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Relevant bibliographies by topics / So-Precipitation

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Journal articles

Academic literature on the topic 'So-Precipitation'

Author: Grafiati

Published: 29 March 2025

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Journal articles on the topic "So-Precipitation"

1

Taylor, W. J., T. Y. Tan, and U. Gösele. "Carbon precipitation in silicon: Why is it so difficult?" Applied Physics Letters 62, no. 25 (1993): 3336–38. http://dx.doi.org/10.1063/1.109063.

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2

Müller, Timo, G. Kissinger, P. Krottenthaler, C. Seuring, R. Wahlich, and Wilfried von Ammon. "Precipitation Enhancement of "so Called" Defect-Free Czochralski Silicon Material." Solid State Phenomena 108-109 (December 2005): 11–16. http://dx.doi.org/10.4028/www.scientific.net/ssp.108-109.11.

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Thermal treatments to enhance precipitation like RTA, ramp anneal and argon anneal were performed on low oxygen 300 mm wafers without vacancy or interstitial agglomerates (“so called” defect-free material). Best results were achieved using high temperature argon anneal leading to a homogenous BMD and denuded zone formation. Furthermore the getter efficiency was positively tested by intentional Ni-contamination. Concepts to overcome the slip danger like improved support geometries and nitrogen codoping were also evaluated and are seen to be beneficial.

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3

Sutanto, Ahmad, Anwar Annas, Mohammad Ardha, Taufif Hidayat, and Muhammad Rokhis Khomarudin. "AUTOMATION OF DAILY LANDSLIDE POTENTIAL INFORMATION BASED ON REMOTE SENSING SATELLITE IMAGERY USING OPEN-SOURCE SOFTWARE TECHNOLOGY." International Journal of Remote Sensing and Earth Sciences (IJReSES) 20, no. 1 (2023): 37. http://dx.doi.org/10.30536/j.ijreses.2023.v20.a3836.

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This automation system automatically generated landslide potential information based on daily precipitation data. This system is essential to replace the previous manual processing system with an automated and integrated system. The results of the developed system are the distribution of areas with landslide potential based on daily precipitation data. The system was built using geographic information systems and web service techniques. This allows the automation process to be performed quickly and accurately. The landslide susceptibility map used is from the National Disaster Management Agenc

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4

Nowobilska-Majewska, Elwira, Tomasz Kotowski, and Piotr Bugajski. "Impact of atmospheric precipitation on the volume of wastewater inflowing to the treatment plant in Nowy Targ." E3S Web of Conferences 171 (2020): 01009. http://dx.doi.org/10.1051/e3sconf/202017101009.

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The study determines the impact of precipitation on the amount of wastewater flowing into the treatment plant in Nowy Targ. The research period covered the years 2016 and 2017, in which the amount of precipitation and average daily wastewater inflows (during the so-called dry period, i.e. days without precipitation and in the so-called wet period, i.e. days with precipitation) were analyzed. The research period was divided into 5 characteristic ranges in terms of the amount of precipitation. It was found that on days with different intensity of precipitation, the amount of rainwater (in the to

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5

Jiang, Hongli, Graham Feingold, and Armin Sorooshian. "Effect of Aerosol on the Susceptibility and Efficiency of Precipitation in Warm Trade Cumulus Clouds." Journal of the Atmospheric Sciences 67, no. 11 (2010): 3525–40. http://dx.doi.org/10.1175/2010jas3484.1.

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Abstract Large-eddy simulations of warm, trade wind cumulus clouds are conducted for a range of aerosol conditions with a focus on precipitating clouds. Individual clouds are tracked over the course of their lifetimes. Precipitation rate decreases progressively as aerosol increases. For larger, precipitating clouds, the polluted clouds have longer lifetimes because of precipitation suppression. For clean aerosol conditions, there is good agreement between the average model precipitation rate and that calculated based on observed radar reflectivity Z and precipitation rate R relationships. Prec

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6

Nastos, P. T., and C. S. Zerefos. "Cyclic modes of the intra-annual variability of precipitation in Greece." Advances in Geosciences 25 (March 9, 2010): 45–50. http://dx.doi.org/10.5194/adgeo-25-45-2010.

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Abstract. The application of harmonic analysis to the annual variability of precipitation is the object of this study, so that the modes, which compose the annual variability, be elicited. For this purpose, monthly precipitation totals from 30 meteorological stations of the Hellenic National Meteorological Service (HNMS), for the period 1950–2000, were used. The initial target is to reduce the number of variables and to detect structure in the relationships between the variables. The most commonly used technique for this purpose is the application of Factor Analysis (FA) resulted in five main

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7

Juliá, Cristóbal, David A. Rahn, and José A. Rutllant. "Assessing the Influence of the MJO on Strong Precipitation Events in Subtropical, Semi-Arid North-Central Chile (30°S)." Journal of Climate 25, no. 20 (2012): 7003–13. http://dx.doi.org/10.1175/jcli-d-11-00679.1.

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Abstract Annual precipitation in subtropical, semiarid north-central Chile (30°S) during rainy years comprises a few (3–5) strong events in the fall and winter, which are presumably modulated by the Madden–Julian oscillation (MJO). Precipitation from 1979–2009 was recorded daily at three stations along the Elqui Valley. The relationship between the MJO and precipitation is investigated from two perspectives: 1) examining a MJO index (MJOI) based on the actual precipitation events and 2) examining the likelihood of precipitation based on a favorable MJOI. About 80% of the strong precipitation e

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8

Chou, Chia, Chao-An Chen, Pei-Hua Tan, and Kuan Ting Chen. "Mechanisms for Global Warming Impacts on Precipitation Frequency and Intensity." Journal of Climate 25, no. 9 (2012): 3291–306. http://dx.doi.org/10.1175/jcli-d-11-00239.1.

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Global warming mechanisms that cause changes in frequency and intensity of precipitation in the tropics are examined in climate model simulations. Under global warming, tropical precipitation tends to be more frequent and intense for heavy precipitation but becomes less frequent and weaker for light precipitation. Changes in precipitation frequency and intensity are both controlled by thermodynamic and dynamic components. The thermodynamic component is induced by changes in atmospheric water vapor, while the dynamic component is associated with changes in vertical motion. A set of equations is

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9

Wang, Xi An, Fei Mao, Qi Min Zhang, and Jun Lian He. "Study on Paraffin Precipitation for Dalaoba Condensate Gas Reservoir." Applied Mechanics and Materials 121-126 (October 2011): 423–27. http://dx.doi.org/10.4028/www.scientific.net/amm.121-126.423.

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High content of paraffin for condensate gas reservoir in Dalaoba and the precipitation of paraffin seriously affect the production and safety to bring about greater economic loss, therefore, it is necessary to develop the study on the precipitation of paraffin,deposition mechanism, variation discipline of phase state, prediction technology as well as the discipline for precipitation of paraffin of shaft.The paper establish the predication method on phase state simulation for paraffin precipitation. In order to better realize the site application, the predicted drawing version on paraffin preci

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10

Chou, Chia, and Jien-Yi Tu. "Hemispherical Asymmetry of Tropical Precipitation in ECHAM5/MPI-OM during El Niño and under Global Warming." Journal of Climate 21, no. 6 (2008): 1309–32. http://dx.doi.org/10.1175/2007jcli1928.1.

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Abstract Similarities and differences between El Niño and global warming are examined in hemispherical and zonal tropical precipitation changes of the ECHAM5/Max Planck Institute Ocean Model (MPI-OM) simulations. Similarities include hemispherical asymmetry of tropical precipitation changes. This precipitation asymmetry varies with season. In the boreal summer and autumn (winter and spring), positive precipitation anomalies are found over the Northern (Southern) Hemisphere and negative precipitation anomalies are found over the Southern (Northern) Hemisphere. This precipitation asymmetry in bo

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