Sentence examples for mean warming of from inspiring English sources

These models simulate, in response to 5 EgC of CO2 emissions, global mean warming of 6.4 9.5 °C, mean Arctic warming of 14.7 19.5 °C, and mean regional precipitation increases by more than a factor of four.

Here we calculate warming and carbon budgets relative to the decade 2006 2015, which eliminates model observation differences in the climate carbon response over the historical period9, and increases the median remaining carbon budget to 208 PgC (33 66% range of 130 255 PgC) from January 2016 (with mean warming of 0.89 °C for 2006 2015 relative to 1861 188013,14,15,16,17,18).

We calculated cumulative future emissions of 496 (282 to 701 in lower- and upper-bounding scenarios) gigatonnes of CO2 from combustion of fossil fuels by existing infrastructure between 2010 and 2060, forcing mean warming of 1.3°C (1.1° to 1.4°C) above the pre-industrial era and atmospheric concentrations of CO2 less than 430 parts per million.

Even so, mean warming of at least 0.2°C was recorded up to 4 mm from the plate's surface at both medium and high current speeds.

The scenarios take into account the Intergovernmental Panel on Climate Change (IPCC) range of greenhouse gas emission scenarios (IS92a-f), and the IPCC range of climate sensitivity (a global mean warming of 1.5°C to 4.5°C for an equivalent doubling of pre-industrial CO2 concentrations).

higher in our fully coupled simulation than in uncoupled carbon models2, resulting in a global-mean warming of 5.5 K, as compared to 4 K without the carbon-cycle feedback.

These analyzes give us a better understanding about the chalky dynamics with global-mean warming of roughly 4 °C in rice grains.

Average warming of 4ºC globally means warming during the summer months over the U.S., Europe, Africa and Australia; winter temperatures in the Arctic will increase 12-16ºC 12-16ºC

On Earth, naturally occurring amounts of greenhouse gases have a mean warming effect of about.

Using the same approach for the observed permafrost distribution and air temperature, we estimate a sensitivity of permafrost area loss to global mean warming at stabilization of million km2 °C−1 (1σ confidence), which is around 20% higher than previous studies9.

A 2°C increase in global temperatures which appears inevitable as greenhouse-gas emissions soar would mean Arctic warming of 3-6°C.Almost 3-6°C.Almostlallers hArcticceded.