Storms and shoreline retreat in the southern Gulf of St. Lawrence   总被引：1，自引：0，他引：1  

Donald L. Forbes  George S. Parkes  Gavin K. Manson  Lorne A. Ketch 《Marine Geology》2004,210(1-4):169-204

Storms play a major role in shoreline recession on transgressive coasts. In the southern Gulf of St. Lawrence (GSL), southeastern Canada, long-term relative sea-level rise off the North Shore of Prince Edward Island has averaged 0.3 m/century over the past 6000 years (>0.2 m/century over 2000 years). This has driven long-term coastal retreat at mean rates >0.5 m/a but the variance and details of coastal profile response remain poorly understood. Despite extensive sandy shores, sediment supply is limited and sand is transferred landward into multidecadal to century-scale storage in coastal dunes, barrier washover deposits, and flood-tidal delta sinks. Charlottetown tide-gauge records show mean relative sea-level rise of 3.2 mm/a (0.32 m/century) since 1911. A further rise of 0.7±0.4 m is projected over the next 100 years. When differenced from tidal predictions, the water-level data provide a 90-year record of storm-surge occurrence. Combined with wind, wave hindcast, and sea-ice data, this provides a catalogue of potentially significant coastal storms. We also document coastal impacts from three recent storms of great severity in January and October 2000 and November 2001. Digital photogrammetry (1935–1990) and shore-zone surveys (1989–2001) show large spatial and temporal variance in coastal recession rates, weakly correlated with the storm record, in part because of wave suppression or coastal protection by sea ice. Large storms cause rapid erosion from which recovery depends in part on local sand supply, but barrier volume may be conserved by washover deposition. Barrier shores with dunes show high longshore and interdecadal variance, with extensive multidecadal healing of former inlet and overwash gaps. This reflects recovery from an episode of widespread overwash prior to 1935, possibly initiated by intense storms or groups of storms in the latter half of the 19th century. With evidence from the storms of 2000–2001, this points to the importance of storm clustering on scales of weeks to years in determining erosion vulnerability, as well as the need for a long-term, large-scale perspective in assessing coastal stability. The expected acceleration in relative sea-level rise, together with projections of increasing storm intensity and greatly diminished winter ice cover in the southern GSL, implies a significant increase in coastal erosion hazards in future.  相似文献   

Epistemological possibilities and imperatives of complexity research: a reply to Reitsma     

Steven M Manson 《Geoforum》2003,34(1):17-20

Reitsma (A response to ‘simplifying complexity’. Geoforum 34 (1) (2003) 13), in response to the article ‘Simplifying Complexity’ (Manson, S.M., Simplifying complexity: a review of complexity theory. Geoforum 32 (3) (2001) 405), highlights a number of interesting and important aspects of complexity theory that invite further discussion. In particular, there are three areas of complexity research that are open to deeper exploration: (1) the width and breadth of ‘complexity’ defined as a scientific endeavor; (2) the role of theory relative to practice and their relationship with pattern and process in complex systems; and (3) the need for greater discussion and exploration in order to define the conceptual bounds of complexity theory.  相似文献   

Gravity wave exclusion circles in background flows modulated by the semidiurnal tide     

L. Zhong  A. H. Manson  L. J. Sonmor  C. E. Meek 《Annales Geophysicae》1996,14(5):557-565

In this short paper the exclusion circles and vertical phase locities for gravity waves launched from the ground into a time-varying wind are studied using a ray-tracing technique. It is shown that waves with initial observed phase speeds that should place them within the local temporally varying exclusion circle, are often Doppler shifted outside of the circle. This, and the finite lifetime of some critical levels, allow waves to survive the critical layer and reach higher altitudes. Also, for slower phase-speed waves, the temporally varying wind can shift the observed frequency to negative values, so that the observed phase motions will be opposite (i.e. horizontally reversed and vertically upward), even though the energy still propagates upward. This effect can also cause the phase velocity to move inside the local exclusion circle. Due to the directional filtering of wave sources by the stratospheric wind, the percentage of such reverse-propagating waves will change systematically with local time and height in our simplified but realistic model. These results are related to ground-based systems, optical and radar, which sample the wind field and gravity waves in the middle atmosphere.  相似文献   

Submicroscopic texture in titanomagnetite grains in basalt studied using the torque magnetometer and electron microscope     

A.J. Manson  W. O&#x;Reilly 《Physics of the Earth and Planetary Interiors》1976,11(3):173-183

Samples of basalt containing homogeneous titanomagnetite have been subjected to heat treatment in air, in the laboratory, under conditions which produce multiphase oxidation products. The evolution of the microstructure in the titanomagnetite was monitored using the electron microscope and by measuring the rotational-hysteresis characteristics of the samples. This latter technique proves to be very sensitive to small changes which are undetectable by the optical or electron microscopes. Rotational-hysteresis curves and coercivity spectra, derived from acquisition of IRM and AF demagnetization of IRM, all indicate an appreciable fraction of coercivities in excess of 1 kOe in optically homogeneous (Class I) titanomagnetitie with submicroscopic microstructure. It is possible to divide Class I of the petrological scale into three or four subclasses. Class-I basalts may be assigned to the subclasses on the basis of the effect of slight laboratory heating on the rotational-hysteresis characteristic.  相似文献   

The effect of atmospheric gravity waves upon wind determinations in the lower thermosphere (80–100 km)     

A.H. Manson  J.B. Gregory  D.G. Stephenson 《Planetary and Space Science》1974,22(1):181-183

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Spatial simulation: exploring pattern and process     

S.M. Manson 《International journal of geographical information science》2013,27(8):1506-1507

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CONCENTRATIONS OF NONEMPLOYMENT INCOME IN THE UNITED STATES *     

Gary A. Manson  Richard E. Groop 《The Professional geographer》1988,40(4):444-450

Nonemployment income from investments, pensions, welfare benefits, and so forth provides one third of total personal income in the United States. Spatial concentrations of this income occur in places such as Florida, Michigan, Arkansas and the Great Plains. These concentrations result largely from the presence of older persons who are the principal recipients of nonemployment income. In turn, spatial concentrations of older persons result from “aging in place,” which typifies the Great Plains, or from amenity-bound immigration by older persons, which characterizes Florida.  相似文献   

Does scale exist? An epistemological scale continuum for complex human-environment systems   总被引：3，自引：0，他引：3  

Steven M. Manson 《Geoforum》2008,39(2):776-788

Scale pervades interdisciplinary research on human-environment systems that exhibit hallmarks of complexity such as path dependence, nonlinearity, and surprise. Although scale concepts are woven through the data, methodology, and theory of human-environment research, the question remains: does scale exist? More broadly, can a single definition of scale suffice for human-environment systems? The meaning and use of scale is contested across the social, natural, and information sciences. Given that the study of human-environment systems spans many of these disciplines, specific research problems inherit a broad range of conflicting scale concepts. This paper proposes an epistemological scale continuum that arrays scale perspectives from the realist contention that there are natural scales independent of observers through to the constructionist view that scale is subjective and socially mediated. As seen in biocomplexity and human-environment research more broadly, this scale continuum establishes that scale is not a single measure or object of study, nor is any single definition of scale sufficient for human-environment systems. Viewpoints and tensions among scale epistemologies also suggest several general principles for using scale effectively in human-environment research.  相似文献   

Terra Populus’ architecture for integrated big geospatial services          下载免费PDF全文

David Haynes  Steve Manson  Eric Shook 《Transactions in GIS》2017,21(3):546-559

Big geospatial data is an emerging sub‐area of geographic information science, big data, and cyberinfrastructure. Big geospatial data poses two unique challenges. First, raster and vector data structures and analyses have developed on largely separate paths for the last 20 years. This is creating an impediment to geospatial researchers seeking to utilize big data platforms that do not promote heterogeneous data types. Second, big spatial data repositories have yet to be integrated with big data computation platforms in ways that allow researchers to spatio‐temporally analyze big geospatial datasets. IPUMS‐Terra, a National Science Foundation cyberInfrastructure project, addresses these challenges by providing a unified framework of integrated geospatial services which access, analyze, and transform big heterogeneous spatio‐temporal data. As IPUMS‐Terra's data volume grows, we seek to integrate geospatial platforms that will scale geospatial analyses and address current bottlenecks within our system. However, our work shows that there are still unresolved challenges for big geospatial analysis. The most pertinent is that there is a lack of a unified framework for conducting scalable integrated vector and raster data analysis. We conducted a comparative analysis between PostgreSQL with PostGIS and SciDB and concluded that SciDB is the superior platform for scalable raster zonal analyses.  相似文献   

Spatial variability of factors influencing coastal change in the Western Canadian Arctic     

G. K. Manson  S. M. Solomon  D. L. Forbes  D. E. Atkinson  M. Craymer 《Geo-Marine Letters》2005,25(2-3):138-145

Coastal change in the western Canadian Arctic is influenced by coastal morphology, relative sea-level trend and sea-ice and storm climates. The spatial variability of these factors tends to follow general east–west trends suggesting similar trends in coastal erosion hazard, processes and rates of coastal change. The spatial variability in the causes of coastal change is examined in the communities of Tuktoyaktuk, Sachs Harbour, Holman and Kugluktuk.  相似文献