Relevant bibliographies by topics / Temperature measurents

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Temperature measurents'

Author: Grafiati
Published: 30 June 2021
Last updated: 7 February 2022

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Journal articles on the topic "Temperature measurents"

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Yuanqin Xia, Yuanqin Xia, Yang Zhao Yang Zhao, Tiantian Zhang Tiantian Zhang, Ping He Ping He, Rongwei Fan Rongwei Fan, Zhiwei Dong Zhiwei Dong, Deying Chen Deying Chen, and Zhonghua Zhang Zhonghua Zhang. "Measurements of flame temperature by femtosecond CARS." Chinese Optics Letters 10, s1 (2012): S13002–313003. http://dx.doi.org/10.3788/col201210.s13002.

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Görsdorf, Ulrich. "Über die Genauigkeit von Temperaturmessungen mit RASS." Meteorologische Zeitschrift 7, no. 5 (November 2, 1998): 241–47. http://dx.doi.org/10.1127/metz/7/1998/241.

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Shuang Chen, Shuang Chen, Tie Su Tie Su, Furong Yang Furong Yang, Long Zhang Long Zhang, and Yaobang Zheng Yaobang Zheng. "Calibration method for 2D instantaneous OH-PLIF temperature measurements in flame." Chinese Optics Letters 11, no. 5 (2013): 053001–53004. http://dx.doi.org/10.3788/col201311.053001.

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Barth, Manuela, Gabi Fischer, Armin Raabe, Astrid Ziemann, and Frank Weiße. "Remote sensing of temperature and wind using acoustic travel-time measurements." Meteorologische Zeitschrift 22, no. 2 (April 1, 2013): 103–9. http://dx.doi.org/10.1127/0941-2948/2013/0385.

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Lipka, Tomasz. "Badania temperaturowe gazomierzy – metody chłodzenia strumienia gazu." Nafta-Gaz 74, no. 2 (February 2018): 106–12. http://dx.doi.org/10.18668/ng.2018.02.04.

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Harris, Stuart A., and John H. Pedersen. "Comparison of three methods of calculating air temperature from electronic measurements." Zeitschrift für Geomorphologie 39, no. 2 (June 29, 1995): 203–10. http://dx.doi.org/10.1127/zfg/39/1995/203.

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Hernández, Eduardo, Joel Recalde, and Andrés Guananga. "INFLUENCIA DE LA VELOCIDAD DEL VIENTO EN LAS MEDIDAS DE TEMPERATURA MEDIANTE TERMOGRAFÍA INFRARROJA." Revista de Investigación Talentos 7, no. 1 (June 30, 2020): 12–21. http://dx.doi.org/10.33789/talentos.7.1.119.

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Fuchang Chen, Fuchang Chen, Jiacheng Hu Jiacheng Hu, Chengtao Zhang Chengtao Zhang, and Zunqi Lin Zunqi Lin. "Dual-source distributed optical fiber sensor for simultaneous temperature and strain measurements." Chinese Optics Letters 10, no. 6 (2012): 060601–60603. http://dx.doi.org/10.3788/col201210.060601.

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Wells, M. R., and L. A. Melton. "Temperature Measurements of Falling Droplets." Journal of Heat Transfer 112, no. 4 (November 1, 1990): 1008–13. http://dx.doi.org/10.1115/1.2910472.

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The temperature of 225-μm-dia decane droplets, which have fallen 100 mm through a hot quiescent, oxygen-free environment, has been measured using exciplex fluorescence thermometry. The droplets were doped with pyrene, and the relative intensities of pyrene monomer and excimer emissions were used to determine the droplet temperatures. The droplet temperature increases approximately 0.4°C per °C increase in the ambient temperature up to an ambient temperature of 200°C. Less than 10 percent evaporation was observed for the droplets at the highest ambient temperatures.
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Raupp-Pereira, F., M. J. Ribeiro, A. M. Segadães, and J. A. Labrincha. "Fraguado de cementos basados en residuos estimado por espectroscopia de impedancia y medidas en temperatura." Boletín de la Sociedad Española de Cerámica y Vidrio 46, no. 2 (April 30, 2007): 91–96. http://dx.doi.org/10.3989/cyv.2007.v46.i2.255.

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Dissertations / Theses on the topic "Temperature measurents"

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Jacobi, Christoph, and Dierk Kürschner. "Mesopause region temperatures and plasma scale height estimations from VHF meteor radar and LF absolute reflection height measurements at Collm." Universitätsbibliothek Leipzig, 2017. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-219583.

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The change of ionospheric absolute reflection heights h of low-frequency (LF) radio waves at oblique incidence in the course of the day is measured at Collm Observatory (51.3°N, 13.0°E) using 1.8 kHz sideband phase comparisons between the sky-wave and the ground wave of a commercial 177 kHz transmitter (Zehlendorf, reflection point 52.1°N, 13.2°E). Plasma scale height estimates H are calculated from the decrease/increase of h in the morning/evening. The day-to-day variations of H are compared with those of daily mean temperatures at 90 km, measured with a VHF meteor radar (36.2 MHz) at Collm utilising the amplitude decay of meteor reflections. A good qualitative correspondence is found between the two data sets. Since mesospheric long-period temperature variations are generally accepted to be the signature of atmospheric planetary waves, this shows that LF reflection height measurements can be used for monitoring the dynamics of the upper middle atmosphere.
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Wolf, Kevin, André Ehrlich, and Manfred Wendisch. "Temperature profiles from airborne pyrgeometer measurements of broadband terrestrial radiation." Universität Leipzig, 2016. https://ul.qucosa.de/id/qucosa%3A16702.

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Profiles of broadband terrestrial radiation from airborne pyrgeometer measurements aboard research aircraft Polar 5 obtained during the VERDI campaign in 2012 were used to derive vertical temperature profiles. The retrievals were performed utilizing radiative transfer simulations by libRadtran (Mayer and Kylling, 2005). Manually changing the temperature of the input file for the simulations resulting calculated profiles of terrestrial irradiance were compared with measured profiles and iterated until best agreement. The selected test case shows the possibility of this technique and reveals several possible improvements. The algorithm has to be optimized to adapt the modelling temperature profile automatically using least-square error minimization between measured and modelled irradiance profiles. Additionally the vertical resolution has to be increased to consider small-scale variations. Using humidity and pressure profiles from ground-based observations and nearby radiosoundings significantly improves the retrieved temperature profiles.
Vertikalprofile der breitbandigen terrestrischen Strahlung von flugzeuggetragenen Pyrgeometermessungen an Bord des Forschungsflugzeuges Polar 5 während der VERDI Kampagne in 2012 wurden genutzt, um Vertikalprofile der Temperatur abzuleiten. Das Retrieval erfolgte mit Hilfe von Strahlungstransfersimulationen unter der Verwendungung von libRadtran (Mayer and Kylling, 2005). Dazu wurde die Temperatur der Modellatmosphäre variert, bis eine bestmögliche Übereinstimmung von gemessenem und modellierten Irradianzprofil erzielt wurde. Der ausgesuchte Testfall zeigt das Potential dieser Technik und mögliche Verbessungsansätze. So muss der verwendete Algorithmus automatisiert werden, indem das modellierte Strahlungsprofil mit Hilfe eines Iterationsverfahrens und der Methode der kleinsten Fehlerquadrate an das gemessene Profil angepasst wird. Zusätzlich ist eine Erhöhung der vertikalen Auflösung von 50 m auf 10 m Schritte nötig, um kleinskalige Fluktuationen zu berücksichtigen. Die Verwendung von bodengebundenen Beobachtungen und nahegelegenen Radiosondenaufstiegen in der Modellatmosphäre führt zu einer weiteren signifikanten Verbesserung der abgeleiteten Temperaturprofile.
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Samtleben, Nadja, and Christoph Jacobi. "Long-period oscillations derived from mesosphere/lower thermosphere meteor radar temperature measurements." Universität Leipzig, 2015. https://ul.qucosa.de/id/qucosa%3A16649.

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Using measurements, derived from a meteor radar in Collm (51.3°N, 13°E), the mesopause region is analyzed with respect to the temperature distribution at an altitude of 90 km over a period of 10 years. The analyzed period lasts from 2005 till 2013. Based on these measurements, the typical temperature seasonal cycle of the mesopause region can be observed. The temperature reaches its minimum of about 130 K in summer and its maximum of about 220 K in winter. At this altitude, also strong day-today- fluctuations of up to 35 K exist, which are probably partly induced by planetary waves. Shorter-period oscillations with a period between 2 and 6 days have maximum amplitudes during summer, while longer-period oscillations with a period between 7 and 20 days maximize during winter. During the measurement period the amplitudes of oscillations with periods between 4 and 6 days, which may be attributed to the quasi-5-day-wave, increase with time.
Auf der Grundlage von Messungen eines Meteorradars in Collm (51.3°N, 13°E), die in einer Höhe von 90 km erfolgten, was in etwa der Mesopause entspricht, wird die Temperatur hinsichtlich ihres Jahresganges und insbesondere ihrer Variationen in einem Messzeitraum von 10 Jahren analysiert. Der analysierte Zeitraum erstreckt sich von 2005 bis 2013. Anhand der Daten kann man den typischen Jahresgang der Temperatur in der Mesopausenregion erkennen. Die Temperatur erreicht im Sommer das Minimum bei etwa 130 K und im Winter das Maximum bei etwa 220 K. Zudem treten starke Tag-zu-Tag-Fluktuationen auf, die im Maximum 35 K betragen. Diese werden vermutlich durch planetare Wellenaktivität der Atmosphäre hervorgerufen. Hierbei spielen im Sommer die kurzwelligen und im Winter die langwelligen Oszillationen, letztere mit Perioden größer 7 Tage, die wesentliche Rolle. Ferner sind innerhalb des Messzeitraums zunehmende Amplituden von Oszillationen mit Perioden zwischen 4 und 6 Tagen (quasi 5-Tage-Welle) zu erkennen.
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Jorge, Alfredo. "Medidas elétricas no policarbonato durolon e o metododa temperatura oscilante." Universidade de São Paulo, 1991. http://www.teses.usp.br/teses/disponiveis/54/54132/tde-21072009-174821/.

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Nesta tese procuramos caracterizar o Policarbonato Bisfenol-A, Durolon® sob o ponto de vista elétrico, separando a reação dipolar e os processos de condução. Apesar de preparadas de forma análoga, as amostras (≅ 30μm de espessura) mostraram comportamento pouco reprodutível, principalmente da componente condutiva. Várias anomalias foram detectadas embora não estudadas em detalhe pela pobre reprodutibilidade já mencionada. Além das técnicas usuais de polarização e despolarização isotérmicas, despolarização termoestimulada e de polarização termoestimulada, empregou-se pela primeira vez, em medidas desta natureza, a técnica de oscilação senoidal da temperatura, estando o campo elétrico aplicado. Media-se a corrente daí decorrente, procurando-se trabalhar sempre com uma mesma amostra. Na região de 50°C a 70°C, diferenças de fase superiores a 90° foram encontradas (o sinal de corrente atrasado em relação ao de temperatura). Uma análise simples destes resultados indica que, neste caso, tanto a condutividade como a suscetibilidade diminuem com o crescimento da temperatura (dX/dT≅ -1x10-3/°C). Medidas de polarização termoestimulada, também, mostram uma inversão da corrente em relação ao campo aplicado desde cerca da temperatura ambiente ate ≅ 90°C. Um estudo sistemático da condução a 120°C indica que portadores são emitidos do eletródio, e que o trânsito dos mesmos é rápido (menor do que o tempo em que a polarização se estabelece, ≅ 2 min). Tensões e correntes espontâneas foram detectadas mesmo em amostras providas de eletródios de mesmo metal (uma correlação com a ordem empregada na metalização foi suspeitada, seguindo observação anteriormente feita pelo Prof. B. Gross). Algumas medidas com eletródios Al-Al, Al-Au e Au-Au foram feitas. Finalmente, sugestões para trabalhos futuros são feitas.
In this work the electrical characterization of the Polycarbonate Bisphenol-A, Durolon ® was attempted, trying to separate the dipole and the conduction processes. However, poor reproducibility, mainly in the conductivity, was achieved even for samples (≅ 30μm thick usually) taken from the same batch. Anomalies were detected but not studied in detail owing the poor reproducibility referred above. Beside the usual techniques like the isothermal polarization and depolarization in short-circuit, thermally depolarization currents and thermally stimulated polarization, in a new one, employed by the first time for the study of transport and polarization, the temperature was oscillated and the ensuing current oscillation was monitored. Large phase shifts (the current lagging the temperature oscillation), even greater ≅ 90° were found in the range 50°C 70°C. A simple analysis indicates that in this case both the conductivity as well as the susceptibility are decreased for increasing temperature (dX/dT≅ -1x10-3/°C). Accordingly thermally stimulated polarization shows a current reversal with respect to the electric field from room temperature to ≅ 90°C. A systematic study of the conduction process at 120°C was carried out, the analysis of which indicates that carriers are emitted from the electrode, whose transit across the sample is shorter than the duration of the polarization current (≅ 2 min). Spontaneous tensions and currents were detected even for samples provisioned with similar electrodes (a correlation with the actual sequence of metallization, following a suggestion by Prof. B. Gross, was surmised). A few measurements with Al-Al, Al-Au and Au-Au electrodes were carried out. Finally suggestions for future work are given.
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Dugay, Murielle Boetcher Sandra Kathleen Sparr. "Errors in skin temperature measurements." [Denton, Tex.] : University of North Texas, 2008. http://digital.library.unt.edu/permalink/meta-dc-9786.

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Dugay, Murielle. "Errors in skin temperature measurements." Thesis, University of North Texas, 2008. https://digital.library.unt.edu/ark:/67531/metadc9786/.

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Numerical simulation is used to investigate the accuracy of a direct-contact device for measuring skin-surface temperature. A variation of thermal conductivity of the foam has greater effect on the error rather than a variation of the blood perfusion rate. For a thermal conductivity of zero, an error of 1.5 oC in temperature was identified. For foam pad conductivities of 0.03 and 0.06 W/m-oC, the errors are 0.5 and 0.15 oC. For the transient study, with k=0 W/m-oC, it takes 4,900 seconds for the temperature to reach steady state compared with k=0.03 W/m-oC and k=0.06 W/m-oC where it takes 3,000 seconds. The configuration without the foam and in presence of an air gap between the skin surface and the sensor gives the most uniform temperature profile.
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Stolle, Claudia, Martin Lange, and Christoph Jacobi. "Validation of atmospheric temperature profiles and electron densities derived from CHAMP radio occultation measurements during measurement campaigns at Andøya (69.28°N, 16.02°E)." Universitätsbibliothek Leipzig, 2017. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-217064.

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Several measurement campaigns took place at the ALOMAR observatory at Andøya, Northern Norway during July-November 2001 to validate ionospheric electron density and dry temperature profiles in the troposphere and lower stratosphere derived from radio occultation measurements of the low earth orbiter satellite CHAMP. For temperature sounding, three balloons are released around GPS satellite occultation events that occurred inbetween a distance of 200 km around Andøya. At altitudes of 7–20 km the CHAMP profile shows a positive mean deviation increasing with height by about 1.5-2 Kelvin/ 10 km overlayed with variations of ±1 K when compared to the radiosonde. Taking into account the previous and following radiosonde ascents the mean deviation seems to be of systematic nature due to the occultation principle or the retrieval algorithm and the variations are related to geographical variations of temperature and to the horizontal averaging by the radio occultation technique. During the period from mid July to mid August, four occultations for ionospheric soundings occurred. The values of the F2 layer calculated from the CHAMP derived electron density profiles are compared to the readings of the Alomar and Tromsø ionosondes for these times. Comparison shows that using the radio occultation technique electron densities of the maximum value layer are calculated inbetween the same order of magnitude as the ionosondes measurements, however, they overestimate it in the cases discussed here
Zur Validierung von Elekronendichte- und Temperaturprofilen, abgeleitet aus Radiookkultationsmessungen von CHAMP wurden im Juli-November 2001 mehrere Messkampagnen am ALOMAR Institut auf Andøya, Nordnorwegen durchgeführt. Zur Temperatursondierung wurden drei aufeinanderfolgende Radiosonden um den Zeitpunkt von Okkultationsereignissen im Umkreis von weniger als 200 km gestartet. Das hier diskutierte Temperaturprofil von CHAMP zeigt im Höhenbereich 7-20 km eine mit der Höhe zunehmende positive Abweichung von ca. 1,5-2 K/10 km mit Variationen um ±1 K verglichen mit dem Temperaturprofil der zum Okkultationszeitpunkt fliegenden Radiosonde. Der Vergleich mit den vorhergehenden und nachfolgenden Sondierungen lässt darauf schließen, dass die mittlere Abweichung durch systematische Fehler des Okkultationsverfahrens oder den Retrieval-Algorithmus bedingt sind, die Variationen jedoch durch die örtliche Abweichung und die horizontale Mittelung des Messverfahrens. Während des Zeitraumes von Mitte Juli bis Mitte August ereigneten sich vier Okkultationen zur Sondierung der Ionosphäre. Von den abgeleiteten Elektronendichteprofilen werden jeweils die Werte der F2-Schicht mit den zur gleichen Zeit gemessenen Elektronendichten der Ionosonden auf Andøya und bei Tromsø verglichen. Der Vergleich zeigt, dass mit Hilfe der Radiookkultaktionstechnik die Elektronendichtewerte der F2-Schicht in der gleichen Größenordnung berechnet, in diesen konkreten Fällen jedoch überschätzt werden
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Jacobi, Christoph, and Dierk Kürschner. "Mesopause region temperatures and plasma scale height estimations from VHF meteor radar and LF absolute reflection height measurements at Collm." Meteorologische Arbeiten aus Leipzig … und Jahresbericht … des Instituts für Meteorologie der Universität Leipzig ; 11 (2006), S. 1-10, 2006. https://ul.qucosa.de/id/qucosa%3A15363.

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The change of ionospheric absolute reflection heights h of low-frequency (LF) radio waves at oblique incidence in the course of the day is measured at Collm Observatory (51.3°N, 13.0°E) using 1.8 kHz sideband phase comparisons between the sky-wave and the ground wave of a commercial 177 kHz transmitter (Zehlendorf, reflection point 52.1°N, 13.2°E). Plasma scale height estimates H are calculated from the decrease/increase of h in the morning/evening. The day-to-day variations of H are compared with those of daily mean temperatures at 90 km, measured with a VHF meteor radar (36.2 MHz) at Collm utilising the amplitude decay of meteor reflections. A good qualitative correspondence is found between the two data sets. Since mesospheric long-period temperature variations are generally accepted to be the signature of atmospheric planetary waves, this shows that LF reflection height measurements can be used for monitoring the dynamics of the upper middle atmosphere.
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Blyth, William. "Temperature measurements of optically ionised plasmas." Thesis, University of Oxford, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.386826.

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Hopper, Richard. "Accurate temperature measurements on semiconductor devices." Thesis, De Montfort University, 2010. http://hdl.handle.net/2086/3315.

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Self-heating can have a detrimental effect on the performance and reliability of high power microwave devices. In this work, the thermal performance of the gallium arsenide (GaAs) Gunn diode was studied. Infrared (IR) thermal microscopy was used to measure the peak operating temperature of the graded-gap structured device. Temperature measurements were experimentally validated using micro-thermocouple probing and compared to values obtained from a standard 1D thermal resistance model. Thermal analysis of the conventionally structured Gunn diode was also undertaken using high resolution micro-Raman temperature profiling, IR thermal microscopy and electro/thermal finite element modeling. The accuracy of conventional IR temperature measurements, made on semiconductor devices, was investigated in detail. Significant temperature errors were shown to occur in IR temperature measurements made on IR transparent semiconductors layers and low emissivity/highly reflective metals. A new technique, employing spherical carbon microparticles, was developed to improve the measurement accuracy on such surfaces. The new ‘IR microparticle’ technique can be used with existing IR microscopes and potentially removes the need to coat a device with a high emissivity layer, which causes damage and heat spreading.
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Books on the topic "Temperature measurents"

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service), ScienceDirect (Online, ed. Radiometric temperature measurements: Applications. Amsterdam: Elsevier/Academic Press, 2010.

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R, White D., ed. Traceable temperatures: An introduction to temperature measurement and calibration. Chichester [England]: Wiley, 1994.

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Nicholas, J. V. Traceable temperatures: An introduction to temperature measurement and calibration. 2nd ed. Chichester: Wiley, 2001.

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1961-, Streluk Angella, ed. Temperature. Oxford: Heinemann Library, 2008.

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Rand, Casey. Temperature. Chicago, Ill: Heinemann Library, 2011.

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Angella, Streluk, ed. Temperature. Oxford: Heinemann Library, 2003.

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Rand, Casey. Temperature. Chicago, Ill: Heinemann Library, 2010.

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K, Eckersdorf, and McGhee J, eds. Temperature Measurement. Chichester, West Sussex, England: J. Wiley, 1991.

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Hiroyuki, Fukuyama, Hasegawa M, Inoue A, Kobayashi N, Sakurai T, Waseda Yoshio, Wille L, and SpringerLink (Online service), eds. High-Temperature Measurements of Materials. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009.

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Randa, J. Noise temperature measurements on wafer. Boulder, Colo: U.S. Dept. of Commerce, Technology Administration, National Institute of Standards and Technology, 1997.

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Book chapters on the topic "Temperature measurents"

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Polak, T. A., and C. Pande. "Temperature Measurement." In Engineering Measurements, 53–69. Chichester, UK: John Wiley & Sons, Ltd, 2014. http://dx.doi.org/10.1002/9781118903148.ch5.

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Venkateshan, S. P. "Measurements of Temperature." In Mechanical Measurements, 103–82. Chichester, UK: John Wiley & Sons, Ltd, 2015. http://dx.doi.org/10.1002/9781119115571.ch4.

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Venkateshan, S. P. "Measurements of Temperature." In Mechanical Measurements, 109–96. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-73620-0_4.

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Plessers, Ir J. "Temperature Measurements." In Measurement and Control in Liquid Metal Processing, 3–9. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3599-0_1.

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Yates, John T. "Temperature Measurements." In Experimental Innovations in Surface Science, 405–17. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-17668-0_36.

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Pearce, John A., Jonathan W. Valvano, and Stanislav Emelianov. "Temperature Measurements." In Optical-Thermal Response of Laser-Irradiated Tissue, 399–453. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-8831-4_11.

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Valvano, Jonathan W., and John Pearce. "Temperature Measurements." In Optical-Thermal Response of Laser-Irradiated Tissue, 489–534. Boston, MA: Springer US, 1995. http://dx.doi.org/10.1007/978-1-4757-6092-7_15.

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Kemper, Clarence A., and Göran S. Bringert. "Temperature Measurements." In Handbook of Validation in Pharmaceutical Processes, 159–78. 4th ed. Boca Raton: CRC Press, 2021. http://dx.doi.org/10.1201/9781003163138-9.

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Venkateshan, S. P. "Stagnation and Bulk Mean Temperature." In Mechanical Measurements, 343–56. Chichester, UK: John Wiley & Sons, Ltd, 2015. http://dx.doi.org/10.1002/9781119115571.ch10.

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Venkateshan, S. P. "Systematic Errors in Temperature Measurement." In Mechanical Measurements, 183–203. Chichester, UK: John Wiley & Sons, Ltd, 2015. http://dx.doi.org/10.1002/9781119115571.ch5.

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Conference papers on the topic "Temperature measurents"

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Gatti, Flavio. "Direct measurements of neutrino mass." In LOW TEMPERATURE DETECTORS: Ninth International Workshop on Low Temperature Detectors. American Institute of Physics, 2002. http://dx.doi.org/10.1063/1.1457679.

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Lin, Y. H., T. C. Lee, J. J. Lin, H. M. Chang, and Y. S. Huang. "Electrical Measurements on Iridium Dioxide Nanorods." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2355264.

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Blumberg, G., A. Mialitsin, B. S. Dennis, and J. Karpinski. "Superconductivity in MgB2: Magneto-Raman Measurements." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2354846.

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Bourgeois, O., F. Ong, S. E. Skipetrov, and J. Chaussy. "Specific Heat Measurements of Mesoscopic Loops." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2354916.

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Tahar, Mohammed Z., and George O. Zimmerman. "Automated Magnetic Susceptibility Measurements Using a Microcontroller." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2355344.

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Ishiguro, Ryosuke, and Sébastien Balibar. "New Measurements of Wetting by Helium Mixtures." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2354641.

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Wu, Fan, Leif Roschier, Taku Tsuneta, Mikko Paalanen, Taihong Wang, and Pertti Hakonen. "Setup for shot noise measurements in carbon nanotubes." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2355263.

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Yamaguchi, Akira, Hirofumi Nema, Yuichi Tanaka, and Hidehiko Ishimoto. "Magnetization Measurements of 3He Monolayer Film on Graphite." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2354718.

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Sakurai, T., A. Taketani, S. Kimura, M. Yoshida, S. Okubo, H. Ohta, H. Tanaka, and Y. Uwatoko. "ESR Measurements of KCuCl3 under Multi Extreme Conditions." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2355067.

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Bunkov, Yu M., J. Elbs, H. Godfrin, and C. B. Winkelmann. "Ultra Low Temperature Instrumentation for Measurements in Astrophysics : ULTIMA." In LOW TEMPERATURE PHYSICS: 24th International Conference on Low Temperature Physics - LT24. AIP, 2006. http://dx.doi.org/10.1063/1.2355329.

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Reports on the topic "Temperature measurents"

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Auerbach, D. W., D. N. Hill, and H. S. McLean. Ion Temperature Measurements in SSPX. Office of Scientific and Technical Information (OSTI), August 2001. http://dx.doi.org/10.2172/15013407.

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Williams, Theodore F., Marlin D. Vangsness, James R. Shardo, and Jamie S. Ervin. Refueling Tanker Truck Temperature Measurements. Fort Belvoir, VA: Defense Technical Information Center, February 2005. http://dx.doi.org/10.21236/ada435147.

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Goodrich, L. F., and T. C. Stauffer. Variable-Temperature Critical-Current Measurements. Office of Scientific and Technical Information (OSTI), May 2009. http://dx.doi.org/10.2172/952565.

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Randa, James. Noise temperature measurements on wafer. Gaithersburg, MD: National Bureau of Standards, 1997. http://dx.doi.org/10.6028/nist.tn.1390.

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Holmes, N. C., M. Ross, and W. J. Nellis. Temperature measurements of shock-compressed deuterium. Office of Scientific and Technical Information (OSTI), November 1994. http://dx.doi.org/10.2172/90225.

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Ludington, A., D. Hill, H. McLean, J. Moller, and R. Wood. Time-resolved Temperature Measurements in SSPX. Office of Scientific and Technical Information (OSTI), August 2006. http://dx.doi.org/10.2172/892077.

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Randa, James. Uncertainties in NIST noises-temperature measurements. Gaithersburg, MD: National Bureau of Standards, 1998. http://dx.doi.org/10.6028/nist.tn.1502.

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J. L. Rempe, K. G. Condie, D. L. Knudson, and L. L. Snead. Silicon Carbide Temperature Monitor Measurements at the High Temperature Test Laboratory. Office of Scientific and Technical Information (OSTI), January 2010. http://dx.doi.org/10.2172/974782.

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Gauvreau, Jean Luc. Ion temperature measurements in the Maryland Spheromak. Office of Scientific and Technical Information (OSTI), January 1992. http://dx.doi.org/10.2172/10140798.

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Dolan, Daniel H.,, Christopher Seagle, and Tommy Ao. Dynamic temperature measurements with embedded optical sensors. Office of Scientific and Technical Information (OSTI), October 2013. http://dx.doi.org/10.2172/1096517.

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