Source code in hfpytrace/model/rt2d.py
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oblique_trace(freq_hz, elevation_deg, *, coordinate_system='cartesian', nhops=1, **kwargs)
¶
Unified gradient tracer entry point for oblique propagation.
Parameters¶
coordinate_system
"cartesian" or "spherical" (aliases accepted).
int, optional
Number of ionospheric hops to attempt (default 1). For nhops > 1 each time a hop reaches the ground the ray direction is reflected (vz → −vz) and a new ODE restarts from that ground-hit point. All segments are concatenated in the returned namespace.
Source code in hfpytrace/model/rt2d.py
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trace(freq_hz, elevation_deg, cfg=None)
¶
Legacy finite-difference tracer retained for backward compatibility.
Source code in hfpytrace/model/rt2d.py
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trace_fan(freqs_hz, elevations_deg, cfg=None)
¶
Run a finite-difference fan sweep over frequencies and elevations.