Description Details References See Also
Satellite data collected between 1998 and 2018 (SeaWiFS, MODIS, MERIS, VIIRS), in conjonction with GEBCO gridded bathymetric data (15 arc seconds), are used to estimate, at a nearly global scale, the irradiance reaching the bottom of the coastal ocean.
This package has two goals :
calculate the surface area of the sea floor which receives more than a given threshold of irradiance.
get various geographic and optical data from a database consisting of files to download
:
function cl_surface()
is the main function;
it returns the surface areas receiving irradiance above given thresholds,
or the P-functions (see Gattuso et al. - reference below) for three standard regions;
NonPolar, Arctic, and Antarctic;
It is the only function to use if you are interested in one of these
standard regions;
P-functions for these regions have been tabulated and
the tables included in the package.
function cl_subregion()
is used to produce the P-functions
of a subregion of one of the three standard regions;
it connects to a server that does the calculations and offers to download
a file containing the P-functions for this subregion;
this file is ready to be used by the function cl_surface()
.
:
function cl_DownloadData()
downloads the data;
function cl_GetData()
gets the data on a geographic zone defined by the user;
function cl_PlotData()
plots the data, as returned by function cl_GetData()
.
function cl_Transect()
complements function cl_GetData()
for the extraction of data along a transect.
Data and units :
P-functions : %
longitude : decimal \, degree \; [-180 ; 180]
latitude : decimal \, degree \; [-90 ; 90]
depth : m
area : km^{2}
par, parbottom : mol.photons \; m^{-2} \; d^{-1}
kdpar : m^{-1}
Gattuso J.-P., Gentili B., Antoine D. & Doxaran D., 2020. Global distribution of photosynthetically available radiation on the seafloor. Earth System Science Data 12:1697-1709. http://dx.doi.org/10.5194/essd-12-1697-2020
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