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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:71/0  |  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.


  
Focus on the role of forests and soils in meeting climate change mitigation goals: summary 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2020, 15 (4)
作者:  Moomaw, William R.;  Law, Beverly E.;  Goetz, Scott J.
收藏  |  浏览/下载:17/0  |  提交时间:2020/07/02
natural climate solutions  forest and soil carbon  tropical forests  carbon sequestration  forest products carbon storage  forest carbon accounting  forest bioenergy accounting  
Oceanic forcing of penultimate deglacial and last interglacial sea-level rise 期刊论文
NATURE, 2020, 577 (7792) : 660-+
作者:  Rizal, Yan;  Westaway, Kira E.;  Zaim, Yahdi;  van den Bergh, Gerrit D.;  Bettis, E. Arthur, III;  Morwood, Michael J.;  Huffman, O. Frank;  Grun, Rainer;  Joannes-Boyau, Renaud;  Bailey, Richard M.;  Sidarto;  Westaway, Michael C.;  Kurniawan, Iwan;  Moore, Mark W.;  Storey, Michael;  Aziz, Fachroel;  Suminto;  Zhao, Jian-xin;  Aswan;  Sipola, Maija E.;  Larick, Roy;  Zonneveld, John-Paul;  Scott, Robert;  Putt, Shelby;  Ciochon, Russell L.
收藏  |  浏览/下载:22/0  |  提交时间:2020/05/13

Sea-level histories during the two most recent deglacial-interglacial intervals show substantial differences(1-3) despite both periods undergoing similar changes in global mean temperature(4,5) and forcing from greenhouse gases(6). Although the last interglaciation (LIG) experienced stronger boreal summer insolation forcing than the present interglaciation(7), understanding why LIG global mean sea level may have been six to nine metres higher than today has proven particularly challenging(2). Extensive areas of polar ice sheets were grounded below sea level during both glacial and interglacial periods, with grounding lines and fringing ice shelves extending onto continental shelves(8). This suggests that oceanic forcing by subsurface warming may also have contributed to ice-sheet loss(9-12) analogous to ongoing changes in the Antarctic(13,14) and Greenland(15) ice sheets. Such forcing would have been especially effective during glacial periods, when the Atlantic Meridional Overturning Circulation (AMOC) experienced large variations on millennial timescales(16), with a reduction of the AMOC causing subsurface warming throughout much of the Atlantic basin(9,12,17). Here we show that greater subsurface warming induced by the longer period of reduced AMOC during the penultimate deglaciation can explain the more-rapid sea-level rise compared with the last deglaciation. This greater forcing also contributed to excess loss from the Greenland and Antarctic ice sheets during the LIG, causing global mean sea level to rise at least four metres above modern levels. When accounting for the combined influences of penultimate and LIG deglaciation on glacial isostatic adjustment, this excess loss of polar ice during the LIG can explain much of the relative sea level recorded by fossil coral reefs and speleothems at intermediate- and far-field sites.


  
Pathways to a Resource-Efficient and Low-Carbon Europe 期刊论文
ECOLOGICAL ECONOMICS, 2019, 155: 88-104
作者:  Distelkamp, Martin;  Meyer, Mark
收藏  |  浏览/下载:5/0  |  提交时间:2019/04/09
Economy-energy-environment modelling  Material and energy use  Decoupling  Resource efficiency  Consumption-based accounting  Multi-region input-output model  Material footprint  Raw material equivalents  Dynamic assessment models  Macro-econometric models  
From resource extraction to outflows of wastes and emissions: The socioeconomic metabolism of the global economy, 1900-2015 期刊论文
GLOBAL ENVIRONMENTAL CHANGE-HUMAN AND POLICY DIMENSIONS, 2018, 52: 131-140
作者:  Krausmann, Fridolin;  Lauk, Christian;  Haas, Willi;  Wiedenhofer, Dominik
收藏  |  浏览/下载:5/0  |  提交时间:2019/04/09
Material flow accounting  Sustainable resource use  Waste and emissions  In-use material stocks  Great acceleration  Dematerialization  
The Socio-Economic Metabolism of an Emerging Economy: Monitoring Progress of Decoupling of Economic Growth and Environmental Pressures in the Philippines 期刊论文
ECOLOGICAL ECONOMICS, 2018, 147: 155-166
作者:  Martinico-Perez, Marianne Faith G.;  Schandl, Heinz;  Fishman, Tomer;  Tanikawa, Hiroki
收藏  |  浏览/下载:9/0  |  提交时间:2019/04/09
Material flow accounting (MFA)  Decoupling of economic growth and material use  Material footprint  Services-led industrialization  Sustainable development goals  
On the role of efficient cogeneration for meeting Mexico's clean energy goals 期刊论文
ENERGY POLICY, 2018, 112: 173-183
作者:  Llamas, Armando;  Probst, Oliver
收藏  |  浏览/下载:1/0  |  提交时间:2019/04/09
Combined heat and power  Fuel-free electricity  Clean energy  Accounting practices  
The global CO2 emissions growth after international crisis and the role of international trade 期刊论文
ENERGY POLICY, 2017, 109
作者:  Jiang, Xuemei;  Guan, Dabo
收藏  |  浏览/下载:5/0  |  提交时间:2019/04/09
Global CO2 emissions  Structural decomposition  Consumption-based accounting  International financial crisis  OECD and non-OECD economies  
Simulated exchange values and ecosystem accounting: Theory and application to free access recreation 期刊论文
ECOLOGICAL ECONOMICS, 2017, 139
作者:  Caparros, Alejandro;  Oviedo, Jose L.;  Alvarez, Alejandro;  Campos, Pablo
收藏  |  浏览/下载:6/0  |  提交时间:2019/04/09
Green accounting  Recreation  Non-market goods and services  Andalusia  AAS  SEEA  SNA  Forests  Discrete choice  
Energy costs in Germany and Europe: An assessment based on a (total real unit) energy cost accounting framework 期刊论文
ENERGY POLICY, 2017, 104
作者:  Kaltenegger, Oliver;  Loeschel, Andreas;  Baikowski, Martin;  Lingens, Joerg
收藏  |  浏览/下载:8/0  |  提交时间:2019/04/09
Input-output based (total real unit) energy cost accounting  Environmental-economic accounting  Monitoring energy transition  Direct and indirect energy costs of intermediate consumption  Real unit energy costs  Energy cost analysis