PTR integrates rainfall and land surface temperature to measure climate stress on vegetation.
High PTR indicates favorable moisture and cooler conditions, while low PTR indicates heat–dry stress.
1. Scientific Definition
PTR relates rainfall availability to thermal conditions. It is widely used in
crop-climate analysis, drought studies, and vegetation stress assessment.
Formula
PTR = Rain / LST
Interpretation
PTR high → good moisture + cooler temperatures (healthy vegetation)