View source: R/RSAGA-modules.R
rsaga.pisr2 | R Documentation |
This function calculates the potential incoming solar radiation in an area using different atmospheric models; This function reflects changes to the module with SAGA 2.2.2+.
For SAGA versions 2.0.6 to 2.2.1 please see rsaga.pisr()
.
rsaga.pisr2( in.dem, in.svf.grid = NULL, in.vapour.grid = NULL, in.linke.grid = NULL, out.direct.grid, out.diffuse.grid, out.total.grid = NULL, out.ratio.grid = NULL, out.duration, out.sunrise, out.sunset, local.svf = TRUE, location = c("latitude", "grid"), latitude = 53, unit = c("kWh/m2", "kJ/m2", "J/cm2"), solconst = 1367, method = c("height", "components", "lumped", "hofierka"), hgt.atmosphere = 12000, cmp.pressure = 1013, cmp.water.content = 1.68, cmp.dust = 100, lmp.transmittance = 70, time.range = c(0, 24), time.step = 0.5, start.date = list(day = 31, month = 10, year = 2015), end.date = NULL, day.step = 5, env = rsaga.env(), ... )
in.dem |
name of input digital elevation model (DEM) grid in SAGA grid format (default extension: |
in.svf.grid |
Optional input grid in SAGA format: Sky View Factor; see also |
in.vapour.grid |
Optional input grid in SAGA format: Water vapour pressure (mbar), for use with |
in.linke.grid |
Optional input grid in SAGA format: Linke turbidity coefficient, for use with |
out.direct.grid |
Output grid: Direct insolation (unit selected by |
out.diffuse.grid |
Output grid: Diffuse insolation |
out.total.grid |
Optional output grid: Total insolation, i.e. sum of direct and diffuse incoming solar radiation |
out.ratio.grid |
Optional output grid: Direct to diffuse ratio |
out.duration |
Optional output grid: Duration of insolation |
out.sunrise |
Optional output grid: time of sunrise; only calculated if time span is set to single day |
out.sunset |
Time of sunset; see |
local.svf |
logical (default: |
location |
specified whether to use constant latitude supplied by |
latitude |
Geographical latitude in degree North (negative values indicate southern hemisphere) |
unit |
unit of insolation output grids: |
solconst |
solar constant, defaults to 1367 W/m2 |
method |
specifies how the atmospheric components should be accounted for: either based on the height of atmosphere and vapour pressure ( |
hgt.atmosphere |
Height of atmosphere (in m); default 12000 m. For use with |
cmp.pressure |
atmospheric pressure in mbar, defaults to 1013 mbar. For use with |
cmp.water.content |
water content of a vertical slice of the atmosphere in cm: between 1.5 and 1.7cm, average 1.68cm (default). For use with |
cmp.dust |
dust factor in ppm; defaults to 100 ppm. For use with |
lmp.transmittance |
transmittance of the atmosphere in percent; usually between 60 (humid areas) and 80 percent (deserts) |
time.range |
numeric vector of length 2: time span (hours of the day) for numerical integration |
time.step |
time step in hours for numerical integration |
start.date |
list of length three, giving the start date in |
end.date |
see |
day.step |
if |
env |
RSAGA geoprocessing environment obtained with |
... |
optional arguments to be passed to |
According to SAGA GIS 2.0.7 documentation, "Most options should do well, but TAPES-G based diffuse irradiance calculation ("Atmospheric Effects" methods 2 and 3) needs further revision!" I.e. be careful with method = "components"
and method = "lumped"
.
SAGA_CMD uses zero-based months, but this R function uses the standard one-based months (e.g. day 1 is the first day of the month, month 1 is January) and translates to the SAGA system.
This function uses module Potential Incoming Solar Radiation from SAGA library ta_lighting
in SAGA version 2.0.6+.
Changes to the module with SAGA 2.2.2+ include adding year
to the *.date
arguments to allow calculation across years.
The method of Hofierka and Suri (2009) is added, which uses the Linke turbidity coefficient.
Duration of insolation ("out.duration"
) is only calculated when the time period is set to a single day.
Alexander Brenning & Donovan Bangs (R interface), Olaf Conrad (SAGA module)
Boehner, J., Antonic, O. (2009): Land surface parameters specific to topo-climatology. In: Hengl, T. and Reuter, H. I. (eds.): Geomorphometry - Concepts, Software, Applications. Elsevier.
Oke, T.R. (1988): Boundary layer climates. London, Taylor and Francis.
Wilson, J.P., Gallant, J.C. (eds.), 2000: Terrain analysis - principles and applications. New York, John Wiley and Sons.
Hofierka, J., Suri, M. (2002): The solar radiation model for Open source GIS: implementation and applications. International GRASS users conference in Trento, Italy, September 2002
rsaga.pisr()
; for similar modules in older SAGA versions (pre-2.0.6) see rsaga.solar.radiation()
and rsaga.insolation()
; rsaga.hillshade()
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