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The projected timing of abrupt ecological disruption from climate change 期刊论文
NATURE, 2020, 580 (7804) : 496-+
作者:  Gorgulla, Christoph;  Boeszoermenyi, Andras;  Wang, Zi-Fu;  Fischer, Patrick D.;  Coote, Paul W.;  Padmanabha Das, Krishna M.;  Malets, Yehor S.;  Radchenko, Dmytro S.;  Moroz, Yurii S.;  Scott, David A.;  Fackeldey, Konstantin;  Hoffmann, Moritz;  Iavniuk, Iryna;  Wagner, Gerhard;  Arthanari, Haribabu
收藏  |  浏览/下载:56/0  |  提交时间:2020/05/13

As anthropogenic climate change continues the risks to biodiversity will increase over time, with future projections indicating that a potentially catastrophic loss of global biodiversity is on the horizon(1-3). However, our understanding of when and how abruptly this climate-driven disruption of biodiversity will occur is limited because biodiversity forecasts typically focus on individual snapshots of the future. Here we use annual projections (from 1850 to 2100) of temperature and precipitation across the ranges of more than 30,000 marine and terrestrial species to estimate the timing of their exposure to potentially dangerous climate conditions. We project that future disruption of ecological assemblages as a result of climate change will be abrupt, because within any given ecological assemblage the exposure of most species to climate conditions beyond their realized niche limits occurs almost simultaneously. Under a high-emissions scenario (representative concentration pathway (RCP) 8.5), such abrupt exposure events begin before 2030 in tropical oceans and spread to tropical forests and higher latitudes by 2050. If global warming is kept below 2 degrees C, less than 2% of assemblages globally are projected to undergo abrupt exposure events of more than 20% of their constituent species  however, the risk accelerates with the magnitude of warming, threatening 15% of assemblages at 4 degrees C, with similar levels of risk in protected and unprotected areas. These results highlight the impending risk of sudden and severe biodiversity losses from climate change and provide a framework for predicting both when and where these events may occur.


Using annual projections of temperature and precipitation to estimate when species will be exposed to potentially harmful climate conditions reveals that disruption of ecological assemblages as a result of climate change will be abrupt and could start as early as the current decade.


  
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.


  
Can reanalysis products with only surface variables assimilated capture Madden-Julian oscillation characteristics? 期刊论文
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2019
作者:  Cui, Jingxuan;  Wang, Lu;  Li, Tim;  Wu, Bo
收藏  |  浏览/下载:5/0  |  提交时间:2019/11/27
data assimilation  ERA and NOAA 20C-reanalysis datasets  Madden-Julian oscillation  
Inconsistent Wind Speed Trends in Current Twentieth Century Reanalyses 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2019, 124 (4) : 1931-1940
作者:  Wohland, Jan;  Omrani, Nour-Eddine;  Witthaut, Dirk;  Keenlyside, Noel S.
收藏  |  浏览/下载:6/0  |  提交时间:2019/04/09
wind  reanalysis  spurious trend  discrepancy  ERA20C  20CR  
Estimation of economic losses from tropical cyclones in China at 1.5 degrees C and 2.0 degrees C warming using the regional climate model COSMO-CLM 期刊论文
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2019, 39 (2) : 724-737
作者:  Wen, Shanshan;  Wang, Yanjun;  Su, Buda;  Gao, Chao;  Chen, Xue;  Jiang, Tong;  Tao, Hui;  Fischer, Thomas;  Wang, Guojie;  Zhai, Jianqing
收藏  |  浏览/下载:8/0  |  提交时间:2019/04/09
1.5 degrees C and 20 degrees C warming  China  economic loss  influential tropical cyclone  
Using GRACE to Explain Variations in the Earth's Oblateness 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2019, 46 (1) : 158-168
作者:  Sun, Yu;  Riva, Riccardo;  Ditmar, Pavel;  Rietbroek, Roelof
收藏  |  浏览/下载:4/0  |  提交时间:2019/04/09
Earth'  s dynamic oblateness  J(2)  GRACE  C-20  geoid fingerprints  mass redistribution  
Northern Hemisphere extratropical winter cyclones variability over the 20th century derived from ERA-20C reanalysis 期刊论文
CLIMATE DYNAMICS, 2019, 52: 1027-1048
作者:  Varino, Filipa;  Arbogast, Philippe;  Joly, Bruno;  Riviere, Gwendal;  Fandeur, Marie-Laure;  Bovy, Henry;  Granier, Jean-Baptiste
收藏  |  浏览/下载:14/0  |  提交时间:2019/04/09
Storm track  Cyclone tracking  20th century  ERA-20C  Arctic warming  Climate change  
On the ability of RCMs to capture the circulation pattern of Etesians 期刊论文
CLIMATE DYNAMICS, 2018, 51: 1687-1706
作者:  Dafka, Stella;  Toreti, Andrea;  Luterbacher, Juerg;  Zanis, Prodromos;  Tyrlis, Evangelos;  Xoplaki, Elena
收藏  |  浏览/下载:5/0  |  提交时间:2019/04/09
Etesians  Extreme wind  RCMs evaluation  Added value  20CR-v2c  ERA-20C  
A critical assessment of the long-term changes in the wintertime surface Arctic Oscillation and Northern Hemisphere storminess in the ERA20C reanalysis 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2018, 13 (9)
作者:  Bloomfield, H. C.;  Shaffrey, L. C.;  Hodges, K., I;  Vidale, P. L.
收藏  |  浏览/下载:2/0  |  提交时间:2019/04/09
ERA20C  reanalysis trends  Arctic Oscillation  extratropical cyclones  
Modelling extreme dry spells in the Mediterranean region in connection with atmospheric circulation 期刊论文
ATMOSPHERIC RESEARCH, 2018, 202: 40-48
作者:  Tramblay, Yves;  Hertig, Elke
收藏  |  浏览/下载:5/0  |  提交时间:2019/04/09
Extreme  Dry spells  GEV  Mediterranean  ERA-20C