Cumulative Emissions to Temperature Rise Calculator

Estimate global warming from cumulative CO2 emissions using the approximately linear TCRE relationship.

🌡️ Cumulative Emissions to Temperature Rise Calculator
Cumulative CO2 emissions2500
GtCO2
06000
TCRE (transient climate response to cumulative emissions)
°C / 1000 GtCO2
0.270.63
Central warming estimate
—
Low bound (TCRE 0.27)
—
High bound (TCRE 0.63)
—
Step-by-step working

🌡️ What is the Cumulative Emissions to Temperature Rise Relationship?

The transient climate response to cumulative carbon emissions (TCRE) describes an approximately linear relationship between the total amount of CO2 humanity has ever emitted and how much global average temperature has risen as a result. Instead of tracking annual emissions rates or atmospheric CO2 concentration directly, TCRE lets scientists estimate warming from a single running total, expressed as degrees C of warming per unit of cumulative CO2, commonly per 1000 GtCO2.

This relationship shows up throughout climate science and policy: it is the mathematical basis the IPCC uses to translate a temperature limit like 1.5 or 2 degrees C into a remaining carbon budget, it lets researchers quickly estimate the warming implied by different future emissions scenarios without running a full climate model, it helps communicate why "when" emissions happen matters less than "how much total" gets emitted, and it explains why net-zero targets focus on cumulative totals rather than simply slowing the rate of increase.

A common misconception is that warming tracks the current annual emissions rate. It actually tracks the running cumulative total; even if annual emissions fell to zero today, past cumulative emissions would still be reflected in warming that has already effectively been locked in. Another misconception is that TCRE is a single precise number. The IPCC reports it as a likely range, reflecting genuine scientific uncertainty in how the climate system responds to cumulative carbon.

This calculator applies the TCRE relationship directly, converting a cumulative CO2 emissions figure and a chosen TCRE value into an estimated warming figure, alongside the low and high bounds from the IPCC AR6 likely range so the underlying uncertainty stays visible.

📐 Formula

ΔT  ≈  TCRE × Ecum ÷ 1000
ΔT = estimated global average temperature rise (°C)
TCRE = transient climate response to cumulative carbon emissions (°C per 1000 GtCO2), IPCC AR6 likely range approximately 0.27 to 0.63, central estimate 0.45
Ecum = cumulative CO2 emissions (GtCO2)
Example: Ecum = 2500 GtCO2, TCRE = 0.45 → ΔT = 0.45 × 2500 ÷ 1000 = 1.125 °C.

📖 How to Use This Calculator

Steps

1
Enter cumulative CO2 emissions. Type or slide to the cumulative CO2 emissions in GtCO2 you want to convert into an estimated warming figure.
2
Enter or keep the default TCRE value. Type or slide to a TCRE value in degrees C per 1000 GtCO2, or keep the 0.45 central estimate.
3
Read the warming estimate and uncertainty range. The calculator reports the central warming estimate along with the low and high bounds from the IPCC AR6 likely TCRE range.

💡 Example Calculations

Example 1 — Historical Cumulative Emissions

Cumulative emissions = 2500 GtCO2 (roughly since 1850), TCRE = 0.45

1
ΔT = 0.45 × 2500 ÷ 1000 = 1.125 °C
2
Low bound: 0.27 × 2500 ÷ 1000 = 0.675 °C. High bound: 0.63 × 2500 ÷ 1000 = 1.575 °C
ΔT = 1.125 °C (range 0.675 to 1.575 °C), broadly consistent with observed historical warming.
Try this example →

Example 2 — Approaching the 1.5 Degree C Threshold

Cumulative emissions = 3333 GtCO2, TCRE = 0.45

1
ΔT = 0.45 × 3333 ÷ 1000 = 1.500 °C
2
Low bound: 0.27 × 3333 ÷ 1000 = 0.900 °C. High bound: 0.63 × 3333 ÷ 1000 = 2.100 °C
ΔT = 1.500 °C (range 0.900 to 2.100 °C) at this cumulative emissions total.
Try this example →

Example 3 — Using a Higher TCRE Estimate

Cumulative emissions = 2000 GtCO2, TCRE = 0.55

1
ΔT = 0.55 × 2000 ÷ 1000 = 1.100 °C
2
Low bound: 0.27 × 2000 ÷ 1000 = 0.540 °C. High bound: 0.63 × 2000 ÷ 1000 = 1.260 °C
ΔT = 1.100 °C (range 0.540 to 1.260 °C) using a higher-than-central TCRE choice.
Try this example →

❓ Frequently Asked Questions

What is TCRE (transient climate response to cumulative carbon emissions)?+
TCRE is the approximately linear relationship between cumulative CO2 emissions and global mean surface temperature rise, expressed as degrees C of warming per unit of cumulative CO2 emitted, commonly per 1000 GtCO2. It is one of the most robust findings in climate science.
What TCRE value should I use?+
The IPCC AR6 likely range is about 0.27 to 0.63 degree C per 1000 GtCO2, with 0.45 degree C per 1000 GtCO2 widely cited as a central estimate. Use the central value unless you have a specific reason, such as matching a particular study, to use the low or high bound.
What formula does this calculator use?+
Delta T is approximately equal to TCRE times cumulative CO2 emissions divided by 1000, when TCRE is expressed in degrees C per 1000 GtCO2 and cumulative emissions are expressed in GtCO2.
How much has the world already warmed from cumulative CO2 emissions?+
Using roughly 2500 GtCO2 of historical cumulative emissions since around 1850 and the 0.45 degree C per 1000 GtCO2 central TCRE estimate gives about 1.125 degrees C, broadly consistent with observed warming, though observed warming also includes non-CO2 forcings this calculator does not include.
Why is the TCRE relationship approximately linear instead of curved?+
Climate models show that as CO2 accumulates, the warming effect per additional tonne is roughly offset by slower ocean heat uptake and carbon-cycle feedbacks over the timescales relevant to policy, so the net relationship between cumulative emissions and warming stays close to linear across a wide range, unlike the logarithmic relationship between CO2 concentration and radiative forcing.
Does TCRE include non-CO2 greenhouse gases like methane?+
No. TCRE as used here is a CO2-only relationship. Total observed and projected warming also reflects methane, nitrous oxide, other greenhouse gases, and a partial cooling offset from aerosols, so this calculator's output is a CO2-attributable component, not the full picture.
Why does this calculator show a low, central, and high warming estimate?+
Because TCRE itself carries significant scientific uncertainty, stated by the IPCC as a likely range, about 0.27 to 0.63 degree C per 1000 GtCO2, rather than a single number. Showing all three values makes that uncertainty visible instead of implying false precision from one number alone.
How is TCRE related to the remaining carbon budget?+
TCRE is the underlying science IPCC teams use to derive remaining carbon budgets: given a temperature limit and a chosen TCRE value or distribution, they calculate the cumulative emissions consistent with that limit, then subtract emissions already released to get the remaining budget (see the Carbon Budget Calculator).
Is TCRE the same for every level of cumulative emissions?+
It is approximately constant across the cumulative emissions range relevant to current policy discussions, but climate models show it can behave differently at very high cumulative totals over long, multi-century timescales. For near-term and mid-century estimates, treating it as constant is a standard simplification.
Can this calculator be used to estimate warming from a specific country's emissions?+
Not directly. TCRE describes the global relationship between global cumulative CO2 emissions and global mean temperature; it is not meant to be applied to a single country's or company's emissions in isolation, since climate response depends on the cumulative total from all sources worldwide.
Where does the default 2500 GtCO2 cumulative emissions figure come from?+
It is a rounded, illustrative approximation of global cumulative CO2 emissions since the start of industrialization, around 1850, through the early 2020s, based on Global Carbon Project style estimates. Replace it with a more current cumulative figure for a more accurate estimate.

What is TCRE (transient climate response to cumulative carbon emissions)?

TCRE is the approximately linear relationship between cumulative CO2 emissions and global mean surface temperature rise, expressed as degrees C of warming per unit of cumulative CO2 emitted, commonly per 1000 GtCO2. It is one of the most robust findings in climate science.

What TCRE value should I use?

The IPCC AR6 likely range is about 0.27 to 0.63 degree C per 1000 GtCO2, with 0.45 degree C per 1000 GtCO2 widely cited as a central estimate. Use the central value unless you have a specific reason (such as matching a particular study) to use the low or high bound.

What formula does this calculator use?

Delta T is approximately equal to TCRE times cumulative CO2 emissions divided by 1000, when TCRE is expressed in degrees C per 1000 GtCO2 and cumulative emissions are expressed in GtCO2.

How much has the world already warmed from cumulative CO2 emissions?

Using roughly 2500 GtCO2 of historical cumulative emissions since around 1850 and the 0.45 degree C per 1000 GtCO2 central TCRE estimate gives about 1.125 degrees C, broadly consistent with observed warming, though observed warming also includes non-CO2 forcings this calculator does not include.

Why is the TCRE relationship approximately linear instead of curved?

Climate models show that as CO2 accumulates, the warming effect per additional tonne is roughly offset by slower ocean heat uptake and carbon-cycle feedbacks over the timescales relevant to policy, so the net relationship between cumulative emissions and warming stays close to linear across a wide range, unlike the logarithmic relationship between CO2 concentration and radiative forcing.

Does TCRE include non-CO2 greenhouse gases like methane?

No. TCRE as used here is a CO2-only relationship. Total observed and projected warming also reflects methane, nitrous oxide, other greenhouse gases, and a partial cooling offset from aerosols, so this calculator's output is a CO2-attributable component, not the full picture.

Why does this calculator show a low, central, and high warming estimate?

Because TCRE itself carries significant scientific uncertainty, stated by the IPCC as a likely range (about 0.27 to 0.63 degree C per 1000 GtCO2) rather than a single number. Showing all three values makes that uncertainty visible instead of implying false precision from one number alone.

How is TCRE related to the remaining carbon budget?

TCRE is the underlying science IPCC teams use to derive remaining carbon budgets: given a temperature limit and a chosen TCRE value (or distribution), they calculate the cumulative emissions consistent with that limit, then subtract emissions already released to get the remaining budget (see the Carbon Budget Calculator).

Is TCRE the same for every level of cumulative emissions?

It is approximately constant across the cumulative emissions range relevant to current policy discussions, but climate models show it can behave differently at very high cumulative totals over long, multi-century timescales. For near-term and mid-century estimates, treating it as constant is a standard simplification.

Can this calculator be used to estimate warming from a specific country's emissions?

Not directly. TCRE describes the global relationship between global cumulative CO2 emissions and global mean temperature; it is not meant to be applied to a single country's or company's emissions in isolation, since climate response depends on the cumulative total from all sources worldwide.

Where does the default 2500 GtCO2 cumulative emissions figure come from?

It is a rounded, illustrative approximation of global cumulative CO2 emissions since the start of industrialization (around 1850) through the early 2020s, based on Global Carbon Project style estimates. Replace it with a more current cumulative figure for a more accurate estimate.