Source structure and dynamics of Pc 1 pulsations at low latitudes     

D.J. Webster  B.J. Fraser 《Planetary and Space Science》1984,32(8):935-947

Structured Pc 1 signals propagate in the ionospheric F2 region duct from their secondary sources at high latitudes to lower latitudes. Propagation directions to low latitude stations can be inferred from measurements of polarization parameters. The analysis of five events recorded at two low latitude stations (L = 1.9) are presented. Direction of arrival measurements are used to investigate the spatial and temporal structure of Pc 1 sources. Results show a close relationship between the structure of events identified in the frequency-time representation and direction of arrival measurement patterns. Multiple sources are sometimes indicated.  相似文献   

High technology, space and society: Castells, M. (ed.) Beverly Hills: Sage, Urban Affairs Annual Reviews, Volume 28, 1985. 320 pp. £31 hardback, £15.50 paperback.     

Clive Morphet 《Applied geography (Sevenoaks, England)》1986,6(4)

  相似文献   

Small power adaptation: The case of Denmark and the aw of the sea: by Finn Laursen Department of Public Finance and Policy,Odense University,Occasional Papers No 3, 1983, 37 pp     

Clive Archer 《Marine Policy》1983,7(4):320

  相似文献   

Spatial and temporal correlation of underwater sunlight fluctuations in the sea     

Fraser  A. Walker  R. Jurgens  F. 《Oceanic Engineering, IEEE Journal of》1980,5(3):195-198

A submerged linear array of photodetectors was used to measure sunlight irradiance fluctuations caused by ocean surface waves. Decorrelation times and lengths were found to be functions of depth. It was also found that the sensor depth selects a dominant temporal frequency from the random surface waves.  相似文献   

First results from the Very Small Array – I. Observational methods     

Robert A. Watson  Pedro Carreira  Kieran Cleary  Rod D. Davies  Richard J. Davis  Clive Dickinson  Keith Grainge †  Carlos M. Gutiérrez  Michael P. Hobson  Michael E. Jones  Rüdiger Kneissl  Anthony Lasenby  Klaus Maisinger  Guy G. Pooley  Rafael Rebolo  José Alberto Rubiño-Martin ‡  Ben Rusholme §  Richard D. E. Saunders  Richard Savage  Paul F. Scott  An&#;e Slosar  Pedro J. Sosa Molina  Angela C. Taylor  David Titterington  Elizabeth Waldram  Althea Wilkinson 《Monthly notices of the Royal Astronomical Society》2003,341(4):1057-1065

  相似文献   

MOSSBAUER STUDY OF THE ALLENDE METEORITE     

Frederick W. Oliver  Edet E. Isuk  Clive Wynter 《Meteoritics & planetary science》1984,19(1):25-27

  相似文献   

Adsorption of As on hydroxy-Fe-montmorillonite complexes     

Donald G. Fraser 《中国科学D辑(英文版)》2005,48(12):2155-2165

DOI: 10.1360/03yd0553 Arsenic, a toxic element, is ubiquitous in the earth’s crust and may lead to health risks for humans. This may come about as a result of oxidative weathering and dissolution of As-containing minerals, use of ar-senical pesticides, excess use of some fertilizers and from mine drainage, smelter wastes and agricultural drainage water from certain arid regions. The dis-solved inorganic arsenic is transported in surface or2156 Science in China Ser. D Earth Sciences groun…  相似文献   

Responses of the polar ionosphere to the Bastille Day solar event   总被引：1，自引：0，他引：1  

Liu  Rui-yuan  Hu  Hong-qiao  Liu  Yong-hua  Xu  Zhong-hua  Sato  N.  Fraser  B.J. 《Solar physics》2001,204(1-2):305-313

Simultaneous observations at Zhongshan Station, Antarctica, are presented for the interval of 13–17 July 2000 to show responses of the polar ionosphere to the Bastille Day (14 July 2000) solar event. The polar ionosphere was highly disturbed, as shown by frequently large deviations of the geomagnetic H-component, large riometer absorption events and strong ULF waves. Associated with the huge solar proton event produced by the X5/3B flare, a polar cap absorption (PCA) was observed. It began at ∼ 10:40 UT on 14 July and ended at ∼ 19:40 UT on 17 July. Superposed on it, there was a large absorption event with a peak of 26 dB, starting at ∼ 03:00 UT and ending at ∼ 11:10 UT on 15 July. This kind of absorption was probably produced by an intense `cloud of energetic electrons' during an auroral substorm. The ULF waves were very intense during the main phase and the recovery phase of the severe magnetic storm on 15 and 16 July. The ionospheric absorption was so strong that the digisonde signal was blacked out most of the time. The ionosphere returned to normal in the afternoon on 17 July.  相似文献   

The ‘throwntogetherness’ of research: Reflections on conducting fieldwork in South Africa     

Alistair Fraser 《Singapore journal of tropical geography》2012,33(3):291-295

  相似文献   

Preface     

Xiushu Qie  Clive Saunders   《Atmospheric Research》2009,91(2-4):137

  相似文献