Expectations for Cassini observations of ring material with nearby moons     

Mark C. Lewis  Glen R. Stewart 《Icarus》2005,178(1):124-143

This paper describes N-body simulations of two regions of the saturnian ring system and examines what we might expect the Cassini orbiter to see in those areas. The first region is the edge of the Encke gap in the A ring that is perturbed by the satellite, Pan. Our previous simulations of this region neglected particle self-gravity [Lewis and Stewart, 2000a, Bull. Am. Astron. Soc. 34, 883]. Here we examine the interactions of the wakes caused by Pan with the wakes that form from local gravitational instabilities. We find that the two phenomena do not normally coexist and predict that measurements of particle sizes between the moon wakes should reflect the true particle size distribution of the region and not what is caused by gravitational aggregation. The region between the Encke gap edge and the first wake peak is an exception to this rule because our simulations exhibit the formation of exceptionally large gravity-induced wakes in this region. We also describe simulations of the F ring and explain the nature of braid-like structures that form naturally when the ring is perturbed by a single moon on an eccentric orbit. Finally, we discuss the very dynamic nature of the F ring system and how this should be taken into account when interpreting observations and even when planning future observations of this system.  相似文献   

Fluvial system dynamics derived from distributed sediment budgets: perspectives from an uncertainty‐bounded application          下载免费PDF全文

Peter W. Downs  Scott R. Dusterhoff  Glen T. Leverich  Philip J. Soar  Michael B. Napolitano 《地球表面变化过程与地形》2018,43(6):1335-1354

The utility of sediment budget analysis is explored in revealing spatio‐temporal changes in the sediment dynamics and morphological responses of a fluvial system subject to significant human impacts during the recent Anthropocene. Sediment budgets require a data‐intensive approach to represent spatially‐differentiated impacts adequately and are subject to numerous estimation uncertainties. Here, field and topographic surveys, historical data, numerical modelling and a representative‐area extrapolation method are integrated to construct a distributed, process‐based sediment budget that addresses historical legacy factors for the highly regulated Lagunitas Creek (213 km²), California, USA, for the period 1983–2008. Independent corroboration methods and error propagation analysis produce an uncertainty assessment unique to a catchment of this size. Current sediment yields of ~20 000 t a^‐1 ± 6000 t a^‐1 equate to unit rates of ~300 t km^‐2 a^‐1 ± 90 t km^‐2 a^‐1 over the effective sediment contributing area of 64 km². This is comparable with yields associated with early Euro‐American settlement in the catchment, despite loss of sediment supply upstream of the two large dams. It occurs because ~57% of the sediment is now derived from incision‐related channel erosion. Further, the highly efficient routing of channel‐derived sediments in these incised channels suggests an efflux of 84% of contemporary sediment production, contrasting with the efflux of ≈10–30% reported for unregulated agricultural catchments. The results highlight that sediment budgets for regulated rivers must accommodate channel morphological responses to avoid significantly misrepresenting catchment yields, and that volumetric precision in sediment budgets may best be improved by repeat, spatially dense, channel cross‐section surveys. Human activities have impacted every aspect of the sediment dynamics of Lagunitas Creek (production, storage, transfer, rates of movement through storage), confirming that, while distributed sediment budgets are data demanding and subject to numerous error sources, the approach can provide valuable insights into Anthropocene fluvial geomorphology. Copyright © 2017 John Wiley & Sons, Ltd.  相似文献   

Local and Target Exploration of Conglomerate-Hosted Gold Deposits Using Machine Learning Algorithms: A Case Study of the Witwatersrand Gold Ores,South Africa     

Nwaila  Glen T.  Zhang  Steven E.  Frimmel  Hartwig E.  Manzi  Musa S. D.  Dohm  Christina  Durrheim  Raymond J.  Burnett  Mark  Tolmay  Leon 《Natural Resources Research》2020,29(1):135-159

  相似文献   

What do we know about the labour market for seafarers?: A view from the UK     

David Glen 《Marine Policy》2008

This paper considers the evidence that exists on the global demand and supply of seafarers, and their age profiles. New information on the age profiles of deck and engine officers is presented, drawn from records held by the UK Maritime and Coastguard Agency. Detailed age profiles for certain countries are constructed and compared with that of the UK, as well as with estimates published elsewhere. Using the data derived from the MCA, it is shown that there is a significant positive correlation between the age profiles of seafarer supplying countries and their level of economic development, as measured by GDP per capita. This evidence is consistent with the view that the future supply of seafaring officers will increasingly be oriented towards countries at lower levels of development, as the existing pool of highly qualified officers from traditional maritime countries continues to diminish.  相似文献   

A note on the relocation of marsh debris during a storm surge     

Courtney T. Hackney  T. Dale Bishop 《Estuarine, Coastal and Shelf Science》1981,12(5):621-624

  相似文献   

POPPER'S PRINCIPLE OF FALSIFIABILITY AND THE IRREFUTABILITY OF THE DAVISIAN CYCLE     

Paul Bishop 《The Professional geographer》1980,32(3):310-315

Many “sociological”factors can account for the initial acceptance and continued persistence of W. M. Davis's Geographical Cycle. Such factors include Davis's attractive and forceful presentation of the cycle and the role of the cycle as a unifier of the discipline of physical geography, to name two. An analysis of the scientific character of the cycle, in the light of Karl Popper's criteria for demarcating between science and non-science, suggests that persistence of the cycle can also be attributed to a “logical”factor, the irrefutability of the central concept, stage.  相似文献   

Rapid Holocene hydrologic change along boreal treeline revealed by δ13C and δ18O in organic lake sediments, Northwest Territories, Canada     

Brent B. Wolfe  Thomas W. D. Edwards  Ramon Aravena  Glen M. MacDonald 《Journal of Paleolimnology》1996,15(2):171-181

Analysis of ¹⁸O_cellulose, ¹³C_{organic matter}, and ¹³C_cellulose at about 100 year intervals from organic matter deposited in Toronto Lake, Northwest Territories, Canada, revealed an 8000-year history of rapid, post-glacial hydrologic change at the treeline zone. Several mid-Holocene phases of enriched ¹³C_org and ¹³C_cell, caused by elevated lake productivity, declining [CO_2(aq)], and closed basin conditions, were abruptly terminated by intervals of open hydrology recorded by sharply depleted ¹⁸O_cell. Two of these events, at 5000 and 4500 BP, are correlated with increased total organic content and Picea mariana pollen concentration, which indicate that high levels of productivity were also accompanied by northern treeline advances. A third treeline advance at about 2500 BP is also marked by an apparent outflow event from Toronto Lake, but this was not associated with ¹³C_org/cell enrichment in the sediment record because rapid and substantial lake water renewal probably prevented productivity-driven enrichment of the dissolved inorganic carbon and replenished the CO_2(aq) supply to thriving phytoplankton. However, high sediment organic content during this period suggests increased productivity. Increases in the inflow:evaporation ratio at about 6500 and 3500 BP were also sufficient to cause Toronto Lake to overflow but the prevailing climate during these periods apparently did not favour appreciable northward treeline migration or changes in lake productivity.This is the 14th in a series of papers published in this special AMQUA issue. These papers were presented at the 1994 meeting of the American Quaternary Association held 19–22 June, 1994, at the University of Minnesota, Minneapolis, Minnesota, USA. Dr Linda C. K. Shane served as guest editor for these papers  相似文献   

Scale-dependent analysis of satellite imagery for characterization of glacier surfaces in the Karakoram Himalaya   总被引：1，自引：0，他引：1  

Michael P. Bishop  John F. Shroder  Jr.  Betty L. Hickman  Luke Copland 《Geomorphology》1998,21(3-4)

Information regarding process-structure relationships and change in the Karakoram Himalaya is of great importance in studying glacier hydrollogy, mass balance, and dynamic environmental change. Such information is not readily available. Detailed spatio-temporal assessment requires field investigation coupled with quantitative remote sensing studies. We conducted an investigation of the large Batura Glacier in Pakistan to determine if spectral variability can be quantified and used to characterize glacier surfaces. Specifically, SPOT Panchromatic satellite data were evaluated for differentiating features of glacier structure resulting from ice movement, ablation, and supraglacial fluvial action. Image semivariogram analysis was conducted. for assessing spectral variability patterns and fractal analysis was used to examine scale-dependent variation in the data. Results indicate that spectral variability from fields of ice seracs can exhibit fractal characteristics, although most surface features on the glacier exhibit a change in the fractal dimension over different ranges in scale. The fractal dimension was found to be useful for differentiating between glacier surfaces such as white ice and debris-covered ice. Characteristics of the debris-load and the scale-dependent nature of calculating the fractal dimension ultimately determined the potential of class separability.  相似文献   

The assumption of uniform specific discharge: unsafe at any time?          下载免费PDF全文

R. H. Karlsen  J. Seibert  T. Grabs  H. Laudon  P. Blomkvist  K. Bishop 《水文研究》2016,30(21):3978-3988

Nearby catchments in the same landscape are often assumed to have similar specific discharge (runoff per unit catchment area). Five years of streamflow from 14 nested catchments in a 68 km² landscape was used to test this assumption, with the hypothesis that the spatial variability in specific discharge is smaller than the uncertainties in the measurement. The median spatial variability of specific discharge, defined as subcatchment deviation from the catchment outlet, was 33% at the daily scale. This declined to 24% at a monthly scale and 19% at an annual scale. These specific discharge differences are on the same order of magnitude as predicted for major land‐use conversions or a century of climate change. Spatial variability remained when considering uncertainties in specific discharge, and systematic seasonal patterns in specific discharge variation further provide confidence that these differences are more than just errors in the analysis of catchment area, rainfall variability or gauging. Assuming similar specific discharge in nearby catchments can thus lead to spurious conclusions about the effects of disturbance on hydrological and biogeochemical processes. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

Aqua temporaria incognita     

H. J. Ilja van Meerveld  Eric Sauquet  Francesc Gallart  Catherine Sefton  Jan Seibert  Kevin Bishop 《水文研究》2020,34(26):5704-5711

  相似文献