Добірка наукової літератури з теми "Dati A Terra"
Оформте джерело за APA, MLA, Chicago, Harvard та іншими стилями
Ознайомтеся зі списками актуальних статей, книг, дисертацій, тез та інших наукових джерел на тему "Dati A Terra".
Біля кожної праці в переліку літератури доступна кнопка «Додати до бібліографії». Скористайтеся нею – і ми автоматично оформимо бібліографічне посилання на обрану працю в потрібному вам стилі цитування: APA, MLA, «Гарвард», «Чикаго», «Ванкувер» тощо.
Також ви можете завантажити повний текст наукової публікації у форматі «.pdf» та прочитати онлайн анотацію до роботи, якщо відповідні параметри наявні в метаданих.
Статті в журналах з теми "Dati A Terra"
Colabella, Sabrina. "La terra e l’εὕρησις del fuoco nella Grecia Antica". Humanitas 68 (29 грудня 2016): 11–30. http://dx.doi.org/10.14195/2183-1718_68_1.
Повний текст джерелаBrown, A. G., and C. Ellis. "People, climate and alluviation: theory, research design and new sedimentological and stratigraphic data from Etruria." Papers of the British School at Rome 63 (November 1995): 45–73. http://dx.doi.org/10.1017/s0068246200010199.
Повний текст джерелаDei Cas, Luca. "Complementarietà fra i dati dell'interferometria satellitare e quelli ottenuti con strumentazione a terra sui versanti in dissesto." Rendiconti Online della Società Geologica Italiana 42 (March 2017): 18–22. http://dx.doi.org/10.3301/rol.2017.04.
Повний текст джерелаBertini, R., G. Chirici, P. Corona, and D. Travaglini. "Comparison between parametric and non-parametric methods for the spazialization of forest standing volume by integrating field measures, remote sensing data and ancillary data." Forest@ - Rivista di Selvicoltura ed Ecologia Forestale 4, no. 1 (March 21, 2007): 110–17. http://dx.doi.org/10.3832/efor0439-0040110.
Повний текст джерелаRe, Mario. "Gestione della terra ed esercizio del potere in Valle Tuccio (fine secolo XII): due casi esemplari. Edizione, commento, dati prosopografici e analisi paleografica di ADM 1324, 1368 e 1333." Jahrbuch der Österreichischen Byzantinistik 58 (2008): 131–46. http://dx.doi.org/10.1553/joeb58s131.
Повний текст джерелаTjen, Anwar. "Dari Terra Sancta ke Terra Incognita." Indonesian Journal of Theology 2, no. 1 (September 7, 2014): 23–41. http://dx.doi.org/10.46567/ijt.v2i1.78.
Повний текст джерелаTibiriçá Amaral, Sérgio, and Maria Fernanda De Toledo Pennacchi Tibiriçá Amaral. "Os Povos Originários No Brasil e o Marco Temporal para Demarcação de Terras como Retrocesso." Revista Jurídica Mario Alario D´Filippo 14, no. 27 (January 15, 2022): 20–46. http://dx.doi.org/10.32997/2256-2796-vol.14-num.27-2022-3807.
Повний текст джерелаBarni, Paulo, Reinaldo Imbrozio Barbosa, Antônio Ocimar Manzi, and Philip Martin Fearnside. "Simulated deforestation versus satellite data in Roraima, Northern Amazonia, Brazil." Sustentabilidade em Debate 11, no. 2 (August 31, 2020): 81–94. http://dx.doi.org/10.18472/sustdeb.v11n2.2020.27493.
Повний текст джерелаGarcia, Deyvison Aguiar, Sérgio Souza Costa, and Evaldinolia Gilbertoni Moreira. "PUBLICAÇÃO DE DADOS CONECTADOS PARA MODELOS DE USO E COBERTURA DA TERRA." REVISTA GEONORTE 10, no. 36 (December 19, 2019): 77–94. http://dx.doi.org/10.21170/geonorte.2019.v.10.n.36.a77.94.
Повний текст джерелаBarroso, Lucas Abreu, and Guilherme Viana de Alencar. "O Cadastro Ambiental Rural (CAR) como instrumento de regularização ambiental em assentamentos de reforma agrária." Revista Brasileira de Gestão Ambiental e Sustentabilidade 1, no. 1 (2014): 5. http://dx.doi.org/10.21438/rbgas.010102.
Повний текст джерелаДисертації з теми "Dati A Terra"
Angelica, Carmelo. "Potenziale sismogenetico dell'Italia, da dati sismici e geodetici." Doctoral thesis, Università di Catania, 2012. http://hdl.handle.net/10761/1085.
Повний текст джерелаLACEDELLI, GAIA. "Ricerca e caratterizzazione di sistemi planetari multipli tramite dati da terra e da spazio." Doctoral thesis, Università degli studi di Padova, 2022. http://hdl.handle.net/11577/3449035.
Повний текст джерелаPlanets in multiplanetary systems offer a unique opportunity for comparative planetology. The study of well-characterized systems allow us to investigate the formation and evolution processes, by constraining theory and helping to discriminate among competing models. To better understand exoplanetary systems complexity, it is essential to build a robust sample of well-characterized multiplanetary systems. Currently, ultra-precise photometers and high-resolution spectrographs can be used to infer accurate planetary radii and masses, needed to determine the average density and provide clues on the inner bulk composition, which is fundamental to obtain a complete characterization of a system in combination with the orbital architecture. This thesis is motivated by improving our knowledge of multiplanetary systems. On one side, we focused on the characterization of a new multiplanetary system orbiting the star TOI-561. This star was initially observed by TESS, which identified the presence of three transiting candidates. We followed-up the system with HARPS-N, collecting 82 high-resolution radial velocities (RVs). TOI-561, an old, metal-poor, and alpha-enhanced late-G dwarf, belongs to the thick-disk, and it is one of the few stars of this Galactic population that hosts a multiplanetary system. From the RV analysis we discovered two additional external planets. However, RVs could not confirm the outermost TESS candidate, which would also make the system dynamically unstable. We demonstrated that the two transits initially associated with this candidate are instead due to single transits of the two planets discovered using RVs. We proposed a final configuration with four transiting planets: an ultra-short period (USP) super-Earth (TOI-561 b) and three mini-Neptunes (TOI-561 c, d, and e). The unusual density of TOI-561 b, which is the lowest density USP planet known to date, and the interesting system configuration called for follow-up studies. We therefore collected a second season of 62 HARPS-N RVs. Moreover, we collected ultra-high precision photometric data with CHEOPS, observing various transits of TOI-561 b and c, and one transit of the previously single-transiting planet TOI-561 d. Our global analysis, including also new TESS observations, confirmed the four-planet configuration, as well as the low density of TOI-561 b, which, given the low stellar metallicity, is effectively consistent with the general bulk density-stellar metallicity trend. The precise masses and radii obtained for the four planets allowed us to conduct interior structure and atmospheric escape modelling. Finally, we identified an additional long-period signal in the RVs, which could be due to either an external planetary companion or to stellar magnetic activity. In the second part of the thesis, we focused on the development of a new tool for the characterization of interacting multiplanetary systems showing transit time variations (TTVs). In presence of mutual gravitational interactions, the most consistent way to analyze photometric and spectroscopic data is through the photodynamical approach, which combines photometric and dynamical analysis to simultaneously determine mass and radius of both the star and planets accounting for the gravitational dynamic interactions via an N-body simulations. We implemented our Python version of a photodynamical code, using the the batman package for transit modelling, the orbital integrator rebound for N-body integration, and determining the best combination of the orbital parameters using a Bayesian analysis. We started testing the code on the well-known WASP-47 system, obtaining promising results. We also used some code functionalities to perform new dynamical analysis of the TOI-836 and Kepler-37 systems. Once completed, optimized, and definitely validated, we will publicly release the code, which will be an an important tool for the characterization of known and newly-detected systems showing TTVs.
Tripone, Daniele <1978>. "Tecniche di elaborazione di dati macrosismici per la definizione di sorgenti sismogenetiche." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2009. http://amsdottorato.unibo.it/1518/1/tripone_daniele_tesi.pdf.
Повний текст джерелаTripone, Daniele <1978>. "Tecniche di elaborazione di dati macrosismici per la definizione di sorgenti sismogenetiche." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2009. http://amsdottorato.unibo.it/1518/.
Повний текст джерелаACCAINO, FLAVIO. "MODELLIZZAZIONE DI DATI SISMICI A RIFLESSIONE, RIFRAZIONE E TERRA-MARE PER L'ANALISI DEL RISCHIO VULCANICO E SISMICO NELLA SICILIA ORIENTALE." Doctoral thesis, Università degli studi di Trieste, 1998. http://thesis2.sba.units.it/store/handle/item/13010.
Повний текст джерелаComandini, Luca. "Analisi statistiche di dati idro-meteorologici del bacino del fiume Santerno (BO) nell'ultimo secolo." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2015. http://amslaurea.unibo.it/9300/.
Повний текст джерелаMartinico, Bruno. "Applicazione di tecniche di clustering spaziale su dati macrosismici di felt reports per stimare i parametri dei terremoti." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2021. http://amslaurea.unibo.it/24993/.
Повний текст джерелаCavicchioli, Niccolò. "Verifica preliminare di ricezione di dati di telemetria da satelliti radioamatoriali mediante l'Alma Mater Ground Station." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2018. http://amslaurea.unibo.it/15854/.
Повний текст джерелаGastaldo, Thomas. "Assimilazione dati di precipitazione in un modello meteorologico ad alta risoluzione (MOLOCH): sviluppo ed applicazione alla previsione di eventi intensi in Liguria." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amslaurea.unibo.it/11165/.
Повний текст джерелаFabbri, Julius. "Contributo di dati di gravità nella valutazione del vulcanismo CAMP in Africa Nord-Occidentale." Doctoral thesis, Università degli studi di Trieste, 2015. http://hdl.handle.net/10077/10927.
Повний текст джерелаLa domanda alla base di questa ricerca è stata se il metodo della gravimetria satellitare possa essere utilizzato per seguire le unità geologiche anche in luoghi difficilmente accessibili. L’obiettivo di questa ricerca è di verificare se le missioni satellitari di nuova generazione permettano di identificare la più grande delle province ignee della Terra (Bertrand et al., 2013), nota come CAMP (Central Atlantic Magmatic Province) in Africa nord-occidentale. Oltre alle motivazioni scientifiche, una possibile applicazione è l’esplorazione di risorse minerarie e lo sfruttamento di energia geotermica. Tale provincia ignea è una LIP (Large Igneous Province) che si estende in Nord e Sud America, Atlantico, Europa ed Africa (istituita in Marzoli et al. 1999). Essa si è sviluppata a seguito della frammentazione del super-continente Pangea al limite Triassico-Giurassico, ca. 200 Ma fa. A causa probabilmente del riscaldamento globale del mantello e/o dalla convezione dello stesso innescata da dislivelli di blocchi litosferici, dai dicchi-sorgente si produssero i cosiddetti basalti da flusso e si verificò un intenso vulcanismo con imponenti colate laviche tali da suggerire a taluni ricercatori che gli elementi volatili presenti nel magma abbiano contribuito ad aumentare i gas serra con conseguenze nel clima globale e nelle estinzioni di massa. I depositi in esame sono costituiti da lave, tholeiti continentali, doleriti, basalti e gabbri. Ciò che rimane di questa attività vulcanica sono dicchi singoli o in sciami, batoliti, sill, colate laviche e plateau basaltici (nei fondali oceanici). L’Africa nord-occidentale è costituita principalmente da un cratone composto da rocce molto antiche dell’Archeano (3000-2500 Ma). Esso emerge a nord nello scudo Reguibat e, a sud, la dorsale dell’Uomo o del Leone (Lucazeau et al., 1991). Il cratone è circondato dalle zone di geosutura (greenstone e cinture mobili) associate al cosiddetto evento termo-tettonico Pan-Africano, verificatosi ca. 650 Ma fa con l’assemblaggio del continente africano da blocchi crostali più piccoli. Nelle Mauritanidi affiora il basamento ercinico (ca. 350 Ma) mentre negli Atlas e nelle Magrebidi prevalgono rocce più recenti connesse all’orogenesi alpina (0-150 Ma). Al centro del cratone si trova il bacino paleozoico Taoudenni che riempie una vasta area depressa. Tutto il territorio in esame è caratterizzato da una forte presenza di rocce metamorfiche dense e magmatiche di ogni età, con presenza di più di un “punto caldo” che potrebbe essere definito un terreno igneo (Bryan et al. (2008) con più LIP spesso sovrapposte o limitrofe. Mediamente, tutte queste rocce magmatiche e metamorfiche hanno una densità di 3000 kg/m3 (Kröner, 1977 ), maggiore di quella della crosta standard e dei sedimenti. Particolare attenzione è stata dedicata ad un lineamento tettonico noto come Pelusium Megashare System (PMS) che attraversa tutta l’Africa nord-occidentale (Neev et al., 1982) chiaramente visibile in tutte le immagini satellitari di Google Earth ma che è riportato solo in pochissime pubblicazioni. Per la prima volta in questa tesi si ipotizza un collegamento tra la CAMP e PMS. La gravimetria satellitare consente di rilevare variazioni di densità nella crosta terrestre. Ove vi sono rocce più dense, il segnale rilevato (detto anomalia gravimetrica) è positivo e viceversa. La gravimetria da satellite si è rivelata un valido strumento per identificare le aree con surplus di massa. La risposta all’interrogativo iniziale è dunque affermativa anche se, da quanto esposto, risulta difficile o impossibile associare ad un certo segnale positivo una data LIP. L’elaborazione dei segnali è avvenuta partendo dai dati del satellite GOCE (ultima generazione, a un’orbita di 250 km ma già ammarato) e GRACE (obsoleto ma tuttora in orbita a ca. 450 km). I dati utilizzati sono dei modelli del campo di gravità terrestre che contengono i coefficienti di Stokes per lo sviluppo in armoniche sferiche del potenziale. I modelli utilizzati sono l’EGM2008 (comprendente anche dati di terra, con risoluzione massima 10 km se sviluppato al massimo ordine di 2159) e GOCO TIM R4 (con una risoluzione massima di 80 km, la migliore mai ottenuta da dati satellitari globali). Il modello EGM2008 è stato sviluppato fino all’ordine e grado 720 per eliminare dati spuri (Pavlis, 2012) e, in tal modo, ha permesso di raggiungere una risoluzione di ca. 27 km se si considera metà lunghezza d’onda. Dopo il controllo della qualità dei dati, essi sono stati elaborati nel seguente modo, come esposto nei capitoli 2, 3 e 4. Ai dati grezzi sono state applicate tre riduzioni per sottrarre gli effetti di gravità indesiderati che mascherano il segnale cercato più debole. È stato sottratto l’effetto di gravità della topografia, dei sedimenti e dell’interfaccia crosta-mantello (ICM). Partendo dall’anomalia “in aria libera” (FA), è stata quindi ottenuta l’anomalia di Bouguer (BA) e la BA corretta per i sedimenti. Poi, calcolata la Moho (ICM) isostatica, si è prodotto il residuo isostatico corretto per i sedimenti. I campi elaborati sono la gravità gz (espressa in milli Gal, mGal) ed il gradiente Tzz (misurato in Eötvös, E). Sono state usate le risoluzioni di 0.5° e di 0.05°, computati ad una quota di 4000 m s.l. m perché maggiore del più altro rilievo montuoso dell’area. Dopo aver modellato dei casi a geometria semplice (cap. 6) si è passati alla modellizzazione di tre casi reali. I tre siti scelti per l’approfondimento sono: Tindouf (Algeria), Taoudenni (Mali), Timbuktu (Mali). Nel bacino di Tindouf un sill doleritico CAMP è annesso al suo probabile dicco-sorgente reso evidente dalla gravimetria che identifica bene anche una vicina miniera di Ferro. Nel bacino Taoudenni, le due anomalie principali suggeriscono la presenza di cumuliti magmatici spessi una dozzina di chilometri e connessi con la superficie attraverso dicchi obliqui. Il sito presso Timbuktu è trattato nel dettaglio perché al di sotto del vicino lago Faguibine è stata rivelata un’intrusione magmatica lunga ca. 250 km. In superficie vi sono evidenze di magmatismo (per es. fumarole) tali da preoccupare le popolazioni locali (El Abbass et al., 1993). Tra i risultati inaspettati, si ricorda il forte segnale gravimetrico generato dalle peridotiti in Marocco ed un’importante anomalia (80 mGal) nel Grand Erg Occidental (Algeria) al di sotto del Sahara che sembrerebbe essere causata da un corpo denso lungo ca. 600 km.
The question behind this research was whether the method of satellite gravimetry can be used to follow the geological units even in inaccessible places. The goal of this research is to verify if the new generation of satellite missions serve to identify the largest of the Earth's igneous provinces (Bertrand et al., 2013), known as CAMP (Central Atlantic Magmatic Province) in Northwest Africa . Besides the scientific reasons, a possible application is the exploration of mineral resources and the exploitation of geothermal energy. This is an igneous province (LIP Large Igneous Provinces) that extends throughout North and South America, the Atlantic Ocean, Europe and Africa (established in Marzoli et al. 1999). It developed as a result of the fragmentation of the super-continent Pangea at Triassic-Jurassic limit, ca. 200 My ago. Probably because of mantel global warming and/or its convection triggered by differences in thickness of lithospheric blocks, from source-dikes were produced the so-called continental flow basalts (CFB) and there was an intense volcanism with massive lava flows that this would suggest to certain researchers volatile elements present in the magma have contributed to increasing greenhouse gases with consequences in the global climate and mass extinctions. The deposits in question consist of lavas, tholeites continental dolerites, basalts and gabbros. What remains of this volcanic activity are individual dykes or in swarms, batholiths, sills, lava flows and basaltic plateau (in the ocean). The north-western Africa consists mainly of a craton made of most ancient rocks dell'Archean (3000-2500 Ma). It emerges in the shield Reguibat north and on the south, the Man or the Lion shield (Lucazeau et al., 1991). The craton is surrounded by areas of geosutura (greenstone belts and mobile belts) associated with the so-called Pan-African thermo-tectonic event, occurred ca. 650 Ma ago with the assembly of the African continent by smaller crustal blocks. Mauritanides emerges in the Hercynian basement (ca. 350 Ma) while in the Atlas and Magrebides prevail younger rocks (Alpine orogenesis, 0-150 Ma). At the center of the craton is the Paleozoic basin Taoudenni that fills a large area depressed. All the territory concerned is characterized by a strong presence of dense magmatic and metamorphic rocks of all ages, with the presence of more than a "hot spot" that could be called “igneous terrane” (Bryan et al. (2008) with more LIPs overlapping or adjacent. On average, these igneous and metamorphic rocks have a density of 3000 kg / m3 (Kröner, 1977), greater than that of the standard crust and the sediments. Particular attention was dedicated to a tectonic lineament known as Pelusium Megashare System (PMS) that runs through the north-western Africa (Neev et al., 1982) clearly visible in all the satellite images of Google Earth but is reported only in very few publications. For the first time this thesis suggests a link between CAMP and PMS. Satellite gravimetry can detect density variations in the Earth's crust. Where there are rocks denser, the detected signal (called gravity anomaly) is positive and vice versa. The gravimetry by satellite has proved a valuable tool to identify areas with surplus Mass. The initial response to the question is therefore affirmative although, from the above, it is difficult or impossible to associate a positive signal a date LIP. Signals processing occurred from the data of the GOCE satellite (last generation, in an orbit of 250 km, mission already finished) and GRACE (obsolete but still in orbit at ca. 450 km). The data used are the models of the Earth's gravity field containing the coefficients of Stokes for the development of potential in spherical harmonics. The models used are the EGM2008 (also including land data, with a maximum resolution 10 km if developed to the maximum order of 2159) and TIM GOCO R4 (with a maximum resolution of 80 km, the best ever obtained by global satellite data). The model EGM2008 has been developed up to the order and degree 720 to remove spurious data (Pavlis, 2012) and, thus, allowed to reach a resolution of ca. 27 km considering half wavelength. After quality control of the data, they were processed in the following flowchart, as discussed in Chapters 2, 3 and 4. Raw data were processed applying three reductions to subtract the effects of gravity that mask the signal. It was reduced by the effect of gravity of the topography, sediment and crust-mantle interface (CMI). Starting by the anomaly "free air" (FA), was thus obtained the Bouguer anomaly (BA) and BA correct for sediment. Then, once calculated the isostatic Moho (CMI), has produced the sediment-corrected-isostatic residual. The fields processed are gravity gz (in milli Gal, mGal) and gradient tzz (measured in Eötvös, E). It has been used the resolutions of 0.5 ° and 0.05 °, computed at an altitude of 4000 m a.s.l., higher of mountains in the area. After mng cases with simple geometry (ch. 6) we moved to the modeling of three real case histories. The three sites chosen for the study are: Tindouf (Algeria), Taoudenni (Mali), Timbuktu (Mali). In the basin of Tindouf a CAMP doleritic sill is attached to its likely source source-dyke evident by gravimetry that identifies well a nearby mine of Iron. In the Taoudenni basin, the two main anomalies suggest the presence of magmatic cumulites a dozen kilometers thick and connected with the surface through oblique dikes. The site at Timbuktu is discussed in detail because in the nearby lake Faguibine was revealed a magmatic intrusion long ca. 250 km. On the surface there is evidence of magmatism (e.g. Fumaroles) such that worry local populations (El Abbass et al., 1993) .Among the unexpected results, please note the strong signal generated by gravimetric peridotites in Morocco and a major anomaly (80 mGal) in the Grand Erg Occidental (Algeria) below the Sahara that would seem to be caused by a dense body ca. 600 km long.
XXVI Ciclo
1972
Книги з теми "Dati A Terra"
Cantone, Francesca. La "donna-fiore" nel santuario di Hera alla foce del Sele: Un progetto per l'informatizzazione dei dati. Napoli: Naus editoria, 2016.
Знайти повний текст джерелаM, Mather Paul, Remote Sensing Society, British Aerospace (Firm), and Natural Environment Research Council (Great Britain), eds. TERRA-2: Understanding the terrestrial environment : remote sensing data systems and networks. Chichester: Wiley, 1995.
Знайти повний текст джерелаUnited States. National Aeronautics and Space Administration, ed. EOSDIS Terra Data Sampler #1, Version 1, Western U.S. Wildfires 2000, (CD-ROM). [S.l: s.n., 2001.
Знайти повний текст джерелаWalker, J. Douglas. The geoscience handbook: AGI data sheets. 4th ed. Alexandria, Va: American Geological Institute, 2009.
Знайти повний текст джерелаUnited States. National Aeronautics and Space Administration, ed. Terra MODIS Oceans Data, etc., Vol. 2, Disk 1-2, Issued Janauary 2003, (CD-ROM). [S.l: s.n., 2003.
Знайти повний текст джерелаNT Writers' Festival (Darwin, N.T.). Terra: A bilingual anthology from WordStorm, the NT Writers' Festival = Antologi dwi bahasa dari WordStorm, Festival Sastra Northern Territory, Australia. Darwin: NT Writers' Centre, 2007.
Знайти повний текст джерелаDivision, Newfoundland Water Resources, and Canada. Inland Waters Directorate. Atlantic Region. Water Quality Branch., eds. Water quality data: Newfoundland, 1981-1985 = Données sur la qualité des eaux : Terre-Neuve, 1981-1985. St. Johnʼs, Newfoundland: Dept. of Environment, Water Resources Division, 1988.
Знайти повний текст джерелаinterviewer, De Vries Walter, Bass Jack interviewer, Southern Oral History Program, University of North Carolina at Chapel Hill. Documenting the American South (Project), and University of North Carolina at Chapel Hill. Library, eds. Oral history interview with Terry Sanford, date unknown: Interview A-0140, Southern Oral History Program Collection (#4007). [Chapel Hill, N.C.]: University Library, UNC-Chapel Hill, 2006.
Знайти повний текст джерелаauthor, Kostelecký Jan, Cílek Václav author, and Bezděk Aleš author, eds. Subglacial and underground structures detected from recent gravito-topography data. Newcastle upon Tyne, UK: Cambridge Scholars Publisher, 2020.
Знайти повний текст джерелаBartoli, Maria Teresa, and Monica Lusoli, eds. Le teorie, le tecniche, i repertori figurativi nella prospettiva d'architettura tra il '400 e il '700. Florence: Firenze University Press, 2015. http://dx.doi.org/10.36253/978-88-6655-884-2.
Повний текст джерелаЧастини книг з теми "Dati A Terra"
Fridlyand, Jane. "Microarray Data Analysis." In Selected Works of Terry Speed, 585–642. New York, NY: Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4614-1347-9_15.
Повний текст джерелаHaynes, David, Suprio Ray, and Steven Manson. "Terra Populus: Challenges and Opportunities with Heterogeneous Big Spatial Data." In Advances in Geocomputation, 115–21. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-22786-3_11.
Повний текст джерелаDunlop, John, Demessie Girma, and James Irvine. "The Data Link Layer." In Digital Mobile Communications and the Tetra System, 259–332. West Sussex, England: John Wiley & Sons, Ltd., 2013. http://dx.doi.org/10.1002/9781118832585.ch7.
Повний текст джерелаKang, U., and Christos Faloutsos. "Mining Tera-Scale Graphs with “Pegasus”: Algorithms and Discoveries." In Large-Scale Data Analytics, 75–99. New York, NY: Springer New York, 2013. http://dx.doi.org/10.1007/978-1-4614-9242-9_3.
Повний текст джерелаPardasani, R. T., and P. Pardasani. "Paramagnetic Curie constant of tetra-μ-squaratooctaaquapyrazinetetramanganese(II)." In Magnetic Properties of Paramagnetic Compounds, Magnetic Susceptibility Data, Volume 1, 857–59. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-62478-4_350.
Повний текст джерелаJohnsen, Klaus-Peter. "NWP Model Specific Humidities Compared with CHAMP/GPS and TERRA/MODIS Data." In First CHAMP Mission Results for Gravity, Magnetic and Atmospheric Studies, 473–78. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-540-38366-6_64.
Повний текст джерелаMachiraju, Raghu, James E. Fowler, David Thompson, Bharat Soni, and Will Schroeder. "EVITA — Efficient Visualization and Interrogation of Tera-Scale Data." In Data Mining for Scientific and Engineering Applications, 257–79. Boston, MA: Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-1733-7_15.
Повний текст джерелаPardasani, R. T., and P. Pardasani. "Molar magnetic moment of µ-pyromellitato-tetra[diaminoethane]diiron(II)." In Magnetic Properties of Paramagnetic Compounds, Magnetic Susceptibility Data, Volume 2, 57–58. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-62466-1_19.
Повний текст джерелаRemedios, John J., and Nigel A. D. Richards. "Retrieval of CO Column and Profile Data from the MOPITT Instrument on EOS-TERRA." In Sounding the Troposphere from Space, 125–36. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18875-6_16.
Повний текст джерелаPardasani, R. T., and P. Pardasani. "Molar magnetic moment of µ-pyromellitato-tetra[1,3-diaminopropane]diiron(II)." In Magnetic Properties of Paramagnetic Compounds, Magnetic Susceptibility Data, Volume 2, 59–60. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-62466-1_20.
Повний текст джерелаТези доповідей конференцій з теми "Dati A Terra"
Mantovani, Valentina, and Roby Stuani. "Terra sigillata decorata a matrice di media età imperiale da Verona: nuovi dati sulle produzioni Nord-Italiche." In 31st Congress of the Rei Cretariae Romanae Fautores, Cluj-Napoca, Romania. Archaeopress Archaeology, 2020. http://dx.doi.org/10.32028/9781789697483-17.
Повний текст джерелаBallarin, Matteo, and Nadia D'Agnone. "Paesaggio, suolo, tempo: la rappresentazione dei tempi geologici nella citta' di Catania." In International Conference Virtual City and Territory. Roma: Centre de Política de Sòl i Valoracions, 2014. http://dx.doi.org/10.5821/ctv.8041.
Повний текст джерелаBarkstrom, Bruce R., Bruce A. Wielicki, G. Louis Smith, Robert B. Lee III, Kory J. Priestley, Thomas P. Charlock, and David P. Kratz. "Validation of CERES/TERRA data." In Europto Remote Sensing, edited by Hiroyuki Fujisada, Joan B. Lurie, Alexander Ropertz, and Konradin Weber. SPIE, 2001. http://dx.doi.org/10.1117/12.417139.
Повний текст джерелаBurnette, Maxwell, Rob Kooper, J. D. Maloney, Gareth S. Rohde, Jeffrey A. Terstriep, Craig Willis, Noah Fahlgren, et al. "TERRA-REF Data Processing Infrastructure." In PEARC '18: Practice and Experience in Advanced Research Computing. New York, NY, USA: ACM, 2018. http://dx.doi.org/10.1145/3219104.3219152.
Повний текст джерелаChu, Xu, Yeye He, Kaushik Chakrabarti, and Kris Ganjam. "TEGRA." In SIGMOD/PODS'15: International Conference on Management of Data. New York, NY, USA: ACM, 2015. http://dx.doi.org/10.1145/2723372.2723725.
Повний текст джерелаRuggles, Steven, Tracy A. Kugler, Catherine A. Fitch, and David C. Van Riper. "Terra Populus: Integrated Data on Population and Environment." In 2015 IEEE International Conference on Data Mining Workshop (ICDMW). IEEE, 2015. http://dx.doi.org/10.1109/icdmw.2015.204.
Повний текст джерелаWald, Andrew, Jake Brinkmann, Aisheng Wu, and Jack Xiong. "Estimating terra MODIS polarization effect using ocean data." In SPIE Defense + Security, edited by Weilin W. Hou and Robert A. Arnone. SPIE, 2016. http://dx.doi.org/10.1117/12.2222585.
Повний текст джерелаDespini, Francesca, Sergio Teggi, Lorenza Bovio, and Francesco Immordino. "Applications of Terra MODIS data for Iraq marshland monitoring." In SPIE Europe Remote Sensing, edited by Ulrich Michel and Daniel L. Civco. SPIE, 2009. http://dx.doi.org/10.1117/12.830065.
Повний текст джерелаMasahiro Seguchi, Masumi Koriyama, and Yonghee Shin. "Measurement of LAI in the Watershed Using Terra-ASTER Data." In 2009 Reno, Nevada, June 21 - June 24, 2009. St. Joseph, MI: American Society of Agricultural and Biological Engineers, 2009. http://dx.doi.org/10.13031/2013.27151.
Повний текст джерелаWolfe, Robert E., and Hampapuram K. Ramapriyan. "Scaling the pipe: NASA EOS Terra data systems at 10." In IGARSS 2010 - 2010 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2010. http://dx.doi.org/10.1109/igarss.2010.5652069.
Повний текст джерелаЗвіти організацій з теми "Dati A Terra"
Smidt, Mathew, Jason Thompson, Tim McDonald, and Yuting Ma. Terra-mechanical and statistical analyses of four-wheel grapple skidder performance data. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station, 2023. http://dx.doi.org/10.2737/srs-rp-66.
Повний текст джерелаBrodaric, B. Groundwater Information Network: GIN. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/329087.
Повний текст джерелаTerra Nova sediment data compilation, Petro-Canada 1997 geotechnical investigations. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210731.
Повний текст джерелаSimulated monthly hydrologic data and estimated flood characteristics for Cherry Creek at a proposed reservoir site near Terry, Montana. US Geological Survey, 1995. http://dx.doi.org/10.3133/wri944230.
Повний текст джерела