GSTDTAP

浏览/检索结果: 共10条,第1-10条 帮助

已选(0)清除 条数/页:   排序方式:
全球碳项目发布《2023年全球碳预算》报告 快报文章
气候变化快报,2023年第24期
作者:  刘莉娜 廖琴
Microsoft Word(17Kb)  |  收藏  |  浏览/下载:454/0  |  提交时间:2023/12/20
Global Carbon Budget  Carbon Emissions  Global Carbon Project  
2021年全球化石燃料CO2排放量将反弹至疫情爆发前水平 快报文章
气候变化快报,2021年第23期
作者:  董利苹
Microsoft Word(32Kb)  |  收藏  |  浏览/下载:717/0  |  提交时间:2021/12/07
Global Carbon Budget  COVID-19  
IRENA分析国家自主贡献中的可再生能源能源目标 快报文章
气候变化快报,2021年第2期
作者:  裴惠娟
Microsoft Word(14Kb)  |  收藏  |  浏览/下载:511/0  |  提交时间:2021/01/20
Global Carbon Budget  Fossil CO2 emissions  Global Carbon Project  
GCP发布《2020年全球碳预算》报告 快报文章
气候变化快报,2021年第1期
作者:  曾静静
Microsoft Word(16Kb)  |  收藏  |  浏览/下载:504/0  |  提交时间:2021/01/04
Global Carbon Budget  Fossil CO2 emissions  Global Carbon Project  
Implications of non-linearities between cumulative CO(2)emissions and CO2-induced warming for assessing the remaining carbon budget 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2020, 15 (7)
作者:  Nicholls, Z. R. J.;  Gieseke, R.;  Lewis, J.;  Nauels, A.;  Meinshausen, M.
收藏  |  浏览/下载:10/0  |  提交时间:2020/08/18
climate change  global warming  remaining carbon budget  peak temperature  IPCC  
The fate of carbon in a mature forest under carbon dioxide enrichment 期刊论文
NATURE, 2020, 580 (7802) : 227-+
作者:  Sun, P. Z.;  Yang, Q.;  Kuang, W. J.;  Stebunov, Y. V.;  Xiong, W. Q.;  Yu, J.;  Nair, R. R.;  Katsnelson, M. I.;  Yuan, S. J.;  Grigorieva, I. V.;  Lozada-Hidalgo, M.;  Wang, F. C.;  Geim, A. K.
收藏  |  浏览/下载:70/0  |  提交时间:2020/05/13

Carbon dioxide enrichment of a mature forest resulted in the emission of the excess carbon back into the atmosphere via enhanced ecosystem respiration, suggesting that mature forests may be limited in their capacity to mitigate climate change.


Atmospheric carbon dioxide enrichment (eCO(2)) can enhance plant carbon uptake and growth(1-5), thereby providing an important negative feedback to climate change by slowing the rate of increase of the atmospheric CO2 concentration(6). Although evidence gathered from young aggrading forests has generally indicated a strong CO2 fertilization effect on biomass growth(3-5), it is unclear whether mature forests respond to eCO(2) in a similar way. In mature trees and forest stands(7-10), photosynthetic uptake has been found to increase under eCO(2) without any apparent accompanying growth response, leaving the fate of additional carbon fixed under eCO(2) unclear(4,5,7-11). Here using data from the first ecosystem-scale Free-Air CO2 Enrichment (FACE) experiment in a mature forest, we constructed a comprehensive ecosystem carbon budget to track the fate of carbon as the forest responded to four years of eCO(2) exposure. We show that, although the eCO(2) treatment of +150 parts per million (+38 per cent) above ambient levels induced a 12 per cent (+247 grams of carbon per square metre per year) increase in carbon uptake through gross primary production, this additional carbon uptake did not lead to increased carbon sequestration at the ecosystem level. Instead, the majority of the extra carbon was emitted back into the atmosphere via several respiratory fluxes, with increased soil respiration alone accounting for half of the total uptake surplus. Our results call into question the predominant thinking that the capacity of forests to act as carbon sinks will be generally enhanced under eCO(2), and challenge the efficacy of climate mitigation strategies that rely on ubiquitous CO2 fertilization as a driver of increased carbon sinks in global forests.


  
Preindustrial (CH4)-C-14 indicates greater anthropogenic fossil CH4 emissions 期刊论文
NATURE, 2020, 578 (7795) : 409-+
作者:  Keener, Megan;  Hunt, Camden;  Carroll, Timothy G.;  Kampel, Vladimir;  Dobrovetsky, Roman;  Hayton, Trevor W.;  Menard, Gabriel
收藏  |  浏览/下载:25/0  |  提交时间:2020/05/13

Atmospheric methane (CH4) is a potent greenhouse gas, and its mole fraction has more than doubled since the preindustrial era(1). Fossil fuel extraction and use are among the largest anthropogenic sources of CH4 emissions, but the precise magnitude of these contributions is a subject of debate(2,3). Carbon-14 in CH4 ((CH4)-C-14) can be used to distinguish between fossil (C-14-free) CH4 emissions and contemporaneous biogenic sources  however, poorly constrained direct (CH4)-C-14 emissions from nuclear reactors have complicated this approach since the middle of the 20th century(4,5). Moreover, the partitioning of total fossil CH4 emissions (presently 172 to 195 teragrams CH4 per year)(2,3) between anthropogenic and natural geological sources (such as seeps and mud volcanoes) is under debate  emission inventories suggest that the latter account for about 40 to 60 teragrams CH4 per year(6,7). Geological emissions were less than 15.4 teragrams CH4 per year at the end of the Pleistocene, about 11,600 years ago(8), but that period is an imperfect analogue for present-day emissions owing to the large terrestrial ice sheet cover, lower sea level and extensive permafrost. Here we use preindustrial-era ice core (CH4)-C-14 measurements to show that natural geological CH4 emissions to the atmosphere were about 1.6 teragrams CH4 per year, with a maximum of 5.4 teragrams CH4 per year (95 per cent confidence limit)-an order of magnitude lower than the currently used estimates. This result indicates that anthropogenic fossil CH4 emissions are underestimated by about 38 to 58 teragrams CH4 per year, or about 25 to 40 per cent of recent estimates. Our record highlights the human impact on the atmosphere and climate, provides a firm target for inventories of the global CH4 budget, and will help to inform strategies for targeted emission reductions(9,10).


Isotopic evidence from ice cores indicates that preindustrial-era geological methane emissions were lower than previously thought, suggesting that present-day emissions of methane from fossil fuels are underestimated.


  
Climate and carbon budget implications of linked future changes in CO2 and non-CO2 forcing 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2019, 14 (4)
作者:  Feijoo, Felipe;  Mignone, Bryan K.;  Kheshgi, Haroon S.;  Hartin, Corinne;  McJeon, Haewon;  Edmonds, Jae
收藏  |  浏览/下载:6/0  |  提交时间:2019/11/26
carbon budget  non-CO2  cumulative carbon emissions  global temperature  radiative forcing  
Can India grow and live within a 1.5 degree CO2 emissions budget? 期刊论文
ENERGY POLICY, 2018, 120: 24-37
作者:  Parikh, Kirit S.;  Parikh, Jyoti K.;  Ghosh, Probal P.
收藏  |  浏览/下载:5/0  |  提交时间:2019/04/09
Intended Nationally Determined Contributions  Low carbon pathways  Energy transition  Energy efficiency  India'  s share in 1.5 degrees global emissions budget  Economy wide input-output model  
Warning signs for stabilizing global CO2 emissions 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2017, 12 (11)
作者:  Jackson, R. B.;  Le Quere, C.;  Andrew, R. M.;  Canadell, J. G.;  Peters, G. P.;  Roy, J.;  Wu, L.
收藏  |  浏览/下载:6/0  |  提交时间:2019/04/09
climate change  fossil fuel and industrial CO2 emissions  global carbon budget  greenhouse gas emissions