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Nature:大西洋经向翻转环流未来变化新趋势 快报文章
地球科学快报,2025年第11期
作者:  王立伟,王高苗
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:411/0  |  提交时间:2025/06/10
Ocean Current  Climate Change  
国际研究指出南极冰架加速融化减缓南极环流强度 快报文章
气候变化快报,2025年第6期
作者:  秦冰雪
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:380/0  |  提交时间:2025/03/20
Antarctic Circumpolar Current  Ice Shelves  Meltwater  
美研究指出微生物通过洋流进入海洋深处 快报文章
资源环境快报,2024年第9期
作者:  牛艺博
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:579/4  |  提交时间:2024/05/15
Marine Microbial Life  Ocean Current  Deep Sea  
地幔流模式可能取决于板块俯冲类型 快报文章
地球科学快报,2024年第5期
作者:  王晓晨
Microsoft Word(14Kb)  |  收藏  |  浏览/下载:649/0  |  提交时间:2024/03/10
subduction zone  mantle current  
国际研究指出南极附近的深海洋流即将崩溃 快报文章
资源环境快报,2023年第07期
作者:  薛明媚,王金平
Microsoft Word(19Kb)  |  收藏  |  浏览/下载:560/1  |  提交时间:2023/04/15
Antarctic  Overturning Current  Sea Ice  
NOAA资助420万美元用于北加利福尼亚洋流生态系统研究 快报文章
资源环境快报,2022年第21期
作者:  薛明媚,吴秀平
Microsoft Word(16Kb)  |  收藏  |  浏览/下载:706/0  |  提交时间:2022/11/17
Northern California Current Ecosystem  National Marine Sanctuary  Climate Change  
全球仅8个主要排放国与地区有望实现最新的NDC目标 快报文章
气候变化快报,2021年第20期
作者:  董利苹
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:685/0  |  提交时间:2021/10/20
Greenhouse Gas Mitigation Scenarios  Major Emitting Countries  Current Climate Policies  Mitigation Commitments  
新型冠状病毒肺炎对全球气候的影响微不足道 快报文章
气候变化快报,2020年第17期
作者:  董利苹
Microsoft Word(13Kb)  |  收藏  |  浏览/下载:395/0  |  提交时间:2020/09/04
Climate Impacts  COVID-19  Current and Future  
Current European flood-rich period exceptional compared with past 500 years 期刊论文
NATURE, 2020, 583 (7817) : 560-+
作者:  ;  nter Blö;  schl;  Andrea Kiss;  Alberto Viglione;  Mariano Barriendos;  Oliver Bö;  hm;  Rudolf Brá;  zdil;  Denis Coeur;  Gaston Demaré;  e;  Maria Carmen Llasat;  Neil Macdonald;  Dag Retsö;  Lars Roald;  Petra Schmocker-Fackel;  Inê;  s Amorim;  Monika Bě;  ;  nová;  Gerardo Benito;  Chiara Bertolin;  Dario Camuffo;  Daniel Cornel;  Radosł;  aw Doktor;  ;  bor Elleder;  Silvia Enzi;  Joã;  o Carlos Garcia;  ;  diger Glaser;  Julia Hall;  Klaus Haslinger;  Michael Hofstä;  tter;  ;  rgen Komma;  Danuta Limanó;  wka;  David Lun;  Andrei Panin;  Juraj Parajka;  Hrvoje Petrić;  Fernando S. Rodrigo;  Christian Rohr;  Johannes Schö;  nbein;  Lothar Schulte;  Luí;  s Pedro Silva;  Willem H. J. Toonen;  Peter Valent;  ;  rgen Waser;  Oliver Wetter
收藏  |  浏览/下载:80/0  |  提交时间:2020/08/09

There are concerns that recent climate change is altering the frequency and magnitude of river floods in an unprecedented way(1). Historical studies have identified flood-rich periods in the past half millennium in various regions of Europe(2). However, because of the low temporal resolution of existing datasets and the relatively low number of series, it has remained unclear whether Europe is currently in a flood-rich period from a long-term perspective. Here we analyse how recent decades compare with the flood history of Europe, using a new database composed of more than 100 high-resolution (sub-annual) historical flood series based on documentary evidence covering all major regions of Europe. We show that the past three decades were among the most flood-rich periods in Europe in the past 500 years, and that this period differs from other flood-rich periods in terms of its extent, air temperatures and flood seasonality. We identified nine flood-rich periods and associated regions. Among the periods richest in floods are 1560-1580 (western and central Europe), 1760-1800 (most of Europe), 1840-1870 (western and southern Europe) and 1990-2016 (western and central Europe). In most parts of Europe, previous flood-rich periods occurred during cooler-than-usual phases, but the current flood-rich period has been much warmer. Flood seasonality is also more pronounced in the recent period. For example, during previous flood and interflood periods, 41 per cent and 42 per cent of central European floods occurred in summer, respectively, compared with 55 per cent of floods in the recent period. The exceptional nature of the present-day flood-rich period calls for process-based tools for flood-risk assessment that capture the physical mechanisms involved, and management strategies that can incorporate the recent changes in risk.


Analysis of thousands of historical documents recording floods in Europe shows that flooding characteristics in recent decades are unlike those of previous centuries.


  
Ice retreat in Wilkes Basin of East Antarctica during a warm interglacial 期刊论文
NATURE, 2020, 583 (7817) : 554-+
作者:  T. Blackburn;  G. H. Edwards;  S. Tulaczyk;  M. Scudder;  G. Piccione;  B. Hallet;  N. McLean;  J. C. Zachos;  B. Cheney;  J. T. Babbe
收藏  |  浏览/下载:59/0  |  提交时间:2020/08/09

Uranium isotopes in subglacial precipitates from the Wilkes Basin of the East Antarctic Ice Sheet reveal ice retreat during a warm Pleistocene interglacial period about 400,000 years ago.


Efforts to improve sea level forecasting on a warming planet have focused on determining the temperature, sea level and extent of polar ice sheets during Earth'  s past interglacial warm periods(1-3). About 400,000 years ago, during the interglacial period known as Marine Isotopic Stage 11 (MIS11), the global temperature was 1 to 2 degrees Celsius greater(2)and sea level was 6 to 13 metres higher(1,3). Sea level estimates in excess of about 10 metres, however, have been discounted because these require a contribution from the East Antarctic Ice Sheet(3), which has been argued to have remained stable for millions of years before and includes MIS11(4,5). Here we show how the evolution of(234)U enrichment within the subglacial waters of East Antarctica recorded the ice sheet'  s response to MIS11 warming. Within the Wilkes Basin, subglacial chemical precipitates of opal and calcite record accumulation of(234)U (the product of rock-water contact within an isolated subglacial reservoir) up to 20 times higher than that found in marine waters. The timescales of(234)U enrichment place the inception of this reservoir at MIS11. Informed by the(234)U cycling observed in the Laurentide Ice Sheet, where(234)U accumulated during periods of ice stability(6)and was flushed to global oceans in response to deglaciation(7), we interpret our East Antarctic dataset to represent ice loss within the Wilkes Basin at MIS11. The(234)U accumulation within the Wilkes Basin is also observed in the McMurdo Dry Valleys brines(8-10), indicating(11)that the brine originated beneath the adjacent East Antarctic Ice Sheet. The marine origin of brine salts(10)and bacteria(12)implies that MIS11 ice loss was coupled with marine flooding. Collectively, these data indicate that during one of the warmest Pleistocene interglacials, the ice sheet margin at the Wilkes Basin retreated to near the precipitate location, about 700 kilometres inland from the current position of the ice margin, which-assuming current ice volumes-would have contributed about 3 to 4 metres(13)to global sea levels.