^{1}School of Civil and Construction Engineering, Oregon State University, Corvallis, OR, United States^{2}Department of Naval Architecture and Ocean Engineering, United States Naval Academy, Annapolis, MD, United States

This study investigates the potential of a *Rhizophora* mangrove forest of moderate cross-shore thickness to attenuate wave heights using an idealized prototype-scale physical model constructed in a 104 m long wave flume. An 18 m long cross-shore transect of an idealized red mangrove forest based on the trunk-prop root system was constructed in the flume. Two cases with forest densities of 0.75 and 0.375 stems/m^{2} and a third baseline case with no mangroves were considered. LiDAR was used to quantify the projected area per unit height and to estimate the effective diameter of the system. The methodology was accurate to within 2% of the known stem diameters and 10% of the known prop root diameters. Random and regular wave conditions seaward, throughout, and inland of the forest were measured to determine wave height decay rates and drag coefficients for relative water depths ranging 0.36 to 1.44. Wave height decay rates ranged 0.008–0.021 m^{–1} for the high-density cases and 0.004–0.010 m^{–1} for the low-density cases and were found to be a function of water depth. Doubling the forest density increased the decay rate by a factor two, consistent with previous studies for other types of emergent vegetation. Drag coefficients ranged 0.4–3.8, and were found to be dependent on the Reynolds number. Uncertainty in the estimates of the drag coefficient due to the measured projected area and measured wave attenuation was quantified and found to have average combined standard deviations of 0.58 and 0.56 for random and regular waves, respectively. Two previous reduced-scale studies of wave attenuation by mangroves compared well with the present study when their Reynolds numbers were re-scaled by *λ ^{3/}*

^{2}where λ is the prototype-to-model geometric scale ratio. Using the combined data sets, an equation is proposed to estimate the drag coefficient for a

*Rhizophora*mangrove forest:

*C*

_{D}= 0.6 + 3e04/

*Re*

_{DBH}with an uncertainty of 0.69 over the range 5e03 <

*Re*

_{DBH}< 1.9e05, where

*Re*

_{DBH}is based on the tree diameter at breast height. These results may improve engineering guidance for the use of mangroves and other emergent vegetation in coastal wave attenuation.

## Introduction

As coastal communities search for effective, resilient adaptation strategies to coastal hazards including sea level rise, erosion, and storm-driven wave and surge events, natural and nature-based systems have gained attention for their ecological, social, and engineering benefits. In particular, emergent vegetation such as mangroves in subtropical and tropical regions have been lauded for their ability to sequester carbon (Alongi, 2008), improve water quality (Struve and Falconer, 2001; Wang et al., 2010), provide habitat for shorebirds, juvenile fish, and other species (Odum et al., 1982; USFWS, 1999), supply resources and opportunities for recreation and tourism (Situmorang, 2018; Spalding and Parrett, 2019), and provide engineering services including shoreline stabilization (Pennings et al., 2021), wave attenuation (Mazda et al., 1997a,2006; Kibler et al., 2019) and damage mitigation during tsunami or tropical cyclone events (Danielsen et al., 2005; Das and Vincent, 2009; Krauss et al., 2009; Goda et al., 2019; Tomiczek et al., 2020a; Zhu et al., 2020). Observations of these services have led to an exponential increase in interest in natural and nature-based solutions in academic publications (UNDRR, 2021) and have engendered national and global initiatives for integrating natural and nature-based systems into conventional infrastructure. Several organizations including the United States Army Corps of Engineers (Bridges et al., 2015), Environmental Defense Fund (Cunniff and Schwartz, 2015), Federal Highways Administration (Webb et al., 2019), World Association for Waterborne Transport Infrastructure (PIANC, 2018), European Commission (Science for Environmental Policy, 2021), United Nations (UNDRR, 2020, 2021), and World Bank (Browder et al., 2019) have supported implementation, monitoring, and research of natural infrastructure to facilitate development of design guidelines for utilizing these systems.

While the benefits of natural infrastructure systems are increasingly documented, uncertainty remains about the effects of these systems on engineering performance metrics such as wave height attenuation, load mitigation, or overtopping reduction, and on parameters including uncertainty required for design. The uniqueness, natural variability, and inconsistent characterization of natural systems create challenges in predicting their performance, ultimately leading to a lack of rigorous engineering standards for widespread implementation (Browder et al., 2019; UNDRR, 2021). Therefore, a robust characterization and a greater understanding of wave interaction with natural and nature-based infrastructure are required in order to develop rigorous design guidance for these systems. This paper addresses these knowledge gaps through a prototype-scale physical model investigation of wave attenuation through a *Rhizophora* sp. forest of moderate (18 m) cross-shore width to quantify relationships between incident conditions, wave height decay, and associated uncertainties. The next section presents details of the specimen, which was designed based on field measurements of the *Rhizophora* sp., as well as experimental configurations tested. Hydrodynamic conditions considered in this study are then detailed. A practical methodology is then described to determine the projected area of a mangrove forest using LiDAR scanning that captures the added complexity of the intertwined root structure. The method also allows for cross-sections to be selected at intermediate points within the mangrove forest, which can then be analyzed to estimate the average projected area and associated uncertainty for the entire model forest. The following section presents calculated wave decay and drag coefficients, which include the projected area uncertainty and hydrodynamic uncertainty. Results from two reduced-scale experiments published previously are used to verify a Reynolds scaling relationship that allows for future comparison with reduced-scale models. Using the combined three data sets, a general equation is proposed to estimate the drag coefficient as a function of the Reynolds number for a *Rhizophora* mangrove forest.

### Previous Studies of Wave Height Attenuation Through Emergent Vegetation

Previous studies have investigated the effects of emergent vegetation on wave attenuation through theoretical, field, computational, and physical model investigations. Theoretical equations posed by the National Academy of Sciences (1977), Dalrymple et al. (1984), and Mendez and Losada (2004), among others, have related wave height decay to incident wave conditions, vegetation characteristics, and an empirical drag coefficient, *C*_{D}, specific to the vegetation. The equations proposed initially by National Academy of Sciences (1977) assumed linear wave theory and shallow-water wave conditions. These equations were extended by Dalrymple et al. (1984) for intermediate and deep-water wave conditions. In their formulation, the transmitted wave height, *H*_{t}, normalized by the incident wave height, *H*_{i}, is a function of the cross-shore distance of vegetation, *x*, through which the wave propagates, given by

where α is the wave height decay coefficient expressed as

where $\overline{{A}_{t}}$ is the mean projected area per unit height per tree, *N* is the number of vegetation elements per unit area, *h* is the water depth, *d* is the mean wetted height of the vegetation, *k* is the wave number (2π/*L*), and *L* is the wavelength. Mendez and Losada (2004) later extended the equation of Dalrymple et al. (1984) for random waves, assuming a Rayleigh distribution and considering peak wavenumber *k*_{p} associated with the peak period *T*_{p} and the incident and transmitted root-mean-squared wave heights, *H*_{rms,i} and *H*_{rms,t}, respectively. The wave height decay coefficient for random waves, $\stackrel{~}{\mathrm{\alpha}}$, is given as

Equations (1) and (3) have been used extensively to model wave height attenuation by vegetation. The quantification of *C*_{D}, $\overline{{A}_{t}}$, $\stackrel{~}{\mathrm{\alpha}}$ and related uncertainties for a mangrove forest are the focus of this investigation.

Field studies have measured wave height attenuation through mangroves for wind waves, reporting wave height attenuation rates ranging 0.002–0.012 m^{–1} (Mazda et al., 1997a; Quartel et al., 2007; Bao, 2011; Horstman et al., 2014), boat wakes (La et al., 2015; Ismail et al., 2017; Thuy et al., 2017). Similar studies considering storm surge and tidal currents have shown that mangroves can build the substrate and mitigate inland flooding over larger spatial scales (Furukawa et al., 1997; Mazda et al., 1997b; Krauss et al., 2009; Montgomery et al., 2018). Numerical simulations have further investigated wave interaction with vegetation by modeling separately energy dissipation terms and expanding analyses to conditions not observed in the field or physical models (Zhang et al., 2012; Guannel et al., 2015; Maza et al., 2015; Narayan et al., 2016; Chella et al., 2020; Niazi et al., 2021). Physical models investigating wave propagation through live vegetation (Ozeren et al., 2014) or vegetation mimics (Augustin et al., 2009; Anderson and Smith, 2014; Ozeren et al., 2014; Wu and Cox, 2015, 2016) have identified relationships between *C*_{D} and parameters including the Reynolds number, *Re*, and Keulegan–Carpenter number, *KC*.

Several physical modeling studies have focused on mangroves of the *Rhizophora* genus to investigate wave attenuation by the species’ complex trunk-aerial prop root system (Strusińska-Correia et al., 2014; Zhang et al., 2015; Maza et al., 2017, 2019; Chang et al., 2019; Tomiczek et al., 2020b). Chang et al. (2019) constructed a 1:7-geometric scale physical model based on 3D scan measurements of a 19-year old tree in Vietnam and estimated drag and inertial coefficients for regular wave conditions. The authors presented relationships between the drag coefficient and Reynolds number and Keulegan–Carpenter number, as well as between the inertial coefficient and the Keulegan–Carpenter number. Maza et al. (2017) used a parameterized model of the *Rhizophora* proposed by Ohira et al. (2013) to construct a 1:12-scale forest to investigate turbulent kinetic energy and *C*_{D} values for unidirectional flow. The authors quantified uncertainty in the drag coefficient due to the estimation of the projected area. Later, Maza et al. (2019) used the same model at 1:6-scale to investigate wave attenuation and drag forces for regular and random waves, presenting *C*_{D} as a function of the Reynolds number calculated using the depth-averaged velocity and equivalent mean diameter. Strusińska-Correia et al. (2014) considered interaction of solitary waves and tsunami bores with mangrove forest models constructed at a geometric scale of 1:20 and reported tsunami transmission rates of 20% through the forest models. Similarly, Tomiczek et al. (2020b) used a 1:16-scale model of a *Rhizophora* mangrove forest sheltering an idealized urban array to show that mangrove forests of moderate cross-shore width caused cross-shore force reductions of 11–65% on sheltered structures for transient wave conditions compared to the baseline configuration. Zhang et al. (2015) considered interaction of unidirectional flow with a 1:7.5-scale model to estimate turbulent kinetic energy and drag coefficients and found that measured drag coefficients were consistent with values reported in previous field studies.

Many previous studies have advanced the understanding of wave attenuation through emergent vegetation by presenting relationships between incident hydrodynamic conditions, forest configurations and wave height decay. However, several issues should be addressed to increase wide-spread adoption of these systems in coastal engineering design. Few field studies presented their results in terms of a drag coefficient (Mazda et al., 1997b; Quartel et al., 2007; La et al., 2015), in part owing to the difficulty in separating the effects of the mangrove forest from other wave attenuation processes such as bottom friction, substrate percolation, and wave breaking (Horstman et al., 2014). The accuracy of computational models depends on accurate parameterization of the vegetation, such as the projected area and drag coefficient (Guannel et al., 2015). While several physical model studies have suggested relationships between *C*_{D} and *Re* (e.g., Chang et al., 2019; Maza et al., 2019), questions arise about interpretation of these values, because Reynolds similitude cannot be maintained when Froude similitude is achieved in reduced-scale tests. Furthermore, uncertainty owing to the determination of the projected area as well as the measurement of wave height decay propagate into the uncertainty in the drag coefficient. These uncertainties must be quantified and aggregated to improve confidence in a system’s performance and to allow, for example, a reliability analysis consistent with other types of engineered coastal structures (e.g., Burcharth, 1997; Goda and Takagi, 2000). This study addresses these questions through a prototype-scale physical model investigation of wave transformation through a fringe *Rhizophora* forest, in which the complex, overlapping system of above-ground prop roots (Figure 1a) causes energy dissipation.

**Figure 1.** **(a)** Intertwined trunk-prop root system of *R. mangle* in St. Lucie Inlet State Park, FL. **(b)** Physical model of *Rhizophora* sp. trunk-prop root system.

## Physical Model Setup

### Mangrove Specimen

The mimics were designed based on previous field measurements of *Rhizophora mangle* and other mangrove species at sites in Florida (Jimenez et al., 1985; Dawes et al., 1999; Novitzky, 2010) and the Caribbean (Jimenez et al., 1985; Loría-Naranjo et al., 2014). Reported diameters at breast height *D*_{BH} ranged from 0.056 to 0.176 m, with a maximum *D*_{BH} of approximately 0.10 m at many sites. Reported forest densities ranged from 0.112 to 2.02 stems/m^{2} (Jimenez et al., 1985; Dawes et al., 1999; Novitzky, 2010; Loría-Naranjo et al., 2014). These reported parameters are similar to those reported for *Rhizophora* sp. sites in India (Danielsen et al., 2005), Vietnam (Bao, 2011), and Malaysia (Ong et al., 1995), although unique sites exhibit variability in both *D*_{BH} and stem density. For the present study, a nominal value of *D _{BH}* = 0.1 m and two tree densities, 0.75 trees/m

^{2}and 0.375 trees/m

^{2}were selected to model a mature mangrove forest.

Methods have been proposed to parameterize emergent vegetation including wetland plants (Feagin et al., 2011; Liu et al., 2021; Niazi et al., 2021) and specifically the trunk-prop root system of the *Rhizophora* genus (Ohira et al., 2013; Niazi et al., 2021). The model of Ohira et al. (2013) was used as the basis of the design of the idealized mangrove tree for this study because it was the basis of previous laboratory studies (Maza et al., 2017, 2019; Tomiczek et al., 2020b) and an ongoing study at another laboratory (Tomiczek et al., 2021) and would facilitate comparisons of the results. Commercially available polyvinyl chloride (PVC) pipe with an outside diameter of 0.1143 m was used for the trunk, resulting in *D*_{BH} = 0.1143 m. Following Ohira et al. (2013) yielded a representative model tree with 14 roots and a mean root diameter, *D _{Root}*, of 0.0286 m with the tallest root,

*H*, located 1.35 m from the ground. The maximum horizontal extent of the tallest root,

_{Rmax}*X*, was 2.10 m from the base of the model tree. This parameterization was modified for constructability (Tomiczek et al., 2020b), with seven root pairs (i.e., duplicate roots on either side of the tree); the vertical position above ground,

_{Rmax}*H*, maximum root spreading distance,

_{Ri}*X*

_{Ri}, and orientation, θ, (relative to the lowest root pair) for each root are listed in Appendix Table A1. Commercially available cross-linked polyethylene (PEX) with an outside diameter of 0.0286 m was used for the prop roots (Figure 1b).

### Bathymetry, Instrumentation, and Test Configurations

The mangrove specimens were installed in the 104 m long × 3.66 m wide Large Wave Flume (LWF) at Oregon State University (OSU) as shown in Figure 2. A piston-type wavemaker was located at the far end of the flume for wave generation. An 18 m long constant-depth section was followed by a piecewise continuous, impermeable bathymetry constructed using 3.6 m by 3.6 m concrete slabs at predetermined locations (termed “bays”) numbered 1–22 in Figure 2. The bathymetry started with a 7 m long 1:12 slope, led to a second 35 m long constant-depth section, and ended with a second 1:12 slope for energy dissipation. The 18 m long mangrove forest was placed on the second constant depth section, set back 11 m from the crest of the first 1:12 slope to minimize effects of wave transformation to the test section.

**Figure 2.** **(a)** Profile view of flume showing bathymetry, location of mangrove forest, and numbered bays 1–22. **(b)** Detail profile view of horizontal test section between bays 5–15 showing instrumentation locations in test section.

Figures 2a,b show the locations of instrumentation used during experiments. The seaward-most wave gage (WG1) was positioned at the onset of the foreshore slope, and the landward-most wave gage (WG13) was positioned near the start of the beach to record wave conditions before and after propagating through the test section. Within the forest test section (Figure 2b), a total of 13 wire-resistance wave gages (WG), 6 PDCR 1830 pressure gages (PD18), 6 ultrasonic wave gages (USWG), 3 RBR solo3D pressure loggers, and 6 acoustic-Doppler velocimeters (ADV) were installed to measure hydrodynamic conditions in front of, within, and leeward of the mangrove forest. All WGs, PD18s, USWGs, and ADVs were synchronized to the start of the wavemaker displacement time series and sampled at a rate of 100 Hz. Measured water levels by PD18s were corrected to the free surface accounting for dynamic wave pressure attenuation with depth.

Figure 3a shows a plan view of the LWF. Three configurations were tested for this study: a baseline configuration (BL) with no mangroves to determine the wave attenuation due to bottom and sidewalls and two configurations with a high-density (HD, 0.75 stems/m^{2}, Figure 3b) and low-density (LD, 0.375 stems/m^{2}, Figure 3c) mangrove forest. When installing the trees (Figure 4a), roots of mangrove specimens that were positioned in locations where their horizontal spreading would intersect the flume walls were precut to account for the flume walls. The model trees were then secured to bases in the test section. A 0.076 m thick concrete cap was used to secure the root ends of the model trees.

**Figure 3.** **(a)** Plan view of large wave flume showing baseline (BL) configuration. **(b,c)** Detailed view of mangrove test section showing mangrove locations in **(b)** high-density (HD) and **(c)** low-density (LD) configurations.

**Figure 4.** **(a)** Construction of the model mangrove test section, high-density (HD) configuration; view toward wavemaker with **(b)** high-density (HD) mangrove configuration, *h _{v}* = 0.73 m,

*H*= 0.19 m,

_{mo}*T*= 4.82 s, and

_{p}**(c)**low-density (LD) mangrove configuration,

*h*= 1.85 m,

_{v}*H*= 0.73 m,

_{mo}*T*= 7.45 s.

_{p}As seen in Figure 3b, the specimens were positioned in a staggered arrangement for the HD configuration, similar to many previous laboratory studies that used artificial vegetation. By nature of the construction, mangrove specimens were removed from the HD configuration to create the LD configuration. To avoid introducing circulation or cross-mode effects into the model owing to positioning of the specimens, mangroves were selected for removal such that the number of specimens in each 3.66 m by 3.66 m section was reduced from 10 to 5 and such that each cross-shore row (spaced regularly in the alongshore*-*direction) had a total of 5 trees. This procedure resulted in a non-uniform positioning of specimens for the LD configuration. While forces on individual stems can vary from uniform to random arrangements, idealized and random arrangements have been shown numerically to produce comparable results for overall wave height attenuation (Maza et al., 2015).

## Hydrodynamic Conditions

Random and regular waves were generated for the HD, LD, and BL configurations to assess wave attenuation and load reduction by the model mangrove forest (Kelty et al., 2021). Photographs of the HD configuration construction and waves interacting with the HD and LD configurations are shown in Figures 4a–c, respectively. Table 1 lists the wave conditions measured at the seaward-most pressure gage in the mangrove forest section (PD18-1), including water depth at the vegetation *h _{v}*, significant wave height

*H*, peak period

_{m0}*T*

_{p}and wavelength

*L*

_{p}calculated using the peak period. Wave conditions were selected such that three non-dimensional cases of relative wave height

*H*and relative water depth

_{mo}/h_{v}*k*were considered for random waves and six non-dimensional cases of relative wave height

_{p}h_{v}*H/h*and relative water depth

_{v}*kh*were considered for regular waves across varying water depths, wave periods, and wave heights. For random waves, dimensionless ratios of water depth at the vegetation to wavelength (

*h*), significant wave height to water depth (

_{v}/L_{p}*H*), vegetation cross-shore length,

_{m0}/h_{v}*L*, to wavelength (

_{veg}*L*) and wavelength to flume width,

_{veg}/L_{p}*W*, (

*L*) are also presented in Table 1. Hydrodynamic conditions for regular wave cases are listed in Appendix Table A2.

_{p}/WA range of wave conditions were run initially at three water depths at the vegetation test section (*h*_{v} = 1.85 m, 1.03 m, 0.73 m) for the HD, LD, and BL configurations. A fourth water depth (*h*_{v} = 1.48 m) was added for the LD and BL configurations because of additional availability of the facility, but it was not possible to repeat the HD configuration at *h*_{v} = 1.48 m. In general, the significant wave height, *H*_{m0}, and peak period, *T*_{p}, were chosen for a given water depth *h*_{v} to correspond to non-dimensional values of *H _{m0}/h_{v}* = 0.18 or 0.36 and

*h*= 0.06 or 0.11 or 0.22. The purpose was to choose large waves so that the wave decay could be measured accurately, but not so large to avoid depth-limited and steepness-limited wave breaking, ensuring that the primary dissipation mechanisms were due to the wave interaction with the mangroves and due to the side wall and bottom friction. For each trial, 300 individual waves were generated using a JONSWAP spectrum with γ = 3.3.

_{v}/L_{p}## Projected Area

The total projected area in the direction of flow is essential to estimating the drag coefficient via the Dalrymple et al. (1984) and Mendez and Losada (2004) formulations. For simple geometries such as vertical rods, the estimation is relatively straightforward. However, estimating the projected area of the complex aerial root structures associated with *Rhizophora* sp. is more involved. Previous studies have utilized photogrammetry in the field (Zhang et al., 2015) and laboratory (Maza et al., 2017, 2019), or 3D laser scanning (Chang et al., 2019) to derive the projected area of a single tree specimen. For fringing mangrove forests, roots of neighboring trees may overlap, creating a dense network (Figure 1). The intertwined root system alters the projected area seen per tree and thus calls for a practical methodology that can extract the projected area of these complex root systems, yet allow for comparison on a per-tree basis.

The HD and LD forests were scanned using a LiDAR system (BLK 360, Leica-Geosystems). The time-of-flight unit used a range 1 laser with a wavelength of 830 nm, and had a 360° and 300° field of view in the horizontal and vertical, respectively. The scanner was equipped with a 15 Mpixel 3-camera system and a 150 Mpixel full-dome capture for high dynamic range (HDR) and light emitting diode (LED) flash calibrated spherical images. For both configurations, seven overhead scans of the forest were taken, with the LiDAR scanner mounted above the test section. Scans were performed at the midpoint of bays numbered 7 – 14 (see Figure 2a). Figure 5 shows an example of the process for scanning the forest and analyzing the LiDAR images for the HD configuration.

**Figure 5.** **(a)** Head-on photograph of HD model forest. **(b)** Scanned LiDAR image. **(c)** Extracted stencil showing measurements of trunk and prop roots. **(d)** Pixelated image for calculating projected area per unit height.

The HD and LD model forest LiDAR scans (Figure 5b) were transferred from the LiDAR scanner and registered using a proprietary software (Cyclone, Leica-Geosystems) to relate multiple scans on a common coordinate system. An alongshore *Y-Z* cut plane was established at the seaward boundary of the forest section. For the LD configuration, a stencil of 2.0 m cross-shore width (repeating pattern of trees) was identified within the forest to comprise two rows of model specimens, and seven stencils were extracted from bays 10–13. For the HD configuration, five stencils of 2.0 m cross-shore width were extracted from bays 10–13, which were then split into ten half stencils of 1.0 m cross-shore width to minimize under-prediction of the projected area due to root overlap. Extracted stencils and half stencils were manually cleaned for scatter and drift points. Manual measurements of the trunk and root diameters of the first extracted HD stencil (Figure 5c) were taken and compared to the known values of *D*_{BH} = 0.1143 m and *D*_{Root} = 0.0286 m. The LiDAR measurements underestimated the trunk and root diameter by 2 and 10%, respectively.

The cleaned stencils were then rasterized to create a 1 cm × 1 cm pixelated image of the LiDAR cross section (Figure 5d). Image analysis tools (Matlab R2017) were then used to discretize the pixelated image into horizontal slices of 1 cm height. The projected area was calculated by counting the number of pixels in every horizontal slice and multiplying by the dimensions of one cell (1 cm × 1 cm). The projected area per unit height, *A*, was then determined by dividing the projected area by the height of the horizontal slice. To check for bias in view direction (landward or seaward), a HD half stencil cross-section was rotated 180° around the *z*-axis. Its projected area per unit height was compared to that of the original cross-section, and the average variance was negligible. Therefore, the analysis method was not impacted by the direction (landward or seaward) that the cross-section was analyzed. An average was taken of the projected area per unit height for all of the HD and LD model forest stencils to create the representative mean profile and quantify uncertainty of the HD or LD model forest projected area. The mean profiles were divided by the mean number of trees in the analyzed cross-sections to allow for the mean projected area per unit height of the HD and LD model forests to be compared on a per tree basis, *A*_{t}. On a per-tree basis, the profiles of the HD mean half stencil and the LD mean stencil show good agreement: the HD mean half stencil’s projected area per unit height per tree was, on average, 1.4% smaller than the LD mean stencil for the root section (0 ≤ *h*_{v} ≤ 1.35 m), and 1.9% smaller for the trunk section (*h*_{v} > 1.35 m). The HD mean half stencil profile was used for further analysis in the study.

Extracting stencils at different cross-shore positions throughout the forest allowed for the determination of the uncertainty associated with the projected area, as shown in Figure 6. Figure 6a shows the mean projected area per unit height per tree for the HD half stencil (blue line, circles), determined by taking the mean projected area of the ten half-stencils of the HD forest. Horizontal lines denote error bars (one standard deviation) for each 1 cm bin. The mean projected area per unit height per tree, $\overline{{A}_{t}}$, calculated by integrating the HD mean half stencil curve to each tested water level, is shown as a vertical solid black line with height equal to its respective water depth. As indicated in the figure, at the lowest two water depths (*h _{v}* = 0.73 m and

*h*

_{v}= 1.03 m), $\overline{{A}_{t}}$ values are similar; as water depth increases above the root structure, $\overline{{A}_{t}}$ decreases due to the influence of the trunks. The root section (0 ≤

*h*

_{v}≤ 1.35 m) exhibits greater variability in $\overline{{A}_{t}}$ for the measured projected area per unit height per tree than the trunk section (

*h*

_{v}> 1.35 m). The standard deviation at each bin was used to calculate a mean standard deviation, $\overline{{\mathrm{\sigma}}_{At}}$, of the mean projected area per unit height per tree, using the same integration routine for the $\overline{{A}_{t}}$ values. These parameters were used to calculate the drag coefficient,

*C*, and a range of uncertainty around

_{D}*C*

_{D}due to the variability of $\overline{{A}_{t}}$.

**Figure 6.** **(a)** Projected area per unit height per tree, *A*_{t}, versus the water depth at the vegetation, *h*_{v}, for the high-density (HD) mean half stencil. Error bars represent one standard deviation and vertical lines show mean projected area per unit height per tree, $\overline{{A}_{t}}$. **(b)** Comparison of the projected area per unit height per tree, *A*_{t}, for high-density (HD) mean half stencil (blue line and markers), prototype-scale Maza et al. (2019) (black line and markers), and prototype-scale Chang et al. (2019) (red line and markers) model tree profiles. Note change in *x-*axis scale from **(a)** to **(b)**.

The HD mean half stencil profile of the projected area per unit height per tree, *A*_{t}, was compared with those of the studies by Chang et al. (2019) and Maza et al. (2019) in Figure 6b, rescaling the model trees considered in each study to full-scale. Figure 6b shows elevation *z* on the *y-*axis and the projected area per unit height per tree, *A*_{t}, on the *x-*axis, with the prototype-scale specimens of the present study, Chang et al. (2019) and Maza et al. (2019) represented by blue, black, and red lines and markers, respectively. As seen in the figure, differences are observed between the specimens, because each study considered a model tree with a different root structure, trunk diameter, and thus overall projected area per unit height per tree, reflective of the natural variability in real-world *Rhizophora* systems. The present study shows a reduction in *A*_{t} at lower elevations, while the models of Chang et al. (2019) and Maza et al. (2019) consistently increase toward the base of the specimen. This difference may be owing to root overlap in the analyzed stencils causing underestimation of the per-tree projected area per unit height. The present study’s projected area per unit height per tree was generally between those of Chang et al. (2019) and Maza et al. (2019). However, the authors note that the comparison shown in Figure 6b is for the projected area per unit height on a per-tree basis. The three studies considered a range of stem densities during test conditions, which affected the overall blockage provided by the mangrove models.

In the constructed *Rhizophora* model, the trunk diameter is an order of magnitude larger than the root diameter. That difference affects how fluid flows around either the trunks or the roots, characterized by parameters such as the Reynolds number, *Re* and Keulegan–Carpenter number, *KC.* The effective diameter, *D*_{e} can be used to characterize the flow around the model trees by taking a weighted average of the trunk and root diameters. The effective diameter was calculated at each water level as

where $\overline{{n}_{R}}$ is the mean number of roots at each tested water level, determined though visual analysis. Table 2 presents the mean projected area per unit height per tree, standard deviation of mean projected area per unit height per tree, mean number of roots, and effective diameter for each water depth at the vegetation tested. In general, *D*_{e} values were consistent, ranging from 0.034 m at the lowest water level to 0.041 m at the highest water level.

## Wave Attenuation Rates and Drag Coefficients for Random Wave Trials

### Wave Attenuation Rates

The wave gage arrays positioned at Array 1 (seaward) and Array 2 (inland) of the mangrove forest (Figure 2b) were used to analyze the incident spectral estimate of the significant wave height, *H*_{m0,i}, and the reflected spectral estimate of the significant wave height, *H*_{m0,} using the methods proposed by Zelt and Skjelbreia (1993) and Gronbech et al. (1997). The total (incident plus reflected) spectral estimate of the significant wave height, *H _{m0}*, was used for the WGs and PD18s in the test section. An example of the cross-shore variation of

*H*

_{m0}with respect to the neutral position of the wavemaker (

*x*= 0 m) is shown in Figure 7 for WGs (blue circles) and PD18s (green diamonds) for wave case TI-h3-3, with

*h*

_{v}= 1.03 m,

*H*= 0.310 m, and

_{m0}*T*

_{p}= 3.10 s for the HD (dark colors), LD (intermediate colors), and BL (light colors) configurations. The incident (triangles) and reflected (squares) wave heights at WG arrays seaward and inland of the mangrove forest are also shown. At Array 2, the wave reflection from the 1:12 impermeable slope was estimated to be in the range 0.02 <

*H*0.03 m with an average reflection coefficient of 18% and standard deviation of 4%, which is close to the limits of this methodology. At Array 1, the reflected wave was slightly higher with an average reflection of 22% and standard deviation of 7%. This larger value could be due to reflection from the mangrove forest.

_{m0}<**Figure 7.** Total spectral estimate of the significant wave height with respect to *x*-location for WGs (blue circles) and PD18s (green diamonds) and the incident spectral estimate of the significant wave height (orange triangles), and reflected spectral estimate of the significant wave height (orange squares) for the high-density (dark colors), low-density (intermediate colors), and baseline (light colors) configurations for random wave case TI-h3-3, *h*_{v} = 1.03 m, *H*_{m0} = 0.310 m, *T*_{p} = 3.10 s.

The *H*_{m0} values from the pressure gages located in the start and end of the mangrove forest (PD18-1 and PD18-6) were similar to the mean *H*_{m0} values from Array 1 and 2, respectively. Therefore, the *H*_{m0} values from the pressure gages in the mangrove forest (PD18-1 to PD18-6, 35.9 m < *x* < 54.2 m) were used to fit wave height decay curves (solid line in Figure 7) for each case using Equation (1), using the least squares method and setting the *y-*intercept to the value of *H*_{m0} at PD18-1, returning a value of the decay rate, $\stackrel{~}{\mathrm{\alpha}}$. For all layouts, *H _{m0}* decreased landward and decay rate $\stackrel{~}{\mathrm{\alpha}}$ increased with forest density.

As seen in Figure 7, there was measurable wave height attenuation due to side wall and bottom friction in the baseline case. Therefore, the wave attenuation due to the mangrove forest, ${\stackrel{~}{\mathrm{\alpha}}}_{m}$, was calculated by subtracting $\stackrel{~}{\mathrm{\alpha}}$ of the BL configuration from those of the HD and LD configurations. Figure 8 shows ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ versus *h*_{v} for the HD (dark blue circles) and LD (intermediate blue circles) configurations for random wave trials. For both the HD and LD configurations, ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ is greatest at the shallowest water depths, where the mean projected area per unit height, $\overline{{A}_{t}},$ was the largest. The ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ coefficient decreases approximately linearly as water depth increases. The figure shows that ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ does not vary significantly between the different non-dimensional wave cases for each water depth, suggesting that ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ is predominantly dependent on the water depth at the vegetation, and subsequently, the mean projected area per unit height influencing the fluid flow. The average ratio of the ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ coefficients for the HD to LD configurations for a given water depth and wave condition was 2.0 for random waves, with a standard deviation of 0.12. This ratio is the same as the HD/LD forest density ratio of the mangrove forests, suggesting a linear relationship between the decay rate and forest density, similar to the relationship between the wave height decay coefficient and stem density was found for emergent vegetation by Anderson and Smith (2014).

**Figure 8.** Wave height decay coefficient, ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ versus the water depth at the vegetation, *h*_{v}, for random wave cases for the high-density (HD) (dark blue circles) and low-density (LD) (intermediate blue circles) configurations.

The uncertainty in the decay rate, ${\mathrm{\sigma}}_{{\stackrel{~}{\mathrm{\alpha}}}_{m}},$was characterized based on the difference between measured wave heights and predicted values from the best-fit curves for each wave case and layout. This uncertainty did not include potential bias in estimating *H*_{m0} from the pressure transducers from linear wave theory. Table 3 lists ${\stackrel{~}{\mathrm{\alpha}}}_{m}$, ${\mathrm{\sigma}}_{{\stackrel{~}{\mathrm{\alpha}}}_{m}},$ and the average HD to LD ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ coefficient ratio for each random wave case, with hydrodynamic conditions reported at the seaward-most pressure gage (PD18-1). Corresponding values for regular waves were similarly determined and are presented in Appendix Table A2.

**Table 3.** Measured *H*_{m0} and *T*_{p} values at PD18-1, ${\stackrel{~}{\mathrm{\alpha}}}_{m}$, HD/LD ratio of the ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ coefficient, *k _{p}h_{v}*,

*H*,

_{m0}/D_{e}*Re*

_{U,De},

*KC*

_{U,De}, and

*C*

_{D}values for random wave cases.

### Drag Coefficients

The drag coefficient, *C*_{D}, for each wave case and configuration was calculated using ${\stackrel{~}{\mathrm{\alpha}}}_{m}$ and Equation (3). The *C*_{D} values were then related to the Reynolds number, *Re*_{U,De}, calculated using the depth-averaged velocity, *U*, and the effective diameter, *D*_{e}. Table 3 further lists *C*_{D} values for each random wave case with hydrodynamic conditions given at PD18-1 for the HD and LD layouts, as well as *Re*_{U,De} and the Keulegan–Carpenter number, *KC*_{U,De}, determined using the depth-averaged velocity and effective diameter, while Appendix Table A2 provides corresponding values for regular waves, where Equation (2) was used to calculate *C*_{D} values. While for most trials *KC*_{U,De} was large, indicating drag dominance, a few cases were identified with *KC*_{U,De} ≤ 15, where the inertial force contributions are expected to be significant.

Relationships between the calculated drag coefficient and the Reynolds number were investigated for random and regular wave conditions as shown in Figure 9. Figure 9a shows *C*_{D} versus *Re*_{U,De} on a linear scale for the HD (squares) and LD (triangles) configurations for random wave conditions. Colors indicate the three tested ranges of relative water depth, *k _{p}h_{v}*, for random waves: 0.30 <

*k*< 0.40 (dark red), 0.70 <

_{p}h_{v}*k*< 0.80 (intermediate red), and 1.30 <

_{p}h_{v}*k*< 1.45 (light red). As seen in Figure 9a,

_{p}h_{v}*C*

_{D}values show a consistent dependence on Reynolds number for the forest densities and relative water depth ranges considered in these experiments. Lower

*C*

_{D}values are observed for higher Reynolds numbers and lower relative water depths. Cases with larger

*C*

_{D}values correspond with cases that indicated inertial force predominance. The minimum

*C*

_{D}value observed in this study for random waves was 0.85, occurring at the second largest

*Re*

_{U,De}value and smallest

*k*range, and the largest observed

_{p}h_{v}*C*

_{D}value was 3.75, corresponding to the lowest

*Re*

_{U,De}value and largest

*k*range. Figure 9b shows

_{p}h_{v}*C*

_{D}versus

*Re*

_{U,De}on a linear scale for the HD (squares) and LD (triangles) configurations for regular wave conditions, with colors indicating tested ranges of relative water depth,

*kh*0.30 <

_{v}:*kh*

_{v}< 0.45 (dark orange), 0.45 <

*kh*

_{v}< 0.80 (intermediate orange), and 1.10 <

*kh*

_{v}< 1.40 (light orange).

*C*

_{D}values for regular waves varied from 0.37 to 1.74 for the range of

*Re*

_{U,De}tested and in general showed agreement with

*C*

_{D}values for random waves for similar Reynolds numbers.

**Figure 9.** Drag coefficient, *C*_{D}, versus the Reynolds number, *Re*_{U,De} on a linear scale for high-density (squares) and low-density (triangles) configurations designated by relative water depth. **(a)** Random wave cases, 0.30 < *k _{p}h_{v}* < 0.40 (dark red), 0.70 <

*k*< 0.80 (intermediate red), and 1.30 <

_{p}h_{v}*k*< 1.45 (light red).

_{p}h_{v}**(b)**Regular wave cases, 0.30 <

*kh*

_{v}< 0.45 (dark orange), 0.45 <

*kh*

_{v}< 0.80 (intermediate orange), and 1.10 <

*kh*

_{v}< 1.40 (light orange). Vertical bars show combined uncertainty due to $\overline{{A}_{t}}$ and ${\stackrel{~}{\mathrm{\alpha}}}_{m}.$ Note change in

*x-*axis scale from

**(a)**to

**(b)**.

The combined uncertainty, σ_{CD}, due to estimates of the projected area per unit height, $\overline{{A}_{t}}$, and measured decay rate, ${\stackrel{~}{\mathrm{\alpha}}}_{m}$, was determined by:

where $\overline{{\mathrm{\sigma}}_{At}}$ and $\overline{{\mathrm{\sigma}}_{\stackrel{~}{\mathrm{\alpha}}m}}$ are the estimated uncertainties in the projected area and decay rate, respectively (Table 3 and Appendix Table A2), and are shown as vertical bars in Figures 9a,b. In general, uncertainty in *C*_{D} increases slightly as the Reynolds number decreases. The overall mean value of the uncertainty is $\overline{{\mathrm{\sigma}}_{CD}}$ was 0.58 and 0.56 for random and regular waves, respectively.

### Scaling Law for Comparison With Reduced-Scale Data and Design Equation for *C*_{D}

The data from the present study were compared to data from the 1:6- and 1:7- reduced-scale experiments of Chang et al. (2019) and Maza et al. (2019), respectively. Maza et al. (2019) considered regular and random waves, and Chang et al. (2019) considered regular waves. Both Chang et al. (2019) and Maza et al. (2019) reported drag coefficients as a function of the Reynolds number. Maza et al. (2019) determined *Re* based on the projected area per unit width, and thus had larger overall values of *Re* than if the characteristic length scale had been taken as the diameter of the trunk or root as is more common in studies of emergent vegetation. Chang et al. (2019) used the *D*_{BH} as the characteristic length scale to determine *Re.*

It is well known that Reynolds similitude does not hold in a reduced-scale hydraulic model test when Froude similitude is used for the kinematic scaling. Therefore, to compare the two previous reduced-scale studies with the current prototype-scale study, a scaling relation is proposed for the Reynolds number:

where λ is the prototype-to-model geometric scale ratio and *Re* with subscripts *p* and *m* refer to the prototype- and reduced-scale Reynolds numbers, respectively, and the 3/2 results from Froude scaling. Similar scaling of the Reynolds number has also been used in reduced-scale studies focused on permeable core material for rubble mound breakwaters (e.g., Jensen and Klinting, 1983; Martín et al., 2003; Losada et al., 2016), which also relies on turbulence to dissipate wave energy.

Equation (6) was applied to the data of Chang et al. (2019) and Maza et al. (2019) with λ 6 and λ 7, respectively, as shown in Figure 10. As noted earlier, Maza et al. (2019) used the projected area as the characteristic length scale for *Re*. To provide a consistent basis for comparison, *D*_{BH} was used as the characteristic length scale to rescale their reported values of *Re*. In the figure, drag coefficients from the present study for regular and random wave cases are shown as light red squares and dark red circles, respectively. Drag coefficients reported by Maza et al. (2019) for regular and random wave cases are shown as light green squares and dark green circles, respectively. Drag coefficients reported by Chang et al. (2019) are shown as light blue squares. As seen in the figure, rescaling the Reynolds number results in good agreement across all three studies, despite the differences in the studies’ scales, wave conditions, and model tree geometries, suggesting that the method is fairly robust.

**Figure 10.** Drag coefficient, *C*_{D}, versus the Reynolds number, *Re*_{U,DBH}, on a linear scale for data from present study random (dark red circles) and regular (light red squares) waves, Maza et al. (2019) random (dark green circles) and regular (light green squares) waves, and Chang et al. (2019) regular (light blue squares) waves. Solid black line indicates the fitted equation with asymptote value 0.6 [Equation (8)]. Dashed black lines indicate 95% confidence intervals.

A best-fit line using the empirical equation of the form *C*_{D} = *a _{1}* + (

*a*)

_{2}/Re_{U,DBH}*was found for the combined data (Chang et al., 2019; Maza et al., 2019, and present study) with coefficients*

^{a3}*a*= 0.70,

_{1}*a*= 26,000,

_{2}*a*= 1.0, and

_{3}*R*

^{2}= 0.63 for the range 4.9e03 <

*Re*

_{U,DBH}< 1.9e05:

Equation (7) was modified by setting the asymptote value *a*_{1} = 0.60, consistent with results from Sarpkaya and Isaacson (1981), an accepted value for waves on vertical piles, giving an alternative best-fit line with *a _{2}* = 30,000,

*a*= 1.0:

_{3}Equation (8) results in similar estimations of *C*_{D} based on *Re*_{U,DBH} and is shown as a solid line in Figure 10, with dashed lines showing 95% confidence intervals assuming a normal distribution of the data. As seen in Figure 10, Equation (8) shows good agreement with the combined data, with *R*^{2} = 0.63. Data are generally within confidence intervals, particularly for higher Reynolds numbers. Equation (8) may therefore be used in engineering design to determine the appropriate drag coefficient for mangroves over the range of hydrodynamic conditions considered here. This drag coefficient may then be used to calculate wave height decay and attenuation via the equations proposed by Mendez and Losada (2004) for random waves.

### Comparison With Drag Coefficient Relations for Emergent Vegetation

It is of some interest to show the comparison of the three mangrove studies of Figure 10 with previous studies considering emergent wetland vegetation (e.g., *Spartina alterniflora*) modeled using rigid cylinders (Hu et al., 2014; Ozeren et al., 2014) or flexible tubing (Anderson and Smith, 2014), since these studies also model *C*_{D} as a function of *Re* in the form of Equation (8). Table 4 lists the vegetation studied, wave conditions, range of Reynolds numbers considered, and proposed equation for the drag coefficient as a function of the Reynolds number for the combined data of this study (Chang et al., 2019; Maza et al., 2019, and present study) and the previous investigations of emergent vegetation.

The equations presented in the studies listed in Table 4 are shown in Figure 11, which shows *C*_{D} plotted against *Re* on a logarithmic scale. The black dash-dot line indicates the best-fit line developed from the combined data focusing on the *Rhizophora* sp. of this study (red circles) and rescaled data of Chang et al. (2019) (blue circles) and Maza et al. (2019) (green circles). Drag coefficient relations for emergent wetland vegetation are shown as dashed lines for random wave data from Anderson and Smith (2014) (orange), regular wave with current data from Hu et al. (2014) (red), and regular and random wave data from Ozeren et al. (2014) (light and dark blue, respectively). As seen in the figure, the *Rhizophora* studies report higher Reynolds numbers (under prototype conditions) than the emergent wetland vegetation studies, which is reasonable considering the stem diameters of the emergent wetland vegetation studies were 1–2 orders of magnitude smaller than the *D*_{BH} values of the *Rhizophora* studies. The *Rhizophora* studies were also tested under larger wave conditions than the emergent vegetation studies. The three emergent vegetation studies show a fair amount of variability in *C*_{D}. Had the results of Chang et al. (2019) and Maza et al. (2019) not been rescaled, these data would have appeared among the dashed lines of Figure 11, and could have been misinterpreted as having good agreement with previous studies of emergent wetland vegetation with smaller characteristic length-scales. However, there is a clear separation between the previous studies of emergent wetland vegetation and the mangrove studies at prototype-scale. This comparison reinforces the necessity of proper consideration of Reynolds-dependent *C*_{D} values estimated from reduced-scale tests based on the vegetation archetype considered.

**Figure 11.** Drag coefficient *C*_{D} vs. Reynolds number *Re*_{DBH} on logarithmic scale for comparison of previous studies of emergent wetland vegetation (dashed lines): Anderson and Smith (2014) (random waves, orange), Hu et al. (2014) (regular waves + current, red), Ozeren et al. (2014) (regular and random waves, light and dark blue, respectively) to the proposed equations for the combined mangrove data (black dash-dot line) of present study (red circles), Chang et al. (2019) (blue circles), and Maza et al. (2019) (green circles). Note *x-*axis origin is at 1.00e02.

## Discussion

### Implications for Shoreline Protection

Results of this study can be used to inform coastal engineers and stakeholders on the potential of leveraging mangroves in engineering with nature projects. The methodology presented here for LiDAR-based characterization of the projected area and effective diameter of the mangrove forest can be extended to field applications to complement conventional methods (i.e., calipers, rulers, and measuring tape) for determining mangrove geometric characteristics. The method further can provide a non-destructive and accurate process for estimating *D*_{BH} and *D*_{Root} values of complex sites. While previous studies have used terrestrial-based LiDAR to quantify the biomass of mangrove forests (Feliciano et al., 2014; Olagoke et al., 2016) using non-destructive methods, these studies did not report projected area. Therefore, the methodology proposed here may expand upon ecological studies that use terrestrial-based LiDAR scanning for engineering applications to obtain a representative cross-section of the projected area of a mangrove forest for predicting the forest’s effects on wave attenuation. LiDAR measurements taken at different points in time can be used to assess how the projected area changes as a forest matures, after a system is damaged by a storm event (Lagomasino et al., 2021), and throughout the recovery process. The effect of uncertainty in the projected area on the drag coefficient and ultimately hydrodynamic transformation through a mangrove forest can also be quantified. Accurately characterizing the uncertainty of a system’s performance is essential for making conservative design decisions and incorporating redundancy in a shoreline protection project.

Results of this study indicate that even mangrove forests of moderate cross-shore width (∼10–50 m) can provide measurable reduction in wave heights, building on previous studies that have considered greater forest expanses (e.g., Maza et al., 2019). For random waves, wave height reductions of 13–28% and 6–16% were observed over the 18 m cross-shore forest distance for the HD and LD configurations, respectively, and for regular waves, wave height reductions of 12–32% and 6–22% were observed for the HD and LD configurations, respectively. The proposed Equation (8), which synthesizes the results of the present prototype-scale tests and two previous reduced-scale tests from the literature, can be used for a specific site given information about the mangrove forest geometry and design hydrodynamic conditions. This study also confirms that a relatively simple scaling relation of the Reynolds number can be used to compare data of reduced-scale tests under Froude similitude. The agreement between the present study’s data collected at prototype scale and the rescaled data of Chang et al. (2019) and Maza et al. (2019) based on Equation (6) supports the use of reduced-scale models, which are often more cost-, time-, and labor- effective, to improve the robustness of *C*_{D} vs. *Re* relationships for investigation of wave attenuation through vegetation, provided that Reynolds number scaling is considered.

### Physical Model Considerations

Sources of uncertainty in addition to the two discussed in this study may affect the drag coefficient of *Rhizophora* sp. trees. The LiDAR methodology presented here may result in increased uncertainty in geometric measurements at field sites owing to challenges with determining the projected area of submerged portions of a mangrove forest or due to blockage by the forest canopy. While the majority of the cases tested fell within the drag-dominated regime, several cases were located within the inertia-dominated regime as indicated by the *KC* number in Table 3 and Appendix Table A2. These cases correspond to the largest relative water depths tested for the study. The inertial predominance indicated for these cases could lead to higher estimations of the drag coefficient, *C*_{D}, from the Mendez and Losada (2004) *C*_{D} equation [Equation (3)], which neglects inertial force in the derivation. This study did not collect direct force measurements on the model tree specimens, so the possible *C*_{D} overestimation by the Mendez and Losada (2004) equation for these cases could not be fully quantified. In addition, the derived equations came from studies that did not include a canopy for the idealized model tree. The canopy’s added effects, especially at higher water depths and milder wave conditions, could alter the drag coefficients from those presented in this study. Similarly, both the present study and Maza et al. (2019) only considered the primary prop root in constructing the model trees, while Chang et al. (2019) included the primary roots with the secondary and tertiary prop roots branching off of the primary roots. The tertiary and secondary roots provide more projected area and potentially more protection. Therefore, neglecting the canopy and additional prop roots provides conservative estimations of the protection provided by the mangroves for the range of hydrodynamic conditions considered.

In nature, mangrove forests comprise trees of different ages, growth stages, and species. The protection that mangrove forests provide can change depending on biological variables such as forest age, growth, and structure, or damage sustained during an extreme event such as a hurricane or tsunami. To assess the protection provided at various stages of the forest’s lifetime, a weighted average drag coefficient could be calculated if the percentage makeup of the forest for the different diameters at breast height are known. Similarly, natural variation in projected area through the forest may affect wave attenuation, and therefore protocols for assessing the geometric properties at various cross-shore locations within a forest are required. Understanding the temporal and spatial variation of the protection provided by mangroves is essential to quantifying the long-term protection that these forests can provide. In addition to wave height reduction, other performance metrics such as load reduction on sheltered structures or overtopping reduction of inland infrastructure may also be considered for engineering design.

Implementing mangroves and other natural systems at ecologically viable sites is critical to ensure that these systems can mature and provide the desired engineering services. For example, the day-to-day wave climate, hydrologic connectivity, and water quality can affect mangrove growth and vulnerability, and disruptions such as extreme storms, prolonged flooding, and sediment smothering can cause significant die off (Lagomasino et al., 2021). Threshold conditions at which natural systems fail to perform their design engineering service must be identified. Similarly, the ecology of these systems must be considered in engineering design to determine where these nature-based solutions are viable adaptation alternatives and understand what conditions may threaten the survivability of a project. The ability of mangroves to keep up with relative sea level rise at local sites must also be considered (Saintilan et al., 2020). Incorporating gray infrastructure such as rubble mound sills could protect the shoreline and juvenile green infrastructure systems as the vegetation matures; however, best practices for combining green and gray infrastructure must be developed, as well as methods to assess the combined performance of these hybrid systems. The most resilient mangrove system may not necessarily be the same system that optimizes engineering performance, and so a balance between ecological requirements and engineering performance must be achieved. Future research focused on these hybrid systems is needed to fully answer these questions and identify the critical components for successful design.

## Conclusion

This paper presents results of an idealized, prototype-scale physical model to quantify protection provided by a *Rhizophora* sp. mangrove forest of moderate (18 m) cross shore width for use in engineering with nature projects. Results of this study lead to the following six conclusions:

(1) The LiDAR methodology developed for this study accurately characterized the representative projected area per unit height and associated uncertainty of the mangrove forest, allowing for an effective diameter of the system to be determined. Trunk and prop root LiDAR measurements were accurate to within 2 and 10% of known values, respectively.

(2) Mangroves of moderate cross-shore width had a measurable effect on wave attenuation for the range of wave conditions tested here. Wave height decay rates of 0.008–0.021 m^{–1} and 0.004–0.010 m^{–1} were observed for the high-density and low-density configurations, respectively.

(3) Increasing the density of the mangrove forest by a factor of two increased the wave decay coefficient by a factor of 2.0 on average for the random wave conditions and by 2.2 for regular wave conditions. This result is consistent with similar observations in the literature and suggests that the wave height decay was not affected by gridded or random mangrove layouts, but rather by the density variation, in agreement with the numerical findings of Maza et al. (2015).

(4) Drag coefficients were Reynolds number dependent and ranged from 3.8 to 0.4 over the range of Reynolds numbers from 4.6e03 to 119e03 with a combined uncertainty from the projected area and hydrodynamic measurements of σ = 0.58 for random waves and σ = 0.56 for regular waves.

(5) Two previous reduced-scale studies of wave attenuation by mangroves compared well with the present study when their Reynolds numbers were re-scaled by λ* ^{3/2}*, where λ is the prototype-to-model geometric scale ratio.

(6) An equation is proposed to estimate the drag coefficient for a *Rhizophora* mangrove forest: *C*_{D} = 0.6 + 3 × 10^{4}/*Re*_{DBH} with an uncertainty of σ = 0.69 over the range 5e03 < *Re*_{DBH} < 1.9e05, where *Re*_{DBH} is based on the tree diameter at breast height.

As coastal flood hazards continue to threaten nearshore communities, engineers, planners, and stakeholders are challenged to redefine conventional definitions of coastal infrastructure to include a broader suite of adaptation options that leverage natural and nature-based solutions in addition to or in tandem with gray alternatives. This shift requires transdisciplinary approaches to identify best practices for engineering with nature. A deeper understanding is required of not only the engineering performance, but also the ecological, policy, and social requirements for successful implementation of green and hybrid systems.

## Data Availability Statement

The datasets presented in this study can be found in online repositories. The names of the repository/repositories and accession number(s) can be found below: Kelty et al. (2021) “Prototype-Scale Physical Model Study of Wave Attenuation by an Idealized Mangrove Forest of Moderate Cross-shore Width,” in Experimental Investigation of Wave, Surge, and Tsunami Transformation over Natural Shorelines. DesignSafe-CI. https://doi.org/10.17603/ds2-znjw-1f81.

## Author Contributions

KK, TT, DC, and PL conceived and planned the experiments. KK, DC, PL, and WM carried out the experiments. All authors contributed to the interpretation of the results. KK and TT took the lead in writing the manuscript. All authors provided critical feedback and helped to shape the research, analysis, and manuscript.

## Funding

This project was funded by the National Science Foundation Grants #1519679, #1825080, #1661315, and #2037914, and by the United States Army Corps of Engineers’ Engineering Research and Development Center. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the National Science Foundation, United States Army Corps of Engineers, or United States Naval Academy.

## Conflict of Interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

## Publisher’s Note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

## Acknowledgments

The authors gratefully acknowledge Esteban Biondi, Greg Braun, Mike Jenkins, Diego Delgado, Carmon Vare, Dave Carson, and Chris O’Day, who contributed to the success of field work. Duncan Bryant, Mary Bryant, Leigh Provost, Nia Hurst, and Anna Wargula contributed to discussions on the construction of the idealized mangrove forest. Rebekah Miller, Tim Maddux, Bruce Kim, Jamie Shultz, Courtney Beringer, and Chuan Li aided in model design, construction, and experimentation. Michael Olsen assisted with LiDAR analysis. Eric Anderson provided the authors an opportunity to disseminate project outcomes to stakeholders in southeastern Florida. Alexis Lipovich and Kayla Ostrow provided feedback on an original draft of this manuscript. The experimental data are available by contacting the authors and are available on DesignSafe.org (https://doi.org/10.17603/ds2-znjw-1f81).

## Supplementary Material

The Supplementary Material for this article can be found online at: https://www.frontiersin.org/articles/10.3389/fmars.2021.780946/full#supplementary-material

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Keywords: * Rhizophora mangle* (red mangroves), wave attenuation by vegetation, physical modeling, drag coefficient, natural and nature-based features, engineering with nature, LiDAR

Citation: Kelty K, Tomiczek T, Cox DT, Lomonaco P and Mitchell W (2022) Prototype-Scale Physical Model of Wave Attenuation Through a Mangrove Forest of Moderate Cross-Shore Thickness: LiDAR-Based Characterization and Reynolds Scaling for Engineering With Nature. *Front. Mar. Sci.* 8:780946. doi: 10.3389/fmars.2021.780946

Received: 22 September 2021; Accepted: 17 December 2021;

Published: 12 January 2022.

Edited by:

Maria Maza, University of Cantabria, SpainReviewed by:

Thorsten Stoesser, University College London, United KingdomMaike Paul, Leibniz University Hannover, Germany

Copyright © 2022 Kelty, Tomiczek, Cox, Lomonaco and Mitchell. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Tori Tomiczek, toritomi11@gmail.com