2021 Nobel Prize in Physics(1)
Reason for Award
for the physical modelling of Earth’s climate, quantifying variability and reliably predicting global warming
Laureates
United States of America
Germany
Explanation
Earth is warmed by sunlight, and the air keeps some of that heat. Mr. Manabe and Mr. Hasselmann built a giant "Earth board game" that shows how air and oceans move heat around. By running the game many times they proved that adding more carbon-dioxide makes the ground hotter. It is like wearing an extra coat—you feel warmer. Their work tells us we must cut the CO2 we put into the air.
Related Keywords
climate model
A climate model is a numerical laboratory that represents atmosphere, ocean, land and ice through differential equations solved on a space-time grid. Variables such as temperature, precipitation and wind are discretized, and the governing dynamics and energy balances are integrated forward in time. By constructing ‘what-if’ Earths—for instance with doubled CO2—scientists estimate future warming and the probability of extreme events. Continuous comparison with observations refines model skill. The results inform policy design and adaptation planning.
greenhouse effect
The greenhouse effect is the process by which atmospheric gases such as CO2 and water vapor absorb infrared radiation emitted by Earth and re-radiate it, warming the surface. Without it, the global mean temperature would drop to about −18 °C. Since the Industrial Revolution fossil-fuel combustion has raised CO2 levels by over 40 %, amplifying the effect. Consequently, global surface temperature has risen roughly 1 °C in 150 years. The strength of the effect depends on greenhouse-gas concentrations and atmospheric temperature profiles.
climate fingerprint
Fingerprint analysis statistically identifies the unique space-time patterns left by specific forcings in the climate field. For instance, rising CO2 produces tropospheric warming combined with stratospheric cooling. Observations are projected onto model-derived fingerprints; if the resulting statistic exceeds a threshold, the forcing is deemed detected. This approach distinguished anthropogenic warming from natural variability. Handling multiple fingerprints simultaneously allows estimation of contributions from aerosols, solar variability and more.
internal variability
Internal variability denotes fluctuations arising spontaneously within the coupled climate system through nonlinear interactions, even in the absence of external forcing. ENSO and the North Atlantic Oscillation are classic examples spanning months to decades. Internal variability drives forecast uncertainty and acts as ‘noise’ when detecting long-term trends. Hasselmann formalized it as white noise in a stochastic climate framework. Today, large-ensemble simulations estimate internal spectra and underpin probabilistic assessments of extremes.
radiative forcing
Radiative forcing quantifies, in W m⁻², the change in Earth’s top-of-atmosphere energy balance caused by an external agent before temperature adjusts. A CO2 doubling exerts about +3.7 W m⁻². Positive forcing warms, negative forces cool. Aerosols and volcanic eruptions give negative forcing, whereas greenhouse gases give positive forcing. Radiative forcing is central to estimating climate sensitivity and comparing emission scenarios.
climate sensitivity
Climate sensitivity measures the steady-state global surface temperature response to an external forcing, most commonly expressed as equilibrium climate sensitivity (ECS) for doubled CO2. The IPCC places ECS likely between 2.5 and 4 °C. Manabe’s 1967 model yielded 2.3 °C, close to today’s lower bound. Uncertainty stems mainly from cloud and albedo feedbacks. Bayesian constraints combining paleoclimate evidence and modern energy-budget observations are actively pursued to narrow ECS.