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. 2021 Jul 23;31(6):1843–1859. doi: 10.1111/ina.12900

Simulating near‐field enhancement in transmission of airborne viruses with a quadrature‐based model

Laura Fierce 1,*,, Alison J Robey 2, Cathrine Hamilton 3
PMCID: PMC8447483  PMID: 34297863

Abstract

Some infectious diseases, such as influenza, tuberculosis, and SARS‐CoV‐2, may be transmitted when virus‐laden particles expelled from an infectious person are inhaled by someone else, which is known as the airborne transmission route. These virus‐laden particles are more concentrated in the expiratory jet of an infectious person than elsewhere in a well‐mixed room, but this near‐field enhancement in virion exposure has not been well quantified. Transmission of airborne viruses depends on factors that are inherently variable and, in many cases, poorly constrained, and quantifying this uncertainty requires large ensembles of model simulations that span the variability in input parameters. However, models that are well‐suited to simulate the near‐field evolution of respiratory particles are also computationally expensive, which limits the exploration of parametric uncertainty. In order to perform many simulations that span the wide variability in factors governing airborne transmission, we developed the Quadrature‐based model of Respiratory Aerosol and Droplets (QuaRAD). QuaRAD is an efficient framework for simulating the evolution of virus‐laden particles after they are expelled from an infectious person, their deposition to the nasal cavity of a susceptible person, and the subsequent risk of initial infection. We simulated 10 000 scenarios to quantify the risk of initial infection by a particular virus, SARS‐CoV‐2. The predicted risk of infection was highly variable among scenarios and, in each scenario, was strongly enhanced near the infectious individual. In more than 50% of scenarios, the physical distancing needed to avoid near‐field enhancements in airborne transmission was beyond the recommended safe distance of two meters (six feet) if the infectious person is not wearing a mask, though this distance defining the near‐field extent was also highly variable among scenarios; the variability in the near‐field extent is explained predominantly by variability in expiration velocity. Our findings suggest that maintaining at least two meters of distance from an infectious person greatly reduces exposure to airborne virions; protections against airborne transmission, such as N95 respirators, should be available when distancing is not possible.

Keywords: aerosol modeling, airborne transmission, respiratory particles


Practical Implications.

  • The risk of airborne transmission is orders of magnitude greater in the expiratory jet of an infectious person than in a well‐mixed room.

  • The horizontal extent of near‐field airborne transmission extends beyond the travel distance of large droplets.

  • Variability in the horizontal extent of near‐field effects is driven primarily by variability in the expiration velocity.

1. INTRODUCTION

Airborne transmission of pathogens was first recognized over 50 years ago 1 and has since been acknowledged as an important transmission route for a number of infectious diseases. 2 , 3 , 4 , 5 , 6 Even so, the risks posed by airborne spread remain poorly addressed by many safety standards, 7 a trend that continued with dire consequences during the early phases of the COVID‐19 pandemic. 8 It is now apparent that transmission of SARS‐CoV‐2, the virus causing COVID‐19, occurs primarily through the inhalation of airborne virions, 9 , 10 as opposed to impaction to a susceptible persons eyes, nostrils, and lips. Though long‐range airborne transmission is possible due to the small size and long transport distances of many infectious respiratory particles, the risk of infection is greatest near infectious individuals where the concentration of virions is highest. 11 These near‐field enhancements in transmission must be understood to design and implement effective mitigation strategies, such as selecting the distance needed between desks in a classroom or between workers in a factory. However, near‐field increases in virion exposure are subject to variable and poorly constrained parameters, and this uncertainty in factors controlling transmission is not easily represented in models.

A key challenge in quantifying near‐field effects is the inherent variability in factors governing transmission risk. For example, the rate at which different individuals expel virions varies by orders of magnitude, 12 , 13 and epidemiological data suggests that the risk of infection at a given virion dose is also highly variable. 14 These uncertainties in the physiological characteristics of both infectious and susceptible individuals lead to large uncertainty in predictions of transmission risk. 15 , 16 Large ensembles of model simulations are needed to quantify this uncertainty. However, while computational fluid dynamics models simulate airflows within a room in great detail and are, therefore, able to resolve heterogeneity in virion concentrations, 17 , 18 these models are computationally expensive, 17 , 18 limiting the number of simulations that can be performed. Multi‐zone models that simulate airflow within buildings typically track the average concentration in each room, 19 , 20 but by assuming virions are well mixed within each room, these models neglect local increases in virion concentrations near an infectious person. To represent airborne transmission across a wide range of conditions, a model framework is needed that accurately represents processes governing near‐field and far‐field transmission but is efficient enough to perform large ensembles of simulations.

To address this need, we introduce the Quadrature‐based model for Respiratory Aerosol and Droplets (QuaRAD), an efficient framework for simulating the full life cycle of virus‐laden particles within indoor spaces—from their initial creation and expulsion from an infectious person to their eventual removal from the space or their inhalation by a new host. This model framework is an alternative to Monte Carlo models for simulating the dispersion and evolution of respiratory particles. In contrast to Monte Carlo models, which represent particle size distributions using thousands of randomly sampled particles, quadrature‐based moment methods have been shown to accurately represent low‐order distribution moments—as well as other integrated quantities—using only a small number of quadrature points. 21 , 22 In this study, the quadrature representation was used to quantify the rate at which particles deposit onto the most likely initial infection site of SARS‐CoV‐2, the nasal epithelium. This paper describes the QuaRAD model (Section 2) and its application to simulation across a wide range of scenarios (Section 3), followed by discussion (Section 4) and conclusions (Section 5). Though we focus here specifically on SARS‐CoV‐2, most aspects of this model are equally applicable and easily adaptable to studying the airborne transmission of any disease.

2. MODEL DESCRIPTION

The respiratory particles that carry airborne viruses are created in the respiratory system through expiratory activities such as sneezing, coughing, talking, or breathing. A particle's size at the time it is expelled dictates the distance it travels before settling to the ground. If a particle is transported to another individual and inhaled, its size influences if and where in the respiratory system it is most likely to deposit. For this reason, the QuaRAD model is designed to accurately and efficiently represent the size distribution of expelled particles and its evolution through evaporation, transport, and removal.

The processes simulated in QuaRAD are shown in Figure 1. The model represents mechanisms governing the transport and evolution of virus‐laden particles (boxes 1−4), as well those governing virion deposition and initial infection within the potential host (boxes 5−6). Before describing the model components in detail, we first provide an overview of the connections between model components (labeled with letters in Figure 1).

FIGURE 1.

FIGURE 1

QuaRAD represents processes governing the evolution of expelled particles (left) and processes governing infection in a new host (right). Model inputs are provided in Table 1. The model components (1–6) and the connections components (a–h) are described in the text of Section 2

TABLE 1.

Sample distributions for each varied parameter, using minimum and maximum for uniform distributions, mean and standard deviation for normal distributions, and geometric mean and geometric standard deviation for lognormal distributions
Variable Dist. min/mean/geom. mean max/st. dev./geom. st. dev Nominal value Ref.
Expiration parameters
Dmouth Normal 0.02 2 × 10−4 0.02
S 0 Normal 1 5 × 10−3 1 1
T 0 Normal 310.15 0.1 310.15
u 0 Normal 4 2 4 2
z 0 Normal 1.5 0.07 1.5 3
Size distribution parameters
μ b Normal 1.60 × 10−6 2.56 × 10−7 1.60 × 10−6
μ l Normal 2.50 × 10−6 3.75 × 10−7 2.50 × 10−6 4
μ o Normal 1.45 × 10−4 1.16 × 10−6 1.45 × 10−4
N b Normal 6.75 1.08 6.75
N l Normal 8.55 1.28 8.55 4
N o Normal 1.58 × 10−3 1.3 × 10−3 1.58 × 10−3
σ b Normal 1.30 0.02 1.30
σ l Normal 1.66 0.05 1.66 4
σ o Normal 1.80 0.01 1.80
Aerosol parameters
κ Uniform 0.3 1.2 1.1 5
ρ aero Uniform 1000 1600 1300 6
Vfaero Uniform 0.01 0.09 0.05 7
N v Lognormal 7 1.2 7 8
f v Lognormal 3.60 × 10−2 1.2 3.60 × 10−2
Room parameters
ACH Uniform 0.3 2.7 1.5 9
H Normal 2.74 0.38 2.74 10
S Uniform 0.25 0.6 0.5 11
T v,∞ Normal 293.4 2 293.15 12
L Uniform 7 15 10 13
W Uniform 7 15 10
Inhalation & deposition parameters
I rate Uniform 12 20 16 14
I vol Uniform 3.75 × 10−4 6.25 × 10−4 4.69 × 10−4 15
a Normal −3.9 × 10−3 2.33 × 10−3 −3.9 × 10−3
b Normal −16.6 4.5 −16.6 16
c Normal 0.5 0.02 0.5
d Normal −0.28 0.09 −0.28
Infection parameters
[Mucfree] Normal 1.18 × 10−7 2.04 × 10−8 1.18 × 10−7 17
Kmucin Lognormal 1000 2 1000
p cell Uniform 0.1 0.9 0.1 18
p pfu lognormal 2.8 × 10−3 1.2 2.8 × 10−3
Nominal values are those used when that parameter is not varied.
References: 1. Wei and Li 29 , 2. Chao et al. 61 , Tang et al. 62 , 3. NCHS 63 , 4. Johnson et al. 23 , 5. Petters and Kreidenweis 33 , Vejerano and Marr 28 , 6. Stadnytskyi et al. 64 , 7. Vejerano and Marr 28 , 8. Milton et al. 25 , 9. USEPA 65 , Bennett et al. 66 , Turk et al. 67 , 10. GSA 68 , 11. Nguyen et al. 69 , 12. Antretter et al. 70 , 13. NYSDOH 71 , 14. Flenady et al. 72 , 15. Flenady et al. 72 , Sidebotham 73 , 16. Cheng 31 , 17. Gale 15 , Kesimer et al. 51 , 18. Gale. 15
.  

Each of our QuaRAD simulations begins by replacing the continuous size distribution of expiratory particles with a quadrature approximation consisting of six weighted particles (see Section 2.1). Taking as inputs the (a) initial diameter of each quadrature point, as well as the chemical properties of the constituent aerosol, we then simulate water evaporation to predict particle sizes as they shrink over time (see Section 2.2). Using the (b) time‐dependent size of each particle, we then predict how it would move within the expiratory jet if it were released at the jet center; the (c) time‐dependent position of the center line particles and the (d) quadrature weights are taken as inputs to a model that represents particle dispersion using a Gaussian puff within a turbulent jet (see Section 2.3). The (e) velocity of the particle relative to the gas is fed back to the evaporation scheme to represent enhancements in evaporation rates through convection.

The output of the particle dispersion model is used to predict deposition to the nasal cavity of a new host and the probability of initial infection. Using the (f) size of each quadrature point and the (g) virion concentration associated with each quadrature point, we predict the total virion dose reaching the nasal epithelium of a susceptible person as a function of their location relative to the infectious person and the duration of the encounter. From the (h) virion dose, we then predict the probability that each deposited virion finds an ACE2 receptor, binds to it, and begins replication (Section 2.4). For convenience, all variables used in this section are also defined in Table 2.

TABLE 2.

Each variable used in this paper, along with its definition, units, and (if treated as a constant) its value

Definition of variables
Variable Definition Units
A Surface area available for deposition m2
A 0 Cross‐sectional area of the jet orifice m2
ACH Air changes per hour h−1
Ar0 Archimedes number
a, b, c, d Nasal deposition efficiency coefficients
b Gaussian half‐width of jet m
C D Drag coefficient
ci Concentration associated with quadrature point i particles/m3
C p Specific heat of particle J/(K kg)
C T Correction factor for diffusion coefficient
D 0 Initial particle diameter m
D p Particle diameter m
D a Particle aerodynamic diameter m
D d Particle dry diameter m
D diff Molecular diffusion coefficient of particle m2/s
D Diffusivity of water in air 2.42 × 10−5 m2/s
D mouth Diameter of infectious individual's mouth m
e d Deposition efficiency to nasal epithelium
F c Fraction of virions in exposure dose already bound to cells
F trans Fraction of virions in exposure dose transported to the infection site
F v Fraction of virions in exposure dose not bound to mucin
f v Fraction of virions residing in coarse particles
g Acceleration due to gravity 9.81 m/s2
H Height of the room (z‐direction) m
hi Quadrature abscissas
Hn Hermite polynomial
I rate Average adult inhalation rate breath/min
I vol Average adult inhalation volume m3/breath
k Fresh air ventilation rate s−1
kg Thermal conductivity of air 0.2529 W/(m K)
K mucin Association constant for binding between virion and mucin M−1
κ Effective hygroscopicity parameter of aerosol contained in particle
L Length of the room (x‐direction) m
L v Latent heat of vaporization 2.45 × 106 J/kg
m p Mass of aqueous particle p kg
M w Molecular weight of water 0.018 kg/mol
μb, μl, μo Geometric mean diameter of particles in the b‐, l‐, and o‐mode, respectively m
[Mucfree] Concentration of free mucin molecules molecules/mm3
N b, N l, N o Particulate number emission rate for the b‐, l‐, and o‐mode, respectively particles/s
N deposit Rate of virion deposition into the nasal epithelium virions/s
N p Overall number concentration of particles particles/m3
N v Overall number concentration of virions virions/m3
N v,i Virions associated with quadrature point i virions/m3
Nu The Nusselt number
ν Dynamic viscosity Pa s
N˙v
Number emission rate of virions virions/s
p Ambient pressure Pa
p 1 Probability that a single virion initiates an infection
p cell Probability, given a bound virion, that a cell becomes infected 0.5
p infect Probability of initial infection given an exposure dose
p pfu Probability that a given virion is capable of initiating infection in a cell
p v,0 Saturation vapor pressure of the air Pa
p v,∞ Vapor pressure far from droplet surface Pa
p v,p Vapor pressure at droplet surface Pa
Pr The Prandtl number
R 0 Radius of the jet's potential core m
R Universal gas constant 8.314 J/(mol K)
r Radial distance from the jet center line m
Rx , R y, R z Reflection terms in the x‐, y‐, and z‐directions, respectively
Re The Reynolds number
RH Relative humidity %
ρ 0 Density of expired air kg/m3
ρ Density of background air kg/m3
ρ aero Density of aerosol in particle kg/m3
ρ g Density of gas kg/m3
ρ p Density of particle kg/m3
ρv,c Center line water vapor density kg/m3
ρw Density of water 1000 kg/m3
S 0 Initial plume saturation ratio
S Background saturation ratio
s Distance traveled along center line of the jet m
Sc The Schmidt number
Sh The Sherwood number
σs/a Surface tension on particle surface N/m
σb, σl, σo Geometric standard deviation of particle diameter in the b‐, l‐, and o‐mode, respectively
t Time s
T 0 Initial plume temperature K
T v,∞ Background temperature K
T p Particle temperature K
T v Vapor temperature K
T v,c Centerline temperature K
u 0 Initial expiration velocity m/s
u g Gas velocity in the x‐direction m/s
u p Particle velocity in the x‐direction m/s
V Room volume m3
V˙breath
Volumetric breathing rate m3/s
V e Number of virions in airborne exposure dose virions
Vfaero Bulk volume fraction of aerosol in droplet m3/m3
v g GAS velocity in the y‐direction 0 m/s
vi Viral load associated with quadrature point i virions/m3
v p Particle velocity in the y‐direction m/s
W Width of the room (y‐direction) m
w d Deposition rate onto surfaces m/s
w g Gas velocity in the z‐direction 0 m/s
w i Weight associated with quadrature point i
w p Particle velocity in the z‐direction m/s
x 0 x location of source m
x c x location of jet center line for each particle m
x near Threshold distance at which local enhancement in virion concentration increases transmission risk by >5% m
y 0 y location of source m
y c y location of jet center line for each particle m
z 0 z location of source (mouth height) m
z c z location of jet center line for each particle m

2.1. Quadrature approximation of particle size distributions

QuaRAD uses numerical quadrature to obtain an accurate and efficient representation of the size distribution of expelled aerosol particles and droplets. To construct the quadrature approximation, we follow the approach of Johnson et al. 23 and represent expired particles through three different mechanisms, resulting in three lognormal distributions. Breath and speech create near continuous flows of small aerosol particles through the bronchial fluid film burst mechanism, the process of thin mucus films rupturing as the alveoli open and close deep in the lung (referred to as bronchial or b‐mode particles); activities that vibrate the vocal cords create slightly larger particles through laryngeal vibrations (referred to as laryngeal or l‐mode particles); and expulsion of mucus from the mouth or nose generates the largest particles (referred to as oral or o‐mode particles).

In QuaRAD, each of the three lognormal distributions is approximated using Gauss‐Hermite quadrature. We found that one‐point, three‐point, and two‐point quadrature were sufficient for representing the b‐, l‐, and o‐modes, respectively, such that the overall distribution is represented with only six weighted particles; adding additional particles did not improve simulation accuracy (see Appendix A.1).

Gauss‐Hermite quadrature approximates integrals of the form exp(x2)f(x)dx f(lnDp); with a change of variables, integrals over lognormal distributions can also be expressed in this form. The expected value of a function of the natural logarithm of the diameter, f(InD p), over a continuous lognormal distribution is given by:

Ef(lnDp)=1σ2πexp(lnDpμ)22σ2flnDpdlnDp, (1)

where μ is the natural logarithm of the geometric mean and σ is the natural logarithm of the geometric standard deviation, the parameters of the lognormal distribution. With the following change of variables:

x=lnDpμ2σ, (2)

the integral over the continuous distribution is estimated by a quadrature approximation of the form:

Ef(lnDp)1πi=1nwif2σhi+μ, (3)

where the abscissas hi are the roots of the physicists’ Hermite polynomial:

Hn(x)=(1)nexp(x2)dndxnexpx2, (4)

and the weights are given by:

wi=2n1n!πn2[Hn1(hi)]2 (5)

The overall number concentration of virions, N v, is then given as the sum over N v,i, the number concentration of virions associated with each quadrature point:

Nv=iNquadNv,i (6)

The number of virions associated with a given quadrature point i is computed as a function of the particle's viral load—that is, the number of virions per volume of respiratory fluid—and its initial diameter:

Nv,i=Npπ6D0,i3viwi, (7)

where N p is the overall particle number concentration and vi is the viral load associated with quadrature point i.

The distribution in virions with respect to particle size is an important parameter when modeling transmission, but the variation of SARS‐CoV‐2 loading within particles of different sizes has not yet been well quantified. A small number of studies have investigated virion expiration rates for other viruses with comparable viral loads 24 in fine and coarse particles using the Gesundheit II (G‐II), an instrument designed to capture and analyze respiratory particles. 13 , 25 We combine the measurements of viral shedding from the G‐II with the measurements of the particle size distributions by Johnson et al., 23 Morawska et al., 26 and Asadi et al. 27 to estimate the viral load for particles in each mode. We assume that all virions in fine particles (D p < 5 μm) are distributed among the b‐ and l‐mode particles and that all virions in coarse particles (D p < 5 μm) are contained in o‐mode particles; we assume the viral load is uniform across fine particles and across coarse particles. The weights corresponding to the distribution in virions, given by N v,i/N v, are shown in Figure 2c.

FIGURE 2.

FIGURE 2

Example of the particle size distribution represented as three separate lognormal modes of particles originating from the bronchial (blue), laryngeal (orange), or oral (green) region of the respiratory system. In QuaRAD, the (A) continuous distributions for the b‐, l‐, and o‐mode particles are represented using (B) 1‐point, 3‐point, and 2‐point quadrature, respectively. Weights representing distributions of virions are shown in (C).

2.2. Water evaporation from particles

Expelled aerosol particles and droplets are predominantly water and contain small amounts of dissolved or suspended aerosol components, such as mucin, salts, and surfactants. 28 After they are expelled, water evaporates, causing the particles to shrink, 26 , 29 which may impact the distance a particle is able to travel before settling through sedimentation 30 and its deposition efficiency to the nasal epithelium. 31 , 32

When first expelled, we assume particles are suspended in air that is saturated with water vapor (RH = 100%) and at a temperature near the average human body temperature (T 0 = 310.15). 29 Following measurements by Vejerano and Marr, 28 we assume that freshly expelled particles and droplets are 1%–9% dry aerosol by volume and that the aerosol mixture has an effective hygroscopicity parameter κ between 0.05 and 1. The effective κ is the volume‐weighted average of κ for all dry aerosol components contained in a particle, and is, therefore, a flexible framework for representing uncertainty in the hygroscopic properties of respiratory aerosol. 33 Once expelled, the particles cool and evaporate, with the rate of evaporation and equilibrium diameter dependent on the particles’ initial size, water content, and the hygroscopic properties of its aerosol constituents.

Following the approach of Kukkonen et al. 34 and Wei and Li, 29 we modeled evaporation by solving the following coupled set of ordinary differential equations:

dmpdt=2πpDpMwDCTShRTv,lnppv,pppv, (8)
dTpdt=1mpCpπDp2kgTv,Tp0.5DpNuLvdmpdt, (9)

where m p is the mass of the aqueous particle, T p is the particle temperature, p is the ambient pressure, p v,p is the vapor pressure at the droplet surface, p v,∞ is the vapor pressure far from the droplet surface, M w is the molecular weight of water, D is the binary diffusion coefficient of water vapor in air far from the droplet surface, R is the universal gas constant, C p is the specific heat of the particle, k g is the thermal conductivity of air, L v is the latent heat of vaporization, C T is a correction factor, Sh is the Sherwood number, and Nu is the Nusselt number. We assume spherical droplets to compute the diameter D p as a function of the mass of aerosol—assumed constant over the simulation—and water, which evolves according to Equation 8.

The evaporation model given in Equation 8 includes enhancement in the evaporation rate due to convection. This effect depends on the Sherwood number, the Nusselt number, and a correction factor C T for the diffusion coefficient due to the temperature difference between the particle and the air:

CT=Tv,TpTv,λ12λTv,2λTp2λ, (10)

where λ is a constant between 1.6 and 2, fixed at λ = 1.6 in this study. The Sherwood number is given by:

Sh=1+0.38Re1/2Sc1/3, (11)

where Sc is the Schmidt number, given by:

Sc=νD, (12)

where ν is the dynamic viscosity. The Nusselt number is given by:

Nu=1+0.3Re1/2Pr1/3, (13)

where Pr is the Prandtl number, given by:

Pr=Cpμkg (14)

The rate at which an aqueous droplet evaporates is driven by the difference between the vapor pressure over the droplet and the vapor pressure of the ambient air, where droplet vapor pressures much larger than the ambient vapor pressure will result in rapid evaporation rates. We compute the vapor pressure over an aqueous particle using the κ‐Köhler model 33 :

pv,p=pv,0Dp3Dd3Dp3Dd31κexp4σs/aMwRTpρwDp, (15)

where p v,0 is the saturation vapor pressure, D d is the particles’ dry diameter, κ is the effective hygroscopicity parameter of the aerosol contained in the particle, σs/a is the surface tension at the particle surface, and ρ w is the density of water. The vapor pressure over an aqueous droplet is computed relative to the saturation vapor pressure over a flat surface of pure water, which is computed as a function of the vapor temperature T v according to the Buck equation 35 :

pv,0=611.21exp19.84Tv234.5Tv273.15Tv16.01. (16)

For the example scenario, the evolution of D p, i (t) is shown in Figure 3 for each quadrature point i = 1,…, N quad, upon exposure to the room‐averaged temperature and relative humidity. All particles, regardless of their initial size, shrink over time, but the timescale for evaporation varies over orders of magnitude, as shown in previous studies. 29 , 36 , 37 The largest particles (o‐mode, green) require more than 10 s to reach their equilibrium size. On the other hand, the fine particles in the b‐mode (blue) and l‐mode (orange) reach equilibrium within 10−3 to 10−1 s, depending on their initial size. A particle's diameter influences its transport through the expiratory jet, as described in the following section.

FIGURE 3.

FIGURE 3

Temporal evolution of the diameter of each quadrature point simulated in the baseline scenario. The diameters at t = 0 correspond to their diameter at emission (shown in Figure 2). Particles in the b‐ and l‐mode, which tend to be on the order of tens of micrometers or smaller, reach their equilibrium size within 10−3 to 10−1 s after expulsion, depending on their size, whereas the large, o‐mode particles evaporate more slowly and typically do not reach their equilibrium sizes before settling.

2.3. Particle dispersion within a turbulent jet

To predict the number concentration of virus‐laden particles at a position (x,y,z), we represent the evolution of each quadrature point using the exposure model for indoor sources from Drivas et al. 38 For an instantaneous source, such as a single cough, the concentration associated with each quadrature point i is a function of position as well as time, denoted ci (x,y,z,t). A continuous emission source, such as talking, is represented as a series of puffs, such that the steady‐state concentration c~i(x,y,z)=ci(x,y,z,t)dt, as shown for each quadrature point in Figure 4.

FIGURE 4.

FIGURE 4

The virion concentration N v, i associated with each of the quadrature points i = 1,…,6, shown in Figure 2. Larger weights in Figure 2 correspond to higher virion concentration. Black dashed lines show the center line trajectory for each quadrature point, whereas the false color plots show the virion concentration, predicted using a Gaussian puff model of dispersion about the center line. The overall virion concentration is then computed as the sum over each quadrature point, shown for this baseline example in Figure 7.

Following Drivas et al., 38 we represent dispersion as the combination of a decay term and reflection terms Rx (t), Ry (t), and Rz (t):

ci(x,y,z,t)=qexpACH3600wdAVtπ3/2b3Rx(t)Ry(t)Rz(t), (17)

where ACH is the ventilation rate in air changes per hour, w d is the deposition velocity, A is the deposition area, and V is the room volume. The reflection terms in Drivas et al. 38 account for reflections from the walls, floor, and ceiling, which are important for dispersion of gas‐phase contaminants and small particles. We represent these wall reflections for particles smaller than 30 μm, and Rx (t), Ry (t), and Rz (t) are given by:

Rx(t)=i=exp(x+2iLxc(t))2b(t)2+exp(x+2iL+xc(t))2b(t)2 (18)
Ry(t)=i=exp(y+2iwyc(t))2b(t)2+exp(y+2iw+yc(t))2b2 (19)
Rz(t)=i=exp(z+2iHzc(t))2b(t)2+exp(z+2iH+zc(t))2b(t)2, (20)

where L, W, and H are the length, width, and height of the room, xc(t),yc(t),zc(t) is the trajectory of a particle located in the center of the puff, and b(t) is the puff width. We assume that the infectious person is standing in the center of the room (x0=L/2,y0=W/2). In Equations (18), (19), (20), each infinite sum is replaced as the sum from −1000 to 1000, which was sufficient for convergence.

For particles larger than 30 μm, we do not include reflections. The terms Rx(t), Ry(t), and Rz(t) are reduced to:

Rx(t)=exp(xxc(t))2b(t)2 (21)
Ry(t)=exp(yyc(t))2b(t)2 (22)
Rz(t)=exp(zzc(t))2b(t)2. (23)

Whereas Drivas et al. 38 represents exposure from the release of a toxin under quiescent conditions, we represent particle dispersion during talking using a turbulent jet model that includes buoyancy and gravitational settling. In the original formulation, x c, y c and z c are fixed at the location of the pollutant source. In contrast, we simulate the trajectory x c (t), y c (t), and z c (t) within the expiratory jet of the infectious person. We assume that breadth of the puff is the same as the breadth of the jet, which is proportional to the distance traveled along the center line of the jet, s(t):

b(t)=0.114s(t). (24)

To compute the position and velocity of a particle with diameter D p at the center of each puff, we follow the general approach of Wei and Li. 29 The temporal evolution of particle position and velocity is determined by solving the set of six ordinary different equations that describe the motion of a particle in a moving gas 39 :

dxcdt=up (25)
dycdt=vp (26)
dzcdt=wp (27)
dupdt=3ρgCD4Dpρp(ugup)ugup (28)
dvpdt=3ρgCD4Dpρp(vgvp)ugup (29)
dwpdt=3ρgCD4Dpρp(wgwp)ugup+g, (30)

where u p, v p, and w p are the particle velocity in the x‐, y‐, and z‐directions, respectively, u g, v g, and w g are the gas velocity in the x‐, y‐, and z‐directions, respectively, C D is the drag coefficient, and g is the acceleration due to gravity. where up=up,vp,wp and ug=ug,vg,wg. The drag force is given by:

CD=24ReifRe124Re(1+0.15Re0.687)ifRe>1, (31)

where Re is the Reynolds number. The Reynolds number for this case is given by:

Re=upugDpν. (32)

In this study, we represent cases with co‐flow only, such that v g =0 and w g =0. The gas velocity is predicted using the turbulent jet model of Lee et al. 40 by modeling the infectious individual's mouth as a circular orifice with diameter D mouth. Under this model, the co‐flow velocity in the flow establishment zone (s ≤ 6.2D mouth) is given by:

ug=u0ifrR0u0exp(rR0)2b2ifr>R0 (33)

where r is the radial distance from the jet center line, b is the Gaussian half‐width, and R0=Dmouth/2s/12.4, where s is the distance traveled along the jet center line. In the zone of established flow (s > 6.2D mouth), the velocity is given by:

ug=u0expr2b2. (34)

The expelled air is typically warmer, moister, and contains more CO2 than the background air. 41 The elevated temperature and water content cause the jet to curve upward due to buoyancy, which is partially offset by the increases in air density from the elevated concentration of CO2 in exhaled breath. We follow the approach of Baturin et al. 42 to model the curve of the jet:

z(x)=0.0354A0Ar0xA03T0Tv,, (35)

where T 0 is the source temperature, T v,∞ is the background temperature, and A 0 is the cross‐sectional area of the jet orifice. The Archimedes number Ar0 is given by:

Ar0=gA0u02Δρρ0, (36)

where Δρ=ρρ0 is the difference between the background density, ρ , and the source density, ρ 0.

Similar to Xie et al. 30 and Wei and Li, 29 we use the relationships from Chen and Rodi 43 to represent the evolution in T v and the water vapor density ρv within the turbulent jet. Once in the zone of established flow (x ≥ 6.2D mouth), the center line temperature Tv ,c and the center line water vapor ρ v both decay with distance s according to the same relationship:

Tv,cTv,Tv,0Tv,=ρv,cρv,ρv,0ρv,=5s/DmouthTv,0Tv,. (37)

In the flow establishment zone of the jet (x < 6.2D mouth), we assume that T v,c = T v,0 and ρ v,c = ρ v,0.

The variation in T v and ρ v with the jet radius is then given by:

TvTv,Tv,cTv,=ρvρv,ρv,cρv,=expr2ln2(0.11s)2. (38)

Water vapor is represented as an ideal gas, such that ρ v is computed from the partial pressure of water vapor p v:

ρv=MwpvRTv. (39)

Using this combined jet dispersion model, we find that the spatial distribution in particles simulated by QuaRAD agrees well with the Discrete Random Walk (DRW) model of Wei & Li 29 (see comparison in Appendix A.2). Whereas the DRW model tracks thousands of Monte Carlo particles, QuaRAD simulates six quadrature points. The spatial distribution in virions associated with each QuaRAD point is shown in Figure 7.

FIGURE 7.

FIGURE 7

Number concentration of SARS‐CoV‐2 virions resulting from continuous talking for 1 h in an example case (see Table 1 for input parameters). The virion concentration is one to two orders of magnitude greater in the expiratory jet than in the well‐mixed room.

2.4. Virion exposure and risk of infection

We applied the infection model described in Gale 15 to quantify the probability of initial SARS‐CoV‐2 infection as a function of the virion exposure level and host defense through the mucus barrier, such that the probability of infection increases with virion exposure and decreases with virion binding affinity to mucin molecules. The greater the number of virions to which a person is exposed, V e, the greater the number of chances that any given virion will successfully infect a cell. Differences in individuals’ immune responses are represented by modifying the probability that a virion infects a single cell, p 1. The probability of initial infection within the host, p infect, is then computed as a function of p 1 and V e:

pinfect=1(1p1)Ve. (40)

To compute V e from the virion concentrations simulated in QuaRAD, we applied a respiratory deposition model to calculate the number of inhaled virions that reach the potential site of infection; this is in lieu of calculating the risk of initial infection from the total number of virions inhaled, since not all will deposit to those places within the respiratory system where infection is likely to initiate. In the case of SARS‐CoV‐2, infection must begin with a virion binding to an angiotensin‐converting enzyme 2, or ACE2, receptor. 44 , 45 As ACE2 expression within the respiratory tract is highest in the nasal epithelium and this is the most likely site of initial infection, 46 , 47 , 48 we assume that V e is the total number of virions that deposit to this region. We applied the model from Cheng 31 to predict the deposition efficiency to the nasal epithelium as a function of particle size:

ed=1expaDa26×104V˙breathe+bDdiffc6×104V˙breathed, (41)

where D a is the aerodynamic diameter of the particle, D diff is the molecular diffusion coefficient of the particle, V˙breathe is the breathing rate, and a, b, c, and d are coefficients of deposition efficiency. We represent the uncertainty reported by Cheng 31 in the coefficients a, b, c, and d, leading to uncertainty in e d even for particles of the same size. Figure 5 shows the resulting variability in the size‐dependent deposition represented across the ensemble of scenarios (Figure 6).

FIGURE 5.

FIGURE 5

The median (orange line), quartiles (boxes), and 95% confidence intervals (whiskers) of the distribution in deposition efficiency as a function of particle size. The parameters within the deposition model (Equation 41) were sampled according to the distributions in Table 1.

FIGURE 6.

FIGURE 6

The median (orange line), quartiles (boxes), and 95% confidence intervals (whiskers) of the probability of initial infection given a SARS‐CoV‐2 virion dose. The parameters within the infection model (Equation 40) were sampled according to the distributions in Table 1.

The overall rate at which virions deposit to the nasal epithelium, dV e/dt, is computed as the sum over the deposition rates associated with each of the quadrature points:

dVedt(x,y,z)=V˙breatheiNquaded,iNv,i(x,y,z), (42)

The probability that a virion infects a single cell, p 1, is given by:

p1=FtransFvFcppfupcell, (43)

where F trans is the fraction of virions that deposit to the infection site, F v is the fraction of virions at the infection site but not bound to the mucin, F c is the fraction of virions already bound to other cells, p pfu is the probability a given virion is capable of initiating an infection, and p cell is the probability that a cell with a bound virus will become infected, defined as the virus successfully entering the cell, replicating, and releasing progeny virions. Following Gale 15 , We assume that p cell = 0.5 and F c = 1 based on Hoffmann et al. 49 and Hui et al. 50 We also assume that the only possible infection site is the nasal epithelium, and thus set F trans = 1 for all virions depositing in this region. The fraction of “free” virions not bound to the mucin, F v, is modeled as:

Fv=1KmucinMucfree, (44)

where K mucin is the association constant for binding of the virions to the mucin molecules and [Mucfree] is the concentration of free mucin molecules remaining. These parameters likely vary widely among individuals, and the distributions in their values remain poorly constrained. Following the reasoning of Gale 15 and the measurements of Hou et al. 46 and Kesimer et al., 51 we assume that K mucin varies between 103 and 106 M−1 and that [Mucfree] = 7.11 × 1010 ± 1.23 × 1010. The probability of initial infection as a function of the virion dose is shown in Figure 6

We chose this dose‐response model instead of the traditional Wells‐Riley model because the dose‐response framework can more easily account for the impact of spatiotemporal variation in virion concentrations on virion exposure. 52 , 53 Furthermore, the typical advantage of using the Wells‐Riley model over a dose‐response model in the study of novel viruses stems from the ease of accurately estimating the quanta emission rate, as compared to measuring the virion emission rate, 52 however, in the case of SARS‐CoV‐2, the quanta emission rate remains uncertain 54 and highly variable, 55 limiting the model's comparative advantage. Utilizing a dose‐response model instead allows consideration of per‐particle variation in viral load and, consequently, the detailed differences in exposure risk between scenarios.

3. RESULTS

We used QuaRAD to quantify the risk of airborne transmission of SARS‐CoV‐2 during a face‐to‐face encounter between an infectious and a susceptible person. Since a significant portion of SARS‐CoV‐2 transmission has been attributed to presymptomatic and asymptomatic carriers, 56 , 57 , 58 who may transmit the virus before symptoms develop or may never develop symptoms, we focused on particles that are expelled when an infectious person is speaking, as opposed to transmission through coughing and sneezing. We quantified the risk of initial infection during a 1‐h conversation as a function of distance between the infectious and the susceptible person, assuming that the infectious person is speaking continuously. To quantify uncertainty in transmission risk stemming from uncertainty in input parameters, we analyzed an ensemble of 10 000 simulations. First, we focus on an example scenario to illustrate how an infectious person influences virion concentrations within an indoor space.

3.1. Spatial variation in virion concentrations

A person shedding SARS‐CoV‐2 virions affects the average virion concentration in a room, but they have a far greater impact on virion concentrations in the region directly in front of them, as shown for the example scenario in Figure 7. The overall concentration of virions, N v, is the sum over the concentration of virions associated with each quadrature point, N v,i for i = 1,…, N quad (see Figure 4). Since this example scenario represents a well‐ventilated space (five air changes per hour), the virion concentration far from the infectious person is relatively low (approximately one virion per m3). However, virion concentrations are orders of magnitude greater directly downwind of the infectious individual than in the rest of the room. A susceptible person standing in the expiratory jet of an infectious person will be exposed to a large concentration of virions, even if they are in a well‐ventilated space.

To identify the particle size ranges that are most important for virion transmission near and far from an infectious individual, we quantified the contribution of each quadrature point to the overall virion concentration, shown as a function of downwind distance (y = y 0, z = z 0) in Figure 8. Virions tend to be concentrated in the fine (b‐ and l‐mode) particles rather than the coarse (o‐mode) particles, regardless of the distance between the infectious and susceptible individual. In this scenario, the contribution of virions in o‐mode particles drops to negligible values beyond 0.5 m from the infectious person, reflecting the general pattern that the large o‐mode particles quickly fall to the ground. On the other hand, the long residence times of b‐ and l‐mode particles allow them to affect virion concentrations elsewhere in the well‐mixed room, albeit in lower concentrations than in the expiratory jet of an infectious person, and to persist much longer within the jet itself. This near‐field enhancement in airborne transmission from these fine particles in the b‐ and l‐modes extends much farther than the reach of the larger o‐mode particles.

FIGURE 8.

FIGURE 8

Number concentration of virions N v, i associated with each quadrature point i = 1,…, N quad. The values shown here correspond to a slice at z = 0 in Figure 4, and the values at x = 0 scale with the weights in Figure 2c.

3.2. Near‐field enhancement in the risk of airborne transmission

For the full ensemble of 10 000 simulations, the absolute risk of initial infection is shown as a function of distance downwind of an infectious person (y = y0 , z = z 0) in Figure 9a. The risk of an initial infection after an encounter with an infectious individual is orders of magnitudes higher when directly downwind of the infectious individual than the average risk within the room. At any location, the risk of infection varies by over two orders of magnitude, due to the inherent variability in the parameters governing transmission. We caution that while this model is useful for comparing risk, predictions of absolute risk of initial infection (Figure 9a) depend strongly on the assumed distribution in input parameters, many of which are poorly constrained.

FIGURE 9.

FIGURE 9

The median (orange line), quartiles (boxes), and 95% confidence intervals (whiskers) for (A) the absolute risk of initial infection and (B) enhancement in transmission risk relative to the risk in a well‐mixed room. Each quantity is shown as a function of distance at which a susceptible person is standing downwind from an infectious individual. Across cases, we find wide variability in (C) distance wherein near‐field enhancements strongly impact transmission; we define this threshold distance as the distance at which local enhancements account for 5% of total transmission. All cases represent a person speaking at a medium volume for 1 h.

At distances greater than three meters, the risk of initial infection by the susceptible person is equal to risk in a well‐mixed room (assuming uniform concentration), whereas the risk of infection is orders of magnitude greater if the infectious and susceptible person are in a close, face‐to‐face conversation (0.5 m distancing). This enhancement in near‐field risk is shown in Figure 9b. Once the susceptible person moves beyond three meters from the infectious person, they avoid the near‐field increases in virion concentrations and transmission is, thus, governed by the far‐field concentration. The simulated far‐field concentrations are approximately the same as the concentration within a well‐mixed room, reflected by values near unity for distances beyond three meters downwind in Figure 9b.

3.3. Minimum distancing to avoid near‐field enhancement in risk

To quantify the distance that one needs to remain from a potentially infectious person to avoid near‐field enhancements in risk, we identified the distance at which the near‐field impact drops below 5% of total transmission risk. Within this distance, local enhancements in virion concentrations increase transmission risk by more than 5%. We find that this threshold distance, x near, varies between one meter to four meters, suggesting large variability in near‐field effects. In more than 50% of cases, we find x near is greater than the common recommendation of two meters (≈ six feet).

To identify the model parameters that drive variability in x near, we applied the Delta Moment‐Independent Measure 59 within the Sensitivity Analysis in Python (https://salib.readthedocs.io/en/latest/). The sensitivity index for each input parameter quantifies the fractional reduction in the variance of x near if the uncertainty in that parameter is eliminated. Across simulations, variability in x near is driven predominantly by variability in u 0, the velocity at which particles are expelled, with a sensitivity index of 0.9. On the other hand, the most poorly constrained parameters, such as the rate of viral shedding and parameters governing the immune response in the new host, did not strongly affect variability in x near. Whereas the distribution in u 0 applied in this study represents an infectious person who is speaking at normal volume, the value of u 0 will be greater for a person who is sneezing, coughing, or speaking at a louder volume. For these events, we would then expect enhanced near‐field transmission beyond the range of x near shown in Figure 9c.

4. DISCUSSION

Since the risk of airborne transmission is strongly enhanced near infectious individuals, maintaining distance from those outside one's household is a highly effective measure for reducing the spread of airborne pathogens. This suggests that the distancing guidelines that were originally designed to reduce the spread of SARS‐CoV‐2 through large droplets are also effective in reducing airborne transmission of small aerosol particles, which may remain suspended for hours but are most concentrated in the expiratory jet of an infectious person. However, we also showed that near‐field enhancements in airborne transmission extend farther than the travel distance of large droplets, suggesting that larger distances may be needed to avoid the elevation in airborne virions near an infectious individual.

If a susceptible person moves far enough away, they can avoid the local increase in virion concentrations within the infectious person's expiratory jet. At these long‐range distances, airborne transmission is governed by far‐field concentrations. The far‐field concentration of airborne virions depends strongly on the ventilation rate and the duration of the encounter, such that far‐field virion concentrations may be greater than reported here if the infectious person remains in a poorly ventilated space for longer than the 1‐hour encounter considered here. In this study, we also neglect variability in air circulation within the room, which may lead to “dead zones” where particles may accumulate.

The simulations presented in this paper revealed that the elevated risk due to local increases in the virion concentration often extends beyond the typical two‐meter (approximately six‐foot) distancing guidelines, which we found was driven by variability in the expiration velocity. Consequently, near‐field impacts will extend even farther than shown in this study if the infectious person speaks loudly, sings, or even breathes heavily while exercising, as these activities expel particles at higher velocities than conversational speech. On the other hand, if the infectious person is wearing a mask, they will expel particles at a lower velocity than if they are unmasked, 60 reducing the horizontal extent of their near‐field influence. This dependence on expiration velocity may help explain the similarity in infection rates among schools with 1 m and 2 m distancing between masked and unmasked students observed by an van den Berg. our findings suggest that the horizontal extent of near‐field effects will extend farther for unmasked students than for masked students due to differences in expiration velocities.

5. CONCLUSIONS

This paper describes the Quadrature‐based model of Respiratory Aerosol and Droplets (QuaRAD) for simulating the evolution of respiratory particles and its application to simulate near‐field transmission of airborne viruses. We showed that the risk of airborne transmission is elevated by orders of magnitude in the expiratory jet of the infectious person. The horizontal extent of this near‐field increase in transmission risk was highly variable among simulations, and this variability was controlled by the velocity of the expired particles.

Since the risk of airborne transmission is strongly enhanced near infectious individuals, maintaining distance from those outside one's household is a highly effective measure for reducing the spread of airborne pathogens. If a susceptible person moves far enough away, they can avoid the local increase in virion concentrations within the infectious person's expiratory jet, and the elevated risk due to local increases in the virion concentration often extend beyond the typical two‐meter (six‐foot) distancing guidelines. These near‐field impacts will extend even farther if the infectious person speaks loudly, sings, or even breathes heavily while exercising, as these activities expel particles at a higher velocities than conversational speech. On the other hand, if the infectious person is wearing a mask, they will expel particles at a slower velocity than if they are unmasked, 60 reducing the horizontal extent of their near‐field influence.

In general, we found tremendous variability of predicted transmission risk during any given encounter due to the inherent variability in physiological properties of the infectious and susceptible individuals and in room conditions. To avoid the near‐field enhancements in airborne exposure, more than two meters of distance should be maintained. For situations in which distancing is not possible, such as interactions between healthcare workers and patients, it is important to provide protective equipment against airborne transmission, such as N95 respirators.

CONFLICT OF INTEREST

The authors declare no conflicts of interest.

PEER REVIEW

The peer review history for this article is available at https://publons.com/publon/10.1111/ina.12900.

ACKNOWLEDGEMENTS

This research was supported by the DOE Office of Science through the National Virtual Biotechnology Laboratory, a consortium of DOE national laboratories focused on response to COVID‐19, with funding provided by the Coronavirus CARES Act. We thank Michael Dillon, Robert McGraw, and Ernie Lewis for providing helpful feedback. This project was also supported in part by the U.S. Department of Energy through the Office of Science, Office of Workforce Development for Teachers and Scientists (WDTS) under the Science Undergraduate Laboratory Internships Program (SULI) and the Environmental and Climate Sciences Department under the BNL Supplemental Undergraduate Research Program (SURP). The quadrature‐based model was originally developed for simulation of atmospheric aerosol with support from the DOE Atmospheric System Research program at Brookhaven National Laboratory, a multiprogram national laboratory supported by DOE Contract DE‐SC0012704.

APPENDIX A.

QUADRATURE OPTIMIZATION

The size distribution of respiratory particles is represented in QuaRAD using a total of six quadrature points—1‐point, 3‐point, and 2‐point Gauss‐Hermite quadrature for the b‐, l‐, and o‐modes, respectively. We find that further increases in the number of quadrature points did not improve predictions; this is shown through comparison between the 6‐point QuaRAD representation (blacked dashed line in Figure A1) and the same simulations but using 600 quadrature points (green line). On the other hand, if we use only one quadrature point for each of the b‐, l‐, and o‐modes (teal line), we find the model accuracy decreases.

VERIFICATION AGAINST ESTABLISHED MONTE CARLO MODEL

We verified particle dispersion simulated by QuaRAD through comparison with the DRW model from Wei and Li. 29 For each particle size, the DRW tracks the evolution of thousands of Monte Carlo particles. Instantaneous snap shots of particles simulated by DRW are compared with the steady‐state solution from the jet‐puff model (Section 2.3) in Figure A2. The top, middle, and center panels in Figure A2 show predictions for particles of diameter D p = 10 μm, D p = 50 μm, and D p = 100 μm, respectively. In order to compare with the DRW simulations, evaporation and buoyancy were neglected in QuaRAD, and the particle expiration rate was adjusted to 33 particles per second. The steady‐state concentration profiles simulated with QuaRAD agree with the DRW model (Figure A2), particularly in the cases of 10 and 100 μm particles, given the predominance of particles smaller than 10 μm in the b‐ and l‐modes and larger than 100 μm in the o‐mode, these sizes are the most relevant to the dispersion dynamics in QuaRAD. In the case of the 50 μm particles, the centerline trajectory is similar between the DRW and QuaRAD, but the DRW model predicts greater spread about the centerline, likely resulting from the simplification in QuaRAD that b increases linearly with the centerline distance s. As particles smaller than 10 μm or larger than 100 μm account for the overwhelming majority of expired respiratory particles, QuaRAD is able to capture the dispersion dynamics most relevant for airborne transmission.

FIGURE A1.

FIGURE A1

Comparison between optimized quadrature approximation applied in QuaRAD (six points, dashed line) and the same simulation if more quadrature points are used than needed (600 points, green line) or if not enough quadrature points are used (three points, teal line)

FIGURE A2.

FIGURE A2

Comparison between particle concentrations predicted by QuaRAD using three quadrature points (color plot) and instantaneous particle distributions predicted by a DRW model tracking 50 000 particles (scatter plot) 29 under the following conditions: D p = 10 μm, D p = 50 μm, and D p = 100 μm; 33 particles expelled per second in each case, u 0 = 10 m/s, T v,∞ = 298.15 K, T 0 = 308.25 K, and S 0 = 1

Fierce L, Robey AJ, Hamilton C. Simulating near‐field enhancement in transmission of airborne viruses with a quadrature‐based model. Indoor Air. 2021;31:1843–1859. 10.1111/ina.12900

1. DATA AVAILABILITY STATEMENT

The QuaRAD source code, input files, and processing script are available for download at: https://github.com/lfierce2/QuaRAD/. Simulation ensembles were created using latin hypercube sampling with pyDOE: https://pythonhosted.org/pyDOE/. The sensitivity analysis was performed using the Sensitivity Analysis Library in Python, which is available at: https://salib.readthedocs.io/en/latest/.

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Availability Statement

The QuaRAD source code, input files, and processing script are available for download at: https://github.com/lfierce2/QuaRAD/. Simulation ensembles were created using latin hypercube sampling with pyDOE: https://pythonhosted.org/pyDOE/. The sensitivity analysis was performed using the Sensitivity Analysis Library in Python, which is available at: https://salib.readthedocs.io/en/latest/.


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