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Evolution récente des côtes sableuses d'Afrique de l'ouest par traitement d'images Landsat / I.B.N. Faye in Photo interprétation, European journal of applied remote sensing, vol 46 n° 3-4 (septembre 2010)
[article]
Titre : Evolution récente des côtes sableuses d'Afrique de l'ouest par traitement d'images Landsat Type de document : Article/Communication Auteurs : I.B.N. Faye, Auteur ; Françoise Gourmelon, Auteur ; A. Henaff, Auteur ; A.T. Diaw, Auteur Année de publication : 2010 Article en page(s) : pp 116 - 129 Note générale : Bibliographie Langues : Français (fre) Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de télédétection
[Termes IGN] Afrique occidentale
[Termes IGN] Cinématique
[Termes IGN] érosion côtière
[Termes IGN] estuaire
[Termes IGN] Guinée-Bissao
[Termes IGN] image Landsat-ETM+
[Termes IGN] image Landsat-MSS
[Termes IGN] image Landsat-TM
[Termes IGN] littoral
[Termes IGN] Mauritanie
[Termes IGN] sable
[Termes IGN] télédétection spatiale
[Termes IGN] trait de côteRésumé : (Auteur) Cet article décrit l'évolution du trait de côte des estrans sableux ouest-africains, de la Mauritanie à la Guinée-Bissau, entre 1978 et 2001. Les images Landsat utilisées, d'accès libre, ont fait l'objet d'un traitement par équidensitométrie et classification non supervisée (ISODATA). Toutefois, la résolution spatiale des images (30 m à 79 m) et les taux d'évolution relativement faibles observés sur l'essentiel des côtes sableuses (1 à 6 m/an) conduisent à des résultats partiels centrés exclusivement sur des formes très mobiles associées à des systèmes estuariens (flèches, petites îles et cordons sableux isolant des mangroves). Ainsi, seuls 7,5 % du linéaire côtier sableux régional montrent une évolution mesurable avec les données disponibles. Sur cet ensemble, 73,4 % sont en progradation et 26,6 % en érosion avec des vitesses moyennes d'évolution variant généralement de +15 à +140 m/an et de -13 à - 47 m/an. Numéro de notice : A2010-591 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article DOI : sans Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=30782
in Photo interprétation, European journal of applied remote sensing > vol 46 n° 3-4 (septembre 2010) . - pp 116 - 129[article]Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 104-2010031 SL Revue Centre de documentation Revues en salle Disponible Estimating sea floor dynamics in the southern North Sea to improve bathymetric survey planning / L. Dorst (2009)
Titre : Estimating sea floor dynamics in the southern North Sea to improve bathymetric survey planning Type de document : Thèse/HDR Auteurs : L. Dorst, Auteur Editeur : Delft : Netherlands Geodetic Commission NGC Année de publication : 2009 Collection : Netherlands Geodetic Commission Publications on Geodesy, ISSN 0165-1706 num. 69 Importance : 220 p. Format : 17 x 24 cm ISBN/ISSN/EAN : 978-90-6132-311-2 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Bathymétrie
[Termes IGN] bathymétrie
[Termes IGN] covariance
[Termes IGN] déformation de la croute terrestre
[Termes IGN] fond marin
[Termes IGN] géodynamique
[Termes IGN] géostatistique
[Termes IGN] interpolation
[Termes IGN] krigeage
[Termes IGN] marée océanique
[Termes IGN] morphogenèse
[Termes IGN] nivellement indirect
[Termes IGN] Nord, mer du
[Termes IGN] océanographie dynamique
[Termes IGN] port
[Termes IGN] relèvement
[Termes IGN] Rotterdam (Pays-Bas)
[Termes IGN] sable
[Termes IGN] vagueIndex. décimale : 32.10 Bathymétrie Résumé : (Auteur) Safe nautical charts require a carefully designed bathymetric survey policy, especially in shallow sandy seas that potentially have dynamic sea floor patterns. Bathymetric resurveying at sea is a costly process with limited resources, though. A pattern on the sea floor known as tidal sand waves is clearly present in bathymetric surveys, endangering navigation in the Southern North Sea because of the potential dynamics of this pattern. An important factor in an efficient resurvey policy is the type and size of sea floor dynamics. The uncertainties of measurement and interpolation associated with the depth values enable the statistical processing of a time series of surveys, using deformation analysis. Currently, there is no procedure available that satisfies the Royal Netherlands Navy requirements. Therefore, a deformation analysis procedure is designed, implemented and tested in such a way that the procedure works on bathymetric data and satisfies the Royal Netherlands Navy requirements. Also, it is necessary to develop a procedure that translates the results into changes of the resurvey policy, taking into account their confidence intervals.
To describe the sea floor statistically, we assume the sea floor to consist of a spatial trend function (or characterization) and a residual function (or dispersion). Such a description is called a representation. The covariances between positions are expressed in a covariance function, based on the residual function. The covariance function is used by Kriging, an interpolation procedure that propagates the variances and covariances of the data points to variances of the interpolated values. This approach is used widely for spatial analyses, like the interpolation of a bathymetric data set.
The method that we propose uses Kriging to produce a time series of grids of depth values and their variances. Subsequently, it uses deformation analysis, a statistical procedure based on testing theory. Our application of deformation analysis is particularly aimed at the detection of dynamics in areas with tidal sand waves, resulting in parameter estimates for the sea floor dynamics, and their uncertainty. We apply the method to sea floor representations both with and without a sand wave pattern. A test scenario is set up, consisting of a survey of an existing area in the Southern North Sea, for which dynamics are simulated. The results show that the proposed method detects different types of sea floor dynamics well, leading to satisfactory estimates of the corresponding parameters.
We show results for the anchorage area Maas West near the Port of Rotterdam, the Netherlands first. The area is divided into 18 sub-areas. The results show that a sand wave pattern is detected for most of the sub-areas, and a shore-ward migration is detected for a majority of them. The estimated migration rates of the sand waves are up to 7.5 m/yr, with a 95% confidence interval that depends on the regularity of the pattern. The results are in confirmation with previously observed migration rates for the Southern North Sea, and with an idealized process-based model.
Thereafter, we analyze several other areas for which a time series of surveys is available in the bathymetric, archives of the Netherlands Hydrographic Service, to study the spatial variations in sea floor dynamics. We present results for several sand wave areas and a single flat area. In some of those areas, dredging takes place, to guarantee minimum depths. The results indicate sand wave migration in areas close to the coast, and bed level changes of the order of decimeters. The dominant wavelength of the sand waves varies. We compare our results to literature of the same sand wave areas, in which we find similar migration rates, and different wavelengths.
By formulating four indicators, recommendations are made for the resurvey policy on the Belgian and Netherlands Continental Shelf. These indicators follow from the estimates for sea floor dynamics. We present a concept for the shallowest likely depth surface, on which we base two of the indicators. The other two indicators act as a warning: they quantify the potentially missed dynamics, which makes the procedure more robust in case of complicated morphology. We show clear differences in recommended resurvey frequency between the five analyzed regions.
We conclude that the designed method is able to use a time series of bathy-metric surveys for the estimation of sea floor dynamics in a satisfactory way. Those dynamics may be present on the scale of the sea floor, it may be a local effect, or it may be due to a tidal sand wave pattern. Also, the results are successfully reduced to a set of four indicators, used to improve a resurvey policy. Based on these conclusions, we formulate recommendations on the extrapolation of the results in space and time, on potential adaptations to the designed procedure, and on implementation of the procedure.Note de contenu : Preface
1 Introduction
1.1 Nautical charting
1.2 Survey plan design
1.3 Detection of sea floor dynamics
1.4 Tidal sand waves
1.5 The uncertainty of depth measurements
1.6 Problem formulation
1.7 Research question and subquestions
1.8 Research strategy and outline
2 Bathymetric applications of Geostatistics
2.1 Introduction
2.2 Depth as a trend and its residuals
2.3 Covariance functions
2.4 Kriging
2.5 Conclusion
3 Estimating sea floor dynamics
3.1 Introduction
3.2 The method for the estimation of sea floor dynamics
3.3 Specification of a test scenario
3.4 Analysis results of a dynamic sea floor
3.5 Discussion
3.6 Conclusion
3.A Error characteristics
3.B Transformation of the sand wave parameters
3.C The application of statistical estimation and testing
4 The analysis of migrating tidal sand waves
4.1 Introduction
4.2 The application of deformation analysis
4.3 Results of the deformation analysis
4.4 Discussion of results
4.5 Conclusion
4.A Overview of used surveys
4.B Quantification of measurement errors
4.B.1 Covariance function of the error
4.B.2 Variances of the SEES surveys
4.B.3 Variances of the MBES survey
5 Spatial variations in sea floor dynamics
5.1 Introduction
5.2 Deformation analysis
5.3 The Selected Track region: little dynamics
5.4 The Noordhinder region: comparison with other methods
5.5 The region West of IJmuiden: sand wave migration
5.6 The region North of Terschelling: a flat sea floor
5.7 Discussion
5.8 Conclusion
5.A Overview of used surveys
6 Application to the resurvey policy
6.1 Introduction
6.2 Background: Hydrographic practice
6.3 Method: indicators of sea floor dynamicsNuméro de notice : 15495 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Thèse étrangère DOI : sans Accessibilité hors numérique : Non accessible via le SUDOC En ligne : https://www.ncgeo.nl/downloads/69Dorst.pdf Format de la ressource électronique : URL Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=62737 Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 15495-01 32.10 Livre Centre de documentation Topographie Disponible Space analysis and the detection of the changes for the follow-up of the components sand-vegetation in the area of Mecheria, Algeria / I. Haddouch in Revue Française de Photogrammétrie et de Télédétection, n° 185 (Mars 2007)
[article]
Titre : Space analysis and the detection of the changes for the follow-up of the components sand-vegetation in the area of Mecheria, Algeria Type de document : Article/Communication Auteurs : I. Haddouch, Auteur ; K. Mederbal, Auteur ; S. SaÏdi, Auteur Année de publication : 2007 Conférence : ISPRS 2006, Commission 1 Symposium, From sensors to imagery 03/07/2006 06/07/2006 Champs-sur-Marne [Paris Marne-la-Vallée] France OA ISPRS Archives Article en page(s) : pp 26 - 29 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de télédétection
[Termes IGN] analyse diachronique
[Termes IGN] analyse spatiale
[Termes IGN] carte de la végétation
[Termes IGN] désertification
[Termes IGN] détection de changement
[Termes IGN] écologie
[Termes IGN] image Landsat-TM
[Termes IGN] Oran (Algérie)
[Termes IGN] sable
[Termes IGN] système d'information géographiqueRésumé : (Auteur) The Algerian steppe has become for a few years the theatre of an ecological and climatic imbalance. The intense degradation for this fragile medium (stranding wind erosion, overgrazing, clearing, salinisation, ...) inducing the turning into a desertification require a better comprehension in order to see how to fight against this plague and to adapt an adequate installation to him. Thus, this work lies within the scope of the follow-up of the phenomenon of the turning into a desertification on a space with the heart of the high Oranian southern steppe plains, in fact the area of Mecheria. Techniques of numerical cartography, since the satellite image processing until the geographic information systems (SIG) for the realization of the charts sets of themes, being able to highlight this calamity. The use of the approaches based on the exploitation of the satellite data multi dates (1998 & 2004) of the sensor Thematic Mapper (TM) of Landsat 5 permitted us to obtain a gathering of an interpretative photo maps and vegetation index which, in their turn, helped us to see the changes arrived in the medium, copiously regressive that progressive. Copyright SFPT Numéro de notice : A2007-397 Affiliation des auteurs : non IGN Thématique : FORET/IMAGERIE Nature : Article DOI : sans En ligne : https://www.isprs.org/proceedings/XXXVI/part1/Papers/PS1-02.pdf Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=28760
in Revue Française de Photogrammétrie et de Télédétection > n° 185 (Mars 2007) . - pp 26 - 29[article]Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 018-07011 RAB Revue Centre de documentation En réserve L003 Disponible A digital camera as a tool to measure colour indices and related properties of sandy soils in semi-arid environments / N. Levin in International Journal of Remote Sensing IJRS, vol 26 n° 24 (December 2005)
[article]
Titre : A digital camera as a tool to measure colour indices and related properties of sandy soils in semi-arid environments Type de document : Article/Communication Auteurs : N. Levin, Auteur ; Eyal Ben-Dor, Auteur ; A. Singer, Auteur Année de publication : 2005 Article en page(s) : pp 5475 - 5492 Note générale : Bibliographie Langues : Français (fre) Descripteur : [Vedettes matières IGN] Applications de télédétection
[Termes IGN] analyse comparative
[Termes IGN] caméra numérique
[Termes IGN] composition chimique
[Termes IGN] couleur du sol
[Termes IGN] étalonnage des données
[Termes IGN] fer
[Termes IGN] image RVB
[Termes IGN] particule
[Termes IGN] sable
[Termes IGN] spectromètre
[Termes IGN] zone semi-arideRésumé : (Auteur) Soil colour carries important information regarding the soil's chemical and physical properties. However, common practices for measuring soil colour, either by Munsell charts or by field/laboratory spectrometers, are insufficient, due to the subjective and nonquantitative character of the Munsell charts, and to the high cost and inconvenience of field spectrometers. We present herein, a method to characterize the colour of soil samples, and related chemical and physical properties of the soil, using a digital camera, and an array of coloured plastic chips, that are used for calibration purposes. Using 370 samples of sandy soils, we have demonstrated that both RGB values from digital images and their derived soil indices, correlate highly with similar measurements performed by a field spectrometer. When checked against free iron oxide content and against the percentage of fine particles in a subsample set of 42 soils, the redness index as measured by the digital camera gave similar or better correlations than those obtained from a field spectrometer, against both free iron oxides and fine particle contents (R2 of 89% for the iron oxides, and of for the fine particles). We propose the use of a digital camera as a field analytical tool to determine precisely: soil colour, iron oxide and fine particle content. Further study in this direction, with other soil population and more soil properties, is strongly advised in order to launch this as a vastly applicable and generic method. Numéro de notice : A2005-522 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1080/01431160500099444 En ligne : https://doi.org/10.1080/01431160500099444 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=27658
in International Journal of Remote Sensing IJRS > vol 26 n° 24 (December 2005) . - pp 5475 - 5492[article]Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 080-05241 RAB Revue Centre de documentation En réserve L003 Exclu du prêt Apports et limites de l'imagerie spatiale à l'étude des littoraux sableux : cas du littoral de Chaffar, gouvernorat de Sfax (Tunisie méridionale) / R. Bouaziz in Photo interprétation, vol 41 n° 3 (Septembre 2005)
[article]
Titre : Apports et limites de l'imagerie spatiale à l'étude des littoraux sableux : cas du littoral de Chaffar, gouvernorat de Sfax (Tunisie méridionale) Type de document : Article/Communication Auteurs : R. Bouaziz, Auteur ; A. Daoud, Auteur ; S. Dahech, Auteur ; G. Beltrando, Auteur Année de publication : 2005 Article en page(s) : pp 15 - 24 Note générale : Bibliographie Langues : Français (fre) Descripteur : [Vedettes matières IGN] Applications de télédétection
[Termes IGN] analyse diachronique
[Termes IGN] ArcView
[Termes IGN] eau de mer
[Termes IGN] image SPOT
[Termes IGN] littoral méditerranéen
[Termes IGN] occupation du sol
[Termes IGN] photographie aérienne
[Termes IGN] sable
[Termes IGN] sédiment
[Termes IGN] Sfax (Tunisie)Résumé : (Auteur) Ce texte montre l'intérêt et les limites d'une analyse de quatre photographies aériennes (1948, 1963, 1985, 1998) et de deux scènes SPOT (1996 et 2000), utilisées ici pour observer la dynamique sédimentaire sur une période de cinq décennies. L'étude porte sur un littoral sableux du sud tunisien caractérisé par deux courtes flèches de direction opposée qui ont connu une évolution différenciée sur la période d'étude. Numéro de notice : A2006-146 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article DOI : sans Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=27873
in Photo interprétation > vol 41 n° 3 (Septembre 2005) . - pp 15 - 24[article]Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 104-05031 RAB Revue Centre de documentation En réserve L003 Disponible Airborne laser swath mapping: quantifying changes in sandy beaches over time scales of weeks to years / Ramesh L. Shrestha in ISPRS Journal of photogrammetry and remote sensing, vol 59 n° 4 (June - July 2005)PermalinkComment reproduire le MNT d'une rivière ensablée ? / B. Federici in Géomatique expert, n° 44 (01/06/2005)PermalinkA phase signature for detecting wet subsurface structures using polarimetric L-band SAR / Y. Lasne in IEEE Transactions on geoscience and remote sensing, vol 42 n° 8 (August 2004)PermalinkEffect of grain size on remotely sensed spectral reflectance of sandy desert surfaces / G.S. Okin in Remote sensing of environment, vol 89 n° 3 (15/02/2004)PermalinkContribution au développement d'une base de données à référence spatiale pour l'aide à la décision dans la lutte contre la désertification / K. Talbi (2002)PermalinkApproche méthodologique pour l'analyse de l'évolution des littoraux sableux par photo-interprétation : exemple des plages situées entre les embouchures de l'Aude et de l'Hérault (Languedoc, France) / Paul Durand in Photo interprétation, vol 38 n° 1-2 (Mars 2000)PermalinkDétermination par télédétection aérienne et satellitaire du sens des migrations éoliennes de la région de Laghouat (piémont sud de l'atlas saharien, Algérie) / A.N. Taibi in Photo interprétation, vol 36 n° 4 (Novembre 1998)PermalinkMont-Saint-Michel / J.F. Seguin (1998)PermalinkInsulaire 23 [observatoire topographique sur les évolutions de la baie du Mont-Saint-Michel de 1991 à 1995] / D. Deleaz (1995)PermalinkMont Saint-Michel insulaire / A. Chemetoff (1991)Permalink