i.vi(1grass)
π i.vi β the grass manual but make it cute π
okay bestie, so this is i.vi from the GRASS User's Manual, and it's genuinely one of the most iconic ones because it's all about vegetation indices π±β¨. Like, plant vibes, quantified. Let's get into it, no skips, no skimming, we're doing the whole thing.
β¨ NAME β¨
i.vi β bestie it calculates different types of vegetation indices. That's the whole job, that's the main character energy right there.
It uses the red and nir bands mostly (nir = near infrared, iykyk), and honestly some of the indices need extra bands too, so don't come at it with just two bands and expect every single one to work. The module is very "come prepared" about it.
π KEYWORDS π
imageryvegetation indexbiophysical parametersNDVI
π SYNOPSIS π
okay here's the vibe, exactly as it goes:
i.vi
i.vi --help
i.vi output=name viname=type [red=name] [nir=name] [green=name]
[blue=name] [band5=name] [band7=name] [soil_line_slope=float]
[soil_line_intercept=float] [soil_noise_reduction=float]
[storage_bit=integer] [--overwrite] [--help] [--verbose] [--quiet]
[--ui]
note that output and viname are the only ones doing the absolute most without brackets β they're required, everything else in square brackets is optional π
π«Ά Flags π«Ά
--overwriteβ lets your output files just bulldoze whatever existing files are in the way. Yes, it overwrites them. Be so careful with this one, bestie, it does not ask twice.--helpβ prints the usage summary. If you're lost, she'll catch you up π--verboseβ verbose module output, aka the module yaps at you about what it's doing. Some of us love that.--quietβ quiet module output. The opposite. Silence. Peace. π¦--uiβ forces the GUI dialog to launch, so you can click around instead of typing.
πΈ Parameters πΈ
output=name[required] β the name for your output raster map. This one is mandatory, no exceptions, she needs to know where to put the goods.viname=type[required] β the parameter, honestly. This is the type of vegetation index you want.
Options: arvi, ci, dvi, evi, evi2, gvi, gari, gemi, ipvi, msavi, msavi2, ndvi, ndwi, pvi, savi, sr, vari, wdvi
Default: ndvi
And here's the full roster with what each one actually is, because I'm not gatekeeping:
arvi: Atmospherically Resistant Vegetation Indexci: Crust Indexdvi: Difference Vegetation Indexevi: Enhanced Vegetation Indexevi2: Enhanced Vegetation Index 2gvi: Green Vegetation Indexgari: Green Atmospherically Resistant Vegetation Indexgemi: Global Environmental Monitoring Indexipvi: Infrared Percentage Vegetation Indexmsavi: Modified Soil Adjusted Vegetation Indexmsavi2: second Modified Soil Adjusted Vegetation Indexndvi: Normalized Difference Vegetation Indexndwi: Normalized Difference Water Indexpvi: Perpendicular Vegetation Indexsavi: Soil Adjusted Vegetation Indexsr: Simple Ratiovari: Visible Atmospherically Resistant Indexwdvi: Weighted Difference Vegetation Index
red=nameβ name of the input red channel surface reflectance map. Range:[0.0;1.0]β keep it in that range, she checks.nir=nameβ name of the input nir channel surface reflectance map. Range:[0.0;1.0]. This is the one most indices are obsessed with.green=nameβ name of the input green channel surface reflectance map. Range:[0.0;1.0].blue=nameβ name of the input blue channel surface reflectance map. Range:[0.0;1.0].band5=nameβ name of the input 5th channel surface reflectance map. Range:[0.0;1.0].band7=nameβ name of the input 7th channel surface reflectance map. Range:[0.0;1.0].soil_line_slope=floatβ the value of the slope of the soil line. Only used byMSAVIandPVI, so if you're not running those, this is just sitting there.soil_line_intercept=floatβ the value of the intercept of the soil line.MSAVIonly bestie, don't waste it elsewhere.soil_noise_reduction=floatβ the value of the factor of reduction of soil noise.MSAVIonly again. Soil is loud, this turns it down.storage_bit=integerβ maximum bits for digital numbers.
And here's the important bit: if your data is in Digital Numbers (i.e. integer type), give the max bits β like 8 for Landsat, which maps to [0-255].
Options: 7, 8, 10, 16
Default: 8
not me being the responsible one but fr fr, read the parameter list properly before you run her. half the confusion people have withi.viis just pickingvinameand then not supplying the bands that index actually needs π
π DESCRIPTION π
okay so bestie, i.vi is the module that calculates vegetation indices based on biophysical parameters. that's the whole job. it's giving calculator but make it earth-observation. π±
here's the full roster of indices it can do for you:
- ARVI: Atmospherically Resistant Vegetation Index
- CI: Crust Index
- DVI: Difference Vegetation Index
- EVI: Enhanced Vegetation Index
- EVI2: Enhanced Vegetation Index 2
- GARI: Green atmospherically resistant vegetation index
- GEMI: Global Environmental Monitoring Index
- GVI: Green Vegetation Index
- IPVI: Infrared Percentage Vegetation Index
- MSAVI2: second Modified Soil Adjusted Vegetation Index
- MSAVI: Modified Soil Adjusted Vegetation Index
- NDVI: Normalized Difference Vegetation Index
- NDWI: Normalized Difference Water Index
- PVI: Perpendicular Vegetation Index
- RVI: ratio vegetation index
- SAVI: Soil Adjusted Vegetation Index
- SR: Simple Vegetation ratio
- WDVI: Weighted Difference Vegetation Index
π Background for users new to remote sensing π°οΈ
Vegetation Indices are often considered the entry point of remote sensing for Earth land monitoring, bestie. and honestly? they are suffering from their success, in terms that often people tend to harvest satellite images from online sources and use them directly in this module. π like ma'am. please.
From Digital number to Radiance β¨
Satellite imagery is commonly stored in Digital Number (DN) for storage purposes; e.g., Landsat5 data is stored in 8bit values (ranging from 0 to 255), other satellites maybe stored in 10 or 16 bits. If the data is provided in DN, this implies that this imagery is "uncorrected". What this means is that the image is what the satellite sees at its position and altitude in space (stored in DN). This is not the signal at ground yet. We call this data at-satellite or at-sensor. Encoded in the 8bits (or more) is the amount of energy sensed by the sensor inside the satellite platform. This energy is called radiance-at-sensor.
Generally, satellites image providers encode the radiance-at-sensor into 8bit (or more) through an affine transform equation (y=ax+b). In case of using Landsat imagery, look at the i.landsat.toar for an easy way to transform DN to radiance-at-sensor. If using Aster data, try the i.aster.toar module. π
From Radiance to Reflectance π
Finally, once having obtained the radiance at sensor values, still the atmosphere is between sensor and Earth's surface. This fact needs to be corrected to account for the atmospheric interaction with the sun energy that the vegetation reflects back into space. This can be done in two ways for Landsat:
- the simple way is through
i.landsat.toar, use e.g. theDOScorrection - the more accurate way is by using
i.atcorr(which works for many satellite sensors) π
Once the atmospheric correction has been applied to the satellite data, data vales are called surface reflectance. Surface reflectance is ranging from 0.0 to 1.0 theoretically (and absolutely). This level of data correction is the proper level of correction to use with i.vi. periodt. π
πΏ Vegetation Indices πΏ
ARVI: Atmospheric Resistant Vegetation Index π
ARVI is resistant to atmospheric effects (in comparison to the NDVI) and is accomplished by a self correcting process for the atmospheric effect in the red channel, using the difference in the radiance between the blue and the red channels (Kaufman and Tanre 1996).
arvi( redchan, nirchan, bluechan )
ARVI = (nirchan - (2.0*redchan - bluechan)) /
( nirchan + (2.0*redchan - bluechan))
CI: Crust Index π¦
Advantage is taken of a unique spectral feature of soil biogenic crust containing cyanobacteria. It has been shown that the special phycobilin pigment in cyanobacteria contributes in producing a relatively higher reflectance in the blue spectral region than the same type of substrate without the biogenic crust. The spectral crust index (CI) is based on the normalized difference between the RED and the BLUE spectral values (Karnieli, 1997, DOI: 10.1080/014311697218368).
ci ( bluechan, redchan )
CI = 1 - (redchan - bluechan) /
(redchan + bluechan)
DVI: Difference Vegetation Index β
dvi( redchan, nirchan )
DVI = ( nirchan - redchan )
EVI: Enhanced Vegetation Index π
The enhanced vegetation index (EVI) is an optimized index designed to enhance the vegetation signal with improved sensitivity in high biomass regions and improved vegetation monitoring through a de-coupling of the canopy background signal and a reduction in atmosphere influences (Huete A.R., Liu H.Q., Batchily K., van Leeuwen W. (1997). A comparison of vegetation indices global set of TM images for EOS-MODIS. Remote Sensing of Environment, 59:440-451).
evi( bluechan, redchan, nirchan )
EVI = 2.5 * ( nirchan - redchan ) /
( nirchan + 6.0 * redchan - 7.5 * bluechan + 1.0 )
EVI2: Enhanced Vegetation Index 2 ππ
A 2-band EVI (EVI2), without a blue band, which has the best similarity with the 3-band EVI, particularly when atmospheric effects are insignificant and data quality is good (Zhangyan Jiang ; Alfredo R. Huete ; Youngwook Kim and Kamel Didan 2-band enhanced vegetation index without a blue band and its application to AVHRR data. Proc. SPIE 6679, Remote Sensing and Modeling of Ecosystems for Sustainability IV, 667905 (october 09, 2007) doi:10.1117/12.734933).
evi2( redchan, nirchan )
EVI2 = 2.5 * ( nirchan - redchan ) /
( nirchan + 2.4 * redchan + 1.0 )
GARI: green atmospherically resistant vegetation index π’
The formula was actually defined: Gitelson, Anatoly A.; Kaufman, Yoram J.; Merzlyak, Mark N. (1996) Use of a green channel in remote sensing of global vegetation from EOS- MODIS, Remote Sensing of Environment 58 (3), 289-298. doi:10.1016/s0034-4257(96)00072-7
gari( redchan, nirchan, bluechan, greenchan )
GARI = ( nirchan - (greenchan - (bluechan - redchan))) /
( nirchan + (greenchan - (bluechan - redchan)))
GEMI: Global Environmental Monitoring Index π
gemi( redchan, nirchan )
GEMI = (( (2*((nirchan * nirchan)-(redchan * redchan)) +
1.5*nirchan+0.5*redchan) / (nirchan + redchan + 0.5)) *
(1 - 0.25 * (2*((nirchan * nirchan)-(redchan * redchan)) +
1.5*nirchan+0.5*redchan) / (nirchan + redchan + 0.5))) -
( (redchan - 0.125) / (1 - redchan))
GVI: Green Vegetation Index π²
gvi( bluechan, greenchan, redchan, nirchan, chan5chan, chan7chan)
GVI = ( -0.2848 * bluechan - 0.2435 * greenchan -
0.5436 * redchan + 0.7243 * nirchan + 0.0840 * chan5chan-
0.1800 * chan7chan)
IPVI: Infrared Percentage Vegetation Index π₯
ipvi( redchan, nirchan )
IPVI = nirchan/(nirchan+redchan)
MSAVI2: second Modified Soil Adjusted Vegetation Index πͺ¨
msavi2( redchan, nirchan )
MSAVI2 = (1/2)*(2*NIR+1-sqrt((2*NIR+1)^2-8*(NIR-red)))
MSAVI: Modified Soil Adjusted Vegetation Index πͺ¨βοΈ
msavi( redchan, nirchan )
MSAVI = s(NIR-s*red-a) / (a*NIR+red-a*s+X*(1+s*s))
where a is the soil line intercept, s is the soil line slope, and X is an adjustment factor which is set to minimize soil noise (0.08 in original papers).
NDVI: Normalized Difference Vegetation Index π
ndvi( redchan, nirchan )
Satellite specific band numbers ([NIR, Red]):
MSS Bands = [ 7, 5]
TM1-5,7 Bands = [ 4, 3]
TM8 Bands = [ 5, 4]
Sentinel-2 Bands = [ 8, 4]
AVHRR Bands = [ 2, 1]
SPOT XS Bands = [ 3, 2]
AVIRIS Bands = [51, 29]
NDVI = (NIR - Red) / (NIR + Red)
NDWI: Normalized Difference Water Index (after McFeeters, 1996) π§
This index is suitable to detect water bodies. π
ndwi( greenchan, nirchan )
NDWI = (green - NIR) / (green + NIR)
The water content of leaves can be estimated with another NDWI (after Gao, 1996):
ndwi( greenchan, nirchan )
NDWI = (NIR - SWIR) / (NIR + SWIR)
This index is important for monitoring vegetation health (not implemented).
PVI: Perpendicular Vegetation Index π
pvi( redchan, nirchan, soil_line_slope )
PVI = sin(a)NIR-cos(a)red
SAVI: Soil Adjusted Vegetation Index πͺ¨π±
savi( redchan, nirchan )
SAVI = ((1.0+0.5)*(nirchan - redchan)) / (nirchan + redchan +0.5)
SR: Simple Vegetation ratio β
sr( redchan, nirchan )
SR = (nirchan/redchan)
VARI: Visible Atmospherically Resistant Index π¨
VARI was designed to introduce an atmospheric self-correction (Gitelson A.A., Kaufman Y.J., Stark R., Rundquist D., 2002. Novel algorithms for estimation of vegetation fraction Remote Sensing of Environment (80), pp76-87.)
vari = ( bluechan, greenchan, redchan )
VARI = (green - red ) / (green + red - blue)
WDVI: Weighted Difference Vegetation Index βοΈ
wdvi( redchan, nirchan, soil_line_weight )
WDVI = nirchan - a * redchan
if(soil_weight_line == None):
a = 1.0 #slope of soil line
π₯ EXAMPLES π₯
okay bestie this is the part where it gets real β¨ all the vibes, all the actual runnable stuff. let's go π
π Calculation of DVI
the way you get DVI out of your reflectance values is literally this:
g.region raster=band.1 -p
i.vi blue=band.1 red=band.3 nir=band.4 viname=dvi output=dvi
r.univar -e dvi
π Calculation of EVI
and EVI? same energy, different index:
g.region raster=band.1 -p
i.vi blue=band.1 red=band.3 nir=band.4 viname=evi output=evi
r.univar -e evi
π Calculation of EVI2
EVI2, she's lowkey the simpler sister π:
g.region raster=band.3 -p
i.vi red=band.3 nir=band.4 viname=evi2 output=evi2
r.univar -e evi2
π Calculation of GARI
GARI time, and yes she needs blue + green + red + nir, the whole squad fr:
g.region raster=band.1 -p
i.vi blue=band.1 green=band.2 red=band.3 nir=band.4 viname=gari output=gari
r.univar -e gari
π Calculation of GEMI
GEMI, no blue needed, she's chill:
g.region raster=band.3 -p
i.vi red=band.3 nir=band.4 viname=gemi output=gemi
r.univar -e gemi
π Calculation of GVI
GVI β aka the Green Vegetation Index, Tasseled Cap edition π β comes outta your reflectance values like so:
g.region raster=band.3 -p
# assuming Landsat-7
i.vi blue=band.1 green=band.2 red=band.3 nir=band.4 band5=band.5 band7=band.7 viname=gvi output=gvi
r.univar -e gvi
(that little comment in there is doing the heavy lifting ngl, she's assuming Landsat-7 π«Ά)
π Calculation of IPVI
IPVI bestie, so simple:
g.region raster=band.3 -p
i.vi red=band.3 nir=band.4 viname=ipvi output=ipvi
r.univar -e ipvi
π Calculation of MSAVI
MSAVI, the soil-adjusted icon:
g.region raster=band.3 -p
i.vi red=band.3 nir=band.4 viname=msavi output=msavi
r.univar -e msavi
π Calculation of NDVI
NDVI. the main character. the moment. π
g.region raster=band.3 -p
i.vi red=band.3 nir=band.4 viname=ndvi output=ndvi
r.univar -e ndvi
π Calculation of NDWI
NDWI needs green + nir, and here we're also slapping a colour table on it because we're extra:
g.region raster=band.2 -p
i.vi green=band.2 nir=band.4 viname=ndwi output=ndwi
r.colors ndwi color=byg -n
r.univar -e ndwi
π Calculation of PVI
PVI! note the soil_line_slope=0.45, she's got a slope parameter bestie:
g.region raster=band.3 -p
i.vi red=band.3 nir=band.4 soil_line_slope=0.45 viname=pvi output=pvi
r.univar -e pvi
π Calculation of SAVI
SAVI serving soil-adjusted realness:
g.region raster=band.3 -p
i.vi red=band.3 nir=band.4 viname=savi output=savi
r.univar -e savi
π Calculation of SR
SR, the simplest ratio lil baby πΈ:
g.region raster=band.3 -p
i.vi red=band.3 nir=band.4 viname=sr output=sr
r.univar -e sr
π Calculation of VARI
VARI, and heads up bestie, look at those band numbers π they go blue=band.2 green=band.3 red=band.4 β she's numbered differently, don't @ me:
g.region raster=band.3 -p
i.vi blue=band.2 green=band.3 red=band.4 viname=vari output=vari
r.univar -e vari
π Landsat TM7 example π
these next ones are all based on a LANDSAT TM7 scene that lives inside the North Carolina sample dataset π¦
π§ Preparation: DN to reflectance
so step one, step ONE, is that those raw DN (digital number) pixel values must get converted to reflectance using i.landsat.toar. and to do that we make a copy (or you can rename the channels, dealer's choice) so the names match what i.landsat.toar wants as input β its input scheme, iykyk:
g.copy raster=lsat7_2002_10,lsat7_2002.1
g.copy raster=lsat7_2002_20,lsat7_2002.2
g.copy raster=lsat7_2002_30,lsat7_2002.3
g.copy raster=lsat7_2002_40,lsat7_2002.4
g.copy raster=lsat7_2002_50,lsat7_2002.5
g.copy raster=lsat7_2002_61,lsat7_2002.61
g.copy raster=lsat7_2002_62,lsat7_2002.62
g.copy raster=lsat7_2002_70,lsat7_2002.7
g.copy raster=lsat7_2002_80,lsat7_2002.8
then we calculate the reflectance values from DN using DOS1 (metadata obtained from p016r035_7x20020524.met.gz, periodt):
i.landsat.toar input=lsat7_2002. output=lsat7_2002_toar. sensor=tm7 \
method=dos1 date=2002-05-24 sun_elevation=64.7730999 \
product_date=2004-02-12 gain=HHHLHLHHL
and the resulting Landsat channels get named lsat7_2002_toar.1 .. lsat7_2002_toar.8. slay β¨
π§ Calculation of NDVI
calculating NDVI from those reflectance values, here's the whole ritual:
g.region raster=lsat7_2002_toar.3 -p
i.vi red=lsat7_2002_toar.3 nir=lsat7_2002_toar.4 viname=ndvi \
output=lsat7_2002.ndvi
r.colors lsat7_2002.ndvi color=ndvi
d.mon wx0
d.rast.leg lsat7_2002.ndvi
North Carolina dataset: NDVI
π§ Calculation of ARVI
ARVI from the reflectance values, same vibe, ARVI edition:
g.region raster=lsat7_2002_toar.3 -p
i.vi blue=lsat7_2002_toar.1 red=lsat7_2002_toar.3 nir=lsat7_2002_toar.4 \
viname=arvi output=lsat7_2002.arvi
d.mon wx0
d.rast.leg lsat7_2002.arvi
North Carolina dataset: ARVI
π§ Calculation of GARI
and GARI from the reflectance values, she wants all four bands:
g.region raster=lsat7_2002_toar.3 -p
i.vi blue=lsat7_2002_toar.1 green=lsat7_2002_toar.2 red=lsat7_2002_toar.3 \
nir=lsat7_2002_toar.4 viname=gari output=lsat7_2002.gari
d.mon wx0
d.rast.leg lsat7_2002.gari
North Carolina dataset: GARI
π NOTES π
this module originally came from kepler.gps.caltech.edu (an FAQ), and here's the whole citation because we give credit in this house π«Ά:
A FAQ on Vegetation in Remote Sensing Written by Terrill W. Ray, Div. of Geological and Planetary Sciences, California Institute of Technology, email: terrill@mars1.gps.caltech.edu Snail Mail: Terrill Ray Division of Geological and Planetary Sciences Caltech, Mail Code 170-25 Pasadena, CA 91125
π REFERENCES π
AVHRR, Landsat TM5:
- Bastiaanssen, W.G.M., 1995. Regionalization of surface flux densities and moisture indicators in composite terrain; a remote sensing approach under clear skies in mediterranean climates. PhD thesis, Wageningen Agricultural Univ., The Netherland, 271 pp. (PDF)
- Index DataBase: List of available Indices
π SEE ALSO π
i.albedo, i.aster.toar, i.landsat.toar, i.atcorr, i.tasscap
like, go read those too bestie, they're the whole ecosystem π
π AUTHORS π
- Baburao Kamble, Asian Institute of Technology, Thailand
- Yann Chemin, Asian Institute of Technology, Thailand
π» SOURCE CODE π»
Available at: i.vi source code (history)
Latest change: Saturday Feb 15 00:20:39 2025 in commit: ea58114c806f4f003104995f3d1798d8e7aceb8a
Main index | Imagery index | Topics index | Keywords index | Graphical index | Full index
Β© 2003-2026 GRASS Development Team, GRASS 8.5.0 Reference Manual
anyway that's the whole page bestie, you ate π
β¨ this was the GRASS 8.5.0 reference manual page for i.vi(1grass) β go forth and compute vegetation indices, you gorgeous nerd π¦π
π¦ where this page comes from
- alpine 3.24: grass-gis-doc 8.5.0-r1 Β· GPL-2.0-or-later
- ubuntu stonking: grass-doc 8.5.0-1ubuntu1 Β· GPL-2.0-or-later
- π girlified by deepseek-ai/DeepSeek-V4.1-Flash on : a language model's rewrite of the original, under its terms