Sentence examples for equilibrium warming from inspiring English sources

With the models MIROC5, NorESM, CanAM4, and CAM4, three sets of scenarios were employed, namely, a historical scenario for the period 2006 2015 (ALL) and 1.5 °C and 2 °C equilibrium warming scenarios for a 10-year period in the beginning of 22nd century (hypothetically for the 2106 2115 period).

The full committed equilibrium warming long after 2100 will be another 75% (IPCC AR5  "For the RCP4.5 and RCP6.0 extension scenarios with early stabilization, it is about 75% at the time of forcing stabilization" (IPCC 2013, WG1, Ch 12, p. 1103), making the full equilibrium commitment 5°C or more.

The equilibrium warming associated with doubled CO2 is estimated to be between three and a half and seven degrees, and with tripled CO2 between six and eleven degrees.

Using a combination of recent climate measurements and a relatively simple climate model, the 'energy budget' approach used in Otto's study yielded a best estimate for the immediate (transient) warming of 1.3°C and equilibrium warming of 2.0°C; within the agreed range, but less than climate model best estimates of 1.8°C and 3.2°C, respectively.

We used MIROC5, NorESM, CanAM4, and CAM4 models and three sets of scenarios, namely, a historical scenario (for the 2006 2015 period) and 1.5 °C and 2 °C equilibrium warming scenarios (for a 10-year period in the beginning of 22nd century. Hypothetically for the 2106 2115 period).

As indicated by Eq. (14), the ratio of transient warming to equilibrium warming is larger when κ is smaller or λ is larger.

From time-resolved x-ray absorption spectroscopy, the temporal evolution of electron temperature is obtained for non-equilibrium warm dense copper heated by an intense femtosecond laser pulse.

With the strong femtosecond optical excitation of a tamped copper nano foil, the initial non-equilibrium warm dense copper (WDCu) states are created and then advance toward equilibrium via energy exchange between the two sub-systems at a constant density.

Huber & Knutti showed that the average climate model output (with an average climate sensitivity of about 3°C global surface warming at equilibrium from a doubling of atmospheric carbon dioxide) produces accurate global temperature predictions.

External warming blankets maintained thermal equilibrium in swine #2 and #3, demonstrating maximum temperature decrease of 1.7°C/hr.

Thus, the shift of ocean heat uptake to the region of a less positive local feedback parameter means greater surface warming remains to occur before the equilibrium.