Background and MotivationAll rates and ages depend on temperature; all AmP parameters are expressed at the reference temperature of 20 °C. The body temperature of aquatic ectotherms is (almost) equal to the water temperature, but that of terrestrial ones depend on a large number of factors. Endotherms regulate their body temperature after birth at species-specific levels, but that of neonates can deviate substantially; the temperature in bird Eggs typically follows a trajectory. Temperature is stored as auxilliary data in the mydata file, and used for calculating model predictions.
Correcting for temperature using the Arrhenius temperature correction model amounts to a simple transformation of ages and rates by multiplying or dividing by temperature correction factor (c_T). What is important to keep in mind though is that metabolic rates depend on temperature in a non linear way. If the temperature was fluctuating rather than constant, the mean temperature has a non-straight-forward relationship with the mean c_T.
Some data sets (field or laboratory) acquire non-constant (fluctuating) temperatures. One is tempted to calculate the mean value of temperatures (T_mean) and then correct the metabolic rates with the c_T for that (T_mean) temperature. The problem arises, however, when the experienced (fluctuating) temperatures had a larger effect in low or high part of the range, which is often the case.
The presented procedure shows how to:
- Obtain environmental temperature values if temperatures are not reported but the geographic location is known;
- Use the temperature values in combination with the Arrhenius temperature correction model
- Obtain and use c_T as a function of time.
The final result is either a (single) temperature (for zero-variate data) or a vector of temperatures (for Uni-variate data) that are taking into account species-specific metabolic traits, and are thus more appropriate in the context of energetic modeling.
- Option 1: Specify time-temperature as a series of knots for a first-order spline function are parameters and estimate these knots from your data.
- Option 2: Use R package link RNCEP: global weather and climate data at your fingertips to make a query and download environmental temperature data. for a given geographic location and a specific timeframe.
- Option 3: Use R to query a global microclimate dataset. These estimates are for the middle day of each month, based on long-term average macroclimates.
- Option 4: If working with a terrestrial ectotherm, you can improve accuracy of your temperature data (obtained via any of the previous steps) by simulating behavior of the species of interest with the NicheMapR microclimate model.
Defining parameters of the Arrhenius temperature correction model
- Option 1: Use data on (developmental, metabolic, or other) rates at several different temperatures to estimate parameters of the Arrhenius temperature correction model (T_ref, T_A, T_AL, T_AH, T_L, T_H).
- Option 2: Find the Arrhenius parameters for your species in literature, and input them directly into your script.
c_T as a function of time and using the back-calculated temperatureUsing the temperature correction model, calculate the temperature correction (c_T) for each temperature point obtained in Step 1.
For associating a temperature with a zero-variate data (e.g. age at puberty at a given food level) calculate the mean of all c_T values. Then convert the obtained mean(c_T) to the equivalent temperature using again the Arrhenius parameters. The back-calculated temperature is the 'constant temperature equivalent'.
For obtaining temperatures for specific time points in Uni-variate data, you will need to interpolate using the pairs of time-c_T values you have obtained in previous steps. It is possible to save either the c_T values or back calculated temperature values as a .csv file. This can then be called in the mydata file and stored in the auxData structure.