Accurate thermophysical properties of pure water at atmospheric pressure. Based on IAPWS 2008 formulation and NIST standard reference data. Instantly compute dynamic viscosity (mPa·s / cP), kinematic viscosity (cSt / mm²/s), and density (kg/m³) for any temperature between 0°C and 100°C.
Water viscosity is a critical parameter in fluid dynamics, heat transfer, and industrial processes. The calculator implements the IAPWS 2008 formulation for the viscosity of ordinary water substance, which agrees with experimental data within ±0.5% for 20–100°C at atmospheric pressure (slightly larger deviation near 0°C, <2%). The dynamic viscosity μ (Pa·s) is given by the Vogel-Fulcher-Tammann type correlation:
where TK is the absolute temperature in Kelvin. This empirical correlation is widely adopted in engineering references (NIST, CRC Handbook). The kinematic viscosity is derived as ν = μ / ρ, with density ρ calculated from the IAPWS-95 based high-accuracy rational function (Thiesen–Scheel–Diesselhorst form) valid for 0–100°C:
Both formulas are valid for pure, air-free water at standard atmospheric pressure (0.101325 MPa). The tool provides immediate output in common engineering units: dynamic viscosity in centipoise (cP = mPa·s) and kinematic viscosity in centistokes (cSt = mm²/s).
Unlike gases, liquid water viscosity decreases exponentially with rising temperature. At 0°C, dynamic viscosity is ≈1.792 cP; at 100°C it drops to ≈0.282 cP — a reduction of about 84%. This strong dependence governs many natural phenomena (ocean currents, magma flow analogs) and engineering operations (selecting optimal operating temperatures).
| Temperature (°C) | Dynamic Viscosity (cP) | Kinematic Viscosity (cSt) | Density (kg/m³) |
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* Reference data computed using the IAPWS-consistent formulation — all values match the interactive calculator output.
For most engineering applications (< 10 MPa), pressure influence on liquid water viscosity is negligible (< 1%). However, in deep-sea or high-pressure systems, a correction factor may be applied. Salinity increases viscosity slightly: seawater at 20°C has about 2–5% higher dynamic viscosity than fresh water. The present calculator focuses on pure water, providing the baseline property essential for more complex mixtures using standard mixing rules.
An engineer designing a district heating network uses water at 80°C. The kinematic viscosity at 80°C is approximately 0.365 cSt, versus 1.00 cSt at 20°C. Using the incorrect (cold) viscosity would overestimate pressure drop by factor of 2.7, leading to oversized pumps and excessive capital cost. Our calculator instantly provides the correct value, ensuring accurate hydraulic modeling and energy-efficient system design.