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Contribution of land use to the interannual variability of the land carbon cycle 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Yue, Chao;  Ciais, Philippe;  Houghton, Richard A.;  Nassikas, Alexander A.
收藏  |  浏览/下载:10/0  |  提交时间:2020/06/29
Patterns and trends of Northern Hemisphere snow mass from 1980 to 2018 期刊论文
NATURE, 2020, 581 (7808) : 294-+
作者:  Ibrahim, Nizar;  Maganuco, Simone;  Dal Sasso, Cristiano;  Fabbri, Matteo;  Auditore, Marco;  Bindellini, Gabriele;  Martill, David M.;  Zouhri, Samir;  Mattarelli, Diego A.;  Unwin, David M.;  Wiemann, Jasmina;  Bonadonna, Davide;  Amane, Ayoub;  Jakubczak, Juliana;  Joger, Ulrich;  Lauder, George V.;  Pierce, Stephanie E.
收藏  |  浏览/下载:16/0  |  提交时间:2020/05/25

Warming surface temperatures have driven a substantial reduction in the extent and duration of Northern Hemisphere snow cover(1-3). These changes in snow cover affect Earth'  s climate system via the surface energy budget, and influence freshwater resources across a large proportion of the Northern Hemisphere(4-6). In contrast to snow extent, reliable quantitative knowledge on seasonal snow mass and its trend is lacking(7-9). Here we use the new GlobSnow 3.0 dataset to show that the 1980-2018 annual maximum snow mass in the Northern Hemisphere was, on average, 3,062 +/- 35 billion tonnes (gigatonnes). Our quantification is for March (the month that most closely corresponds to peak snow mass), covers non-alpine regions above 40 degrees N and, crucially, includes a bias correction based on in-field snow observations. We compare our GlobSnow 3.0 estimates with three independent estimates of snow mass, each with and without the bias correction. Across the four datasets, the bias correction decreased the range from 2,433-3,380 gigatonnes (mean 2,867) to 2,846-3,062 gigatonnes (mean 2,938)-a reduction in uncertainty from 33% to 7.4%. On the basis of our bias-corrected GlobSnow 3.0 estimates, we find different continental trends over the 39-year satellite record. For example, snow mass decreased by 46 gigatonnes per decade across North America but had a negligible trend across Eurasia  both continents exhibit high regional variability. Our results enable a better estimation of the role of seasonal snow mass in Earth'  s energy, water and carbon budgets.


Applying a bias correction to a state-of-the-art dataset covering non-alpine regions of the Northern Hemisphere and to three other datasets yields a more constrained quantification of snow mass in March from 1980 to 2018.


  
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.


  
Carbon declines along tropical forest edges correspond to heterogeneous effects on canopy structure and function 期刊论文
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2020, 117 (14) : 7863-7870
作者:  Ordway, Elsa M.;  Asner, Gregory P.
收藏  |  浏览/下载:10/0  |  提交时间:2020/05/13
Borneo  carbon conservation  forest edge effects  deforestation  leaf traits  
Available capital, utilized capital, and shadow prices in inclusive wealth accounting 期刊论文
ECOLOGICAL ECONOMICS, 2020, 169
作者:  Yamaguchi, Rintaro
收藏  |  浏览/下载:8/0  |  提交时间:2020/07/02
Genuine savings  Inclusive wealth  Unemployment  Shadow prices  Capital utilization  Capacity utilization  Capability approach  Sustainable development  Carbon budget  
Estimating and tracking the remaining carbon budget for stringent climate targets (vol 571, pg 335, 2019) 期刊论文
NATURE, 2020, 580 (7802) : E4-E4
作者:  Zhao, Evan Wenbo;  Liu, Tao;  Jonsson, Erlendur;  Lee, Jeongjae;  Temprano, Israel;  Jethwa, Rajesh B.;  Wang, Anqi;  Smith, Holly;  Carretero-Gonzalez, Javier;  Song, Qilei;  Grey, Clare P.
收藏  |  浏览/下载:7/0  |  提交时间:2020/07/03

An amendment to this paper has been published and can be accessed via a link at the top of the paper.


  
Managing energy infrastructure to decarbonize industrial parks in China 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Guo, Yang;  Tian, Jinping;  Chen, Lyujun
收藏  |  浏览/下载:10/0  |  提交时间:2020/05/13
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.


  
Earlier leaf-out warms air in the north 期刊论文
NATURE CLIMATE CHANGE, 2020, 10 (4) : 370-+
作者:  Xu, Xiyan;  Riley, William J.;  Koven, Charles D.;  Jia, Gensuo;  Zhang, Xiaoyan
收藏  |  浏览/下载:15/0  |  提交时间:2020/05/13
GRACE-based Mass Conservation as a Validation Target for Basin-Scale Evapotranspiration in the Contiguous United States 期刊论文
WATER RESOURCES RESEARCH, 2020, 56 (2)
作者:  Pascolini-Campbell, Madeleine A.;  Reager, John T.;  Fisher, Joshua B.
收藏  |  浏览/下载:13/0  |  提交时间:2020/07/02
evapotranspiration  GRACE  water balance  model evaluation  remote sensing