Load model configuration to the aeme object
Usage
load_configuration(
aeme,
model,
path = ".",
model_controls = NULL,
use_bgc = FALSE,
ext_elev = 0,
calc_wbal = TRUE,
wb_method = 2,
calc_wlev = TRUE,
use_aeme = FALSE,
coeffs = NULL,
hum_type = 3,
est_swr_hr = TRUE
)Arguments
- aeme
aeme; object.
- model
vector; of models to be used. Can be `dy_cd`, `glm_aed`, `gotm_wet`.
- path
filepath; where input files are located relative to the current working directory.
- model_controls
dataframe; of configuration loaded from "model_controls.csv".
- use_bgc
logical; switch to use the biogeochemical model.
- ext_elev
numeric; metres to extend the hypograph by.
- calc_wbal
logical; calculate water balance. Default = TRUE.
- wb_method
numeric; method to use for calculating water balance. Must be 1 (no inflows or outflows) or 2 (outflows calculated) or 3 (Any unexplained gain in lake storage is treated as an effective inflow; any unexplained loss is treated as an effective outflow). Default = 2
- calc_wlev
logical; calculate water level.
- use_aeme
logical; use AEME object to generate model confiuration files.
- coeffs
numeric vector of length two; to be used to estimate surface water temperature for estimating evaporation. Defaults to NULL. If water temperature observations are included in `aeme` object, then it will use those to build a linear relationship between air temperature and water temperature. Otherwise. it uses the simple estimation \(temp_water = 5 + 0.75 * temp_air\) from Stefan & Preud'homme, 2007: www.doi.org/10.1111/j.1752-1688.1993.tb01502.x
- hum_type
numeric; GOTM humidity metric [1=relative humidity ( 2=wet-bulb temperature, 3=dew point temperature, 4=specific humidity (kg/kg)] Default = 3.
- est_swr_hr
logical; estimate hourly shortwave radiation from daily values. Default = TRUE.