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A steep road to climate stabilization
<span title="2008-01-17">2008</span>
<i title="Springer Nature">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/drfdii35rzaibj3aml5uhvr5xm" style="color: black;">Nature</a>
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■ Pierre Friedlingstein is at the Institute Pierre Simon Laplace, Laboratory of Climate and Environment Sciences, CEA-Saclay, 91191 Gif-sur-Yvette, France. ...
This roughly matches the objective proposed A steep road to climate stabilization
Pierre Friedlingstein The only way to stabilize Earth's climate is to stabilize the concentration of greenhouse gases ...
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Changement climatique et cycle du carbone
<span title="">2007</span>
<i title="INIST-CNRS">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/vtwmy4hxgzd65j2c5dymx253qm" style="color: black;">La Météorologie</a>
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Par contre, l'estimation de l'amplitude de cette rétroaction est très différente entre ces deux premières études (Friedlingstein et al., 2003) . ...
IPSL_CM4_Loop a une rétroaction positive qui est inférieure à la moyenne des modèles C 4 MIP [amplif ication variant de +20 à +200 ppm] (Friedlingstein et al., 2006, figure 1b). ...
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Process-based analysis of terrestrial carbon flux predictability
<span title="2021-12-02">2021</span>
<i title="Copernicus GmbH">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/xmod3vi2ybbb5b64zveedgalwu" style="color: black;">Earth System Dynamics</a>
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Introduction As a net sink for atmospheric CO 2 , terrestrial ecosystems absorb around one-third of the anthropogenic emissions (Friedlingstein et al., 2020) . ...
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Constraining uncertainty in projected gross primary production with machine learning
<span title="2020-10-27">2020</span>
<i title="American Geophysical Union (AGU)">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/6e7fuq2ohvhg5i5k5khpwqhwaq" style="color: black;">Journal of Geophysical Research - Biogeosciences</a>
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., 2013; Friedlingstein et al., 2006; Gregory et al., 2009 ). ...
The terrestrial biosphere currently absorbs about 30% of the total anthropogenic CO 2 emissions (Friedlingstein et al., 2019) , yet whether that benefit will perdure in the future remains unclear (Friedlingstein ...
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Comment on "The global tree restoration potential"
<span title="2019-10-17">2019</span>
<i title="American Association for the Advancement of Science (AAAS)">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/qirzh7firjdsjhg4tutxtir6ey" style="color: black;">Science</a>
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Friedlingstein 1 *, Myles Allen 2 , Josep G. ...
lead to weak local cooling, or even to warming, as the positive radiative forcing induced by decreases in albedo can offset the negative radiative forc-Comment on "The global tree restoration potential" Pierre ...
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More frequent moments in the climate change debate as emissions continue
<span title="2015-12-01">2015</span>
<i title="IOP Publishing">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/4gdzpwrn2je35h3xecizajmcna" style="color: black;">Environmental Research Letters</a>
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Lett. 10 (2015) 121001 C Huntingford and P Friedlingstein ...
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The cumulative carbon budget and its implications
<span title="">2016</span>
<i title="Oxford University Press (OUP)">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/mqtsoq7lcvg5bei75h7qjqp3a4" style="color: black;">Oxford review of economic policy</a>
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Friedlingstein et al., 2014; Rogelj et al., in press ), which we intend to explore in this article. ...
oceanic and terrestrial carbon sinks as atmospheric CO2 increases, and from the weakening (and in some models reversal) of CO2 uptake by oceanic and terrestrial sinks due to warming of the climate system (Friedlingstein ...
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<a target="_blank" rel="external noopener noreferrer" href="https://doi.org/10.1093/oxrep/grw009">doi:10.1093/oxrep/grw009</a>
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Terrestrial nitrogen feedbacks may accelerate future climate change
<span title="">2010</span>
<i title="American Geophysical Union (AGU)">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/wulq43nvfbff7hppzu4u6xyaki" style="color: black;">Geophysical Research Letters</a>
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[3] We first use observations from ecosystem manipulation studies to evaluate the sensitivity of C dynamics to N constraints as simulated by the O-CN land-surface model , a component of the Institut Pierre ...
Open diamonds (Figures 3a -3b) ) show sensitivities obtained with coupled carbon-cycle climate models [Friedlingstein et al., 2006 ] that do not account for N dynamics. ...
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Leaching of dissolved organic carbon from mineral soils plays a significant role in the terrestrial carbon balance
<span title="2020-11-28">2020</span>
<i title="Wiley">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/3mxo2eysivhenpbnzfjtn5vjom" style="color: black;">Global Change Biology</a>
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Pierre Friedlingstein and Bertrand Guenet received funding from the European Union's Horizon 2020 research and innovation programme under grant agreements No. 641816 (CRESCENDO) and No. 821003 (4C project ...
| INTRODUC TI ON Earth System Models (ESMs) are process-based models that represent the full climate system including feedbacks with the carbon (C) cycle (Friedlingstein et al., 2006) . ...
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<a target="_blank" rel="external noopener noreferrer" href="https://doi.org/10.1111/gcb.15460">doi:10.1111/gcb.15460</a>
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Projected land photosynthesis constrained by changes in the seasonal cycle of atmospheric CO2
<span title="2016-09-28">2016</span>
<i title="Springer Nature">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/drfdii35rzaibj3aml5uhvr5xm" style="color: black;">Nature</a>
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Research, Korea Meteorological
Administration, Korea
1 (Martin et al. 2011)
18
Inmcm4
Russian Institute for Numerical
Mathematics, Russia
1 (Volodin et al. 2010)
19
IPSL-CM5A-LR
Institut Pierre ...
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Measuring a fair and ambitious climate agreement using cumulative emissions
<span title="2015-10-01">2015</span>
<i title="IOP Publishing">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/4gdzpwrn2je35h3xecizajmcna" style="color: black;">Environmental Research Letters</a>
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The IPCC AR5 WGI used the non-CO 2 emissions (hence forcing) from RCP8.5 (remaining quota 2900 GtCO 2 ), while Friedlingstein et al (2014) used the non-CO 2 emissions from Working Group III's scenarios ...
For the non-CO 2 adjustment we show the IPCC WG1 value (used in our analysis) together with the 5%−95% range used by Friedlingstein et al (2014, 'F14') and the IPCC Synthesis Report (IPCC 2014; 'SYR' ...
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Quantifying uncertainties of permafrost carbon-climate feedbacks
<span title="2017-01-05">2017</span>
<i title="Copernicus GmbH">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/lsqxuqfufrh7bbwdcrceloas2y" style="color: black;">Biogeosciences Discussions</a>
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The climate-carbon response, γ , is formally defined as the change in land carbon per degree of global mean temperature change (Friedlingstein et al., 2006) . ...
This suggests that γ PF could be pathway-and timedependent, and the linear feedback approach developed by Friedlingstein et al. (2006) is not valid when incorporating the response of permafrost carbon ...
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Differences between carbon budget estimates unravelled
<span title="">2016</span>
<i title="Springer Nature">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/v4vwhlgldngztb7nqdzbsjighm" style="color: black;">Nature Climate Change</a>
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This can explain about one third to half of the 260-310 GtCO 2 difference between the TEB estimates from Friedlingstein et al. (Ref. 36) and the IPCC SYR TAB estimates. ...
category 1)
630 to
1180
470 to
1020
IPCC AR5
WGIII
960 to
1430
800 to
1270
1010
(1110 or
1410)
850
(960 or
1250)
750 to
1400
590 to
1240
1150 to
1400
990 to
1240
Friedlingstein ...
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The Origin and Limits of the Near Proportionality between Climate Warming and Cumulative CO2Emissions
<span title="">2015</span>
<i title="American Meteorological Society">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/rse5s4kgqvgutdbgyq2477wlji" style="color: black;">Journal of Climate</a>
</i>
Carbon sensitivity describes the fraction of emitted carbon that remains in the atmosphere given the strength of carbon cycle feedbacks at a given point in time (Friedlingstein et al. 2006) . ...
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Carbon cycle feedbacks and future climate change
<span title="2015-10-05">2015</span>
<i title="The Royal Society">
<a target="_blank" rel="noopener" href="https://fatcat.wiki/container/ercgg4vn2fenngurcnadfzdfri" style="color: black;">Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences</a>
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These developments occurred almost simultaneously at the Hadley Centre, UK and at the Institut Pierre-Simon Laplace (IPSL), France. ...
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