Some high level gravels of North-East Hampshire     

Henry Bury 《Proceedings of the Geologists' Association. Geologists' Association》1922,33(2):81-IN1

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On some further researches in Bone-Caves in North Wales     

Henry Hicks 《Proceedings of the Geologists' Association. Geologists' Association》1887,10(1):14-18

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Notes on the geology and structure of the country around Tunbridge Wells: With report of excursion to Southborough,Tunbridge Wells,High Rocks and Eridge. Saturday,May 20th, 1922     

Henry B. Milner 《Proceedings of the Geologists' Association. Geologists' Association》1923,34(1):47-IN5

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Report of an excursion to Claygate and Oxshott,Surrey: Saturday,June 15th, 1912     

Henry Dewey 《Proceedings of the Geologists' Association. Geologists' Association》1912,23(4):237-IN10

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The last Welsh Ice Cap: Part 1 – Modelling its evolution,sensitivity and associated climate     

Henry Patton  Alun Hubbard  Neil F. Glasser  Tom Bradwell  Nicholas R. Golledge 《Boreas: An International Journal of Quaternary Research》2013,42(3):471-490

A high‐resolution, three‐dimensional, thermomechanical ice‐flow model is used to investigate the glaciodynamics of the Last Glacial Maximum Welsh Ice Cap – a large, independent ice centre of the British–Irish Ice Sheet. The model uses higher‐order physics to solve longitudinal stresses, and is coupled to climate via a distributed, positive degree‐day mass‐balance scheme. A suite of model experiments driven by the GISP2 δ¹⁸O curve was initiated from a climatic optimum at 38.3 ka BP through to the Devensian/Holocene boundary to identify an icecap configuration compatible with available empirical evidence. An enhanced cooling from present of 11.85°C and strong precipitation suppression are required between 27.4 and 23.5 ka BP for the modelled icecap to attain well‐established empirical limits, a scenario probably associated with Heinrich Event‐2 and the potential collapse of thermohaline circulation in the North Atlantic. The experiments indicate ice‐dispersal centres located in North and Mid Wales, the latter being essential for forcing ice southwards of the Brecon Beacons during the Last Glacial Maximum. Deglaciation of the Welsh Ice Cap was relatively rapid, occurring within one millennium. Dynamic stability is governed largely by the dominance and vigour with which fast‐flowing outlet glaciers drain the icecap interior, which in turn are linked to variations in the climatic forcing. The distribution of permanently cold‐based ice across the uplands and summits indicates the probable preservation of relict landscapes in these areas throughout the full glacial cycle.  相似文献   

Changes in volcanic hazard exposure in the Northwest USA from 1940 to 2100     

Stephen M. Strader  Walker Ashley  James Walker 《Natural Hazards》2015,77(2):1365-1392

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An Assessment of Potential Oil Spill Damage to Salt Marsh Habitats and Fishery Resources in Galveston Bay, Texas   总被引：1，自引：0，他引：1  

Lawrence P. Rozas  Thomas J. Minello  Charles B. Henry 《Marine pollution bulletin》2000,40(12):1148-1160

We sampled nekton, benthic infauna, and sediments in salt marshes of upper Galveston Bay, Texas to examine relationships between habitat use and sediment hydrocarbon concentration. Most marsh sediment samples were contaminated with relatively low concentrations of weathered petroleum hydrocarbons. We found few statistically significant negative relationships between animal density and hydrocarbon concentration (6 of 63 taxa examined using simple linear regression). Hydrocarbon concentration did not contribute significantly to Stepwise Multiple Regression models we used to explore potential relationships between animal densities and environmental parameters; in most cases where hydrocarbon concentration was an important variable in the models, the relationship was positive (i.e., animal densities increased with hydrocarbon concentration). Low hydrocarbon concentrations in sediments of upper Galveston Bay marshes could have contributed to our results either because levels were too low to be toxic or levels were toxic but too low to be detected by most organisms.  相似文献   

Offshore Transport of Pesticides in the South Atlantic Bight: Preliminary Estimate of Export Budgets     

Henry A. Alegria  J. Pierre d''Autel  Timothy J. Shaw   《Marine pollution bulletin》2000,40(12):1178-1185

Surface waters of the inner shelf (coast to 20-m isobath) of the South Atlantic Bight (SAB) were sampled in July 1994 and August 1995 for pesticides currently used in the south-eastern United States to estimate offshore transport. Only atrazine was detected at all stations in 1994 and 1995 and simazine was detected at all stations in 1995. Atrazine levels were 5.60–12 ng/l in July 1994 and 3.1–11 ng/l in August 1995 and simazine levels were 0.8–4.6 ng/l in August 1995. We calculated reservoir masses (in inner shelf waters) of 550 kg atrazine in July 1994, and 325 kg atrazine and 180 kg simazine in August 1995. Using these reservoir masses and a previously estimated residence time for waters of the inner shelf of 30 days, annual export budgets were calculated. For 1994, a budget of 6600 kg atrazine was calculated. For 1995, budgets of 3900 kg atrazine and 2150 kg simazine were calculated.

Yearly riverine discharge to estuaries in the study region was estimated to range from 600 to 5600 kg atrazine and 100 to 550 kg simazine. The large budgets for the coastal inner shelf compared with yearly riverine discharge suggest that a significant fraction of atrazine and simazine applied in the region is being transported offshore from coastal waters. This transport pathway needs to be factored in when calculating mass balances and determining the ultimate fate of these pesticides.  相似文献   

A brief history of infrared astronomy     

Helen J Walker  FRAS 《Astronomy& Geophysics》2000,41(5):5.10-5.13

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Address at the opening of the session 1874–75: November 6th, 1874     

Henry Woodward 《Proceedings of the Geologists' Association. Geologists' Association》1875,4(1):1-34

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