Description Usage Arguments Examples
This function allows you to calculate the evaporation to inflow (E:I) ratio of a lake based on a few assumptions and its water isotope value.
1 |
df |
dataframe with your values |
dL |
steady-state lake isotope value (‰) |
dI |
input/source water isotope value (‰) |
dP |
precipitation isotope value (‰) |
temp |
temperature at surface of lake (C) |
humid |
relative humidity (decimal) |
k |
influence of seasonality (0.5: highly seasonal; 1: no seasonality) |
1 2 3 4 5 6 7 | ei_input <- data.frame(dL_permille = c(-11.77, -15.67, -18.23),
dI_permille = c(-20.7, -18.2, -20.2),
dP_permille = c(-23, -28, -32),
temp_C = c(14.3, 12.1, 8.9),
h_dec = c(0.68, 0.71, 0.58),
k = c(0.7, 0.72, 0.65))
eee2eye(ei_input, 'dL_permille', 'dI_permille', 'dP_permille', 'temp_C', 'h_dec', 'k')
|
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.