Skip to main content

Grashof Number Natural Convection Calculator

In natural (free) convection, fluid motion is driven entirely by density differences resulting from temperature gradients in a gravitational field.

Temperature of hot (or cold) heat transfer surface.

Undisturbed bulk fluid temperature.

Vertical height of plate or diameter of cylinder.

Fluid kinematic viscosity at film temperature (default air ~ 1.58e-5).

Thermal expansion coefficient (for ideal gas, beta = 1/T_film).

Calculated Result
9.133e+8

Grashof Number (Gr)

Flow Regime

Laminar Free Convection (Gr < 10^9)

Mean Film Temperature

50.0 °C

Temperature Difference (ΔT)

60.0 K

Calculation Breakdown

  1. Gr = g·β·ΔT·L³ / ν²9.133e+8
  2. Regime Threshold: Gr ~ 10⁹Laminar Free Convection (Gr < 10^9)

What Is the Grashof Number Natural Convection Calculator?

The Grashof number (Gr) characterizes the strength of buoyancy-driven natural convection relative to viscous resistance.

Combined with the Prandtl number, it forms the Rayleigh number (Ra = Gr * Pr).

How Does the Grashof Number Natural Convection Calculator Work?

Calculates film temperature T_film and temperature differential Delta T.

Evaluates Gr = g * beta * Delta T * L^3 / nu^2.

Classifies the boundary layer into laminar (Gr < 10^9) or turbulent (Gr >= 10^9).

Grashof Number Natural Convection Calculator Formula & Variables

The core mathematical equation utilized by this calculator is expressed as:

\text{Gr} = \frac{g \beta (T_s - T_\infty) L^3}{\nu^2}, \quad T_{film} = \frac{T_s + T_\infty}{2}

Ratio of buoyant forces to viscous viscous shear forces in natural convection.

How to Use the Grashof Number Natural Convection Calculator

  1. Enter surface temperature and ambient fluid temperature in °C.
  2. Enter characteristic height or diameter in meters.
  3. Optionally supply fluid viscosity and thermal expansion coefficient.

Step-by-Step Example Calculation

Vertical Heated Electronic Enclosure Wall

Input Values:

surfaceTempC:80
ambientFluidTempC:20
characteristicLengthM:0.5
kinematicViscosityM2S:0.0000158
thermalExpansionBetaPerK:0.0031
Worked Steps: Natural air convection cooling on a 0.5 m vertical electronics chassis.

Understanding Your Result

Gr < 10^9 indicates smooth, laminar boundary layer flow.

Gr >= 10^9 indicates turbulent transition with swirling vortices and enhanced heat transfer.

Factors That Affect the Result

  • Scale length L: Grashof number scales with the cube of length (L^3); doubling height increases Gr by 8-fold.
  • Gravity: In microgravity (spacecraft), Gr drops to zero and natural convection ceases.

When Should You Use This Calculator?

  • Passive cooling design of electronics, solar collectors, and architectural heating radiators.
  • Assessing whether natural convection can be neglected in forced convection flows (Gr / Re^2 << 1).

Assumptions & Limitations

  • Assumes Boussinesq approximation (constant fluid properties except density in gravity term).
  • Assumes steady-state laminar or turbulent boundary layer flow.

Frequently Asked Questions

Calculation Accuracy & Reference Note

Standard dimensionless formulation in transport phenomena (Incropera & DeWitt).

Explore more tools and calculators in Physics Calculators