The partial identity of the amplitude characteristics of broad-band electromagnetic seismographs     

Vladimír Tobyáš 《Studia Geophysica et Geodaetica》1967,11(2):183-193

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Emerging Memorial Landscapes of Labor Conflict in the Cotton Textile South     

Toby Moore 《The Professional geographer》2000,52(4):684-696

While research into the formation of memorial landscapes in the American South has focused on those resulting from racial conflicts, a new landscape memorializing labor conflict and class consciousness is also emerging in the region's textile‐producing Piedmont. This memorialization poses significant challenges to dominant regional discourses of economic development and class mutuality in a region in which labor organizing and radical politics remain anathema. This paper examines this emerging landscape for what it can tell us about class relations in the region and the process by which memorial landscapes are formed.  相似文献   

Timing of glacial retreat in the Wicklow Mountains,Ireland, conditioned by glacier size and topography          下载免费PDF全文

Matt D. Tomkins  Jason M. Dortch  Philip D. Hughes  Jonny J. Huck  Toby N. Tonkin  Iestyn D. Barr 《第四纪科学杂志》2018,33(6):611-623

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Sedimentation patterns caused by scallop dredging in a physically dynamic environment     

Dale AC  Boulcott P  Sherwin TJ 《Marine pollution bulletin》2011,62(11):2433-2441

Scallop dredging grounds in the Firth of Lorn, western Scotland, are juxtaposed with rocky reef habitats raising concerns that reef communities may be impacted by sediment disturbed by nearby scallop dredging. A particle-tracking model of sediment transport and settling is applied at two scales. In the near-field, a suspension of typical sand/gravel-dominated bed sediment is subjected to a steady current across the dredge track. In the far-field, silt particles, which may persist in suspension for multiple tidal cycles, are tracked in the context of a regional model of tidally-driven flow. The principal sedimentary risk to reef habitats is predicted to come from settling sand particles when dredge tracks approach within tens of metres of a reef. The cumulative effect of dredging at the relatively low intensities recorded in this region is not expected to have a significant long-term impact on suspended silt concentrations and settlement in this highly dispersive environment.  相似文献   

Numerical investigation of deep water circulation in the Faroese Channels     

Nataliya Stashchuk  Vasiliy VlasenkoToby J. Sherwin 《Deep Sea Research Part I: Oceanographic Research Papers》2011,58(7):787-799

The overflow of dense water from the Nordic Seas through the Faroese Channels is investigated numerically using the Massachusetts Institute of Technology General Circulation Model. The model is forced by the removal of a barrier that separates different water masses in the bottom layer of the Faroe-Shetland Channel at the north-eastern boundary. An analysis of the output reveals that during its adjustment in the rotating channel the propagating flow is unstable and forms cyclonic and anti-cyclonic eddies in the Faroese Channels. The life-time of the cyclonic eddy is about 10 days, but an anti-cyclonic eddy that is formed upstream of the sill crest of the Faroe Bank Channel has a longer life-time. However, after 50 days it eventually loses its structure below 400 m due to the decay of a counter-rotating current. In the upper 400 m layer this anti-cyclonic eddy remains persistent for longer. Observational evidence of the eddy is confirmed by the tracks of experimental drifters released in the area and by the temperature and salinity fields observed in the Faroese Channels.The pinching of isotherms along the Wyville Thomson Ridge results in the concentration of cold water on the southern side of the Faroese Channels that overflows into the Rockall Trough. The model results demonstrate that the main part of the cold water outflows through the Faroe Bank Channel, rather than across the Wyville Thompson Ridge, due to Earth rotation. The apparent similarity of modelled temperature, salinity and velocity sections to recent measurements in this area adds confidence to these results.  相似文献   

Wyville Thomson Ridge Overflow Water: Spatial and temporal distribution in the Rockall Trough     

Clare Johnson  Toby Sherwin  Denise Smythe-Wright  Tracy Shimmield  William Turrell 《Deep Sea Research Part I: Oceanographic Research Papers》2010,57(10):1153-1162

Wyville Thomson Ridge Overflow Water (WTOW), which is the only part of the outflow from the Norwegian Sea not to directly enter the Iceland Basin, is shown to be a significant water mass in the northern Rockall Trough. It is found primarily at intermediate depths (600–1200 m) beneath the northward flowing warm Atlantic waters, and above recirculating Mediterranean influenced waters and Labrador Sea Water (LSW). The bottom of the WTOW layer can be identified by a mid-depth inflexion point in potential temperature–salinity plots. An analysis of historical data reveals that WTOW has been present in all but eight of the last 31 years at 57.5°N in the Rockall Trough. A denser component of WTOW below 1500 m has also been present, although it appears to be less persistent (12 out of the 31 years) and limited to the west of the section. The signature of intermediate WTOW was absent in two periods, the mid-1980s and early 1990s, both of which coincided with a freshening, and probable increase in volume, of LSW in the trough. Potential temperature–salinity diagrams from historical observations indicate that WTOW persists at least as far south as 55°N (and as far west as 20°W in the Iceland Basin) although its signature is quickly lost on leaving the Rockall Trough. We suggest that a transport of WTOW down the western side of the trough exists, with WTOW at intermediate depths entering the eastern trough either via a cyclonic recirculation, or as a result of eddy activity. Further, WTOW is seen on the Rockall–Hatton Plateau and in the deep channels connecting with the Iceland Basin, suggesting additional possible WTOW transport pathways. These suggested transport routes remain to be confirmed by further observational or modelling studies.  相似文献   

Underground measurements of the seismic noise level     

Vít Kárník  Vladimír Tobyáš 《Studia Geophysica et Geodaetica》1961,5(3):231-236

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Magnification control of electromagnetic seismographs with standard a I–IV characteristics     

Vladimír Tobyáš  Reviewer J. Buben 《Studia Geophysica et Geodaetica》1975,19(3):245-260

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Solving the housing problem: William Mandel's “Soviet but not Russian”, a book review essay     

Toby Terrar 《GeoJournal》1988,17(1):151-151

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Erratum to “Calculations of neutralino–stau coannihilation channels and the cosmologically relevant region of MSSM parameter space” [Astroparticle Physics 13 (2000) 181–213]     

John Ellis  Toby Falk  Keith A. Olive  Mark Srednicki 《Astroparticle Physics》2001,15(4):413-414

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