Water Dynamic (Absolute) and Kinematic Viscosity Calculator

Water Dynamic (Absolute) Viscosity Chart

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Data from Engineering Toolbox — Water Viscosity. Y-axis is logarithmic.

Water Kinematic Viscosity Chart

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Kinematic viscosity in cSt converted from tabulated ft²/s values. Y-axis is logarithmic.

Water Viscosity Calculator
Degrees (°F):
Degrees (°C):
Dynamic (Absolute) Viscosity
mPa·s (= cP):  
Centipoise (cP):  
Poise (g/(cm·s)):  
Pa·s (Poiseuille):  
lbm/(ft·s):  
kg/(m·h):  
Kinematic Viscosity
mm²/s (= cSt):  
Centistokes (cSt):  
Stokes (cm²/s):  
m²/s:  
in²/s:  
ft²/s:  
Dynamic (Absolute) Viscosity of Water
What Is Dynamic (Absolute) Viscosity?

Dynamic (absolute) viscosity (μ) measures a fluid's resistance to shear flow. It is measured in mPa·s (millipascal-seconds), equivalent to cP (centipoise). Newton's law of viscosity is:

τ = μ × (du / dy)

where τ is shear stress and du/dy is the velocity gradient perpendicular to flow.

Why It Matters for Water Systems

Water viscosity decreases significantly with increasing temperature — by nearly a factor of 30 from 32°F to 675°F. This affects pressure drop, pump power requirements, and flow regime. The Reynolds number determines whether flow is laminar or turbulent:

Re = ρ × v × D / μ

At low temperatures, higher viscosity can push systems toward laminar flow (Re < 2300) where heat transfer efficiency drops sharply. At elevated temperatures and pressures (above 212°F), water remains liquid only under pressure — the saturation pressure values in the data table reflect this condition.

Note: Viscosity is highly temperature-dependent. Always check viscosity at the lowest expected operating temperature, not just at design conditions.

Dynamic (Absolute) vs. Kinematic Viscosity
Dynamic (Absolute) Viscosity — μ

Dynamic viscosity (also called absolute viscosity or static viscosity) measures a fluid's resistance to shear — the internal force per unit area required to make one layer of fluid slide past another. It is independent of density. The SI unit is the pascal-second (Pa·s); the common engineering unit is the millipascal-second (mPa·s), numerically equal to centipoise (cP).

τ = μ × (du / dy)

where τ is shear stress [Pa] and du/dy is the velocity gradient [s⁻¹].

Kinematic Viscosity — ν

Kinematic viscosity is the ratio of dynamic viscosity to fluid density. It describes how easily a fluid flows under the influence of gravity or pressure, without needing to separately account for the applied force. The SI unit is m²/s; the common unit is mm²/s, numerically equal to centistokes (cSt).

ν = μ / ρ

Relationship and Unit Conversion

Kinematic viscosity is derived from dynamic viscosity and density:

ν [cSt] = μ [mPa·s] × 1000 / ρ [kg/m³]

Because water has a density very close to 1000 kg/m³ near room temperature, its kinematic viscosity in cSt is numerically very close to its dynamic viscosity in cP. At elevated temperatures, water density decreases, so kinematic viscosity diverges slightly above the cP value.

When to Use Each

Use dynamic (absolute) viscosity for: pump power calculations, pipe pressure drop (Darcy–Weisbach), Reynolds number (Re = ρvD/μ), and any situation where force or stress is the driving input.

Use kinematic viscosity for: gravity-driven flow, lubrication ratings, most viscometer measurements, and flow calculations where density is already embedded in the formula (e.g., Stokes' law, ASTM oil viscosity grades).

Note: "Absolute viscosity" and "static viscosity" are synonyms for dynamic viscosity — they all refer to the same physical property. "Static" distinguishes it from apparent viscosity measured at elevated shear rates in non-Newtonian fluids.

Viscosity Unit Conversion Reference
Dynamic (Absolute) Viscosity

Units: centipoise (cP), poise (P), pascal-second (Pa·s), pound/(foot second) (lb/(ft·s)), pound/(foot hour) (lb/(ft·h))

  • 1 cP = 0.001 Pa·s = 0.01 P = 6.72197×10⁻⁴ lb/(ft·s) = 2.4191 lb/(ft·h)
  • 1 lb/(ft·h) = 2.7778×10⁻⁴ lb/(ft·s) = 4.1338×10⁻⁴ Pa·s = 0.41338 cP
  • 1 lb/(ft·s) = 3600 lb/(ft·h) = 1.48816 Pa·s = 1488.16 cP
  • 1 Pa·s = 1 kg/(m·s) = 1 (N·s)/m² = 10 P = 1000 cP = 0.672197 lb/(ft·s) = 2419.08 lb/(ft·h)
  • 1 P = 1 g/(cm·s) = 0.1 Pa·s = 100 cP = 0.067197 lb/(ft·s) = 241.909 lb/(ft·h)
  • 1 Pa·s = 0.00014504 reyn; 1 reyn = 6894.76 Pa·s
Kinematic Viscosity

Units: centistoke (cSt), stoke (St), ft²/s, ft²/h, in²/s, m²/s

  • 1 cSt = 1 mm²/s = 10⁻⁶ m²/s = 1.07639×10⁻⁵ ft²/s = 0.03875 ft²/h = 1.55×10⁻³ in²/s
  • 1 St = 1 cm²/s = 100 cSt = 10⁻⁴ m²/s = 1.076×10⁻³ ft²/s = 3.875 ft²/h
  • 1 ft²/s = 92903 cSt = 929.03 St = 0.09290 m²/s = 3600 ft²/h = 144 in²/s
  • 1 ft²/h = 2.7778×10⁻⁴ ft²/s = 25.806 cSt = 0.25806 St
  • 1 in²/s = 6.944×10⁻³ ft²/s = 645.16 cSt = 6.4516 St
  • 1 m²/s = 10⁶ cSt = 10⁴ St = 10.764 ft²/s = 1550 in²/s
Water — Viscosity vs. Temperature (°F)
Temp
(°F)
Pressure
(psia)
Dynamic Viscosity Kinematic Viscosity
lbf·s/ft²
(×10⁻⁵)
lbm/(ft·h) cP (mPa·s) ft²/s
(×10⁻⁵)
32.020.95063.74144.33361.79141.9287
340.09623.60474.17521.72591.8579
39.20.11803.28013.79921.57051.6906
400.12173.23403.74581.54841.6668
500.17812.72763.15931.30601.4063
600.25632.34052.71091.12061.2075
700.36342.03372.35560.97371.0503
800.50761.78882.07190.85650.9250
900.69921.58961.84110.76110.8234
1000.95061.42431.64970.68200.7392
1101.2771.28471.48800.61510.6682
1201.6951.16521.34960.55790.6075
1302.2261.06201.23000.50850.5551
1402.8930.97331.12730.46600.5102
1503.7230.89501.03660.42850.4706
1604.7470.82790.95890.39640.4367
1706.0000.76980.89160.36860.4074
1807.5200.71920.83300.34440.3820
1909.3490.67450.78130.32300.3596
20011.5370.63000.72970.30160.3371
21214.7100.58810.68120.28160.3163
22017.2030.56190.65080.26900.3032
24025.0010.50500.58500.24180.2750
26035.2630.45750.52990.21910.2515
28049.2860.41760.48370.20000.2320
30067.2640.38400.44480.18390.2157
350134.730.32020.37080.15330.1853
400247.010.27500.31850.13170.1648
450422.320.24040.27850.11510.1504
500680.560.21260.24630.10180.1398
5501045.00.18880.21870.09040.1322
6001542.10.16730.19370.08010.1270
6251851.20.15620.18090.07480.1252
6502207.80.14380.16660.06890.1239
6752618.70.12920.14960.06190.1230

Data at saturation pressure. Below 212 °F this is effectively atmospheric pressure.

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