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Study of the planetary boundary layer height in an urban environment using a combination of microwave radiometer and ceilometer 期刊论文
ATMOSPHERIC RESEARCH, 2020, 240
作者:  de Arruda Moreira, Gregori;  Luis Guerrero-Rascado, Juan;  Antonio Bravo-Aranda, Juan;  Foyo-Moreno, Inmaculada;  Cazorla, Alberto;  Alados, Inmaculada;  Lyamani, Hassan;  Landulfo, Eduardo;  Alados-Arboledas, Lucas
收藏  |  浏览/下载:26/0  |  提交时间:2020/08/18
Planetary boundary layer  Ceilometer  Microwave radiometer  Remote sensing  
Projected regional responses of precipitation extremes and their joint probabilistic behaviors to climate change in the upper and middle reaches of Huaihe River Basin, China 期刊论文
ATMOSPHERIC RESEARCH, 2020, 240
作者:  Mou, Shiyu;  Shi, Peng;  Qu, Simin;  Feng, Ying;  Chen, Chen;  Dong, Fengcheng
收藏  |  浏览/下载:19/0  |  提交时间:2020/08/18
CMIP5  Precipitation indices  Spatial distribution  Copula function  Kendall return period  
Variability of the aridity index and related drought parameters in Greece using climatological data over the last century (1900-1997) 期刊论文
ATMOSPHERIC RESEARCH, 2020, 240
作者:  Tsiros, Ioannis X.;  Nastos, Panagiotis;  Proutsos, Nikolaos D.;  Tsaousidis, Alexandros
收藏  |  浏览/下载:16/0  |  提交时间:2020/08/18
Drought  Aridity index  Mediterranean basin  Climate variability  Thornthwaite water balance model  
Comparison of three microphysics parameterization schemes in the WRF model for an extreme rainfall event in the coastal metropolitan City of Guangzhou, China 期刊论文
ATMOSPHERIC RESEARCH, 2020, 240
作者:  Huang, Yongjie;  Wang, Yaping;  Xue, Lulin;  Wei, Xiaolin;  Zhang, Lina;  Li, Huaiyu
收藏  |  浏览/下载:13/0  |  提交时间:2020/08/18
Microphysics parameterization  WRF  Extreme rainfall  Latent heat  
Assessments of the factors controlling latent heat flux and the coupling degree between an alpine wetland and the atmosphere on the Qinghai-Tibetan Plateau in summer 期刊论文
ATMOSPHERIC RESEARCH, 2020, 240
作者:  Chen, Jinlei;  Wen, Jun;  Kang, Shichang;  Meng, Xianhong;  Tian, Hui;  Ma, Xin;  Yuan, Yuan
收藏  |  浏览/下载:9/0  |  提交时间:2020/08/18
Wetlands  Latent heat  Coupling  Control factor  CLM  
Spatiotemporal distributions of cloud properties over China based on Himawari-8 advanced Himawari imager data 期刊论文
ATMOSPHERIC RESEARCH, 2020, 240
作者:  Yang, Yikun;  Zhao, Chuanfeng;  Fan, Hao
收藏  |  浏览/下载:18/0  |  提交时间:2020/08/18
Cloud fraction  Cloud top height  Cloud top temperature  Cloud optical thickness  Himawari-8  Diurnal variation  
Vulnerability of vegetation activities to drought in Central Asia 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2020, 15 (8)
作者:  Deng, Haoyu;  Yin, Yunhe;  Han, Xiang
收藏  |  浏览/下载:22/0  |  提交时间:2020/08/18
drought  vegetation  vulnerability  climate change  Central Asia  
Inferring CO(2)fertilization effect based on global monitoring land-atmosphere exchange with a theoretical model 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2020, 15 (8)
作者:  Ueyama, Masahito;  39;omi
收藏  |  浏览/下载:15/0  |  提交时间:2020/08/18
CO(2)fertilization effect  photosynthesis  evapotranspiration  eddy covariance  sun  shade model  
How many sea scallops are there and why does it matter? 期刊论文
FRONTIERS IN ECOLOGY AND THE ENVIRONMENT, 2020
作者:  Stokesbury, Kevin D. E.;  Bethoney, N. David
收藏  |  浏览/下载:7/0  |  提交时间:2020/08/18
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:18/0  |  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.