Academic literature on the topic 'Observations MOZAIC'

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Journal articles on the topic "Observations MOZAIC"

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Staufer, J., J. Staehelin, R. Stübi, T. Peter, F. Tummon, and V. Thouret. "Trajectory matching of ozonesondes and MOZAIC measurements in the UTLS – Part 1: Method description and application at Payerne, Switzerland." Atmospheric Measurement Techniques 6, no. 12 (2013): 3393–406. http://dx.doi.org/10.5194/amt-6-3393-2013.

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Abstract. With the aim of improving ozonesonde observations in the upper troposphere/lower stratosphere (UTLS), we use three-dimensional forward and backward trajectories, driven by ERA-Interim wind fields to match and compare ozonesonde measurements at Payerne (Switzerland) with observations from the MOZAIC aircraft program from 1994–2009. The uncertainties associated with the sonde–MOZAIC match technique were assessed using "self-matches", i.e. matches of instruments of the same type, such as MOZAIC–MOZAIC. Despite strong vertical gradients of ozone at the tropopause, which render the match
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Staufer, J., J. Staehelin, R. Stübi, T. Peter, F. Tummon, and V. Thouret. "Trajectory matching of ozonesondes and MOZAIC measurements in the UTLS – Part 1: Method description and application at Payerne, Switzerland." Atmospheric Measurement Techniques Discussions 6, no. 4 (2013): 7063–98. http://dx.doi.org/10.5194/amtd-6-7063-2013.

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Abstract. With the aim of improving ozonesonde observations in the upper troposphere/lower stratosphere (UTLS), we use three-dimensional forward and backward trajectories, driven by ERA-Interim wind fields to match and compare ozonesonde measurements at Payerne (Switzerland) with observations from the MOZAIC aircraft program from 1994–2009. The uncertainties associated with the sonde–MOZAIC match technique were assessed using "self-matches", i.e. matches of instruments of the same type, such as MOZAIC–MOZAIC. Despite strong vertical ozone gradients of ozone at the tropopause, which render the
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Staufer, J., J. Staehelin, R. Stübi, T. Peter, F. Tummon, and V. Thouret. "Trajectory matching of ozonesondes and MOZAIC measurements in the UTLS – Part 2: Application to the global ozonesonde network." Atmospheric Measurement Techniques 7, no. 1 (2014): 241–66. http://dx.doi.org/10.5194/amt-7-241-2014.

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Abstract. Both balloon-borne electrochemical ozonesondes and MOZAIC (measurements of ozone, water vapour, carbon monoxide and nitrogen oxides by in-service Airbus aircraft) provide very valuable data sets for ozone studies in the upper troposphere/lower stratosphere (UTLS). Although MOZAIC's highly accurate UV-photometers are regularly inspected and recalibrated annually, recent analyses cast some doubt on the long-term stability of their ozone analysers. To investigate this further, we perform a 16 yr comparison (1994–2009) of UTLS ozone measurements from balloon-borne ozonesondes and MOZAIC.
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de Laat, A. T. J., I. Aben, M. Deeter, et al. "Validation of nine years of MOPITT V5 NIR using MOZAIC/IAGOS measurements: biases and long-term stability." Atmospheric Measurement Techniques 7, no. 11 (2014): 3783–99. http://dx.doi.org/10.5194/amt-7-3783-2014.

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Abstract. Validation results from a comparison between Measurement Of Pollution In The Troposphere (MOPITT) V5 Near InfraRed (NIR) carbon monoxide (CO) total column measurements and Measurement of Ozone and Water Vapour on Airbus in-service Aircraft (MOZAIC)/In-Service Aircraft for a Global Observing System (IAGOS) aircraft measurements are presented. A good agreement is found between MOPITT and MOZAIC/IAGOS measurements, consistent with results from earlier studies using different validation data and despite large variability in MOPITT CO total columns along the spatial footprint of the MOZAI
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5

de Laat, A. T. J., I. Aben, M. Deeter, et al. "Validation of nine-years of MOPITT V5 NIR using MOZAIC/IAGOS measurements: biases and long term stability." Atmospheric Measurement Techniques Discussions 7, no. 6 (2014): 5251–91. http://dx.doi.org/10.5194/amtd-7-5251-2014.

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Abstract. Validation results from a comparison between Measurement Of Pollution In The Troposphere (MOPITT) V5 Near InfraRed (NIR) Carbon Monoxide (CO) total column measurements and Measurement of Ozone and Water Vapour on Airbus in-service Aircraft (MOZAIC)/In-Service Aircraft for a Global Observing System (IAGOS) aircraft measurements are presented. A good agreement is found between MOPITT and MOZAIC/IAGOS measurements, consistent with results from earlier studies using different validation data and despite large variability in MOPITT CO total columns along the spatial footprint of the MOZAI
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6

Saunois, M., L. Emmons, J. F. Lamarque, et al. "Impact of sampling frequency in the analysis of tropospheric ozone observations." Atmospheric Chemistry and Physics Discussions 11, no. 10 (2011): 27107–37. http://dx.doi.org/10.5194/acpd-11-27107-2011.

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Abstract. The measurements of the ozone vertical profiles are valuable for the evaluation of atmospheric chemistry models and contribute to the understanding of the processes controlling the distribution of tropospheric ozone. The longest record of the ozone vertical profiles is provided by ozone sondes, which have a low time resolution with a typical frequency of 12 or 4 profiles a month. Here we discuss and quantify the uncertainty in the analysis of such data sets using high frequency MOZAIC (Measurements of OZone, water vapor, carbon monoxide and nitrogen oxides by in-service AIrbus airCra
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Emmons, L. K., D. P. Edwards, M. N. Deeter, et al. "Measurements of Pollution In The Troposphere (MOPITT) validation through 2006." Atmospheric Chemistry and Physics 9, no. 5 (2009): 1795–803. http://dx.doi.org/10.5194/acp-9-1795-2009.

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Abstract. Comparisons of aircraft measurements of carbon monoxide (CO) to the retrievals of CO using observations from the Measurements of Pollution in The Troposphere (MOPITT) instrument onboard the Terra satellite are presented. Observations made as part of the NASA INTEX-B and NSF MIRAGE field campaigns during March–May 2006 are used to validate the MOPITT CO retrievals, along with routine samples from 2001 through 2006 from NOAA and the MOZAIC measurements from commercial aircraft. A significant positive bias, around 20% for total column CO, in MOPITT CO was found in the comparison to in s
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Richards, N. A. D., Q. Li, K. W. Bowman, et al. "Assimilation of TES CO into a global CTM: first results." Atmospheric Chemistry and Physics Discussions 6, no. 6 (2006): 11727–43. http://dx.doi.org/10.5194/acpd-6-11727-2006.

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Abstract. We present results from the first assimilation of carbon monoxide (CO) observations from the Tropospheric Emission Spectrometer (TES) into a global three-dimensional (3-D) chemistry and transport model (CTM). A sequential sub-optimal Kalman filter assimilation scheme (Khattatov et al., 2000) was applied to assimilate TES CO profiles during November 2004 into the GEOS-Chem global 3-D CTM. The assimilation results were compared with MOPITT and MOZAIC observations. The assimilation significantly improves model simulation of CO in the middle to upper troposphere, where the MOPITT versus
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9

Smit, H. G. J., S. Rohs, P. Neis, et al. "Technical Note: Reanalysis of upper troposphere humidity data from the MOZAIC programme for the period 1994 to 2009." Atmospheric Chemistry and Physics Discussions 14, no. 13 (2014): 18905–42. http://dx.doi.org/10.5194/acpd-14-18905-2014.

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Abstract. In-situ observational data on the relative humidity (RH) in the upper troposphere and lowermost stratosphere (UT/LS), or tropopause region, respectively, collected aboard civil passenger aircraft in the MOZAIC (Measurements of OZone, water vapour, carbon monoxide and nitrogen oxides by in-service AIrbus airCraft) programme were reanalysed for the period 2000 to 2009. Previous analyses of probability distribution functions (PDF) of upper troposphere humidity (UTH) data from MOZAIC observations from year 2000 and later indicated a bias of UTH data towards higher RH values compared to d
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Emmons, L. K., D. P. Edwards, M. N. Deeter, et al. "Measurements of Pollution In The Troposphere (MOPITT) validation through 2006." Atmospheric Chemistry and Physics Discussions 8, no. 5 (2008): 18091–109. http://dx.doi.org/10.5194/acpd-8-18091-2008.

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Abstract. Comparisons of aircraft measurements of carbon monoxide (CO) to the retrievals of CO using observations from the Measurements of Pollution in The Troposphere (MOPITT) instrument onboard the Terra satellite are presented. Observations made as part of the NASA INTEX-B and NSF MIRAGE field campaigns during March–May 2006 are used to validate the MOPITT CO retrievals, along with routine samples from 2001 through 2006 from NOAA and the MOZAIC measurements from commercial aircraft. A significant positive bias, around 20% for total column CO, in MOPITT CO was found in the comparison to in s
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Dissertations / Theses on the topic "Observations MOZAIC"

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Cathala, Marie-Laure. "Assimilation de mesures chimiques d'ozone au niveau de la tropopause dans un modèle de chimie-transport global." Toulouse 3, 2004. http://www.theses.fr/2004TOU30034.

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La région de la tropopause est particulièrement importante du point de vue de la dynamique et de la composition chimique de l'atmosphère car elle est le siège d'échanges entre deux milieux très différents, la troposphère et la stratosphère. De forts gradients verticaux rendent toutefois sa représentation difficile dans les modèles numériques de chimie et de transport. L'objectif de cette thèse est de contraindre les simulations numériques à l'aide d'observations de manière à obtenir une meilleure représentation du champ d'ozone dans cette région, qui puisse servir de base pour des études phéno
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Books on the topic "Observations MOZAIC"

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Stendhal. The Lives of Haydn and Mozart: With Observations on Metastasio, and on the Present State of Music in France and Italy. Adamant Media Corporation, 2001.

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Stendhal. Life of Haydn, in a Series of Letters Written at Vienna: Followed by the Life of Mozart, with Observations on Metastasio, and on the Present State of Music in France and Italy. University of Cambridge ESOL Examinations, 2013.

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Book chapters on the topic "Observations MOZAIC"

1

Tuck, Adrian F. "Initial Survey of Observations." In Atmospheric Turbulence. Oxford University Press, 2008. http://dx.doi.org/10.1093/oso/9780199236534.003.0005.

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The observations are our starting point in this book, having been obtained from research aircraft in the last two decades. Justification for this approach can be found in Section 1.3 and by noting that there are no known analytical solutions to the Navier–Stokes equation, preventing the possibility of a priori prediction of the atmosphere’s turbulent structure. We note the pioneering power spectral analysis of wind, temperature, and ozone from commercial Boeing 747 aircraft (Nastrom and Gage 1985) and the more recent data from Airbus 340 aircraft under the aegis of the MOZAIC programme (Marenco et al. 1998). Multifractal analysis was first applied to observations from an IL-12 aircraft in the tropics (Chigirinskaya et al. 1994) and has been applied to a large body of observations taken from ER- 2, WB57F, DC-8, and G4 aircraft, with dropsondes from the last of these; Chapters 2, 4 and 5 are largely devoted to the results. Many of these data were obtained in the lower stratosphere from the ER-2 in the course of investigating ozone loss in both Arctic and Antarctic regions, where there exists a reasonably well-defined, durable circulation system offering clear dynamical, chemical, and radiative signatures. A more climate-driven imperative exists to investigate the tropical upper troposphere and lower stratosphere, largely pursued with the WB57F. The recent G4 and dropsonde data were acquired in the troposphere over the eastern Pacific Ocean, in the course of investigating northern hemisphere winter storms there. The utility of balloons and then, 120 years later, from 1903, of powered aircraft for exploring atmospheric properties, were immediately obvious. The Second World War saw aircraft attaining stratospheric altitudes, revealing a very dry lower stratosphere with westerly winds in winter and easterlies in summer, with accumulation of high ozone abundances in polar regions (Brewer 1944; Dobson et al. 1945; Brewer et al. 1948; Brewer 1949; Murgatroyd and Clews 1949; Bannon et al. 1952).
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2

Reiter, Walter S. "In the Footsteps of Corelli." In The Baroque Violin & Viola. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780190922696.003.0019.

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The influence of Corelli on the op. 2 sonatas of Vivaldi is clear, so in some ways this lesson is a consolidation of the previous ones. It identifies three essential prerequisites to successful interpretation: an unceasing observation and scrutiny of detail, an appraisal of the implications of each detail, and the identification and internalization of the emotions inherent in the music at any given moment. The detailed Observations section incorporates discussions on exclamations, the art of gesture and the use of second position, so important in this repertoire and so often feared by violinists. Alternative methods of shifting are clearly explained and the best places to shift identified, with reference to Tartini and Leopold Mozart. The lesson discusses what the sources say about using open strings, explains why it is important to spot ornamentation within a written text and how that impacts the way we play.
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3

Hepokoski, James. "Mozart, Piano Sonata in B-flat, K. 333/i (Allegro)." In A Sonata Theory Handbook. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197536810.003.0002.

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Chapter 2—which may be read before chapter 1, if that is the preference of the reader—is the book’s first illustration of Sonata Theory in practice. It provides a close reading of the first movement of Mozart’s Piano Sonata in B-flat, K. 333, that simultaneously presents an introduction to the theory’s specific mode of analysis and its most central concepts and terms. Not least of its concerns are its urgings that the listener/analyst is a co-creator of the work’s meaning (resulting ultimately in a responsible hermeneutic reading): Sonata Theory analysis seeks to be an aesthetically receptive, interactive dialogue with an individual work. Even in its most language-technical moments, it tries to integrate methodical observation with a personal sensitivity to the affective contours and colors of music as music. Two other features of the book are also introduced here: a historical/contextual backdrop for the work under consideration (including dating, original purpose, and aesthetic); and the inclusion of other modes of analytical practice to suggest their compatibility with Sonata Theory.
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