Sentences with phrase «eventual warming»

Cumulative emissions of ~ 1000 GtC, sometimes associated with 2 °C global warming, would spur «slow» feedbacks and eventual warming of 3 - 4 °C with disastrous consequences.»

A global warming target is converted to a fossil fuel emissions target with the help of global climate - carbon - cycle models, which reveal that eventual warming depends on cumulative carbon emissions, not on the temporal history of emissions [12].

In contrast, the 1000 GtC scenario, although nominally designed to yield a fast - feedback climate response of ∼ 2 °C, would yield a larger eventual warming because of slow feedbacks, probably at least 3 °C.

In contrast, the 1000 GtC scenario, although nominally designed to yield a fast - feedback climate response of ∼ 2 °C, would yield a larger eventual warming because of slow feedbacks, probably at least 3 °C.

A global warming target is converted to a fossil fuel emissions target with the help of global climate - carbon - cycle models, which reveal that eventual warming depends on cumulative carbon emissions, not on the temporal history of emissions [12].

Cumulative emissions of ∼ 1000 GtC, sometimes associated with 2 °C global warming, would spur «slow» feedbacks and eventual warming of 3 — 4 °C with disastrous consequences.

The eventual warming from 1000 GtC fossil fuel emissions likely would reach well over 2 °C, for several reasons.

Hansen's 2013 paper argued that «cumulative emissions of 1000 billion tons, sometimes associated with 2C global warming, would spur «slow» feedbacks and eventual warming of 3 - 4C with disastrous consequences.»

The eventual warming from 1000 GtC fossil fuel emissions likely would reach well over 2 °C, for several reasons.

This is especially so in Australia, where the economic costs on a carbon - intensive economy are high (our main comparative advantage is in energy, minerals and energy - intensive metals processing; we provide a high proportion of world trade in such areas), and where any impact on eventual warming will be negligible.

Cumulative emissions of ∼ 1000 GtC, sometimes associated with 2 °C global warming, would spur «slow» feedbacks and eventual warming of 3 — 4 °C with disastrous consequences.

The eventual warming from one gigaton fossil fuel emissions likely would reach well over 2C, for several reasons.