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Coastal Stratocumulus Dissipation Dependence on Initial Conditions and Boundary Forcings in a Mixed-Layer Model 期刊论文
Journal of the Atmospheric Sciences, 2020
作者:  Zapata, Mónica Zamora;  Norris, Joel R.;  Kleissl, Jan
收藏  |  浏览/下载:5/0  |  提交时间:2020/07/21
Four-dimensional surface motions of the Slumgullion landslide and quantification of hydrometeorological forcing 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Hu, Xie;  Buergmann, Roland;  Schulz, William H.;  Fielding, Eric J.
收藏  |  浏览/下载:6/0  |  提交时间:2020/06/09
Controls on surface water carbonate chemistry along North American ocean margins 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Cai, Wei-Jun;  Xu, Yuan-Yuan;  Feely, Richard A.;  Wanninkhof, Rik;  Jonsson, Bror;  Alin, Simone R.;  Barbero, Leticia;  Cross, Jessica N.;  Azetsu-Scott, Kumiko;  Fassbender, Andrea J.;  Carter, Brendan R.;  Jiang, Li-Qing;  Pepin, Pierre;  Chen, Baoshan;  Hussain, Najid;  Reimer, Janet J.;  Xue, Liang;  Salisbury, Joseph E.;  Martin Hernandez-Ayon, Jose;  Langdon, Chris;  Li, Qian;  Sutton, Adrienne J.;  Chen, Chen-Tung A.;  Gledhill, Dwight K.
收藏  |  浏览/下载:14/0  |  提交时间:2020/06/09
Subpolar marginal seas fuel the North Pacific through the intermediate water at the termination of the ocean circulation 期刊论文
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2020, 117 (23) : 12665-12673
作者:  Nishioka, Jun;  Obata, Hajime;  Ogawa, Hiroshi;  Ono, Kazuya;  Yamashita, Youhei;  Lee, Keunjong;  Takeda, Shigenobu;  Yasuda, Ichiro
收藏  |  浏览/下载:11/0  |  提交时间:2020/06/01
dissolved iron  macronutrients  North Pacific Ocean  island chains mixing  GEOTRACES  
Ediacaran reorganization of the marine phosphorus cycle 期刊论文
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2020, 117 (22) : 11961-11967
作者:  Laakso, Thomas A.;  Sperling, Erik A.;  Johnston, David T.;  Knoll, Andrew H.
收藏  |  浏览/下载:9/0  |  提交时间:2020/05/20
Ediacaran  biosphere  sulfate  phopshorus  phosphorite  
Significant methane ebullition from alpine permafrost rivers on the East Qinghai-Tibet Plateau 期刊论文
NATURE GEOSCIENCE, 2020, 13 (5)
作者:  Zhang, Liwei;  Xia, Xinghui;  Liu, Shaoda;  Zhang, Sibo;  Li, Siling;  Wang, Junfeng;  Wang, Gongqin;  Gao, Hui;  Zhang, Zhenrui;  Wang, Qingrui;  Wen, Wu;  Liu, Ran;  Yang, Zhifeng;  Stanley, Emily H.;  Raymond, Peter A.
收藏  |  浏览/下载:11/0  |  提交时间:2020/05/13
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.


  
East Siberian Arctic inland waters emit mostly contemporary carbon 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Dean, Joshua F.;  Meisel, Ove H.;  Rosco, Melanie Martyn;  Marchesini, Luca Belelli;  Garnett, Mark H.;  Lenderink, Henk;  van Logtestijn, Richard;  Borges, Alberto, V;  Bouillon, Steven;  Lambert, Thibault;  Rockmann, Thomas;  Maximov, Trofim;  Petrov, Roman;  Karsanaev, Sergei;  Aerts, Rien;  van Huissteden, Jacobus;  Vonk, Jorien E.;  Dolman, A. Johannes
收藏  |  浏览/下载:14/0  |  提交时间:2020/05/13
Urban vacant lands impart hydrological benefits across city landscapes 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Kelleher, Christa;  Golden, Heather E.;  Burkholder, Sean;  Shuster, William
收藏  |  浏览/下载:5/0  |  提交时间:2020/05/13
Ice front blocking of ocean heat transport to an Antarctic ice shelf 期刊论文
NATURE, 2020, 578 (7796) : 568-+
作者:  Alexandrov, Ludmil B.;  Kim, Jaegil;  Haradhvala, Nicholas J.;  Huang, Mi Ni;  Ng, Alvin Wei Tian;  Wu, Yang;  Boot, Arnoud;  Covington, Kyle R.;  Gordenin, Dmitry A.;  Bergstrom, Erik N.;  Islam, S. M. Ashiqul;  Lopez-Bigas, Nuria;  Klimczak, Leszek J.;  McPherson, John R.;  Morganella, Sandro;  Sabarinathan, Radhakrishnan;  Wheeler, David A.;  Mustonen, Ville;  Getz, Gad;  Rozen, Steven G.;  Stratton, Michael R.
收藏  |  浏览/下载:12/0  |  提交时间:2020/05/13

The front of the Getz Ice Shelf in West Antarctica creates an abrupt topographic step that deflects ocean currents, suppressing 70% of the heat delivery to the ice sheet.


Mass loss from the Antarctic Ice Sheet to the ocean has increased in recent decades, largely because the thinning of its floating ice shelves has allowed the outflow of grounded ice to accelerate(1,2). Enhanced basal melting of the ice shelves is thought to be the ultimate driver of change(2,3), motivating a recent focus on the processes that control ocean heat transport onto and across the seabed of the Antarctic continental shelf towards the ice(4-6). However, the shoreward heat flux typically far exceeds that required to match observed melt rates(2,7,8), suggesting that other critical controls exist. Here we show that the depth-independent (barotropic) component of the heat flow towards an ice shelf is blocked by the marked step shape of the ice front, and that only the depth-varying (baroclinic) component, which is typically much smaller, can enter the sub-ice cavity. Our results arise from direct observations of the Getz Ice Shelf system and laboratory experiments on a rotating platform. A similar blocking of the barotropic component may occur in other areas with comparable ice-bathymetry configurations, which may explain why changes in the density structure of the water column have been found to be a better indicator of basal melt rate variability than the heat transported onto the continental shelf(9). Representing the step topography of the ice front accurately in models is thus important for simulating ocean heat fluxes and induced melt rates.