«It's not a time bomb; it's an important additional
cumulative emissions source,» he told me.
Not exact matches
Furthermore, let me come back to the pathway as the
source of
cumulative emissions — energy mix, efficiency, technology finance, population, etc. etc., we believe this is the deeper driver to lead to the landscape of
cumulative emissions.
Following these informal discussions, delegates agreed on text stating that limiting the warming caused by anthropogenic CO2
emissions alone with a probability range of greater than 33 %, 50 %, and 66 %, to less than 2ºC since the period 1861 - 1880, will require
cumulative CO2
emissions from all anthropogenic
sources to stay between 0 and about 1560 GtC, 0 and about 1210 GtC, and 0 and about 1000 GtC.
Cumulative emissions reductions to 2060, by
source of savings.
When the Total GHG
emissions from Annex A
sources is selected as the category, the list contains the five years of the first commitment period of the Kyoto Protocol, from 2008 to 2012 and, in addition, «
Cumulative».
The near - linear rate of anthropogenic warming (predominantly from anthropogenic greenhouse gases) is shown in
sources such as: «Deducing Multidecadal Anthropogenic Global Warming Trends Using Multiple Regression Analysis» «The global warming hiatus — a natural product of interactions of a secular warming trend and a multi-decadal oscillation» «The Origin and Limits of the Near Proportionality between Climate Warming and
Cumulative CO2 Emissions» «Sensitivity of climate to cumulative carbon emissions due to compensation of ocean heat and carbon uptake» «Return periods of global climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mix
Cumulative CO2
Emissions» «Sensitivity of climate to cumulative carbon emissions due to compensation of ocean heat and carbon uptake» «Return periods of global climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mixi
Emissions» «Sensitivity of climate to
cumulative carbon emissions due to compensation of ocean heat and carbon uptake» «Return periods of global climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mix
cumulative carbon
emissions due to compensation of ocean heat and carbon uptake» «Return periods of global climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mixi
emissions due to compensation of ocean heat and carbon uptake» «Return periods of global climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to
cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mix
cumulative carbon
emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mixi
emissions» «The sensitivity of the proportionality between temperature change and
cumulative CO2 emissions to ocean mix
cumulative CO2
emissions to ocean mixi
emissions to ocean mixing»
It states that to stand a good chance (a probability of 66 percent or more) of limiting warming to less than 2 °C since the mid-19th century will require
cumulative CO2
emissions from all anthropogenic
sources to stay under 800 gigatons of carbon.
To put the necessary cap on total
cumulative greenhouse gas (GHG)
emissions, leaders also agreed on net - zero
emissions; that is, there must be «a balance between anthropogenic
emissions by
sources and removals by sinks of greenhouse gases in the second half of this century».1
Limiting the warming caused by anthropogenic CO2
emissions alone with a probability of > 33 %, > 50 %, and > 66 % to less than 2 °C since the period 1861 — 1880, will require
cumulative CO2
emissions from all anthropogenic
sources to stay between 0 and about 1570 GtC (5760 GtCO2), 0 and about 1210 GtC (4440 GtCO2), and 0 and about 1000 GtC (3670 GtCO2) since that period, respectively.
49
cumulative CO2
emissions from fossil
sources and land use change to below 1,000 (1,440) Gt CO2»
The worksheets available below constitute the details each entity's production of oil & NGLs, natural gas, coal, and cement from as early as 1854 to 2010, as well as additional
sources of
emissions (such as vented CO2, flared CO2, own fuel use, and vented or fugitive methane), non-energy uses of oil, gas, and coal,
emission factors for each fuel, calculation of
emissions attributed to each Carbon Major producer, and several summary worksheets by fuel and for
cumulative emissions by all entities.