Assessing the potential of integrated Landsat 8 thermal bands,with the traditional reflective bands and derived vegetation indices in classifying urban landscapes     

Terence Darlington Mushore  Onisimo Mutanga  John Odindi  Timothy Dube 《国际地球制图》2017,32(8):886-899

Reliable and up-to-date urban land cover information is valuable in urban planning and policy development. Due to the increasing demand for reliable land cover information there has been a growing need for robust methods and datasets to improve the classification accuracy from remotely sensed imagery. This study sought to assess the potential of the newly launched Landsat 8 sensor’s thermal bands and derived vegetation indices in improving land cover classification in a complex urban landscape using the support vector machine classifier. This study compared the individual and combined performance of Landsat 8’s reflective, thermal bands and vegetation indices in classifying urban land use-land cover. The integration of Landsat 8 reflective bands, derived vegetation indices and thermal bands overall produced significantly higher accuracy classification results than using traditional bands as standalone (i.e. overall, user and producer accuracies). An overall accuracy above 89.33% and a kappa index of 0.86, significantly higher than the one obtained with the use of the traditional reflective bands as a standalone data-set and other analysis stages. On average, the results also indicate high producer and user accuracies (i.e. above 80%) for most of the classes with a McNemar’s Z score of 9.00 at 95% confidence interval showing significant improvement compared with classification using reflective bands as standalone. Overall, the results of this study indicate that the integration of the Landsat 8’s OLI and TIR data presents an invaluable potential for accurate and robust land cover classification in a complex urban landscape, especially in areas where the availability of high resolution datasets remains a challenge.  相似文献   

Relevance of carbon stocks of marine sediments for national greenhouse gas inventories of maritime nations     

Silvania Avelar  Tessa S. van der Voort  Timothy I. Eglinton 《Carbon balance and management》2017,12(1):10

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The geology of Brighton. Part II     

James Howell 《Proceedings of the Geologists' Association. Geologists' Association》1877,5(2):80-90

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Inference of biological and physical parameters in an internal wave using multiple-frequency, acoustic-scattering data   总被引：1，自引：0，他引：1  

Warren  Joseph D.; Stanton  Timothy K.; Wiebe  Peter H.; Seim  Harvey E. 《ICES Journal of Marine Science》2003,60(5):1033-1046

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Quantitative evaluation of a passively leveled ocean bottom seismometer     

Timothy W. Barash  Charles G. Doll Jr.  John A. Collins  George H. Sutton  Sean C. Solomon 《Marine Geophysical Researches》1994,16(5):347-363

A problem in the use of ocean bottom seismometers is the difficulty in leveling the sensors while ensuring good coupling to the seafloor. We have investigated the coupling characteristics of the seismic sensors in the new ONR ocean bottom seismometer. In the deployable sensor package for that instrument, a three-component seismometer set is suspended on a 2-axis passive leveling gimbal and is immersed in a viscous fluid. We report tests, conducted in a seismic vault, comparing the output of a gimbaled seismometer set to that of a set rigidly coupled to the ground. Our results show that the degree to which the gimbaled set is coupled to ground motion is a function of the viscosity of the coupling fluid. The coherence between the two sensor sets is poor (<0.4) at some frequencies within the band of interest (0.15 to 20 Hz) and on some components when the viscosity of the coupling fluid is comparatively low (14 Pa-s or 0.16 kSt kinematic viscosity). In addition, the outputs of some components over portions of this frequency band are attenuated and are phase-shifted relative to the outputs of the set rigidly coupled to the ground. Coherence and phase response similarity improve as the viscosity of the coupling fluid is increased. With a coupling fluid viscosity of 980 Pa-s (10 kSt), coherence and phase agreement between the two sensor sets is good (>0.9) across nearly the entire band of interest on all three components. A simple analytical model of the gimbaled seismometer set as a damped, driven, compound-pendulum provides a basis for understanding the test results.  相似文献   

Temporal and spatial variability of biogenic particles fluxes during the JGOFS northeast Atlantic process studies at 47°N, 20°W     

Philip P. Newton  Richard S. Lampitt  Timothy D. Jickells  Penny King  Clare Boutle   《Deep Sea Research Part I: Oceanographic Research Papers》1994,41(11-12)

Particle fluxes to 3100 m depth at 45°50′N, 19°30′W were measured using time-series sediment traps during a 17 month period encompassing 1989 and 1990 JGOFS spring bloom process studies in the northeast Atlantic. There was a marked intra-annual variability in fluxes of mass, particulate inorganic carbon (PIC), particulate organic carbon (POC) and opal, appearing as two major flux events in each year. In 1989, the first flux event represented the settlement of spring bloom-type material, whereas the second, in autumn, was heavily enriched in mucopolysaccharides. In 1990, in contrast, the two flux events comprised spring bloom-type material and arrived at depth at different times relative to the 1989 events. The intra- and interannual variability evident for all three biogenic components was most notable for POC: (i) the autumn 1989 event supplied twice as much POC to 3100 m as the earlier spring bloom settlement—a quite unexpected observation—and (ii) the annual average POC flux in 1989 was 3–4 times more than in 1990. A synthesis of process study datasets with sediment trap data enables an evaluation of the coupling of deep fluxes with surface-water events. Spatial variability of the 1989 deep flux events is assessed by comparing the sediment trap data reported here with those from a second site 100 km away (Honjo and Manganini,Deep-Sea Research II,40, 587–607, 1993). The timing and magnitude of the 1989 spring bloom settlement was indistinguishable in the two datasets, indicating no spatial variability in flux between these sites. In contrast, the autumn 1989 flux event was barely recorded at the second site. Given the biogeochemical importance of this latter event to deep waters, most notable in terms of its contribution to POC flux, this observation of deep-water mesoscale flux variability indicates a significant problem in determining regional carbon budgets. Construction of basin-scale budgets is a central goal of JGOFS and for this to be achieved further studies of mesoscale variability of particle flux are essential.  相似文献   

Organic pollution of an inland marine cave from Bermuda     

Thomas M Iliffe  Timothy D Jickells  Martin S Brewer 《Marine environmental research》1984,12(3):173-189

Inland marine caves have served as biological refugia and, as such, frequently contain unique assemblages of taxonomically significant relict populations known only from a single cave or cave system. However, the absence of photosynthesis in this totally lightless environment and the presence of a highly stratified water column and long residence times for cave waters, characteristically result in depleted dissolved oxygen levels. Under such circumstances, organic pollution, even at low levels, can produce anoxic conditions and may consequently result in the extinction of entire species of cavernicolous fauna. We here present data on the normal environment of marine caves in Bermuda and cite as an example a cave which has become grossly polluted as a result of indiscriminate dumping.  相似文献   

Ferrelo Fan,California: Depositional system influenced by Eustatic sea level changes     

D. G. Howell  J. G. Vedder 《Geo-Marine Letters》1983,3(2-4):187-192

Remnants of an Eocene fan system are preserved onshore at San Diego and in the central part of the southern California borderland. Even though faults and erosion have truncated its margins, geophysical data and exploratory wells indicate that remaining parts of the fan extend beneath an offshore area nearly 400-km long and 40- to 100-km wide. Environments representing fluvial, fan-delta, shelf-channel, overlapping inner- to outer-fan, and basin-plain facies are recognized or inferred. Three progradational cycles onshore and two distinct pulses of sand accumulation offshore are attributable to eustatic low sea-level stands rather than to tectonic uplift or shifts in depositional patterns.  相似文献   

Acute toxicity of heavy metals to two species of marine nematodes     

R. Howell 《Marine environmental research》1984,11(3):153-161

The acute toxicity of seawater solutions of copper, zinc, lead, cadmium and mercury to two species of free-living marine nematodes was studied. Enoplus brevis (Bastian) is a euryhaline species inhabitating intertidal estuarinemud. The closely related Enoplus communis (Bastian) is stenohaline and may be found as a commensal in the byssus threads of seed mussels. Specimens of both species were collected from two sites on the Northeast coast of England showing different levels of pollution by heavy metals. Both species were more susceptible to copper, lead and mercury than to zinc and cadmium, but the order of toxicity of the metals changed with exposure concentration. The euryhaline species survived better than the strictly marine species and there is a suggestion that animals from a polluted site were more tolerant of elevated of heavy metals.  相似文献   

Sedimentary,tectonic, and sea-level controls on submarine fan and slope-apron turbidite systems   总被引：1，自引：0，他引：1  

Dorrik A. V. Stow  David G. Howell  C. Hans Nelson 《Geo-Marine Letters》1983,3(2-4):57-64

To help understand factors that influence submarine fan deposition, we outline some of the principal sedimentary, tectonic, and sea-level controls involved in deep-water sedimentation, give some data on the rates at which they operate, and evaluate their probable effects. Three depositional end-member systems, two submarine fan types (elongate and radial), and a third nonfan, slope-apron system result primarily from variations in sediment type and supply. Tectonic setting and local and global sea-level changes further modify the nature of fan growth, the distribution of facies, and the resulting vertical stratigraphic sequences.  相似文献