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与膳食指南相关的温室气体排放因国家而异 快报文章
气候变化快报,2021年第6期
作者:  曾静静
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:486/0  |  提交时间:2021/03/20
Food-based dietary guidelines (FBDG)  food balance sheets  Greenhouse gas emission accounting  
尼罗河流域的水核算 快报文章
资源环境快报,2020年第18期
作者:  吴秀平
Microsoft Word(22Kb)  |  收藏  |  浏览/下载:391/0  |  提交时间:2020/09/29
Nile River Basin  Water accounting  
Ecosystem accounting for marine protected areas: A proposed framework 期刊论文
ECOLOGICAL ECONOMICS, 2020, 173
作者:  Cavalletti, B.;  Di Fabio, C.;  Lagomarsino, E.;  Ramassa, P.
收藏  |  浏览/下载:8/0  |  提交时间:2020/08/18
Ecosystem services  Economic-environmental accounting  SEEA-EEA  
Unequal raw material exchange between and within countries: Galicia (NW Spain) as a core-periphery economy 期刊论文
ECOLOGICAL ECONOMICS, 2020, 172
作者:  Pinero, Pablo;  Perez-Neira, David;  Infante-Amate, Juan;  Chas-Amil, Maria L.;  Doldan-Garcia, Xoan R.
收藏  |  浏览/下载:17/0  |  提交时间:2020/07/02
Unequal exchange  Material footprint  Material flow accounting  Value added  World system theory  Multi-Regional Input-Output  
The evolution of household-induced value chains and their environmental implications 期刊论文
ECOLOGICAL ECONOMICS, 2020, 174
作者:  Solis, Alberto Franco;  Avelino, Andre F. T.;  Carrascal-Incera, Andre
收藏  |  浏览/下载:6/0  |  提交时间:2020/05/13
Temporal Leontief Inverse  Time-series analysis  Trade  Consumption-based accounting  Greenhouse gases emissions  
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.


  
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.


  
Augmenting the World Banks estimates: Ireland's genuine savings through boom and bust 期刊论文
ECOLOGICAL ECONOMICS, 2019, 165
作者:  McGrath, Luke;  Hynes, Stephen;  McHale, John
收藏  |  浏览/下载:10/0  |  提交时间:2019/11/27
Green accounting  Genuine savings  Natural capital  Wealth accounting  Environmental accounting  Sustainable development  
The Role of Technological Progress in Testing Adjusted Net Savings: Evidence from OECD Countries 期刊论文
ECOLOGICAL ECONOMICS, 2019, 164
作者:  Mota, Rui Pedro;  Cunha-e-Sa, Maria A.
收藏  |  浏览/下载:6/0  |  提交时间:2019/11/27
Adjusted net savings  Indicators of weak sustainability  Technological progress  Comprehensive accounting