VPD Equation:
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Vapor Pressure Deficit (VPD) is the difference between the amount of moisture in the air and how much moisture the air can hold when it's saturated. It's an important metric in various fields including agriculture and meteorology, particularly in German contexts.
The calculator uses the VPD equation:
Where:
Explanation: The equation calculates the difference between the actual water vapor pressure and the saturation water vapor pressure at a particular temperature.
Details: VPD is crucial for understanding plant transpiration rates, predicting evaporation, and assessing human comfort levels in different climates.
Tips: Enter SVP in kPa and RH as a percentage (0-100). Both values must be valid (SVP > 0, RH between 0-100).
Q1: Why is VPD important in agriculture?
A: VPD helps determine the rate at which water moves from the plant to the air, affecting plant growth and water needs.
Q2: What are typical VPD values?
A: For most plants, optimal VPD ranges between 0.8-1.2 kPa, though this varies by species and growth stage.
Q3: How does temperature affect VPD?
A: Warmer air can hold more moisture, so temperature directly influences SVP and thus VPD.
Q4: Are there limitations to this calculation?
A: This is a simplified calculation that assumes standard atmospheric conditions and doesn't account for all environmental variables.
Q5: How is this calculator specific to German contexts?
A: The calculation uses metric units (kPa) which are standard in Germany and other European countries.