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A Large Ensemble Approach to Quantifying Internal Model Variability Within the WRF Numerical Model 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2020, 125 (7)
作者:  Bassett, R.;  Young, P. J.;  Blair, G. S.;  Samreen, F.;  Simm, W.
收藏  |  浏览/下载:5/0  |  提交时间:2020/07/02
ensemble  initial conditions  internal model variability (IMV)  regional climate model (RCM)  uncertainty  Weather Research and Forecasting (WRF)  
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:55/0  |  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.


  
Temperate rainforests near the South Pole during peak Cretaceous warmth 期刊论文
NATURE, 2020, 580 (7801) : 81-+
作者:  Johann P. Klages;  Ulrich Salzmann;  Torsten Bickert;  Claus-Dieter Hillenbrand;  Karsten Gohl;  Gerhard Kuhn;  Steven M. Bohaty;  ;  rgen Titschack;  Juliane Mü;  ller;  Thomas Frederichs;  Thorsten Bauersachs;  Werner Ehrmann;  Tina van de Flierdt;  Patric Simõ;  es Pereira;  Robert D. Larter;  Gerrit Lohmann;  Igor Niezgodzki;  Gabriele Uenzelmann-Neben;  Maximilian Zundel;  Cornelia Spiegel;  Chris Mark;  David Chew;  Jane E. Francis;  Gernot Nehrke;  Florian Schwarz;  James A. Smith;  Tim Freudenthal;  Oliver Esper;  Heiko Pä;  like;  Thomas A. Ronge;  Ricarda Dziadek
收藏  |  浏览/下载:12/0  |  提交时间:2020/05/13

The mid-Cretaceous period was one of the warmest intervals of the past 140 million years(1-5), driven by atmospheric carbon dioxide levels of around 1,000 parts per million by volume(6). In the near absence of proximal geological records from south of the Antarctic Circle, it is disputed whether polar ice could exist under such environmental conditions. Here we use a sedimentary sequence recovered from the West Antarctic shelf-the southernmost Cretaceous record reported so far-and show that a temperate lowland rainforest environment existed at a palaeolatitude of about 82 degrees S during the Turonian-Santonian age (92 to 83 million years ago). This record contains an intact 3-metre-long network of in situ fossil roots embedded in a mudstone matrix containing diverse pollen and spores. A climate model simulation shows that the reconstructed temperate climate at this high latitude requires a combination of both atmospheric carbon dioxide concentrations of 1,120-1,680 parts per million by volume and a vegetated land surface without major Antarctic glaciation, highlighting the important cooling effect exerted by ice albedo under high levels of atmospheric carbon dioxide.


  
Mass balance of the Greenland Ice Sheet from 1992 to 2018 期刊论文
NATURE, 2020, 579 (7798) : 233-+
作者:  Scudellari, Megan
收藏  |  浏览/下载:11/0  |  提交时间:2020/04/16

The Greenland Ice Sheet has been a major contributor to global sea-level rise in recent decades(1,2), and it is expected to continue to be so(3). Although increases in glacier flow(4-6) and surface melting(7-9) have been driven by oceanic(10-12) and atmospheric(13,14) warming, the magnitude and trajectory of the ice sheet'  s mass imbalance remain uncertain. Here we compare and combine 26 individual satellite measurements of changes in the ice sheet'  s volume, flow and gravitational potential to produce a reconciled estimate of its mass balance. The ice sheet was close to a state of balance in the 1990s, but annual losses have risen since then, peaking at 345 +/- 66 billion tonnes per year in 2011. In all, Greenland lost 3,902 +/- 342 billion tonnes of ice between 1992 and 2018, causing the mean sea level to rise by 10.8 +/- 0.9 millimetres. Using three regional climate models, we show that the reduced surface mass balance has driven 1,964 +/- 565 billion tonnes (50.3 per cent) of the ice loss owing to increased meltwater runoff. The remaining 1,938 +/- 541 billion tonnes (49.7 per cent) of ice loss was due to increased glacier dynamical imbalance, which rose from 46 +/- 37 billion tonnes per year in the 1990s to 87 +/- 25 billion tonnes per year since then. The total rate of ice loss slowed to 222 +/- 30 billion tonnes per year between 2013 and 2017, on average, as atmospheric circulation favoured cooler conditions(15) and ocean temperatures fell at the terminus of Jakobshavn Isbr AE(16). Cumulative ice losses from Greenland as a whole have been close to the rates predicted by the Intergovernmental Panel on Climate Change for their high-end climate warming scenario(17), which forecast an additional 70 to 130 millimetres of global sea-level rise by 2100 compared with their central estimate.


  
Are mixed-tree plantations including a nitrogen-fixing species more productive than monocultures? 期刊论文
FOREST ECOLOGY AND MANAGEMENT, 2019, 441: 242-252
作者:  Marron, Nicolas;  Epron, Daniel
收藏  |  浏览/下载:9/0  |  提交时间:2019/11/26
Mixed-tree plantations  N-2-fixation  Meta-analysis  Biomass production  Monocultures  Climate conditions  Mixing proportion  Developmental stage  
Hydrological severity assessment of extreme climate conditions 期刊论文
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2019, 39 (5) : 2725-2736
作者:  Park, Jongmin;  Baik, Jongjin;  Choi, Minha;  Jeong, Jaehwan;  Sur, Chanyang
收藏  |  浏览/下载:12/0  |  提交时间:2019/11/26
climate change  extreme climate conditions  GLDAS  hydrological severity index  
Background Conditions Influence the Estimated Cloud Radiative Effects of Anthropogenic Aerosol Emissions From Different Source Regions 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2019, 124 (4) : 2276-2295
作者:  Grandey, Benjamin S.;  Wang, Chien
收藏  |  浏览/下载:4/0  |  提交时间:2019/04/09
aerosols  background conditions  anthropogenic aerosol emissions  climate model  radiative forcing  
Characterising spatiotemporal variability of South Asia's climate extremes in past decades 期刊论文
CLIMATE RESEARCH, 2019, 77 (3) : 249-265
作者:  Chen, Yun;  Xu, Tingbao;  Shui, Junfeng;  Liu, Rui;  Wahid, Shahriar;  Shi, Kaifang;  Yang, Haichang;  Cheng, Zhibo
收藏  |  浏览/下载:9/0  |  提交时间:2019/11/26
Climate variables  Indices of extreme conditions  Gridded daily climate data  Change trend  
Improving sea level simulation in Mediterranean regional climate models 期刊论文
CLIMATE DYNAMICS, 2018, 51 (3) : 1167-1178
作者:  Adloff, Fanny;  Jorda, Gabriel;  Somot, Samuel;  Sevault, Florence;  Arsouze, Thomas;  Meyssignac, Benoit;  Li, Laurent;  Planton, Serge
收藏  |  浏览/下载:5/0  |  提交时间:2019/04/09
Mediterranean  Sea level  Regional climate model  Lateral boundary conditions  Atlantic forcing  
Changing groundwater discharge dynamics in permafrost regions 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2018, 13 (8)
作者:  Lamontagne-Halle, Pierrick;  McKenzie, Jeffrey M.;  Kurylyk, Barret L.;  Zipper, Samuel C.
收藏  |  浏览/下载:23/0  |  提交时间:2019/04/09
permafrost  groundwater modelling  cold regions hydrology  groundwater discharge  arctic baseflow  boundary conditions  climate warming