man/man1/gensdaymtx.1

.\" RCSid $Id: gensdaymtx.1,v 1.16 2022/08/13 17:24:56 greg Exp $
.TH GENSDAYMTX 1 01/19/13 RADIANCE
.SH NAME
gensdaymtx - generate an annual spectral sky matrix from a weather tape
.SH SYNOPSIS
.B gensdaymtx
[
.B "\-v"
][
.B "\-h"
][
.B "\-d|\-s"
][
.B "\-u"
]][
.B "\-r deg"
][
.B "\-m N"
][
.B "\-p Dir"
][
.B "\-n N"
][
.B "-o{f|d}"
]
[
.B "tape.wea"
]
.SH DESCRIPTION
.I Gensdaymtx
takes a weather tape as input and produces a matrix of spectral sky patch
values using the precomputed atmospheric scattering model.
The weather tape is assumed to be in a special form of the .wea file, which contains 
a short header with the site parameters followed
by the month, day, standard time, direct normal and diffuse horizontal
irradiance values, total cloud cover, and broadband aerosol optical depth, one time step per line.
Such file can be generated by 
.I epw2wea 
with appending
.I \-a 
flag.
Each time step line is used to compute a column in the output matrix,
where rows correspond to sky patch positions, starting with 0 for
the ground and continuing to 145 for the zenith using the default
.I "\-m 1"
parameter setting.
.PP
.I Gensdaymtx
uses the OPAC continental average aerosol profile for the Mie scattering calculation. 
For every distinct AOD value in the weather tape, a new set of the atmospheric parameters 
is computed and stored in the atmos_data directory in the current directory, which 
can be changed using the -p flag. This precomputation can be sped up using the
.I \-n NThreads
option. There is no speedup after NTHREADS=16.
.PP
Increasing the
.I \-m
parameter yields a higher resolution
sky using the Reinhart patch subdivision.
For example, setting
.I "\-m 4"
yields a sky with 2305 patches plus one patch for the ground.
Each matrix entry is in fact 20 values, corresponding to
spectra from 380nm to 730nm at 20nm interval (watts/sr/meter^2).
Thus, an hourly weather tape for an entire year would
yield 8760x20 (175200) values per output line (row).
.PP
The
.I \-g
option may be used to specify a ground color.
The default value is
.I "\-g 0.2"
corresponding to a 20% gray.
.PP
If there is a sun in the description,
.I gensdaymtx
will include its contribution in the four nearest sky patches,
distributing energy according to centroid proximity.
The
.I \-d
option may be used to produce a sun-only matrix, with no sky contributions,
and the ground patch also set to zero.
Alternatively, the
.I \-s
option may be used to exclude any direct solar component from the output,
with the other sky and ground patches unaffected.
.PP
The
.I \-u
option ignores input times when the sun is below the horizon.
.PP
By default,
.I gensdaymtx
assumes the positive Y-axis points north such that the first sky patch
is in the Y-axis direction on the horizon, the second patch is just
west of that, and so on spiraling around to the final patch near the zenith.
The
.I \-r
(or
.I \-rz)
option rotates the sky the specified number of degrees counter-clockwise
about the zenith, i.e., west of north.
This is in keeping with the effect of passing the output of
.I gensky(1)
or
.I gendaylit(1)
through
.I xform(1)
using a similar transform.
.PP
The
.I \-of
or
.I \-od
option may be used to specify binary float or double output, respectively.
This is much faster to write and to read, and is therefore preferred on
systems that support it.
(MS Windows is not one of them.)\0
The
.I \-h
option prevents the output of the usual header information.
Finally, the
.I \-v
option will enable verbose reporting, which is mostly useful for
finding out how many time steps are actually in the weather tape.
.SH EXAMPLES
Produce an annual spectral sky matrix without solar direct:
.IP "" .2i
epw2wea Detroit.epw Detroit.wea -a; 
gensdaymtx -m 1 -s Detroit.wea > Detroit.mtx
.PP
Produce an hourly, annual Reinhart sky matrix
with 2306 patches including solar contributions
and send float output to
.I dctimestep(1)
to compute a sensor value matrix:
.IP "" .2i
gensdaymtx -m 4 -of VancouverBC.wea | dctimestep -if -n 8760 DCoef.mtx > res.dat
.SH AUTHORS
Taoning Wang adapted from gendaymtx
.SH "SEE ALSO"
dctimestep(1), genBSDF(1), gendaylit(1), gendaymtx(1), gensky(1), genskyvec(1),
rcollate(1), rcomb(1), rcontrib(1), rfluxmtx(1), xform(1)
Revision:	1.1
Committed:	Fri Aug 2 19:10:18 2024 UTC (10 months, 2 weeks ago) by greg
Branch:	MAIN
Log Message:	feat(gensdaymtx,epw2wea,genssky): Taoning added new gensdaymtx and updated others
#	Content
1	.\" RCSid $Id: gensdaymtx.1,v 1.16 2022/08/13 17:24:56 greg Exp $
2	.TH GENSDAYMTX 1 01/19/13 RADIANCE
3	.SH NAME
4	gensdaymtx - generate an annual spectral sky matrix from a weather tape
5	.SH SYNOPSIS
6	.B gensdaymtx
7	[
8	.B "\-v"
9	][
10	.B "\-h"
11	][
12	.B "\-d\|\-s"
13	][
14	.B "\-u"
15	]][
16	.B "\-r deg"
17	][
18	.B "\-m N"
19	][
20	.B "\-p Dir"
21	][
22	.B "\-n N"
23	][
24	.B "-o{f\|d}"
25	]
26	[
27	.B "tape.wea"
28	]
29	.SH DESCRIPTION
30	.I Gensdaymtx
31	takes a weather tape as input and produces a matrix of spectral sky patch
32	values using the precomputed atmospheric scattering model.
33	The weather tape is assumed to be in a special form of the .wea file, which contains
34	a short header with the site parameters followed
35	by the month, day, standard time, direct normal and diffuse horizontal
36	irradiance values, total cloud cover, and broadband aerosol optical depth, one time step per line.
37	Such file can be generated by
38	.I epw2wea
39	with appending
40	.I \-a
41	flag.
42	Each time step line is used to compute a column in the output matrix,
43	where rows correspond to sky patch positions, starting with 0 for
44	the ground and continuing to 145 for the zenith using the default
45	.I "\-m 1"
46	parameter setting.
47	.PP
48	.I Gensdaymtx
49	uses the OPAC continental average aerosol profile for the Mie scattering calculation.
50	For every distinct AOD value in the weather tape, a new set of the atmospheric parameters
51	is computed and stored in the atmos_data directory in the current directory, which
52	can be changed using the -p flag. This precomputation can be sped up using the
53	.I \-n NThreads
54	option. There is no speedup after NTHREADS=16.
55	.PP
56	Increasing the
57	.I \-m
58	parameter yields a higher resolution
59	sky using the Reinhart patch subdivision.
60	For example, setting
61	.I "\-m 4"
62	yields a sky with 2305 patches plus one patch for the ground.
63	Each matrix entry is in fact 20 values, corresponding to
64	spectra from 380nm to 730nm at 20nm interval (watts/sr/meter^2).
65	Thus, an hourly weather tape for an entire year would
66	yield 8760x20 (175200) values per output line (row).
67	.PP
68	The
69	.I \-g
70	option may be used to specify a ground color.
71	The default value is
72	.I "\-g 0.2"
73	corresponding to a 20% gray.
74	.PP
75	If there is a sun in the description,
76	.I gensdaymtx
77	will include its contribution in the four nearest sky patches,
78	distributing energy according to centroid proximity.
79	The
80	.I \-d
81	option may be used to produce a sun-only matrix, with no sky contributions,
82	and the ground patch also set to zero.
83	Alternatively, the
84	.I \-s
85	option may be used to exclude any direct solar component from the output,
86	with the other sky and ground patches unaffected.
87	.PP
88	The
89	.I \-u
90	option ignores input times when the sun is below the horizon.
91	.PP
92	By default,
93	.I gensdaymtx
94	assumes the positive Y-axis points north such that the first sky patch
95	is in the Y-axis direction on the horizon, the second patch is just
96	west of that, and so on spiraling around to the final patch near the zenith.
97	The
98	.I \-r
99	(or
100	.I \-rz)
101	option rotates the sky the specified number of degrees counter-clockwise
102	about the zenith, i.e., west of north.
103	This is in keeping with the effect of passing the output of
104	.I gensky(1)
105	or
106	.I gendaylit(1)
107	through
108	.I xform(1)
109	using a similar transform.
110	.PP
111	The
112	.I \-of
113	or
114	.I \-od
115	option may be used to specify binary float or double output, respectively.
116	This is much faster to write and to read, and is therefore preferred on
117	systems that support it.
118	(MS Windows is not one of them.)\0
119	The
120	.I \-h
121	option prevents the output of the usual header information.
122	Finally, the
123	.I \-v
124	option will enable verbose reporting, which is mostly useful for
125	finding out how many time steps are actually in the weather tape.
126	.SH EXAMPLES
127	Produce an annual spectral sky matrix without solar direct:
128	.IP "" .2i
129	epw2wea Detroit.epw Detroit.wea -a;
130	gensdaymtx -m 1 -s Detroit.wea > Detroit.mtx
131	.PP
132	Produce an hourly, annual Reinhart sky matrix
133	with 2306 patches including solar contributions
134	and send float output to
135	.I dctimestep(1)
136	to compute a sensor value matrix:
137	.IP "" .2i
138	gensdaymtx -m 4 -of VancouverBC.wea \| dctimestep -if -n 8760 DCoef.mtx > res.dat
139	.SH AUTHORS
140	Taoning Wang adapted from gendaymtx
141	.SH "SEE ALSO"
142	dctimestep(1), genBSDF(1), gendaylit(1), gendaymtx(1), gensky(1), genskyvec(1),
143	rcollate(1), rcomb(1), rcontrib(1), rfluxmtx(1), xform(1)