Preflare activity of solar prominences     

G. Simon  N. Mein  P. Mein  L. Gesztelyi 《Solar physics》1984,93(2):325-336

The preflare activity of a plage filament is analysed from H observations made with the Multichannel Subtractive Double Pass Spectrograph (MSDP) of the Meudon Solar Tower. The June 22, 1980 event is studied and interpreted in terms of preflare heating of a filament, connected to the rise of emerging flux, and the relative approach of pores of different magnetic polarity, prior to the onset of a two-ribbon flare.The region with enhanced magnetic field, around the filament, begins to brighten slowly 20 min before the triggering of the flare, in the center of H. Filament dark material begins to rise rapidly while the brightest point on one side drifts towards it, 6 min before the onset of the two-ribbon flare. Simultaneously the absorbing material separates from the remaining part of the filament.In the discussion, we suggest that most of the observed features may be the consequence of emergence of new magnetic flux and the related reconnection processes.  相似文献   

Natural hazards in Australia: droughts   总被引：3，自引：0，他引：3  

Anthony S. Kiem  Fiona Johnson  Seth Westra  Albert van Dijk  Jason P. Evans  Alison O’Donnell  Alexandra Rouillard  Cameron Barr  Jonathan Tyler  Mark Thyer  Doerte Jakob  Fitsum Woldemeskel  Bellie Sivakumar  Raj Mehrotra 《Climatic change》2016,139(1):37-54

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The impacts of climate change on river flood risk at the global scale   总被引：6，自引：0，他引：6  

Nigel W. Arnell  Simon N. Gosling 《Climatic change》2016,134(3):387-401

This paper presents an assessment of the implications of climate change for global river flood risk. It is based on the estimation of flood frequency relationships at a grid resolution of 0.5?×?0.5°, using a global hydrological model with climate scenarios derived from 21 climate models, together with projections of future population. Four indicators of the flood hazard are calculated; change in the magnitude and return period of flood peaks, flood-prone population and cropland exposed to substantial change in flood frequency, and a generalised measure of regional flood risk based on combining frequency curves with generic flood damage functions. Under one climate model, emissions and socioeconomic scenario (HadCM3 and SRES A1b), in 2050 the current 100-year flood would occur at least twice as frequently across 40 % of the globe, approximately 450 million flood-prone people and 430 thousand km² of flood-prone cropland would be exposed to a doubling of flood frequency, and global flood risk would increase by approximately 187 % over the risk in 2050 in the absence of climate change. There is strong regional variability (most adverse impacts would be in Asia), and considerable variability between climate models. In 2050, the range in increased exposure across 21 climate models under SRES A1b is 31–450 million people and 59 to 430 thousand km² of cropland, and the change in risk varies between ?9 and +376 %. The paper presents impacts by region, and also presents relationships between change in global mean surface temperature and impacts on the global flood hazard. There are a number of caveats with the analysis; it is based on one global hydrological model only, the climate scenarios are constructed using pattern-scaling, and the precise impacts are sensitive to some of the assumptions in the definition and application.  相似文献   

Natural hazards in Australia: floods     

Fiona Johnson  Christopher J. White  Albert van Dijk  Marie Ekstrom  Jason P. Evans  Dörte Jakob  Anthony S. Kiem  Michael Leonard  Alexandra Rouillard  Seth Westra 《Climatic change》2016,139(1):21-35

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Extreme air–sea interaction over the North Atlantic subpolar gyre during the winter of 2013–2014 and its sub-surface legacy     

Jeremy P. Grist  Simon A. Josey  Zoe L. Jacobs  Robert Marsh  Bablu Sinha  Erik Van Sebille 《Climate Dynamics》2016,46(11-12):4027-4045

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GLONASS ionosphere-free ambiguity resolution for precise point positioning   总被引：3，自引：3，他引：0  

Simon Banville 《Journal of Geodesy》2016,90(5):487-496

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Evaluating the importance of different coupled thermal,hydraulic, mechanical and chemical process simulations during fluid flow experiments in fractured novaculite and fractured granite     

Neil Chittenden  Christopher I. McDermott  Alexander E. Bond  James Wilson  Simon Norris 《Environmental Earth Sciences》2016,75(15):1133

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Multiphase lattice Boltzmann simulations for porous media applications   总被引：1，自引：0，他引：1  

Haihu Liu  Qinjun Kang  Christopher R. Leonardi  Sebastian Schmieschek  Ariel Narváez  Bruce D. Jones  John R. Williams  Albert J. Valocchi  Jens Harting 《Computational Geosciences》2016,20(4):777-805

Over the last two decades, lattice Boltzmann methods have become an increasingly popular tool to compute the flow in complex geometries such as porous media. In addition to single phase simulations allowing, for example, a precise quantification of the permeability of a porous sample, a number of extensions to the lattice Boltzmann method are available which allow to study multiphase and multicomponent flows on a pore scale level. In this article, we give an extensive overview on a number of these diffuse interface models and discuss their advantages and disadvantages. Furthermore, we shortly report on multiphase flows containing solid particles, as well as implementation details and optimization issues.  相似文献   

Dissolved noble gases and stable isotopes as tracers of preferential fluid flow along faults in the Lower Rhine Embayment,Germany   总被引：1，自引：0，他引：1  

L. P. Gumm  V. F. Bense  P. F. Dennis  K. M. Hiscock  N. Cremer  S. Simon 《Hydrogeology Journal》2016,24(1):99-108

Groundwater in shallow unconsolidated sedimentary aquifers close to the Bornheim fault in the Lower Rhine Embayment (LRE), Germany, has relatively low δ²H and δ¹⁸O values in comparison to regional modern groundwater recharge, and ⁴He concentrations up to 1.7?×?10^?4 cm³ (STP) g^–1?±?2.2 % which is approximately four orders of magnitude higher than expected due to solubility equilibrium with the atmosphere. Groundwater age dating based on estimated in situ production and terrigenic flux of helium provides a groundwater residence time of ～10⁷ years. Although fluid exchange between the deep basal aquifer system and the upper aquifer layers is generally impeded by confining clay layers and lignite, this study’s geochemical data suggest, for the first time, that deep circulating fluids penetrate shallow aquifers in the locality of fault zones, implying  that sub-vertical fluid flow occurs along faults in the LRE. However, large hydraulic-head gradients observed across many faults suggest that they act as barriers to lateral groundwater flow. Therefore, the geochemical data reported here also substantiate a conduit-barrier model of fault-zone hydrogeology in unconsolidated sedimentary deposits, as well as corroborating the concept that faults in unconsolidated aquifer systems can act as loci for hydraulic connectivity between deep and shallow aquifers. The implications of fluid flow along faults in sedimentary basins worldwide are far reaching and of particular concern for carbon capture and storage (CCS) programmes, impacts of deep shale gas recovery for shallow groundwater aquifers, and nuclear waste storage sites where fault zones could act as potential leakage pathways for hazardous fluids.  相似文献   

The role of porous matrix in water flow regulation within a karst unsaturated zone: an integrated hydrogeophysical approach     

Simon D. Carrière  Konstantinos Chalikakis  Charles Danquigny  Hendrik Davi  Naomi Mazzilli  Chloé Ollivier  Christophe Emblanch 《Hydrogeology Journal》2016,24(7):1905-1918

Some portions of the porous rock matrix in the karst unsaturated zone (UZ) can contain large volumes of water and play a major role in water flow regulation. The essential results are presented of a local-scale study conducted in 2011 and 2012 above the Low Noise Underground Laboratory (LSBB – Laboratoire Souterrain à Bas Bruit) at Rustrel, southeastern France. Previous research revealed the geological structure and water-related features of the study site and illustrated the feasibility of specific hydrogeophysical measurements. In this study, the focus is on hydrodynamics at the seasonal and event timescales. Magnetic resonance sounding (MRS) measured a high water content (more than 10 %) in a large volume of rock. This large volume of water cannot be stored in fractures and conduits within the UZ. MRS was also used to measure the seasonal variation of water stored in the karst UZ. A process-based model was developed to simulate the effect of vegetation on groundwater recharge dynamics. In addition, electrical resistivity tomography (ERT) monitoring was used to assess preferential water pathways during a rain event. This study demonstrates the major influence of water flow within the porous rock matrix on the UZ hydrogeological functioning at both the local (LSBB) and regional (Fontaine de Vaucluse) scales. By taking into account the role of the porous matrix in water flow regulation, these findings may significantly improve karst groundwater hydrodynamic modelling, exploitation, and sustainable management.  相似文献