Comparison of topography- and aperture-dependent motion compensation algorithms for airborne SAR

This letter presents a comparison between threeFourier-based motion compensation (MoCo) algorithms forairborne synthetic aperture radar (SAR) systems. These algorithmscircumvent the limitations of conventional MoCo, namelythe assumption of a reference height and the beam-center approximation.All these approaches rely on the inherent time–frequencyrelation in SAR systems but exploit it differently, with the consequentdifferences in accuracy and computational burden. Aftera brief overview of the three approaches, the performance ofeach algorithm is analyzed with respect to azimuthal topographyaccommodation, angle accommodation, and maximum frequencyof track deviations with which the algorithm can cope. Also, ananalysis on the computational complexity is presented. Quantitativeresults are shown using real data acquired by the ExperimentalSAR system of the German Aerospace Center (DLR).

Synthesis, binding affinity and SAR of new benzolactam derivatives as dopamine D3 receptor ligands

A series of new benzolactam derivatives was synthesized and the derivatives were evaluated for theiraffinities at the dopamine D1, D2, and D3 receptors. Some of these compounds showed high D2 and/orD3 affinity and selectivity over the D1 receptor. The SAR study of these compounds revealed structuralcharacteristics that decisively influenced their D2 and D3 affinities. Structural models of the complexesbetween some of the most representative compounds of this series and the D2 and D3 receptors wereobtained with the aim of rationalizing the observed experimental results. Moreover, selected compoundsshowed moderate binding affinity on 5-HT2A which could contribute to reducing the occurrence of extrapyramidalside effects as potential antipsychotics.

A Small Baseline DIFSAR Approach for Investigating Deformations on Full Resolution SAR Interferograms

This paper presents a differential synthetic apertureradar (SAR) interferometry (DIFSAR) approach for investigatingdeformation phenomena on full-resolution DIFSAR interferograms.In particular, our algorithm extends the capabilityof the small-baseline subset (SBAS) technique that relies onsmall-baseline DIFSAR interferograms only and is mainly focusedon investigating large-scale deformations with spatial resolutionsof about 100 100 m. The proposed technique is implemented byusing two different sets of data generated at low (multilook data)and full (single-look data) spatial resolution, respectively. Theformer is used to identify and estimate, via the conventional SBAStechnique, large spatial scale deformation patterns, topographicerrors in the available digital elevation model, and possibleatmospheric phase artifacts; the latter allows us to detect, onthe full-resolution residual phase components, structures highlycoherent over time (buildings, rocks, lava, structures, etc.), as wellas their height and displacements. In particular, the estimation ofthe temporal evolution of these local deformations is easily implementedby applying the singular value decomposition technique.The proposed algorithm has been tested with data acquired by theEuropean Remote Sensing satellites relative to the Campania area(Italy) and validated by using geodetic measurements.

Interpolation-free Coregistration and Phase-Correction of Airborne SAR Interferograms

This letter discusses the detection and correction ofresidual motion errors that appear in airborne synthetic apertureradar (SAR) interferograms due to the lack of precision in the navigationsystem. As it is shown, the effect of this lack of precision istwofold: azimuth registration errors and phase azimuth undulations.Up to now, the correction of the former was carried out byestimating the registration error and interpolating, while the latterwas based on the estimation of the phase azimuth undulations tocompensate the phase of the computed interferogram. In this letter,a new correction method is proposed, which avoids the interpolationstep and corrects at the same time the azimuth phase undulations.Additionally, the spectral diversity technique, used to estimateregistration errors, is critically analyzed. Airborne L-bandrepeat-pass interferometric data of the German Aerospace Center(DLR) experimental airborne SAR is used to validate the method

Quelbi Bel Hob Sar Mefni ; Quelbi Bel Hob Sar Mefni (suite) / Laazar Sliman, chant [acc. instr.]

[Traditions. Afrique du Nord. Algérie]

Linear and nonlinear terrain deformation maps from a reduced set of interferometric SAR images

In this paper, an advanced technique for the generation of deformation maps using synthetic aperture radar (SAR) data is presented. The algorithm estimates the linear and nonlinear components of the displacement, the error of the digital elevation model (DEM) used to cancel the topographic terms, and the atmospheric artifacts from a reduced set of low spatial resolution interferograms. The pixel candidates are selected from those presenting a good coherence level in the whole set of interferograms and the resulting nonuniform mesh tessellated with the Delauney triangulation to establish connections among them. The linear component of movement and DEM error are estimated adjusting a linear model to the data only on the connections. Later on, this information, once unwrapped to retrieve the absolute values, is used to calculate the nonlinear component of movement and atmospheric artifacts with alternate filtering techniques in both the temporal and spatial domains. The method presents high flexibility with respect to the required number of images and the baselines length. However, better results are obtained with large datasets of short baseline interferograms. The technique has been tested with European Remote Sensing SAR data from an area of Catalonia (Spain) and validated with on-field precise leveling measurements.

SAR Interferometric phase noise reduction using wavelet transform

The problem of synthetic aperture radar interferometric phase noise reduction is addressed. A new technique based on discrete wavelet transforms is presented. This technique guarantees high resolution phase estimation without using phase image segmentation. Areas containing only noise are hardly processed. Tests with synthetic and real interferograms are reported.

Interferometría SAR en las islas Shetlend del Sur: modelo numérico de elevaciones de la Isla Decepción

La interferometría con imágenes de radar de apertura sintética (SAR: Synthetic Aperture Radar) desde satélite es una técnica que permite obtener información altimétrica del relieve terrestre, siendo especialmente útil en áreas remotas. Este trabajo muestra una aplicación de esta técnica en las islas Shetland del Sur (Antártida). Para ello se han utilizado imágenes SAR obtenidas por los satélites ERS (European Remote Sensing) de la Agencia Espacial Europea (ESA: European Space Agency) y un proceso interferométrico desarrollado entre el Departament de Geodinàmica i Geofísica de la Universitat de Barcelona y el Institut Cartogràfic de Catalunya.

SAR-satelliittien hyödyntäminen merivalvonnassa

Yhteiskunnan eri toimijoiden riippuvuus avaruustoiminnasta on kasvamassa. Satelliittien paikka- ja aikatietojen lisäksi satelliittien valvontakyvyn hyödyntäminen on lisääntymässä. Merivoimat on mukana kansainvälisissä merivalvontahankkeissa, muun muassa Euroopan puolustusviraston johtamassa Maritime Surveillance -hankkeessa, jossa hyödynnetään satelliittien valvontakykyä merialueiden valvonnassa. Tämä tutkimuksen tavoitteena on selvittää miten SAR (Synthetic Aperature Radar) -satelliitteja voidaan hyödyntää merivalvonnassa ja mitkä ovat merivalvonnan tietotarpeet sekä SAR-aineistojen saatavuus.

Länsimaisten SAR/GMTI-tutkien suorituskyky

SAR/GMTI-tutka (Synthetic Aperture Radar/Ground Moving Target Indicator) tuottaa tiedustelutietoa johtamisen, tiedustelun, valvonnan ja maalinosoituksen tueksi. SAR/GMTI -tutka on luotettava tiedusteluväline tutkataajuusalueella tapahtuvan tiedustelutiedon tuottamisen ansiosta, jolloin tutkan käyttö ja tiedustelutiedon tuottaminen onnistuvat huonoissakin sääolosuhteissa. SAR/GMTI-tutkien käyttö on yleistynyt sotilaskäytössä viimeisen kahdenkymmenen vuoden aikana ja niillä on ollut suuri merkitys kaikissa suuremmissa konflikteissa kylmän sodan loppumisen jälkeen. SAR-tutka käyttää lavettina liikkuvaa alustaa, useimmiten lentokonetta, muodostaakseen virtuaalisen antenniryhmän ja signaaliprosessoinnin avulla, jolloin vastaanottimeen palautuvat kaiut sijoitetaan kohdilleen ja muodostetaan SAR-kuvaa. Tarkimmillaan nykyisten SARtutkien resoluutio on muutaman kymmenen senttimetrin luokkaa ja mittausetäisyydet suurimmillaan satoja kilometrejä. GMTI-tutka havaitsee liikkuvat kohteet, kun liikkuvista kohteista palautuvat kaiuilla on eri taajuus kuin ympäröivästä maastosta palautuvilla kaiuilla ja kohteet pystytään erottelemaan välkkeen seasta. GMTI-tutkan toiminta perustuu doppler-ilmiöön. SAR-tutkaa pystytään useimmiten käyttämään GMTI-moodissa. Sotilaskäytössä olevat GMTI-tutkat pystyvät havaitsemaan keskimäärin noin henkilöauton kokoisen maalin, joka liikkuu noin 5 km/h nopeudella. SAR/GMTI-tutkia on käytetty menestyksellisesti molemmissa Irakin sodissa Yhdysvaltojen toimesta, kun tasainen aavikko ei aiheuttanut juurikaan ongelmia alueen valvontaan ilmasta käsin. Sen sijaan haasteita SAR/GMTI-tutkille ovat aiheuttaneet operaatiot Balkanilla ja Afganistanissa korkean vuoriston, peitteisen maaston ja kohteiden hankalan tunnistettavuuden takia. Suoraan taistelun tukemiseen liittyen GMTI-tutkat ovat olleet hyödyllisiä, kun valvontakoneilta saadut tiedot liikkuvista vihollisosastoista on voitu lähettää datalinkkien kautta lähestulkoon reaaliajassa. SAR-tutkat ovat olleet hyödyllisiä ennen taisteluiden alkua tiedustelutiedon keräämisessä ja vaikeakulkuisessa maastossa SAR-tutkia on käytetty esimerkiksi taisteluvaikutuksen jälkiarviointiin. SAR/GMTI-tutkien suorituskyky kehittyy jatkuvasti laitteiden resoluution ja koon pienentyessä. Datalinkeillä voidaan välittää tietoa alajohtoportaille ja SAR/GMTI-tutkia on voitu sijoittaa esimerkiksi UAV-lennokkeihin (Unmanned Aerial Vehicle), joilla on voitu suorittaa tarkempaa aluevalvontaa kuin mitä isomman kokoluokan valvontakoneilla voitaisiin toteuttaa.

Development of hypogene and supergene alteration and copper mineralization patterns, Sar Cheshmeh porphyry copper deposits, Iran /

The formation of the Sar Cheshmeh porphyry Cu-Mo deposit is related to the culmination of calc-alkaline igneous activity in the Kerman region. The deposit comprises a suite of Late Cenozoic intrusive sub-volcanic and extrusive rocks emplaced into a folded series of Eocene andesitic lavas and pyroclastic sediments. The earliest stage of magmatism was emplacement of a large granodiorite stock about 29 m.y.b.p. This was followed by intrusion of two separate porphyritic bodies at 15 (Sar Cheshrneh porphyry) and 12 m.y.b.p. (Late porphyry) and a series of sub-volcanic dikes between 12 and 9 m.y.b.p. Magmatic activity terminated with multi-phase extrusion of a Pelean dacitic dome complex between 10 and 2.8 m.y.b.p. The country rocks and the earlier porphyritic intrusions are pervasively altered to biotite-rich potassium silicate (metasomatic and hydrothermal) sericite-clay, phyllic and chlorite-clay, argillic assemblages. These grade outwards to an extensive propylitic zone. Within the ore body, the later intra-. and post-mineral dikes only reach the propylitic grade. At least three different sets of quartz veins are present, including a sericite-chlorite-quartz set which locally retrogrades pervasive secondary biotite to sericite. In the hypogene zone, metasomatic and hydrothermal alteration is related to all stages of magmatism but copper mineralization and veining are restricted to a period of 15 to 9 m.y.b.p.related to the early intrusive phases. The copper mineralization and silicate alteration do not fit a simple annular ring model but have been greatly modified by, 1. The existence of an ititial, outer ring, of metasomatic alteration overprinted by an inner.ring of hydrothermal alteration and, 2. later extensive dilating effects of intra- and post-mineral dikes. The hydrothermal clay mineral assemblage in the hypogene zone is illite-chlorite-kaolinite-smectite (beidellite). Preliminary studies indicate that the amount of each of these clays varies vertically and that hydrothermal zonation of clay minerals is possible. However, these minerals alter to illite-kaolinite assemblages in the supergene sulfide zone and to more kaolinite-rich assemblages in the supergene leached zone. Hydrothermal biotite breaks down readily in the supergene zone and is not well preserved in surface outcrops. The distribution of copper minerals in the supergene sulfide enrichment zone is only partly related to rock type being more dependent on topography and the availability of fractures.

Educación y compromiso : el IES de Sar responde ante la catástrofe del Prestige y la guerra contra Irak.

El artículo forma parte de un monográfico de la revista dedicado a educación ambiental en tiempos de catástrofes