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德国机构发布《气候适应型的水资源管理》报告 快报文章
资源环境快报,2024年第20期
作者:  魏艳红
Microsoft Word(23Kb)  |  收藏  |  浏览/下载:475/0  |  提交时间:2024/10/30
WBGU  Climate-resilient Water Management  Global Water Cycle  
2030年全球有望实现安全饮用水全覆盖 快报文章
资源环境快报,2024年第16期
作者:  董利苹
Microsoft Word(21Kb)  |  收藏  |  浏览/下载:601/0  |  提交时间:2024/09/01
Global Drinking Water Potential  Electricity-free  Solar Water Evaporation Device  
新型食品可显著降低饮食相关的环境影响 快报文章
气候变化快报,2022年第10期
作者:  刘莉娜
Microsoft Word(16Kb)  |  收藏  |  浏览/下载:780/0  |  提交时间:2022/05/19
Novel Foods  Global Warming Potential  Water Use  Land Use  
澳研究人员发现气候变暖正在放大全球水循环 快报文章
气候变化快报,2022年第05期
作者:  廖琴
Microsoft Word(14Kb)  |  收藏  |  浏览/下载:759/0  |  提交时间:2022/03/04
Global Warming  Climate Change  Global Water Cycle  
利用综合战略实现生物多样性、气候与水的目标 快报文章
资源环境快报,2021年第17期
作者:  裴惠娟
Microsoft Word(13Kb)  |  收藏  |  浏览/下载:737/0  |  提交时间:2021/09/20
Biodiversity  Carbon  Water  Global Importance  
《联合国全球水公约:促进可持续发展与和平》报告发布 快报文章
资源环境快报,2021年第2期
作者:  吴秀平
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United Nations  global water conventions  sustainable development  
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:61/0  |  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.


  
Stratospheric Water Vapor Feedback Disclosed by a Locking Experiment 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2020, 47 (12)
作者:  Huang, Yi;  Wang, Yuwei;  Huang, Han
收藏  |  浏览/下载:24/0  |  提交时间:2020/05/25
stratospheric water vapor  radiative feedback  carbon dioxide  global warming  climate model  radiative forcing  
Illuminating water cycle modifications and Earth system resilience in the Anthropocene 期刊论文
WATER RESOURCES RESEARCH, 2020, 56 (4)
作者:  Gleeson, Tom;  Wang-Erlandsson, Lan;  Porkka, Miina;  Zipper, Samuel C.;  Jaramillo, Fernando;  Gerten, Dieter;  Fetzer, Ingo;  Cornell, Sarah E.;  Piemontese, Luigi;  Gordon, Line J.;  Rockstroem, Johan;  Oki, Taikan;  Sivapalan, Murugesu;  Wada, Yoshihide;  Brauman, Kate A.;  Floerke, Martina;  Bierkens, Marc F. P.;  Lehner, Bernhard;  Keys, Patrick;  Kummu, Matti;  Wagener, Thorsten;  Dadson, Simon;  Troy, Tara J.;  Steffen, Will;  Falkenmark, Malin;  Famiglietti, James S.
收藏  |  浏览/下载:40/0  |  提交时间:2020/07/02
water cycle  Anthropocene  global hydrology  planetary boundary  
Tail-propelled aquatic locomotion in a theropod dinosaur 期刊论文
NATURE, 2020
作者:  Banerjee, Antara;  Fyfe, John C.;  Polvani, Lorenzo M.;  Waugh, Darryn;  Chang, Kai-Lan
收藏  |  浏览/下载:93/0  |  提交时间:2020/07/03

Discovery that the giant theropod dinosaur Spinosaurus has a large flexible tail indicates that it was primarily aquatic and swam in a similar manner to extant tail-propelled aquatic vertebrates.


In recent decades, intensive research on non-avian dinosaurs has strongly suggested that these animals were restricted to terrestrial environments(1). Historical proposals that some groups, such as sauropods and hadrosaurs, lived in aquatic environments(2,3) were abandoned decades ago(4-6). It has recently been argued that at least some of the spinosaurids-an unusual group of large-bodied theropods of the Cretaceous era-were semi-aquatic(7,8), but this idea has been challenged on anatomical, biomechanical and taphonomic grounds, and remains controversial(9-11). Here we present unambiguous evidence for an aquatic propulsive structure in a dinosaur, the giant theropod Spinosaurus aegyptiacus(7,12). This dinosaur has a tail with an unexpected and unique shape that consists of extremely tall neural spines and elongate chevrons, which forms a large, flexible fin-like organ capable of extensive lateral excursion. Using a robotic flapping apparatus to measure undulatory forces in physical models of different tail shapes, we show that the tail shape of Spinosaurus produces greater thrust and efficiency in water than the tail shapes of terrestrial dinosaurs and that these measures of performance are more comparable to those of extant aquatic vertebrates that use vertically expanded tails to generate forward propulsion while swimming. These results are consistent with the suite of adaptations for an aquatic lifestyle and piscivorous diet that have previously been documented for Spinosaurus(7,13,14). Although developed to a lesser degree, aquatic adaptations are also found in other members of the spinosaurid clade(15,16), which had a near-global distribution and a stratigraphic range of more than 50 million years(14), pointing to a substantial invasion of aquatic environments by dinosaurs.