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Potential for large-scale CO2 removal via enhanced rock weathering with croplands 期刊论文
NATURE, 2020, 583 (7815) : 242-+
作者:  David J. Beerling;  Euripides P. Kantzas;  Mark R. Lomas;  Peter Wade;  Rafael M. Eufrasio;  Phil Renforth;  Binoy Sarkar;  M. Grace Andrews;  Rachael H. James;  Christopher R. Pearce;  Jean-Francois Mercure;  Hector Pollitt;  Philip B. Holden;  Neil R. Edwards;  Madhu Khanna;  Lenny Koh;  Shaun Quegan;  Nick F. Pidgeon;  Ivan A. Janssens;  James Hansen;  Steven A. Banwart
收藏  |  浏览/下载:57/0  |  提交时间:2020/07/14

Enhanced silicate rock weathering (ERW), deployable with croplands, has potential use for atmospheric carbon dioxide (CO2) removal (CDR), which is now necessary to mitigate anthropogenic climate change(1). ERW also has possible co-benefits for improved food and soil security, and reduced ocean acidification(2-4). Here we use an integrated performance modelling approach to make an initial techno-economic assessment for 2050, quantifying how CDR potential and costs vary among nations in relation to business-as-usual energy policies and policies consistent with limiting future warming to 2 degrees Celsius(5). China, India, the USA and Brazil have great potential to help achieve average global CDR goals of 0.5 to 2gigatonnes of carbon dioxide (CO2) per year with extraction costs of approximately US$80-180 per tonne of CO2. These goals and costs are robust, regardless of future energy policies. Deployment within existing croplands offers opportunities to align agriculture and climate policy. However, success will depend upon overcoming political and social inertia to develop regulatory and incentive frameworks. We discuss the challenges and opportunities of ERW deployment, including the potential for excess industrial silicate materials (basalt mine overburden, concrete, and iron and steel slag) to obviate the need for new mining, as well as uncertainties in soil weathering rates and land-ocean transfer of weathered products.


  
Intraplate volcanism originating from upwelling hydrous mantle transition zone 期刊论文
NATURE, 2020
作者:  Calabrese, Claudia;  Davidson, Natalie R.;  Demircioglu, Deniz;  Fonseca, Nuno A.;  He, Yao;  Kahles, Andre;  Kjong-Van Lehmann;  Liu, Fenglin;  Shiraishi, Yuichi;  Soulette, Cameron M.;  Urban, Lara;  Greger, Liliana;  Li, Siliang;  Liu, Dongbing;  Perry, Marc D.;  Xiang, Qian;  Zhang, Fan;  Zhang, Junjun;  Bailey, Peter;  Erkek, Serap;  Hoadley, Katherine A.;  Hou, Yong;  Huska, Matthew R.;  Kilpinen, Helena;  Korbel, Jan O.;  Marin, Maximillian G.;  Markowski, Julia;  Nandi, Tannistha;  Pan-Hammarstrom, Qiang;  Pedamallu, Chandra Sekhar;  Siebert, Reiner;  Stark, Stefan G.;  Su, Hong;  Tan, Patrick;  Waszak, Sebastian M.;  Yung, Christina;  Zhu, Shida;  Awadalla, Philip;  Creighton, Chad J.;  Meyerson, Matthew;  Ouellette, B. F. Francis;  Wu, Kui;  Yang, Huanming;  Brazma, Alvis;  Brooks, Angela N.;  Goke, Jonathan;  Raetsch, Gunnar;  Schwarz, Roland F.;  Stegle, Oliver;  Zhang, Zemin
收藏  |  浏览/下载:119/0  |  提交时间:2020/05/13

Most magmatism occurring on Earth is conventionally attributed to passive mantle upwelling at mid-ocean ridges, to slab devolatilization at subduction zones, or to mantle plumes. However, the widespread Cenozoic intraplate volcanism in northeast China(1-3) and the young petit-spot volcanoes(4-7) offshore of the Japan Trench cannot readily be associated with any of these mechanisms. In addition, the mantle beneath these types of volcanism is characterized by zones of anomalously low seismic velocity above and below the transition zone(8-12) (a mantle level located at depths between 410 and 660 kilometres). A comprehensive interpretation of these phenomena is lacking. Here we show that most (or possibly all) of the intraplate and petit-spot volcanism and low-velocity zones around the Japanese subduction zone can be explained by the Cenozoic interaction of the subducting Pacific slab with a hydrous mantle transition zone. Numerical modelling indicates that 0.2 to 0.3 weight per cent of water dissolved in mantle minerals that are driven out from the transition zone in response to subduction and retreat of a tectonic plate is sufficient to reproduce the observations. This suggests that a critical amount of water may have accumulated in the transition zone around this subduction zone, as well as in others of the Tethyan tectonic belt(13) that are characterized by intraplate or petit-spot volcanism and low-velocity zones in the underlying mantle.


The widespread intraplate volcanism in northeast China and the unusual '  petit-spot'  volcanoes offshore Japan could have resulted from the interaction of the subducting Pacific slab with a hydrous mantle transition zone.


  
Quantifying human contributions to past and future ocean warming and thermosteric sea level rise 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2019, 14 (7)
作者:  Tokarska, Katarzyna B.;  Hegerl, Gabriele C.;  Schurer, Andrew P.;  Ribes, Aurelien;  Fasullo, John T.
收藏  |  浏览/下载:23/0  |  提交时间:2019/11/27
ocean warming  thermosteric sea level  detection and attribution  climate change  Earth system modelling  
Evaluation of CMIP5 and CORDEX derived wave climate in Indian Ocean 期刊论文
CLIMATE DYNAMICS, 2019, 52: 4463-4482
作者:  Chowdhury, Piyali;  Behera, Manasa Ranjan
收藏  |  浏览/下载:8/0  |  提交时间:2019/11/26
Wave modelling  Wave climate  Seasonality  CMIP5  CORDEX  Indian Ocean  
A statistical seasonal forecast model of North Indian Ocean tropical cyclones using the quasi-biennial oscillation 期刊论文
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2019, 39 (2) : 934-952
作者:  Wahiduzzaman, Md;  Oliver, Eric C. J.;  Klotzbach, Philip J.;  Wotherspoon, Simon J.;  Holbrook, Neil J.
收藏  |  浏览/下载:16/0  |  提交时间:2019/04/09
landfall  North Indian Ocean  quasi-biennial oscillation  statistical modelling  tropical cyclone genesis  tropical cyclone trajectories  
Obtaining the correct sea surface temperature: bias correction of regional climate model data for the Mediterranean Sea 期刊论文
CLIMATE DYNAMICS, 2018, 51 (3) : 1095-1117
作者:  Macias, Diego;  Garcia-Gorriz, Elisa;  Dosio, Alessandro;  Stips, Adolf;  Keuler, Klaus
收藏  |  浏览/下载:12/0  |  提交时间:2019/04/09
Ocean modelling  Mediterranean Sea  Sea surface temperature  Bias correction  
Development of a regional ocean-atmosphere-wave coupled model and its preliminary evaluation over the CORDEX East Asia domain 期刊论文
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2017, 37 (12)
作者:  Zou, Liwei;  Zhou, Tianjun;  Qiao, Fangli;  Zhao, Wei
收藏  |  浏览/下载:12/0  |  提交时间:2019/04/09
regional climate modelling  surface wave  regional ocean atmosphere coupled model  
Impact of the GeoMIP G1 sunshade geoengineering experiment on the Atlantic meridional overturning circulation 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2017, 12 (3)
作者:  Hong, Yu;  Moore, John C.;  Jevrejeva, Svetlana;  Ji, Duoying;  Phipps, Steven J.;  Lenton, Andrew;  Tilmes, Simone;  Watanabe, Shingo;  Zhao, Liyun
收藏  |  浏览/下载:15/0  |  提交时间:2019/04/09
ocean temperatures  circulation modelling  turbulent fluxes  
Workshop on Modelling and Observing the Impacts of Dust Transport/Deposition on Marine Productivity 科技报告
来源:World Meteorological Organization (WMO). 出版年: 2011
作者:  Robert A. Duce;  Peter S. Liss;  World Meteorological Organization
收藏  |  浏览/下载:18/0  |  提交时间:2019/04/05
Oceans  Ocean model  Modelling  Marine environment  Ocean-atmosphere interaction  Global Atmosphere Watch Programme (GAW)  - International  GAW 202