Calculate parcel temperature over time from initial and ambient temperatures, time constant, or lumped heat transfer properties.

Parcel Temperature Calculator

Time constant (ฯ„)
Lumped (mยทc)

Enter any 4 values to calculate the missing variable (uses T(t)=Tโ‚+(Tแตขโˆ’Tโ‚)e^{โˆ’t/ฯ„}).


Related Calculators

Parcel Temperature Formula

The following formulas are commonly used to estimate the temperature of a parcel over time using a lumped-capacitance (Newtonโ€™s law of cooling/heating) approximation.

Tโ‚final) & = Tโ‚ambient) + (Tแตขโ‚™แตขโ‚œแตขโ‚โ‚— - Tโ‚ambient)) eโฝ - (hA) / (m cโ‚š) t)\ & = Tโ‚ambient) + (Tแตขโ‚™แตขโ‚œแตขโ‚โ‚— - Tโ‚ambient)) eโฝ - t /), = (m cโ‚š) / (hA)

Variables:

  • T_final is the final temperature of the parcel (ยฐC, K, or ยฐF)
  • T_initial is the initial temperature of the parcel (ยฐC, K, or ยฐF)
  • T_ambient is the ambient temperature (ยฐC, K, or ยฐF)
  • h is the convective heat transfer coefficient (W/mยฒยทK or Btu/(hยทftยฒยทยฐF))
  • A is the surface area of the parcel (mยฒ, cmยฒ, or ftยฒ)
  • m is the parcel mass (kg, g, or lb)
  • c_p (c) is the specific heat capacity (J/(kgยทK) or Btu/(lbยทยฐF))
  • t is the elapsed time (seconds, minutes, or hours; use consistent units in the exponent)
  • ฯ„ is the time constant ฯ„ = m c_p / (hA) (same time unit as t)

To calculate the final temperature of a parcel, you can either (1) use the full lumped-capacitance model with h, A, m, and c_p, or (2) use the equivalent time-constant form if you already know ฯ„ (for example, from measurement). These models assume the parcel is approximately at a uniform internal temperature (lumped approximation) and that h and ambient conditions are roughly constant over the time interval.

What is Parcel Temperature?

Parcel temperature refers to the temperature of a package or container, which can change over time due to heat transfer with its surroundings. This is particularly important in the context of shipping temperature-sensitive goods, where maintaining a specific temperature range is crucial. In a simple lumped-capacitance model, the rate at which a parcelโ€™s temperature approaches ambient depends on both the external heat transfer (h and surface area A) and the parcelโ€™s thermal mass (mยทc_p).

How to Calculate Parcel Temperature?

The following steps outline how to calculate the final temperature of a parcel.


  1. Determine the initial temperature of the parcel (T_initial).
  2. Determine the ambient temperature (T_ambient).
  3. If using the time-constant method, determine the time constant ฯ„ (for example, from measurement). If using the lumped method, determine h, surface area A, mass m, and specific heat capacity c_p.
  4. Determine the elapsed time t (use seconds, minutes, or hours, but keep units consistent with ฯ„ or within the exponent).
  5. Calculate the final temperature (T_final) using the formula provided (or use the calculator above).

Example Problem : 

Use the following variables as an example problem to test your knowledge.

Initial temperature of the parcel (T_initial) = 5ยฐC

Ambient temperature (T_ambient) = 25ยฐC

Heat transfer coefficient (h) = 5 W/mยฒK

Surface area of the parcel (A) = 0.50 mยฒ

Mass (m) = 5 kg

Specific heat capacity (c_p) = 900 J/kgยทK

Time (t) = 3 hours

(For these values, the time constant is ฯ„ = m c_p /(hA) = 1800 s = 0.5 hr, giving T_final โ‰ˆ 24.95ยฐC after 3 hours.)