On the interference between closely-spacedP arrivals recorded at seismic arrays     

J. A. Lyons  C. Wright 《Pure and Applied Geophysics》1977,115(3):693-705

The arrival at the Yellowknife Array (YKA) of closely-spaced P-waves having slightly different values ofdT/d, azimuth, and amplitude has been simulated using synthetic 1 Hz wavelets. Adaptive-processing determinations of apparent slowness and azimuth show a remarkable pattern of fluctuations with time for varying separations of the interfering pulses. In the critical separation range 0.30 to 0.55 s, these fluctuations greatly exceed the differences in arrival vectors of the primary wavelets themselves. Observation of characteristic interference patterns on real array seismograms might permit the identification of triplications associated with radial velocity anomalies in the lower mantle. Processed YKA seismograms for three events at distances close to 90° are presented, which, despite apparently simple P onsets illustrate the pattern of drift indT/d expected for such a triplication.Contribution from the Earth Physics Branch No. 648.  相似文献   

Multiple CME Events Observed With LASCO     

Lyons  M.A.  Simnett  G.M. 《Solar physics》1999,186(1-2):363-379

Observations are reported of two multiple CME events which were detected on 2–3 June 1997 and 9–10 June 1998, using the LASCO instrument on board SOHO. Each event consists of a group of four related CMEs which emerge from progressively higher latitudes over a time period of approximately 16 hours. In both cases there is on-disk activity visible in EIT EUV images which involves bright emission along the south polar crown filament and there is also ejection of mass from other regions of the corona during the time period of each event. We present a multi-wavelength view of these events (i.e. white-light, H, EUV and, in the case of the 2–3 June 1997 event, soft X-ray), which suggest that ejection of mass from one point in the corona can lead to a destabilization of a previously stable structure and the further ejection of mass from different regions of the corona, in a systematic way. The observations also show that the CME phenomenon is not always a localised event but can occur on a global level; and that complex CME activity can arise at relatively quiet-Sun periods as evidenced by the lack of significant X-ray flares or radio signatures.  相似文献   

A preliminary study of the Hg flux from selected Ohio watersheds to Lake Erie     

T.O. Fitzgibbon  W. Berry Lyons  Christopher B. Gardner  Anne E. Carey   《Applied Geochemistry》2008,23(12):3434-3441

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Clearing enhances dust devil formation     

T.J. Lyons  U.S. Nair  I.J. Foster   《Journal of Arid Environments》2008,72(10):1918-1928

In the southwest of Western Australia, the large scale replacement of native perennial vegetation with agriculture based on winter growing annual species leads to a significant change in the surface albedo and roughness. Whilst the redistribution of the surface energy balance impacts on cloud climatology, the reduced roughness of the agricultural area has enhanced the injection of aerosols into the atmosphere through the increased potential for dust devils. Although the native vegetation experiences a higher sensible heat flux, it is the reduced frictional drag of the cleared agricultural lands that enhances the potential for dust devil formation and thus provides an additional source of atmospheric aerosols.  相似文献   

The Geochemistry of Supraglacial Streams of Canada Glacier,Taylor Valley (Antarctica), and their Evolution into Proglacial Waters     

Sarah?K.?FortnerEmail author  Martyn?Tranter  Andrew?Fountain  W.?Berry?Lyons  Kathleen?A.?Welch 《Aquatic Geochemistry》2005,11(4):391-412

We have investigated the geochemistry of supraglacial streams on the Canada Glacier, Taylor Valley, Antarctica during the 2001–2002 austral summer. Canada Glacier supraglacial streams represent the link between primary precipitation (i.e. glacier snow) and proglacial Lake Hoare. Canada Glacier supraglacial stream geochemistry is intermediate between glacier snow and proglacial stream geochemistry with average concentrations of 49.1 μeq L⁻¹ Ca2+, 19.9 μeq L⁻¹ SO₄²⁻, and 34.3 μeq L⁻¹ HCO₃⁻. Predominant west to east winds lead to a redistribution of readily soluble salts onto the glacier surface, which is reflected in the geochemistry of the supraglacial streams. Western Canada Glacier supraglacial streams have average SO₄²⁻:HCO₃⁻ equivalent ratios of 1.0, while eastern supraglacial streams average 0.5, suggesting more sulfate salts reach and dissolve in the western supraglacial streams. A graph of HCO₃⁻ versus Ca2+ for western and eastern supraglacial streams had slopes of 0.87 and 0.72, respectively with R2 values of 0.84 and 0.83. Low concentrations of reactive silicate (> 10 μmol L⁻¹) in the supraglacial streams suggested that little to no silicate weathering occurred on the glacier surface with the exception of cryoconite holes (1000 μmol L⁻¹). Therefore, the major geochemical weathering process occurring in the supraglacial streams is believed to be calcite dissolution. Proglacial stream, Anderson Creek, contains higher concentrations of major ions than supraglacial streams containing 5 times the Ca²⁺ and 10 times the SO₄²⁻. Canada Glacier proglacial streams also contain higher concentrations (16.6–30.6 μeq L⁻¹) of reactive silicate than supraglacial streams. This suggests that the controls on glacier meltwater geochemistry switch from calcite and gypsum dissolution to both salt dissolution and silicate mineral weathering as the glacier meltwater evolves. Our chemical mass balance calculations indicate that of the total discharge into Lake Hoare, the final recipient of Canada Glacier meltwater, 81.9% is from direct glacier runoff and 19.1% is from proglacial Andersen Creek. Although during a typical, low melt ablation season Andersen Creek contributes over 40% of the water added to Lake Hoare, its overall chemical importance is diluted by the direct inputs from Canada Glacier during high flow years. Decadal warming events, such as the 2001–2002 austral summer produce supraglacial streams that are a major source of water to Lake Hoare.  相似文献   

The potential impact of shell fragment distributions on high-frequency seafloor backscatter     

Lyons  A.P. 《Oceanic Engineering, IEEE Journal of》2005,30(4):843-851

There has been much recent activity on developing and testing high-frequency seafloor volume scattering models and on the related high-resolution characterization of seafloor volumes. This paper will address another plausible volume scattering mechanism that has not yet received much attention-distributions of broken shell fragments in sediment (commonly referred to as shell hash). The shell fragments are modeled as nonaggregating spherical scatterers, and the spatial distribution of the shell pieces is determined using the Percus-Yevick packing factor. Computer simulations of the multiple scattering and a single scattering model are used to study the power backscattered by shell hash sediments as a function of the volume of scatterers and the frequency of the incident wave (10-100 kHz). Parameter values for simulations are obtained by stereological analysis of x-ray computed tomography scans of sediment cores.  相似文献