Formula that takes the coordinates of digitized shell increments and interpolates a number of sub-increments between them to increase the time resolution of the growth model. The number of interpolated shell increments as well as the relative thickness of these increments is determined by a sinusoidal seasonal model that simulates seasonal variations in shell growth rate. de Winter, N. J. (2017) doi:10.5194/gmd-2017-137
incr_matrix: Matrix listing characteristics of each digitized increment
cross_section: Digitized cross section of the shell with shell top, bottom and growth increments relative to a common X-axis
season_length: Length (in days) of the growth season of the studied bivalve
Tstep: The step size (dt) in time (days) used to interpolate the existing shell increments
Xstep: The step size (dx) in X-direction used to interpolate coordinates of shell increments
Details
Sub-increments are reconstructed by interpolating Y-values between the digitized shell increments
Returns
List of two data frames: - IncG: Matrix of X- and Y-coordinates of all interpolated sub-increments
subincr_matrix: Revised version of the "incr_matrix" data frame that contains characteristics (sub-increment number, X-value of start of increment) recalculated for every sub-increment
References
de Winter, N. J.: ShellTrace v1.0 ? A new approach for modelling growth and trace element uptake in marine bivalve shells: Model verification on pacific oyster shells (Crassostrea gigas), Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2017-137, in review, 2017.
Author(s)
Niels J. de Winter
Note
Please cite Geoscientific Model Development paper dealing with the ShellTrace model