The function estimates soil temperature (C) at a given depth and hour by approximating diurnal variation as sinusoidal. The function is adapted from Campbell and Norman (1998) and described in Riddell et al. (2018) .

Tsoil(T_g_max, T_g_min, hour, depth)

Arguments

T_g_max

numeric daily maximum soil surface temperature (C).

T_g_min

numeric daily minimum soil surface temperature (C).

hour

numeric hour of the day.

depth

numeric depth (cm).

Value

numeric soil temperature (C).

References

Campbell GS, Norman JM (1998). Introduction to environmental biophysics, 2nd ed. edition. Springer, New York. ISBN 0387949372.

Riddell EA, Odom JP, Damm JD, Sears MW (2018). “Plasticity reveals hidden resistance to extinction under climate change in the global hotspot of salamander diversity.” Science Advances, 4(4). doi:10.1126/sciadv.aar5471 .

Author

Eric Riddell

Examples

  Tsoil(T_g_max = 30,
        T_g_min = 15,
        hour    = 12,
        depth   = 5)
#> [1] 20.65027