A water stress index that quantifies relative water content at the leaf level. The ratio of 970nm to 900nm reflectance is sensitive to water absorption features and provides information about plant water status.

Used in crop monitoring, and water detection.

When to use

  • Permanent and seasonal water body delineation
  • Flood mapping and emergency response
  • Wetland inventory and change detection
  • Reservoir and lake water level monitoring
  • Coastal shoreline change analysis
  • Plant water content assessment
  • Water stress detection

Limitations

  • Dark surfaces (shadows, asphalt, dark soils) can produce false positives
  • Suspended sediments and algae alter spectral response in shallow water
  • Mixed pixels at water boundaries reduce edge accuracy
  • Atmospheric correction quality directly impacts threshold selection
  • Sun glint over open water can saturate sensors and bias values

What the values mean

-1 Definitely not water
-0.3 Dry / built-up surface
0 Possible moisture / wet soil
0.3 Open water
0.6 Deep / clear water
Surface typeTypical PWI
Built-up, asphalt-0.5 to -0.2
Bare soil, vegetation-0.2 to 0
Wet soil, flooded fields0 to 0.3
Open water, lakes0.3 to 0.7

General Formula

nir_900 900
nir_970 970

Sensor-Specific Formulas

Most-used sensors — click to show code below

SensorProviderFormulaBand Mapping
SPACEWILLNIR2 / NIR1nir_900→NIR1, nir_970→NIR2
MAXARNIR2 / NIR1nir_900→NIR1, nir_970→NIR2
MAXARNIR2 / NIR1nir_900→NIR1, nir_970→NIR2

Spectral Band Visualization — SuperView-2

Code Examples

Adapted for SuperView-2 bands —

pwi_superview-2.py

Frequently Asked Questions

What is the PWI (Plant Water Index) and when should I use it?

A water stress index that quantifies relative water content at the leaf level. The ratio of 970nm to 900nm reflectance is sensitive to water absorption features and provides information about plant water status. Water indices exploit the strong absorption of shortwave infrared and near-infrared radiation by liquid water. They are critical for delineating water bodies, assessing moisture stress in vegetation, and monitoring hydrological changes over time. PWI is particularly suited for plant water content assessment, water stress detection, drought monitoring. The general formula is nir_970 / nir_900, which requires nir_900 and nir_970 spectral bands.

Which satellite sensors can I use to calculate PWI?

PWI is supported by 4 satellite sensors in our database, including SuperView-2, WorldView 2, WorldView 3, WorldView Legion. Each sensor uses different band designations — for example, SuperView-2 uses the formula NIR2 / NIR1, while WorldView 2 uses NIR2 / NIR1. Select a sensor above to see its specific band mapping.

What spectral bands does PWI require and why?

PWI requires nir_900 (900), nir_970 (970). Water absorbs strongly in the near-infrared and shortwave infrared portions of the spectrum, creating a measurable contrast with shorter wavelengths that penetrate the water surface.

How do I calculate PWI in Python or R?

Both Python and R code samples are provided above. In Python, use rasterio to load individual band GeoTIFF files and numpy for the arithmetic. In R, the terra package handles raster operations efficiently. The key is to load bands as floating-point arrays to avoid integer division, and to handle division-by-zero cases where the denominator equals zero. For production use, consider applying a valid data mask to exclude no-data pixels before calculation.

Can PWI distinguish water from other dark surfaces?

PWI is designed to enhance water features, but dark surfaces like shadows, asphalt, and dark soils can produce similar values. For reliable water mapping, consider combining PWI with a threshold analysis and, where possible, a secondary index to reduce false positives. Time-series analysis can also help distinguish permanent water bodies from temporary dark surfaces.

PWI vs other water indices

IndexNameHow it differs
LSWILand Surface Water IndexAlternative water index — different band combination
LWVI-1Leaf Water Vegetation Index 1Alternative water index — different band combination
LWVI-2Leaf Water Vegetation Index 2Alternative water index — different band combination
MNDWIModified Normalized Difference Water IndexRefined formulation for specific conditions

Related Water Indices

References

Peñuelas et al. (1993). The reflectance at the 950–970 nm region as an indicator of plant water status.
Datt (1999). Remote Sensing of Water Content in Eucalyptus Leaves.
Ceccato et al. (2002). Designing a spectral index to estimate vegetation water content from remote sensing data.

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