Flood hazard comes from different sources, including: riverine (or fluvial) flooding, coastal flooding, and stormwater (or urban) flooding - the focus of this InVEST model. Natural infrastructure can play a role for each of these flood hazards. Related to stormwater flooding, natural infrastructure operates mainly by reducing runoff production, slowing surface flows, and creating space for water (in floodplains or basins).
The InVEST model takes a simple curve number approach to calculating rainfall runoff reduction due to land use/land cover and soil characteristics. Runoff reduction can also be thought of as the amount of runoff retained per pixel compared to the storm volume. For each watershed, it also estimates the potential economic damage, and ecosystem service provided, to built infrastructure.
For each pixel i, defined by a land use type and soil characteristics, we estimate runoff Q (mm) with the Curve Number method:
Q_{p,i} = \begin{Bmatrix}
\frac{(P - \lambda S_{max_i})^2}{P + (1-\lambda) S_{max,i}} & if & P > \lambda \cdot S_{max,i} \\
0 & & otherwise
\end{Bmatrix}
Where P is the design storm depth in mm, S_{max,i} is the potential retention in mm, and \lambda \cdot S_{max} is the rainfall depth needed to initiate runoff, also called the initial abstraction (\lambda=0.2 for simplification).
S_{max} (calculated in mm) is a function of the curve number, CN, an empirical parameter that depends on land use and soil characteristics (NRCS 2004):
S_{max,i}=\frac{25400}{CN_i}-254
The model then calculates the fraction of runoff retention per pixel R_i as:
R_i=1-\frac{Q_{p,i}}{P}
And runoff retention volume per pixel R\_m3_i as:
R\_m3_i=R_i\cdot P\cdot pixel.area\cdot 10^{-3}
With pixel.area in m^2.
Runoff volume (also referred to as "flood volume") per pixel Q\_m3_i is also calculated as:
Q\_m3_i=Q_{p,i}\cdot pixel.area\cdot 10^{-3}
First, \text{Affected.build}, the sum of potential damage in currency units to built infrastructure, is calculated for each watershed or sewershed W:
\text{Affected.build}_W = \sum_{b \in B}a(b,W)·d(b)
where
- b is a building footprint in the set of all built infrastructure B
- a(b,W) is the area in m^2 of the building footprint b that intersects watershed W
- d(b) is the damage value in currency/m^2 (from the user-input Damage Loss Table) for building b's type
We then calculate \text{Service.built}, an indicator of avoided damage to built infrastructure, for each watershed W:
\text{Service.built}_W=\text{Affected.build}_W·\sum_{i \in W}R\_m3_i
where
- i is a pixel in watershed W
- R\_m3_i is the runoff retention volume on pixel i
\text{Service.built} is expressed in currency·m^3, and can be used to indicate the ecosystem service of flood retention provided to buildings. Given the simplicity of the model, it should be considered only an indicator, not an actual measure of savings.
Runoff production: the model uses a simple approach (SCS-Curve Number), which introduces high uncertainties. However, the ranking between different land uses is generally well captured by such an approach, i.e. that the effect of natural infrastructure will be qualitatively represented in the model outputs. Future work will aim to include a routing over the landscape: ideas include TOPMODEL (there is an R package), UFORE (used in iTree), CADDIES, etc
Valuation approaches: Currently, a simple approach to value flood risk retention is implemented, valuing flood risk as the potential avoided damage for built infrastructure. This value may prove useful in comparing risk across nearby watersheds, capturing the different amounts of exposed infrastructure for each watershed. However, since the model does not produce inundation maps, there is no way to confirm that the infrastructure is actually exposed. The output therefore remains a potential benefit. Alternative approaches (e.g. related to mortality, morbidity, or economic disruption) could be implemented. Another service metric is the affected population, i.e. the number of people at risk from flooding. This could focus on vulnerable groups only, e.g. related to age, language, etc. See Arkema et al., 2017, for a review of social vulnerability metrics. This metric can be calculated by summing the population in the intersection of the watershed and the flood-prone area.
Note
Spatial layers for Urban Flood Mitigation may have different coordinate systems, but they must all be projected coordinate systems, not geographic.
Note
Raster inputs may have different cell sizes, and they will be resampled to match the cell size of the land use/land cover raster. Therefore, raster model results will have the same cell size as the land use/land cover raster.
:investspec:`urban_flood_risk_mitigation aoi_watersheds_path` These may be watershed or sewershed boundaries.
:investspec:`urban_flood_risk_mitigation rainfall_depth` This is P in equation :eq:`runoff`.
:investspec:`urban_flood_risk_mitigation lulc_path` All outputs will be produced at the resolution of this raster.
:investspec:`urban_flood_risk_mitigation soils_hydrological_group_raster_path`
:investspec:`urban_flood_risk_mitigation curve_number_table_path` table containing model information corresponding to each of the land use classes in the Land Cover Map. All LULC classes in the Land Cover raster MUST have corresponding values in this table. Each row is a land use/land cover class and columns must be named and defined as follows:
Columns:
- :investspec:`urban_flood_risk_mitigation curve_number_table_path.columns.lucode`
- :investspec:`urban_flood_risk_mitigation curve_number_table_path.columns.cn_a`
- :investspec:`urban_flood_risk_mitigation curve_number_table_path.columns.cn_b`
- :investspec:`urban_flood_risk_mitigation curve_number_table_path.columns.cn_c`
- :investspec:`urban_flood_risk_mitigation curve_number_table_path.columns.cn_d`
:investspec:`urban_flood_risk_mitigation built_infrastructure_vector_path`
Field:
:investspec:`urban_flood_risk_mitigation infrastructure_damage_loss_table_path`
Columns:
Parameter log: Each time the model is run, a text (.txt) file will be created in the Workspace. The file will list the parameter values and output messages for that run and will be named according to the service, the date and time. When contacting NatCap about errors in a model run, please include the parameter log.
Runoff_retention_index.tif: raster with runoff retention index values (no unit, values of 0-1, relative to precipitation volume). Calculated from equation :eq:`runoff_retention`.
Runoff_retention_m3.tif: raster with runoff retention volume values (in m^3). Calculated from equation :eq:`runoff_retention_volume`.
Q_mm.tif: raster with runoff values (mm). Calculated from equation :eq:`runoff`.
flood_risk_service.shp: Shapefile with results in the attribute table:
- rnf_rt_idx: average of runoff retention index values (R_i) per watershed
- rnf_rt_m3: sum of runoff retention volumes (R\_m3_i), in m^3, per watershed.
- flood_vol: The flood volume (
Q_m3, equation :eq:`flood_volume`) per watershed.- aff_bld: potential damage to built infrastructure in currency units, per watershed. Only calculated when the Built Infrastructure Vector input is provided. Note that this does not take into account actual flood depth or extent, so should be used as an indicator only.
- serv_blt: Service.built values for this watershed (see equation :eq:`service.built`), in units of currency·m^3. An indicator of the ecosystem service of runoff retention for the watershed. Only calculated when the Built Infrastructure Vector input is provided. Note that this does not take into account actual flood depth or extent, so should be used as an indicator only.
A design storm is a hypothetical rainstorm used for modeling purposes. The design storm precipitation value should be chosen according to the area and goals. For instance, it could be the average precipitation per rain event, the precipitation at a certain percentile, or the maximum precipitation expected to occur once in 100 years.
To calculate the design storm, users can look up intensity-frequency-duration (IFD) tables available for their city. The storm duration is equal to the average time of concentration of the studied watersheds. Time of concentration can be derived from existing studies or from web tools: eg. https://www.lmnoeng.com/Hydrology/TimeConc.php. See Balbi et al. (2017) for a detailed description of these methods.
In the US, HAZUS provides damage data. Globally, a recent report from the European Commission provides useful data: https://publications.jrc.ec.europa.eu/repository/bitstream/JRC105688/global_flood_depth-damage_functions__10042017.pdf
Arkema, K. K., Griffin, R., Maldonado, S., Silver, J., Suckale, J., & Guerry, A. D. (2017). Linking social , ecological , and physical science to advance natural and nature-based protection for coastal communities. https://doi.org/10.1111/nyas.13322
Balbi, M., Lallemant, D., & Hamel, P. (2017). A flood risk framework for ecosystem services valuation: a proof-of-concept.
NRCS-USDA. (2004). Chapter 10. Estimation of Direct Runoff from Storm Rainfall. In United States Department of Agriculture (Ed.), Part 630 Hydrology. National Engineering Handbook. Retrieved from http://www.nrcs.usda.gov/wps/portal/nrcs/detailfull/national/water/?cid=stelprdb1043063
NRCS-USDA Part 630 Hydrology National Engineering Handbook, Chapter 7 Hydrologic Soil Groups. 2007.
NRCS-USDA Part 630 Hydrology National Engineering Handbook, Chapter 9 Hydrologic Soil-Cover Complexes. 2004.
Sahl, J. (2015). Economic Valuation Approaches for Ecosystem Services: a literature review to support the development of a modeling framework for valuing urban stormwater management services.