Auswahl der wissenschaftlichen Literatur zum Thema „SYNOP“

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Zeitschriftenartikel zum Thema "SYNOP"

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Milovidov, V. „To Origins of «Humanitarian Economy»“. World Economy and International Relations, Nr. 7 (2013): 3–11. http://dx.doi.org/10.20542/0131-2227-2013-7-3-11.

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Problems of liberalism in business relationship were designated as early as in Ancient philosophy and culture. The author details the essence of Classical Greek philosophers and thinkers, Diogenes's of Synop and Hesiod's views of these subjects.
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Hintz, K. S., H. Vedel, E. Kaas und N. W. Nielsen. „Estimation of Wind Speed and Roughness Length Using Smartphones: Method and Quality Assessment“. Journal of Atmospheric and Oceanic Technology 37, Nr. 8 (01.08.2020): 1319–32. http://dx.doi.org/10.1175/jtech-d-19-0037.1.

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AbstractCrowdsourced data are now seen as a potential source of high-resolution observations in the atmospheric sciences. In this paper we investigate a potential data source, wind observations obtained using anemometers connected to handheld smartphones. The aim of this paper is twofold: to assess the quality of raw and height-extrapolated wind measurements from the handheld anemometer against professional-grade surface synoptic observation (SYNOP) stations, and to use these data of opportunity to infer a more accurate estimation of terrain roughness lengths. Roughness lengths are essential in numerical weather prediction; however, they are often poorly determined. Roughness lengths are also necessary when correcting near-surface wind observations for height offsets. For the analysis we performed a series of field experiments measuring wind profiles using handheld anemometers at roughly 2 m above ground. These raw measurements were then extrapolated to 10-m height using roughness lengths from three different sources. The extrapolation enabled us to compare the quality of roughness lengths estimated from smartphone measurements with those from traditional sources, as well as to assess the quality of these wind measurements against the professional-grade stations. We find that the handheld wind measurements are comparable in quality to wind measurements from SYNOP stations at 10-m height and that for some cases the handheld measurements can be more representative than SYNOP stations only about a kilometer away. To determine the roughness lengths, we examine a method that is based on the turbulent intensity derived from the high-frequency signal of the smartphone wind measurements. Under certain circumstances, the roughness lengths obtained with the approach presented here are superior to traditional sources.
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Sokol, Z., und J. Štekl. „Dreidimensionale mesoskalige objektive Analyse der ausgewählten Elemente aus den SYNOP und SYRED Meldungen“. Meteorologische Zeitschrift 3, Nr. 4 (02.09.1994): 242–46. http://dx.doi.org/10.1127/metz/3/1994/242.

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Hynčica, Martin, und Radan Huth. „Long-term changes in precipitation phase in Czechia“. Geografie 124, Nr. 1 (2019): 41–55. http://dx.doi.org/10.37040/geografie2019124010041.

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Long-term changes in precipitation phase are investigated at ten stations in Czechia. Trends are calculated from 1983 to 2018 for the period between November and April. Daily SYNOP reports and daily precipitation totals are used at every station, where number and occurrence of specific codes in SYNOP report determine daily precipitation totals as solid, combined (which represents, to a large extent, category of mixed precipitation), or liquid. Thereafter, it is possible to calculate trends of all precipitation phases as well as the proportion of solid to total precipitation (S/P; in %). The average S/P trend over all Czech stations is significantly negative (−0.60%·year-1) and accompanied by a sharp decrease in solid precipitation (−1.66 mm·year-1) and an increase in combined precipitation (1.50 mm·year-1). Thus, our results show a ship of precipitation phase from solid to combined. Because of the dependence of S/P on air temperature, we suppose that the current S/P decline is a manifestation of rising air temperatures in the past decades.
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Arbain, Ardhi Adhary. „KLIMATOLOGI BADAI PETIR DI WILAYAH JAKARTA DAN SEKITARNYA BERDASARKAN OBSERVASI SYNOP TAHUN 2000-2012“. Jurnal Sains & Teknologi Modifikasi Cuaca 17, Nr. 1 (15.06.2016): 1. http://dx.doi.org/10.29122/jstmc.v17i1.1175.

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IntisariKlimatologi badai petir (TS) dianalisis dengan memanfaatkan pengamatan SYNOP per 3-jam dari 8 stasiun cuaca BMKG yang berada di wilayah Jakarta dan sekitarnya selama periode tahun 2000-2012. Frekuensi kejadian TS pada tiap lokasi dihitung berdasarkan perbandingan antara jumlah laporan TS pada data SYNOP dengan jumlah total observasi yang dilakukan oleh stasiun yang bersangkutan. Hasil pengolahan data menunjukkan bahwa TS memiliki dua pola klimatologi yang dominan dan paling sering terjadi pada periode sebelum dan sesudah musim hujan, terutama pada bulan November dan April. Hasil analisis juga menunjukkan bahwa TS sangat bergantung pada topografi dari lokasi yang bersangkutan, yang mengindikasikan pengaruh kuat dari siklus harian akibat konveksi kuat dan pola angin darat-laut di wilayah Jakarta dan sekitarnya. Pada beberapa lokasi yang berdekatan dengan Teluk Jakarta, periode puncak kejadian TS juga terjadi pada puncak musim hujan akibat pengaruh dari monsun barat laut dan seruak dingin yang datang dari Laut Tiongkok Selatan. Variabilitas iklim global seperti ENSO (El Nino Southern Oscillation) dan MJO (Madden-Julian Oscillation) turut memberikan pengaruh signifikan terhadap frekuensi TS. Hasil analisis menunjukkan bahwa frekuensi TS mengalami peningkatan pada periode La Nina kuat, serta pada periode sebelum dan sesudah MJO melintasi Indonesia bagian barat. AbstractThunderstorm (TS) climatology was analyzed by utilizing 3-hourly SYNOP observation of 8 BMKG’s weather stations in Jakarta capital and surrounding area during the period of 2000-2012. The frequency of TS occurrences at each location was calculated based on the ratio of TS reports to the total number of SYNOP observations conducted by the stations. The results show that the TS has two dominant climatological patterns in which most cases, the peak periods both preced and succeed the rainy season, especially in November and April. The results also imply that TS occurences are heavily influenced by the topography at each location, which indicate the great dependency of TS to the diurnal cycle generated by strong convective activity and land-sea breeze circulation over Jakarta and surronding regions. On the other hand, the peak period of TS at some locations close to Jakarta Bay, occurs simultaneously with the peak of rainy season by the influence of north-westerly monsoon and cold surge coming from the South China Sea. Global climate variabilities such as ENSO (El Nino Southern Oscillation) and MJO (Madden-Julian Oscillation) also significantly contribute to the anomaly of TS frequency. The results show an enhancement of TS frequency during the period of strong La Nina, as well as the period before and after MJO passes the western part of Indonesia.
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Kämäräinen, Matti, Otto Hyvärinen, Kirsti Jylhä, Andrea Vajda, Simo Neiglick, Jaakko Nuottokari und Hilppa Gregow. „A method to estimate freezing rain climatology from ERA-Interim reanalysis over Europe“. Natural Hazards and Earth System Sciences 17, Nr. 2 (22.02.2017): 243–59. http://dx.doi.org/10.5194/nhess-17-243-2017.

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Abstract. A method for estimating the occurrence of freezing rain (FZRA) in gridded atmospheric data sets was evaluated, calibrated against SYNOP weather station observations, and applied to the ERA-Interim reanalysis for climatological studies of the phenomenon. The algorithm, originally developed at the Finnish Meteorological Institute for detecting the precipitation type in numerical weather prediction, uses vertical profiles of relative humidity and temperature as input. Reanalysis data in 6 h time resolution were analysed over Europe for the period 1979–2014. Mean annual and monthly numbers of FZRA events, as well as probabilities of duration and spatial extent of events, were then derived. The algorithm was able to accurately reproduce the observed, spatially averaged interannual variability of FZRA (correlation 0.90) during the 36-year period, but at station level rather low validation and cross-validation statistics were achieved (mean correlation 0.38). Coarse-grid resolution of the reanalysis and misclassifications to other freezing phenomena in SYNOP observations, such as ice pellets and freezing drizzle, contribute to the low validation results at station level. Although the derived gridded climatology is preliminary, it may be useful, for example, in safety assessments of critical infrastructure.
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Porter, David L., Ella B. Dobson und Scott M. Glenn. „Measurements of dynamic topography during synop utilizing a Geosat synthetic geoid“. Geophysical Research Letters 19, Nr. 18 (23.09.1992): 1847–50. http://dx.doi.org/10.1029/92gl01881.

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Lopez, Philippe. „Experimental 4D-Var Assimilation of SYNOP Rain Gauge Data at ECMWF“. Monthly Weather Review 141, Nr. 5 (01.05.2013): 1527–44. http://dx.doi.org/10.1175/mwr-d-12-00024.1.

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Abstract Four-dimensional variational data assimilation (4D-Var) experiments with 6-hourly rain gauge accumulations observed at synoptic stations (SYNOP) around the globe have been run over several months, both at high resolution in an ECMWF operations-like framework and at lower resolution with the reference observational coverage reduced to surface pressure data only, as would be expected in early twentieth-century periods. The key aspects of the technical implementation of rain gauge data assimilation in 4D-Var are described, which include the specification of observation errors, bias correction procedures, screening, and quality control. Results from experiments indicate that the positive impact of rain gauges on forecast scores remains limited in the operations-like context because of their competition with all other observations already available. In contrast, when only synoptic station surface pressure observations are assimilated in the data-poor control experiment, the additional assimilation of rain gauge measurements substantially improves not only surface precipitation scores, but also analysis and forecast scores of temperature, geopotential, wind, and humidity at most atmospheric levels and for forecast ranges up to 10 days. The verification against Meteosat infrared imagery also shows a slight improvement in the spatial distribution of clouds. This suggests that assimilating rain gauge data available during data-sparse periods of the past might help to improve the quality of future reanalyses and subsequent forecasts.
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Rohm, Witold, Jakub Guzikowski, Karina Wilgan und Maciej Kryza. „4DVAR assimilation of GNSS zenith path delays and precipitable water into a numerical weather prediction model WRF“. Atmospheric Measurement Techniques 12, Nr. 1 (18.01.2019): 345–61. http://dx.doi.org/10.5194/amt-12-345-2019.

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Abstract. The GNSS data assimilation is currently widely discussed in the literature with respect to the various applications for meteorology and numerical weather models. Data assimilation combines atmospheric measurements with knowledge of atmospheric behavior as codified in computer models. With this approach, the “best” estimate of current conditions consistent with both information sources is produced. Some approaches also allow assimilating the non-prognostic variables, including remote sensing data from radar or GNSS (global navigation satellite system). These techniques are named variational data assimilation schemes and are based on a minimization of the cost function, which contains the differences between the model state (background) and the observations. The variational assimilation is the first choice for data assimilation in the weather forecast centers, however, current research is consequently looking into use of an iterative, filtering approach such as an extended Kalman filter (EKF). This paper shows the results of assimilation of the GNSS data into numerical weather prediction (NWP) model WRF (Weather Research and Forecasting). The WRF model offers two different variational approaches: 3DVAR and 4DVAR, both available through the WRF data assimilation (WRFDA) package. The WRFDA assimilation procedure was modified to correct for bias and observation errors. We assimilated the zenith total delay (ZTD), precipitable water (PW), radiosonde (RS) and surface synoptic observations (SYNOP) using a 4DVAR assimilation scheme. Three experiments have been performed: (1) assimilation of PW and ZTD for May and June 2013, (2) assimilation of PW alone; PW, with RS and SYNOP; ZTD alone; and finally ZTD, with RS and SYNOP for 5–23 May 2013, and (3) assimilation of PW or ZTD during severe weather events in June 2013. Once the initial conditions were established, the forecast was run for 24 h. The major conclusion of this study is that for all analyzed cases, there are two parameters significantly changed once GNSS data are assimilated in the WRF model using GPSPW operator and these are moisture fields and rain. The GNSS observations improves forecast in the first 24 h, with the strongest impact starting from a 9 h lead time. The relative humidity forecast in a vertical profile after assimilation of ZTD shows an over 20 % decrease of mean error starting from 2.5 km upward. Assimilation of PW alone does not bring such a spectacular improvement. However, combination of PW, SYNOP and radiosonde improves distribution of humidity in the vertical profile by maximum of 12 %. In the three analyzed severe weather cases PW always improved the rain forecast and ZTD always reduced the humidity field bias. Binary rain analysis shows that GNSS parameters have significant impact on the rain forecast in the class above 1 mm h−1.
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Laird, Neil, Ryan Sobash und Natasha Hodas. „Climatological Conditions of Lake-Effect Precipitation Events Associated with the New York State Finger Lakes“. Journal of Applied Meteorology and Climatology 49, Nr. 5 (01.05.2010): 1052–62. http://dx.doi.org/10.1175/2010jamc2312.1.

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Abstract A climatological analysis was conducted of the environmental and atmospheric conditions that occurred during 125 identified lake-effect (LE) precipitation events in the New York State Finger Lakes region for the 11 winters (October–March) from 1995/96 through 2005/06. The results complement findings from an earlier study reporting on the frequency and temporal characteristics of Finger Lakes LE events that occurred as 1) isolated precipitation bands over and downwind of a lake (NYSFL events), 2) an enhancement of LE precipitation originating from Lake Ontario (LOenh events), 3) an LE precipitation band embedded within widespread synoptic precipitation (SYNOP events), or 4) a transition from one type to another. In comparison with SYNOP and LOenh events, NYSFL events developed with the 1) coldest temperatures, 2) largest lake–air temperature differences, 3) weakest wind speeds, 4) highest sea level pressure, and 5) lowest height of the stable-layer base. Several significant differences in conditions were found when only one or both of Cayuga and Seneca Lakes, the largest Finger Lakes, had LE precipitation as compared with when the smaller Finger Lakes also produced LE precipitation. In addition, transitional events containing an NYSFL time period occurred in association with significantly colder and drier air masses, larger lake–air temperature differences, and a less stable and shallower boundary layer in comparison with those associated with solitary NYSFL events.
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Dissertationen zum Thema "SYNOP"

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Langer, Ines [Verfasser]. „Objektive Darstellung von Niederschlagsfeldern basierend auf einer Synthese aus Synop- und Satellitendaten / Ines Langer“. Berlin : Freie Universität Berlin, 2009. http://d-nb.info/1023623536/34.

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Grzesiak, Frédéric. „Représentation des connaissances et techniques d'inférence pour le maniement d'objets graphiques application au système expert SYNOP /“. Grenoble 2 : ANRT, 1987. http://catalogue.bnf.fr/ark:/12148/cb37605598h.

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Grzesiak, Frédéric. „Représentation des connaissances et techniques d'inférence pour le maniement d'objets graphiques : application au Système-Expert SYNOP“. Valenciennes, 1987. https://ged.uphf.fr/nuxeo/site/esupversions/fd5e5639-ec92-4d3d-96e8-98f6c14c5743.

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Réalisation d'un outil système expert capable d'appliquer sur une image de surveillance donnée l'ensemble des spécifications graphiques contenues dans ses bases de connaissances. Après la validation du moteur d'inférence, divers travaux ont été réalisés pour préparer l'utilisation effective du système
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Frey, Wiebke. „The Formation of Stratus in Rain“. Thesis, Uppsala universitet, Luft-, vatten och landskapslära, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-303869.

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Data analysis of SYNOP observations was made for investigation of stratus formation in rain. The aim was to find connections between meteorological parameters in the different states of rain to develop a forecast method. 1594 cases of rainfall from the four stations Luleå, Uppsala, Linköping and Såtenäs, Sweden were analysed, 974 cases include stratus formation in rain and the other 620 cases are without stratus formation. The investigation focused on the meteorological parameters wind direction, wind speed, relative humidity, visibility, cloud base height and rain intensity. As rain intensity was not explicitly included in the SYNOP observations it could not be taken as a governing parameter, but classification of the data into four groups of different rain intensity was possible. Also time was a parameter for the investigation. The results show that a more detailed investigation should be made to eliminate several influences of other parameters, for example of radiation or soil conditions. Thus it was too difficult to develop a forecast method for the formation of stratus in rain, but suggestions for further investigations and the development of a numerical model only are made.
En dataanalys av SYNOP-observationer genomfördes för undersökning av stratusbildning i regn. Målet var att hitta samband mellan de meteorologiska parametrarna i olika regntillstånden för att utveckla en prognosmetod. 1594 regntillfällen från fyra stationer, Luleå, Uppsala, Linköping och Såtenäs, analyserades. 974 tillfällen innehåller stratusbildning i regn och de andra 620 tillfällena visar ingen stratusbildning. Undersökningen koncentrerades på de meteorologiska parametrarna vindriktning, vindhastighet, relativ fuktighet, sikt, molnhöjd och regnintensitet. Eftersom regnintensiteten inte var beskriven i SYNOP-observationer kunde den inte tas med som parameter i analysena. Det gick att indela datan i fyra grupper med olika regnintensitet. Tid var också en parameter i den här unders- ökningen. Resultater visar att det behövs en noggrannare undersökning för kunna eliminera påverkan av andra parametrar som till exempel strålning eller marktillstånd. Det var därför för svårt att utveckla en prognosmetod för stratusbildning i regn, så förslag har bara gjorts för vidare undersökningar och utveckling av en numerisk modell.
Für die Untersuchung der Stratusbildung im Regen wurde eine Analyse von SYNOP-Daten durchgeführt. Ziel war es, Zusammenhänge zwischen meteorologischen Parametern in den verschiedenen Stadien von Regen zu finden, um eine Vorhersagemethode zu entwickeln. Es wurden 1594 Regen- F¨alle von den Stationen Luleå, Uppsala, Linköping und Såtenäs in Schweden analysiert, von denen 974 Fälle Stratusbildung in Regen beinhalten. Die anderen 620 Fälle zeigen keine Stratusbildung. Die Untersuchung konzentrierte sich auf die meteorologischen Parameter Windrichtung, Windgeschwindigkeit, relative Feuchte, Sicht, Wolkenhöhe und Regenintensität. Da die Regenintensität nicht direkt in den SYNOP Beobachtungen gemessen wurde, konnte sie nicht als steuernder Parameter verwendet werden, sondern diente nur zur Einteilung der Daten in vier Gruppen verschiedener Regenintensität. Die Zeit ging als ein weiterer Parameter in diese Untersuchung ein. Die Ergebnisse zeigen, dass eine genauere Untersuchung durchgeführt werden sollte, um unterschiedliche Einflüsse anderer Parameter, wie zum Beispiel Strahlung oder Bodenbeschaffenheit, auszuschließen. Wegen der zu großen Unsicherheiten war es zu schwer, eine Prognosemethode f¨ur die Stratusbildung im Regen zu entwickeln. Deswegen wurden Vorschläge für weitere Untersuchungen und f¨ur die Entwicklung eines numerischen Modells gegeben.
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Söderberg, Freja. „Cloud Overlap Assumption and Cloud Cover Validation for HARMONIE-AROME“. Thesis, Uppsala universitet, Luft-, vatten och landskapslära, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-283606.

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One major challenge in representing the state of the atmosphere through weather forecast models, is the parametrization of sub-grid clouds. At every vertical column of grid cells within a weather forecast model, the fractional cloud cover is assumed to overlap according to a prescribed Cloud Overlap Assumption (COA). Since the total cloud cover is used in radiation schemes, the choice of COA affects e.g. radiative fluxes. High-quality weather forecasts is important for many aspects of the society, thus, the analysis of cloud parametrizations is significant. In this study, COAs for the HIRLAM ALADIN Research on mesoscale Modelling for NWP In Euromed (HARMONIE) - Application of Research to Operations at Mesoscale (AROME) model were investigated for two time-periods. Moreover, validation methods of cloud cover for HARMONIE-AROME were analyzed due to uncertainties in cloud observations. Both satellite data derived from geostationary Meteosat Second Generation (MSG) satellite and synoptic ground based observations were used to validate cloud cover in this project. It was found that HARMONIE-AROME underestimates the cloud cover during summer. Therefore, the random (RAN) COA is the preferred COA to use during time periods of mainly convective cloud processes. During the tested winter period, which is assumed to have most clouds of the stratiform type, the results regarding optimal COA were not certain. However, it was concluded that HARMONIE-AROME overestimates the cloud cover during winter, for in which case the maximum-random (MRN) COA is recommended to use. The comparative analysis of cloud cover as obtained from the COAs against observed cloud cover, was shown sensitive to the methods used to the observational data. Using a model grid of 25 km instead of 2.5 km when comparing synoptic observations to modelled cloud cover, the errors were reduced. When using binary satellite data, it was concluded that a 5x5 smoothing algorithm was the most appropriate to use since this averaging of several pixels are sufficient to represent sub-grid clouds.
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Kolski, Christophe. „Contribution à l'ergonomie de conception des interfaces graphiques homme-machine dans les procédés industriels : application au système expert SYNOP“. Valenciennes, 1989. https://ged.uphf.fr/nuxeo/site/esupversions/48d8d47d-0900-46b2-8537-b0a89714a0d9.

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La thèse concerne le développement et la validation du système expert SYNOP pour l'évaluation ergonomique et l’amélioration de vues graphiques exploitées dans les salles de contrôle de procédés industriels. SYNOP utilise un moteur d'inférence du premier ordre et les notions de frame et de réseau sémantique pour la représentation des connaissances. Il est écrit en langage LISP. Ses bases contiennent des concepts ergonomiques de présentation d'information sur écran graphique. Le module d'évaluation de SYNOP, ainsi que ses interfaces expert et utilisateur, sont détaillés. Les principes d'élaboration et de validation des bases de connaissances ergonomiques de SYNOP sont expliqués. Le mémoire décrit également la contribution du système expert SYNOP à l’évaluation et l’amélioration d'une interface graphique dans un contexte industriel. Le mémoire se termine par des perspectives d'évolution de SYNOP
The doctoral thesis concerns the development and validation of the SYNOP expert system for the ergonomic evaluation and improvement of graphic views used in control rooms of industrial processes SYNOP uses a first-order inference engine and the concepts of frame and semantic network for knowledge representation. It is written in LISP language. Its knowledge bases contain ergonomic concepts for information presentation on graphic screens. Its evaluation module, as well as its expert and user interfaces, are detailed. The principles for developing and validating its ergonomic knowledge bases are explained. The thesis also describes the contribution of the SYNOP expert system to the evaluation and improvement of a graphical user interface in an industrial context. The thesis ends with several research perspectives
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Rossow, Timothy A. „Writing a genuinely Missouri Synod parish constitution“. Theological Research Exchange Network (TREN), 2006. http://www.tren.com/search.cfm?p079-0080.

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Okoye, Chukwuma J. „The Synod Challenges the Church in Africa“. Bulletin of Ecumenical Theology, 1994. http://digital.library.duq.edu/u?/bet,455.

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Pallath, Paul. „The synod of bishops of Catholic Oriental Churches /“. Rome : Mar Thoma Yogam, the St Thomas christian fellowship, 1994. http://catalogue.bnf.fr/ark:/12148/cb37618920m.

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Tolles, Sally J. „The diocesan synod some areas of potential particular legislation /“. Theological Research Exchange Network (TREN), 1990. http://www.tren.com.

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Bücher zum Thema "SYNOP"

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Cronin, Meghan. Mooring motion correction of SYNOP central array current meter data. Narragansett, R.I: University of Rhode Island, Graduate School of Oceanography, 1992.

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Fields, Erik. The SYNOP experiment: Inverted echo sounder data report for May 1988 to Aug 1989. Narragansett, R.I: Graduate School of Oceanography, University of Rhode Island, 1990.

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Scholl, Margit Christa. Fallstudie über die Kongruenz von Niederschlagsinformation aus SYNOP-, MODELL- und METEOSAT-Daten: (DK 001.8:551.5/167.7:551.5/519 ... Berlin: D. Reimer, 1991.

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Tarbell, Susan. A compilation of moored current meter data from SYNOP arrays: One and Two (September 1987 to July 1991). Volume XLVI. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1992.

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Methodist Church (Great Britain). Isle of Man District. Synod directory. [Isle of Man: Isle of Man District of the Methodist Church], 2003.

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Uniting Church in Australia. Synod of South Australia. Synod directory. [s.l.]: Uniting Church in Australia, 1994.

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Salīas, E. A. Arakcheevskiĭ synok: Arakcheevskiĭ podkidysh. Sankt-Peterburg: "Pechatnyĭ dvor", 1993.

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Begalieva, Salkyn. Kalem synoo: Yrlar zhyĭnagy. Frunze: "Kyrgyzstan", 1988.

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Beeke, Joel R., und Martin I. Klauber, Hrsg. The Synod of Dort. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.

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Synod Extraordinary: The inside story of the Rome Synod, November-December 1985. Garden City, N.Y: Doubleday, 1986.

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Buchteile zum Thema "SYNOP"

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Poole, Eve. „General Synod Views“. In The Church on Capitalism, 4–40. London: Palgrave Macmillan UK, 2010. http://dx.doi.org/10.1057/9780230290761_2.

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2

Dagher, Carole H. „A Synod for Lebanon“. In Bring Down the Walls, 91–106. New York: Palgrave Macmillan US, 2000. http://dx.doi.org/10.1057/9780230109193_7.

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3

Harding, Matthew Scott. „3. A Voice Among the Restricted French Delegates of Dort: Pierre du Moulin on Providence and Predestination“. In The Synod of Dort, 41–60. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.41.

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4

Klauber, Martin I. „2. Theological Responses to the Synod of Dort in France“. In The Synod of Dort, 27–40. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.27.

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5

Borvan, Dan. „4. Pierre du Moulin’s Use of Scripture and Tradition in the Arminian Controversy“. In The Synod of Dort, 61–74. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.61.

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6

Horton, Michael. „7. Is Particular Redemption “Good News”?“ In The Synod of Dort, 105–32. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.105.

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7

Godfrey, W. Robert. „1. The Synod of Dort and Strategic Thinking“. In The Synod of Dort, 13–26. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.13.

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8

Sinnema, Donald. „8. Church and State Relations at the Synod of Dort (1618–1619)“. In The Synod of Dort, 133–48. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.133.

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9

McWilliams, David B. „9. Sacrosancta Synodus! Cornelius Van Til on Dort and Its Detractors“. In The Synod of Dort, 149–62. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.149.

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10

Telfer, Charles. „10. “The Holy Exercises of Piety” in the Canons of Dort and in Campegius Vitringa (1659–1722) as a Representative of the Nadere Reformatie“. In The Synod of Dort, 163–84. Göttingen: Vandenhoeck & Ruprecht, 2020. http://dx.doi.org/10.13109/9783666540776.163.

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Konferenzberichte zum Thema "SYNOP"

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Kirschenstein, Malgorzata. „DESIGNATION OF THE SURFACE TEMPERATURE USING METEOROLOGICAL DATA FROM DEBLIN/IRENA SYNOP STATION“. In 18th International Multidisciplinary Scientific GeoConference SGEM2018. Stef92 Technology, 2018. http://dx.doi.org/10.5593/sgem2018/4.2/s19.042.

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2

Hanuliaková, Radoslava, und Miriam Jarošová. „Meteorological radiolocator as a tool to improve meteorological information for aviation“. In Práce a štúdie. University of Žilina, 2021. http://dx.doi.org/10.26552/pas.z.2021.1.08.

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The paper deals with meteorological radar as a tool to improve meteorological information for aviation. The first theoretical part is devoted to the history of weather forecasting and its gradual improvement. The part describes the current state of the problem in the Slovak Republic and in the world. The next part characterizes the meteorological radar, what it is used for and what is its essence. The following is the division of radars, characteristics of the radar network in Europe and the radar network in Slovakia. In the last theoretical part, attention was paid to the merged maps, their individual products - Maximum, CAPPI 2 km, EchoTop and 1h total precipitation. The last part consists in a practical representation and description of individual maps of the cold, warm and occlusive front over the territory of the Slovak Republic. These maps show how the radar captured the weather, SYNOP reports were also used, which provide a more detailed weather forecast, maps of dangerous phenomena for aviation and maps from the OPERA network.
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Borssatto, Ítalo B., und Adriel R. Moro. „Medições de uma implementação de MPS.BR nível F“. In Simpósio Brasileiro de Qualidade de Software. Sociedade Brasileira de Computação - SBC, 2007. http://dx.doi.org/10.5753/sbqs.2007.15592.

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A empresa Synos, ao planejar seu primeiro projeto de melhoria do processo de desenvolvimento de software, implementando o nível F do MPS.BR, enfrentou a carência de referências que a auxiliassem nas estimativas de esforço, custo e tempo. Identificando a oportunidade de divulgar estas referências, escassas no mercado, a Synos apresenta a sua experiência, revelando as principais medições coletadas e as lições aprendidas.
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Seda, Degrauwe und Fichtner. „Lazy-expansion symbolic expression approximation in SYNAP“. In IEEE/ACM International Conference on Computer-Aided Design. IEEE Comput. Soc. Press, 1992. http://dx.doi.org/10.1109/iccad.1992.279355.

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de Boer, Erik A., Donald Sinnema und Dolf te Velde. „Discipline Cases at the Synod of Dordt: Introduction“. In Seventh Annnual RefoRC conference. Göttingen: Vandenhoeck & Ruprecht, 2019. http://dx.doi.org/10.13109/9783666570964.287.

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6

Branch, David, Jerod Parrent, M. A. Troxel, D. Casebeer, David J. Jeffery, E. Baron, Wesley Ketchum und Nicholas Hall. „Probing the Nature of Type I Supernovae with SYNOW“. In THE MULTICOLORED LANDSCAPE OF COMPACT OBJECTS AND THEIR EXPLOSIVE ORIGINS. American Institute of Physics, 2007. http://dx.doi.org/10.1063/1.2774879.

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7

SHuvalova, A. N. „КАК ЛЮДИ ОКАЗЫВАЛИСЬ В МОСКОВСКИХ БОГАДЕЛЬНЯХ В XVIII ВЕКЕ?“ In Sbornik izbrannyh statei po materialam nauchnyh konferencii GNII "Nacrazvitie" (Sankt-Peterburg, Mart 2020). ГНИИ "Нацразвитие", 2020. http://dx.doi.org/10.37539/mar184.2020.36.99.006.

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в статье говорится о поступлении нищих, увечных и больных в московскиебогадельни в XVIII веке. Все лица обязаны были написать своего рода прошение ( доношение )в Святейший синод с причиной их поступления в богоугодное учреждение.the article deals with the admission of the poor, the crippled and the sick to Moscowalmshouses in the XVIII century. All persons were required to write a kind of petition( denunciation ) to the Holy Synod with the reason for their admission to a God-pleasing institution.
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Cakir, Cemile. „SYNAP: A GAMIFIED APPROACH TO PREPARING STUDENT FOR THE SOLICITORS QUALIFICATION EXAMINATION“. In 14th International Technology, Education and Development Conference. IATED, 2020. http://dx.doi.org/10.21125/inted.2020.2109.

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te Velde, Dolf. „Collateral Damage? The Condemnation of Conrad Vorstius by the Synod of Dordt“. In Seventh Annnual RefoRC conference. Göttingen: Vandenhoeck & Ruprecht, 2019. http://dx.doi.org/10.13109/9783666570964.321.

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10

Sinnema, Donald. „Procedural Wrangling in the Remonstrant Case at the Synod of Dordt (1618–1619)“. In Seventh Annnual RefoRC conference. Göttingen: Vandenhoeck & Ruprecht, 2019. http://dx.doi.org/10.13109/9783666570964.289.

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Berichte der Organisationen zum Thema "SYNOP"

1

Johns, William E. Acoustic Velocity Profiling in SYNOP. Fort Belvoir, VA: Defense Technical Information Center, Februar 1996. http://dx.doi.org/10.21236/ada306621.

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2

Hallock, Z. R. Objective Daily Maps of Thermocline Depth for the SYNOP Eastern Array. Fort Belvoir, VA: Defense Technical Information Center, Mai 1992. http://dx.doi.org/10.21236/ada252868.

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3

Anderson-Fontana, Sandra, und H. T. Rossby. The SYNOP Experiment: XBT Data for the Period January 1988 to February 1990. Fort Belvoir, VA: Defense Technical Information Center, Mai 1992. http://dx.doi.org/10.21236/ada252666.

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4

Tarbell, Susan A., Scott E. Worrilow und Nelson G. Hogg. A Compilation of Moored Current Meter Data from SYNOP Arrays One and Two (September 1987 to July 1991). Volume 44. Fort Belvoir, VA: Defense Technical Information Center, November 1992. http://dx.doi.org/10.21236/ada261902.

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5

Malanotte-Rizzoli, Paola. Sensitivity Study of the SPEM Model to the Assimilation of Synop Datasets Using Two Assimilation Schemes: (1) Nudging (2) The Kalman Filter/ Smoother. Fort Belvoir, VA: Defense Technical Information Center, Dezember 1993. http://dx.doi.org/10.21236/ada281459.

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