Spatial prediction of coastal bathymetry based on multispectral satellite imagery and multibeam data. Remote Sensing, 7 10— Murray, J. NPWS, Satellite remote sensing as a reconnaissance tool for assessing nautical chart adequacy and completeness. Marine Geodesy, 37 3— Pinto, M. Price Waterhouse Coopers, Options Appraisal Report: Final Report. Reidy, M. The spaces in between: Science, ocean, empire. Isis, 2— Sandwell, D. Science,65— Bathymetric estimation. Satellite altimetry and earth sciences.
Fu, L. Smith, W. Global sea floor topography from satellite altimetry and ship depth soundings. The CSA Group, Seabed geomorphology of the Porcupine Bank, West of Ireland. Journal of Maps, 1— Townsend, N. Feasibility study of a new energy scavenging system for an autonomous underwater vehicle. Autonomous Robots, 1— UNEP, Vilming, S. The development of the multibeam echosounder: A historical account. First identified by Berthois and Brenotthe east—west orientated dendritic canyon sys- tem incises significantly into the seafloor for a distance of over km.
It lies in water depths of between m to m, and is surrounded on four sides by continental shelf, with a restricted opening out onto the Porcupine Abyssal Plain in the southwest Akmetzhanov et al. Downslope sedi- mentary processes within the canyon system were most active during gla- cial low-stand periods via turbidites and other mass wasting events, while interglacial periods have exhibited little or no sediment transfer activity Van Rooij, Direct observations show contemporary sedimentary activity within the system to be minimal, with tidal currents and northward.
Gollum Channel System. Channel nomenclature within the Porcupine Seabight Murphy, The GCS is composed of a series of anastomosing and individually named canyons, the dimensions of which vary significantly throughout Figure 3.
Previous knowledge of the system was based solely on low frequency regional side-scan sonar see Kenyon et al. These predominantly concen- trated on the canyon heads of the northern-most channels e. Beyer et al. Kenyon et al. To date, a number of projects have used the INSS data for various purposes includ- ing geomorphological Dunlop et al.
Previous studies into the GCS have only provided keyhole perspectives into what is potentially a vast system lying deep beneath the ocean sur- face. The concepts of geomorphometry are applied, in order to access the wealth of information contained within the data. Geomorphometry — the science of quantitative land surface analysis Pike et al. Many of the methods used in these investigations, however, have also proven applicable in submarine environ- ments Peakall et al. Pike et al. General geomorphometry treats a continu- ous land surface as one entity, and in this instance it was used to define the true drainage network of the GCS.
This case study focuses on the application of GIS to marine geomorphometric studies. Analysis is undertaken on ArcMap More detailed back- ground information, results and discussions are available in Murphy and Murphy et al. To provide complete analysis of the system, a multibeam dataset collected in by Fugro, in a project managed by the Petroleum Affairs Division PADwas also used.
This data was collected at a much lower spatial resolution than that of the INSS, gridded at approximately m. This resolution is not ideal for morphological analysis, but nevertheless pro- vides valuable information on the deepest sections of the system which is otherwise unavailable. This allowed higher resolution INSS pixels to retain their true values when overlapping areas were being combined in the programme, while the lower resolution PAD data filled gaps to provide full coverage of the study area.
Once combined, a visual inspection of the data identified some issues. In several locations there is no bathymetric information — indicated by white streaks — which also act as spurious drainage sinks in flow accumulation processing.
In addition to this, a significant amount of noise is present over the entire study area, especially obvious when the hillshade or slope effects are used Figure 3.
In these, the systematic and parallel tracklines of the survey vessel are quite obvious, with significant miscalculations of water depth occurring at the limits of multibeam swathe coverages. Scale and orientation are equal for both a and b. Sacchetti,pers. The use of spatial filters reduced noise to some extent; however, not to the point that slope datasets could be used for any meaningful drain- age analysis without additional processing of either the raw data or the out- come of the drainage analyses.
Two methods are available to deal with this noise B. Dorschel,pers. The first involves the com- plete reprocessing of the raw data files for the survey area, but was however beyond the scope of this project. The second option is manual cleaning of flow accumulation datasets, outlined in the section below.
GIS packages, such as ArcGIS, provide a diverse suite of spatial analysis tools which can be harnessed to provide much more information than can be derived manually. General geomorphometry is used here for the automatic extraction of the drainage networks within the study area, similar to those done previously within ter- restrial investigations e. Jenson, ; Saraf et al. The same methods as used in these land-based studies were employed for this project in order to identify any subtle drainage expressions on the seabed which may not be possible with visual analysis.
The methodology used for the extraction of channel networks is similar to that done by Tubau et al. The hydrology toolset in ArcMap Various threshold values can be set depending on the den- sity of the drainage network believed to be present Figure 3. The validity of the lower threshold values, for example Figure 3. The density of the network revealed shows many features not noted in previous surveys, with the dan- ger that this low threshold may be generating drainage networks significantly influenced by data noise to the extent that they may not exist in reality.
The tendency for the drainage network to show a general trend parallel to the sur- vey tracks is especially suspicious. In contrast, the 50, pixel threshold value Figure 3. The 10, pixel threshold value Figure 3. Figure 3. Good cor- relations can be identified between both, with any differences being due to holes in the dataset on the continental rise. In addition to this, the flow accu- mulation dataset picks out all the channels identified by Van Rooij as well as additional channels which were identified in the preliminary manual drainage analysis of this project.
Due to inherent noise on the multibeam datasets, problems also arose with the subsequent flow accumulation raster files. It was found that at several locations, the noise created by the tracklines acted as preferential pathways for the flow network, commonly flowing either in parallel or normal to the tracklines and augmenting the flow pattern seen in the Porcupine Seabight Figure 3.
To remove this error in the results, manual cleaning of the data was done. This action isolated the pixels meeting the terms of the statement, subsequently creating a new vector layer composed of a series of polylines which could then be edited as normal Figure 3. The complete or partial removal of flow lines occurred where a significant proportion of the channel followed a trackline.
Altering the course of a flow line was only done in locations where the source, pourpoint and evidence of channel presence could be identified; otherwise, the existence of the channel could not be verified and was there- fore removed from the analysis. The result of this can be seen in Figure 3. Caution should be taken when analysing the results of the flow accumula- tion datasets presented in Figure 3. Magesh et al. Extracted channels tend to flow parallel and at right angles through the noise augmenting the Geoinformatics for Marine and Coastal Management.
Black lines represent unaltered automatic flow accumulation data, while the red represent the edited polylines. Gollum Watershed. Southern Watershed 0 25 50 Kilometres. Completed flow accumulation for the Porcupine Seabight. In addition, the resolution of the INSS data is 25 m and the PAD data is m; therefore, features smaller than these are not detected but may potentially contribute to the drainage network. The overall aim is to provide a mathematical description of the main channels, primarily using longitudinal and trans- verse profiles.
This detailed analysis of the topographic features gives greater insight into the processes and controls that affect their morphology and also allows the GCS to be compared with other systems worldwide. The methodologies used are also adapted from terrestrial investigations e. Strahler, ; Chopra et al. Flood and Damuth, ; Klaucke et al. A study of the literature reveals the most commonly measured variables in submarine channel analysis and those most applicable to the GCS were selected.
A total of 12 variables are selected and presented in Table 3. The variables in Table 3. This tool produces a 2D graph, where the Y axis plots the magnitude of pixels across the transect with magnitude equated with water depth in metres. Whereas the general geomorphometic analysis is based on the WGS coordinate system, better for the repre- sentation of large areas where data covers several degrees of latitude, this is less applicable on a small scale.
For small scale analysis, the Irish Transverse Mercator system was used where the x axis can be represented in metres. Data analysis of the graphs produced by ArcMap is limited to visual interpre- tation. For more rigorous analysis, the data were extracted from each graph and transferred to Microsoft Excel, which allows for more precise calculations to be carried out.
In addition to the 3D analyst within ArcMap, ArcGlobe was also used to aid the visualization of the channel morphology and any evidence of potential processes or controls in the surrounding environment e. The use of the 3D projections, as well as the 2D profiles, was extremely effective in generating a greater understanding of the study area.
Transverse profiles were taken across the main channels in the Porcupine Seabight e. Each profile was taken perpendicularly to the local channel path, at the start and end of a channel as well as any location along its course where a significant change in morphology or dimension occurred.
This was done in order to effectively characterize the evolution of channel morphology downstream. TABLE 3. Width: depth ratio The width: depth ratio, although not accounted for in many studies, is seen to be an important factor which affects secondary circulation and overbank flow within submarine channels Keevil et al.
This characteristic is important as it generally shows a significant positive correlation with channel width Wynn et al. A channel is meandering if it is greater than or equal to 1. Flood and Damuth and Pirmez and Flood provide slope data in metres of rise per kilometre of run, Peakall et al. Therefore, in order to make this project compatible with previous studies, each of the formats above were calculated however degrees were chosen as the pre- ferred unit of measurement, as it is the most common throughout the literature.
Longitudinal — or axial — profiles were taken along the thalweg of the main channels within the PSB Figure 3. Within the investigation, the thalweg was taken as the deepest point of a V- or U-shaped channel, or the median line within channels that were determined to have a flat floor.
The param- eters measured from the longitudinal profiles taken include the lengths and slopes of channels and valleys, the meander wavelength, the sinuosity Flood and Damuth, and the peak sinuosity Clark et al. Flood and Damuth — as well as numerous subsequent studies e. Kolla et al. This was done in order to avoid miscalculations due to distortion inherent in side- scan sonar investigations.
The nadir line cannot be defined in the multibeam datasets and distortion is not generally a problem. In addition to the distinct channel profiles above, a number of levee and thalweg profiles covering the entire length of the system were produced, in much the same way.
These profiles exhibit the complete transition from the channel heads to the continental rise, effectively showing variations in slope and depth. The levee profiles were taken along the north and south levees, parallel to the axial profiles.
Profile 2 — N S. The parameters were collected for a total of 25 longitudinal channel. This complete dataset is presented within the appen- dices of Murphy and Murphy et al.
Our understanding of the extent of the drainage network has changed significantly from previous studies, due to the use of flow accu- mulation tools and the harnessing of the powerful GIS capabilities within ArcMap and ArcGlobe. Previously, it was thought that the GCS was the main source of downslope sediment transport within the PSB Van Rooij, but this study has revealed that there is a far more expansive dendritic system present, which seems to drain most if not all of the area of the Seabight.
The three innermost channels drain the north- ern, Gollum and southern watersheds located within the Seabight, while the other two diffusely drain the continental margin Figure 3. The drainage network analysis has revealed that previously unidentified downslope flow- ing portions of the Celeborn and Galadriel Channels in the Elven Channel System trace channel expressions across the Seabight.
In addition, they are now revealed as hydrologically separate from one another, occurring within separate watersheds. This is significant, in that links have been found between the previously separate channel systems.
From the channel heads to its basin- ward limit the GCS is on average km long. The GCS is a straight to slightly sinuous dendritic system, with a maximum sinuosity of 1. Slopes range from 0. Meandering is of a low amplitude and is generally confined to the mid-slopes at about a 0. From the combined efforts of the GIS-based specific and general geomor- phometric analyses, several important observations and conclusions about the GCS can be made.
Firstly, there is a significant geological control on chan- nel morphology, orientation and branching patterns. This stems from obser- vations of sudden changes in channel orientation, irregular channel floors and the restricted branching patterns of some channels.
In addition, equi- librium profiles denoting the steady state conditions of a system are usually defined by a smooth concave up shape Pirmez and Flood, ; Babonneau et al. Instead, a two-part equilibrium profile is present Figure 3.
The upper section of this defines a normal canyon-channel transition, in a slightly aggraded state. The lower section begins at the start of the Gollum Channel, where the equilibrium profile diverges from the normal concave up profile. This divergence means that the lower section has been left sediment staved, and also marks the transition back into an erosional and canyonised system. This state of in-equilibrium is thought to have been significantly affected by a Late Palaeogene to Neogene tectonic inversion, where the pre- viously rifted basin was uplifted Van Rooij, This uplift would have affected sedimentation as well as shallowing basement geology.
The use of morphometric parameters commonly used in other submarine investigations allows the GCS to be placed within a global context. This is largely due to its location in the broad, geologically controlled seabight and the abundant sediment source provided by British- Irish Ice Sheet.
The upper sections were correctly characterized by Van Rooij as a canyon-channel transition; however, it was found that the lower sec- tions of the GCS do not exhibit the typical features of a channel system, as pre- viously thought. Instead of transitioning downslope into a channel system, the geological influences on the PSB have altered the flow in the mid to lower sec- tions, where it becomes erosive once again and has extended the canyonised system down to the mouth of the Seabight.
In conclusion, this investigation has added significantly to our knowledge of the morphology and functioning of the Gollum Canyon System, via the use of both specific and general geomorphometric techniques. The hydro- logical toolsets within ArcMap have facilitated the derivation of the true drainage network within the Porcupine Seabight — revealing a vast dendritic system — as well as identifying hydrological connections between the previ- ously separated Gollum, Kings and Elven Channel Systems.
The 3D Analyst toolset in ArcMap, in addition to the 3D visualization of ArcGlobe, allowed for detailed analysis of the entire canyon system, for the first time. This is not only significant for the investigations into the Gollum Canyon System, but is also significant on a larger scale.
There has been an apparent decrease in sub- marine geomorphometric investigations since the mids. This may be due to the rapid advancement of technology and switch from side-scan sonar to multibeam bathymetry as the technology of preference, leaving many of the previous techniques unsuitable.
However, this project has bridged the gap between the side scan and multibeam methodologies. It has shown the power of this approach when applied to multibeam echosounder data — even when noise levels are high — potentially allowing for further comparable projects to commence in the future and therefore advancing our knowledge on the functioning of the submarine environments. References Akhmetzhanov, A. The continental rise west of the Porcupine Seabight, Northeast Atlantic.
In: J. Meinert and P. Weaver, Eds. Heidelberg: Springer-Verlag, pp. Babonneau, N. Morphology and architec- ture of the present canyon and channel system of the Zaire deep-sea fan.
Marine and Petroleum Geology, 19, — Berthois, L. Beyer, A. High resolution bathymetry of the eastern slope of the Porcupine Seabight. Marine Geology, 1—227— Seafloor classification of the mound and channel provinces of the Porcupine Seabight: An application Memories - Eria DOr - Memories (CDr) the multibeam angular backscatter data. International Journal of Earth Sciences, 96 111— Budillon, F. Marine Geophysical Research, 32 1—2 ,83— Chopra, R.
Journal of the Indian Society of Remote Sensing, 2 4— Clark, J. Quantitative analysis of the geometry of submarine channels: Implications for the classification of subma- rine fans.
Geology, 20 July— Dunlop, P. Marine geo- physical evidence for ice sheet extension and recession on the Malin Shelf: New evidence for the western limits of the British Irish Ice Sheet. Marine Geology,86— Estrada, F.
Quantitative study of a Magdalena subma- rine channel Caribbean Sea : Implications for sedimentary dynamics. Marine and Petroleum Geology, 22, — Flood, R.
Quantitative characteristics of sinuous distribu- tary channels on the Amazon Deep-Sea Fan. Geological Society of America Bulletin, 98 June— Guinan, J. Ecological niche mod- elling of the distribution of cold-water coral habitat using underwater remote sensing data. Ecological Informatics, 4, 83— Jenson, S. Applications of hydrologic information automatically extracted from digital elevation models. Hydrological Processes, 5, 31— Keevil, G. The influence of scale, slope and channel geometry on the flow dynamics of submarine channels.
Marine and Petroleum Geology, 24 6—9— Kenyon, N. Channels, canyons and slump folds on the continental slope between South-West lreland and Spain. Oceanologica Acta, 1, — Klaucke, I. Bulletin of the Geological Society of America, 122— Kolla, V.
Evolution of deep-water tertiary sinuous channels offshore Angola west Africa and implications for reservoir architecture. Leopold, L. River channel patterns; braided, meander- ing, and straight.
Paper B. Magesh, N. A GIS based automated extrac- tion tool for the analysis of basin morphometry. Geographical information system-based morphometric analysis of Bharathapuzha river basin, Kerala, India. Applied Water Science, 3, — Murphy, P. Geomorphometry of the Gollum Canyon System. Nakajima, T. Channel-levee complexes, terminal deep-sea fan and sediment wave fields associated with the Toyama Deep-Sea Channel system in the Japan Sea.
Marine Geology,25— Pareta, K. International Journal of Geomatics and Geosciences, 2 1— Peakall, J. Global latitudinal variation in submarine channel sinuosity. Geology, 40 111— A process model for the evolution, mor- phology, and architecture of sinuous submarine channels.
Journal of Sedimentary Research, 70, — Pike, R. Geomorphometry: A brief guide. In: T. Hengl and H. Reuter, Eds. Geomorphometry: Concepts, Software, Applications. Amsterdam: Elsevier, pp. Pirmez, C. Morphology and structure of Amazon Channel. Rengstorf, A. High-resolution habitat suitability modelling can improve conservation of vulnerable marine ecosys- tems in the deep sea. Journal of Biogeography, 40 9— Sacchetti, F.
Georgiopoulou, A. Geomorphology of the Irish Rockall Trough, North Atlantic Ocean, mapped from multibeam bathymetric and backscatter data. Journal of Maps, 7 160— Saraf, A. GIS based surface hydro- logical modelling in identification of groundwater recharge zones. International Journal of Remote Sensing, 25 24— Strahler, A.
Quantitative analysis of watershed geomorphology. Transaction of the American Geophysical Union, 38 6— Tubau, X. Geomorphology,20— Tudhope, A. Processes of sedimentation in the Gollum Channel, Porcupine Seabight: Submersible observations and sediment analysis. Van Rooij, D. Wheeler, A. Canyon heads and channel architecture of the Gollum Channel, Porcupine Seabight.
Mienert and P. European Margin Sediment Dynamics. Berlin: Springer, pp. Whittemore Boggs, S. Problems of water-boundary definition: Median lines and international boundaries through territorial waters. Geographical Review, 27 3— Wynn, R. Sinuous deep-water channels: Genesis, geometry and architecture. Two of these environments are fluid and highly mobile, while the third, the land, is comparatively stable and enduring Bartlett, The interactions between these involve many natural forces such as wind, river discharge, waves, salt spray and ocean currents Bosboom and Stive, Coastal pro- cesses take place at a wide range of spatial and temporal scales Bartlett, Algal blooms, harmful or not, can extend from several hundreds of metres up to several hundreds of kilometres across Smayda, Weather events such as storms and flooding might affect a region, or a bay, or just the area around a particular river mouth.
Cliff erosion as well as beach erosion usually occurs more locally, sometimes affecting stretches of coast only a few metres wide. Coastal vegetation succession or degradation is measurable at a sub-metre scale. In addition to this wide range of spatial scale, coastal processes also work at a variety of temporal scales. Most dramatic are the events of erosion and land loss through single storm events, while other, slower processes such as sea level rise and related changes in nearshore sediment dynamics are pro- gressive, and their results only become visible over decades.
Thus, the only thing that is constant at the coast is that it is in a permanent state of change. Remote sensing, whether from orbiting space-borne or air-borne plat- forms, can greatly assist in the task of monitoring coastal environments. It is striking that despite the long history of multispectral and other remote sensing techniques for land cover assessment in non-coastal, strictly terres- trial environments, a comparative scarcity of published literature suggests that very little operational remote sensing has been applied to similar require- ments at the coast.
The following sections will explore the variety of established and upcom- ing types of remote sensing data, their spatial, temporal and spectral resolu- tion and will give some examples of practical applications in the coastal space. The relation between remote sensing and GIS for effective marine and coastal spatial planning will also be considered, and the chapter will close with.
TABLE 4. Central Intelligence Agency The World Factbook. The earliest form of Earth observation was through the use of aerial photog- raphy, initially from hot air balloons and later from kites, pigeons, rockets and eventually aircraft.
This dates back to the middle of the nineteenth century Anonymous, n. The quality and resolution of the acquired imagery largely depended on camera and flight height, and also on the photographic process collodion, dry plate, etc. The convergence of these two developments led to the increasing use of aerial photography for topographic mapping, reconnaissance and surveying purposes, in and subsequent to the First World War.
This was followed, especially during and after World War II, by the invention and development of radar, infra-red pho- tography and thermal imagery Cracknell and Hayes, From the s onwards, electronic sensors started to appear, and gradu- ally replaced photochemical imagery for collection and storage of images Klemas, The s also saw the birth of space exploration, and this led rapidly to the use of orbiting plat- forms for Earth observation.
Given the wide potential range of methods, platforms and technologies involved, it is clear that many different criteria — and permutations of these — may be used to classify and examine remote sensing as a data acquisition technique.
Adapted from Kramerthese include:. The capture of data relating to the seabed, using multibeam sonar imag- ery a form of ship-based remote sensing has already been introduced and discussed in Chapters 2 and 3 of this volume. In this chapter, the focus of attention and discussion will be primarily on the acquisition of data from space-borne platforms.
Department of Commerce, and demonstrated conclusively the potential that satellites offered for observing global weather and other phenomena from space. Also inthe U. These satellites were able to capture grey-scale i. Inthe fourth version of Corona, KH-4, was developed and launched, with twin cameras that were able to provide stereoscopic pho- tography which, bywas able to provide imagery with ground resolu- tion of 5 ft approximately 1. While this imagery was classified initially, it was declassified under the terms of Executive Order of 22 Februarysigned and ordered by then U.
President Bill Clinton and placed in the public domain for scien- tific and environmental uses. Selected images can now be ordered from the U. Both historic aerial imagery as well as the early reconnaissance data allow — if image quality is adequate — for the identification of small-scale land or sea features such as single trees, cars and ships, roads, buildings, as well as coastal infrastructure such as ports and moorings, and to some extent vegetation borders.
They are therefore a valuable source for historical trend analysis, and can be especially useful for investigations of erosion or deposition, or changes in channel morphology. However, image acquisition intervals and image quality vary tremendously, and comparing images from one sensor with another is usually challenging.
NOAA aims at always operating at least two identical satellites at the same time, resulting in the acquisition of at least four images per day per area. AVHRR with its spectral channels in the visible, near and thermal infrared is therefore one of the most valuable sources for historical time series of ocean and land colour, temperature and because of its infra- red bands vegetation processes on land and the ocean.
A comprehensive review of ocean colour remote sensing and statistical techniques for mapping of phytoplankton blooms can be found at Blondeau-Patissier et al. Following the AVHRR concept, in recent decades several other sensors with low spatial and high temporal resolution have been launched.
Data at m and 1 km resolution are available every 1 to 20 days. They also carry a radar instrument, which will be discussed separately below. All of these sensors are dedicated to monitor land cover and regional ocean colour and phytoplankton Tassan, An example of ocean colour assessment for the Baltic Sea can be found at Kratzer et al.
Current chal- lenges and recommendations for remote sensing of coastal and inland water quality are summarized by Mouw et al. The suc- cessive satellites Landsat 2 and 3 carried the same sensor on board. A pura sangre malaquias 3 almeida watch the voice live online. In france, once sud quarto casal planejado com papel de, back parede?
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He combines impeccable technical credentials with a commitment to customer service and care that is hard to find anywhere just see our Yelp reviews!! Growing up in San Jose Brian played the saxophone throughout childhood and developed a deep love and attachment to jazz and funk. After graduating from Cal State Long Beach with a degree in Political Science, Brian spent time abroad in Ethiopia using his computer skills to help scale a new university network there.
A bit of a renaissance man, Brian continues to develop his technical skills through studying coding Java and Pythonand relaxes through his practices of aqua-scaping, cooking, and horticulture especially Bonsai. She is committed to documenting her life and family history through her camera lens.
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