Готові списки джерел за темами / Meteorology

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Добірка наукової літератури з теми "Meteorology"

Автор: Grafiati
Опубліковано: 4 червня 2021
Оновлено: 29 липня 2024

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Статті в журналах з теми "Meteorology"

1

Lasher, Darlene. "Meteorology." Psychological Perspectives 55, no. 1 (January 2012): 126. http://dx.doi.org/10.1080/00332925.2012.650072.

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2

P., F., and R. G. "Meteorology." Res: Anthropology and Aesthetics 23 (March 1993): 5–6. http://dx.doi.org/10.1086/resv23n1ms20166863.

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3

Raja, Melita Emas Lumban, and Hadiyanto Hadiyanto. "Hubungan Karakteristik Pengguna dan Perilaku Penggunaan Portal Data BMKG dengan Tingkat Kepuasan Perolehan Data Iklim." Jurnal Sains Komunikasi dan Pengembangan Masyarakat [JSKPM] 4, no. 4 (August 4, 2020): 527. http://dx.doi.org/10.29244/jskpm.4.4.527-544.

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Masyarakat dapat mengakses informasi data iklim seperti data Meteorologi, Klimatologi, Kualitas Udara, dan Geofisika dari berbagai media yang digunakan. Lembaga pemerintah non kementerian di Indonesia yang berwenang terhadap data ini adalah Badan Meteorologi, Klimatologi, dan Geofisika (BMKG). BMKG menyediakan portal layanan data online yang berisikan data iklim, Portal ini secara khusus digunakan oleh mahasiswa Departemen Geofisika dan Meteorologi FMIPA IPB Angkatan 2015, 2016, dan 2017. Tujuan penelitian ini adalah untuk menganalisis tingkat kepuasan pengguna portal data terhadap perolehan data iklim yang disediakan oleh BMKG. Pendekatan yang digunakan adalah pendekatan kuantitatif dengan metode survei menggunakan instrumen kuesioner dan didukung dengan data kualitatif dengan metode wawancara. Hasil penelitian ini menunjukkan bahwa mahasiswa Departemen Geofisika dan Meteorologi FMIPA IPB Angkatan 2015, 2016, dan 2017 tidak puas atas perolehan data iklim yang disediakan oleh BMKG. Hal ini ditinjau berdasarkan hubungan karakteristik pengguna dan perilaku penggunaan dengan tingkat kepuasan perolehan data iklim dari portal layanan data online BMKG.Kata Kunci: gratification, tingkat kepuasan, perilaku penggunaan media=====ABSTRACTPublic can access information such as Meteorology, Climatology, Air Quality and Geophysics data from various media used. The non-ministerial government institutions in Indonesia that are authorized for this data are the Badan Meteorologi, Klimatologi, dan Geofisika (BMKG). BMKG provides an online data service portal containing climate data. This portal is specifically used by students of the batch 2015, 2016 and 2017 from Department of Geophysics and Meteorology FMIPA IPB. The aim of this research is analyzing the satisfaction of data portal users on climate data acquisition provided by BMKG. The approach used is a quantitative approach with a survey method using a questionnaire instrument and supported by qualitative data with interview methods. The results of this study indicate that the students of the batch 2015, 2016, and 2017 from Department of Geophysics and Meteorology FMIPA IPB were not satisfied with the acquisition of climate data provided by BMKG. This was reviewed based on the relationship between user characteristics and usage behavior with satisfaction of climate data acquisition from BMKG's online data service portal.Keywords: gratification, satisfaction level, media use behavior
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4

Raja, Melita Emas Lumban, and Hadiyanto Hadiyanto. "Hubungan Karakteristik Pengguna dan Perilaku Penggunaan Portal Data BMKG dengan Tingkat Kepuasan Perolehan Data Iklim." Jurnal Sains Komunikasi dan Pengembangan Masyarakat [JSKPM] 4, no. 4 (August 4, 2020): 535. http://dx.doi.org/10.29244/jskpm.4.4.535-552.

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Masyarakat dapat mengakses informasi data iklim seperti data Meteorologi, Klimatologi, Kualitas Udara, dan Geofisika dari berbagai media yang digunakan. Lembaga pemerintah non kementerian di Indonesia yang berwenang terhadap data ini adalah Badan Meteorologi, Klimatologi, dan Geofisika (BMKG). BMKG menyediakan portal layanan data online yang berisikan data iklim, Portal ini secara khusus digunakan oleh mahasiswa Departemen Geofisika dan Meteorologi FMIPA IPB Angkatan 2015, 2016, dan 2017. Tujuan penelitian ini adalah untuk menganalisis tingkat kepuasan pengguna portal data terhadap perolehan data iklim yang disediakan oleh BMKG. Pendekatan yang digunakan adalah pendekatan kuantitatif dengan metode survei menggunakan instrumen kuesioner dan didukung dengan data kualitatif dengan metode wawancara. Hasil penelitian ini menunjukkan bahwa mahasiswa Departemen Geofisika dan Meteorologi FMIPA IPB Angkatan 2015, 2016, dan 2017 tidak puas atas perolehan data iklim yang disediakan oleh BMKG. Hal ini ditinjau berdasarkan hubungan karakteristik pengguna dan perilaku penggunaan dengan tingkat kepuasan perolehan data iklim dari portal layanan data online BMKG.Kata Kunci: gratification, tingkat kepuasan, perilaku penggunaan media=====ABSTRACTPublic can access information such as Meteorology, Climatology, Air Quality and Geophysics data from various media used. The non-ministerial government institutions in Indonesia that are authorized for this data are the Badan Meteorologi, Klimatologi, dan Geofisika (BMKG). BMKG provides an online data service portal containing climate data. This portal is specifically used by students of the batch 2015, 2016 and 2017 from Department of Geophysics and Meteorology FMIPA IPB. The aim of this research is analyzing the satisfaction of data portal users on climate data acquisition provided by BMKG. The approach used is a quantitative approach with a survey method using a questionnaire instrument and supported by qualitative data with interview methods. The results of this study indicate that the students of the batch 2015, 2016, and 2017 from Department of Geophysics and Meteorology FMIPA IPB were not satisfied with the acquisition of climate data provided by BMKG. This was reviewed based on the relationship between user characteristics and usage behavior with satisfaction of climate data acquisition from BMKG's online data service portal.Keywords: gratification, satisfaction level, media use behavior
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5

Lockwood, Mike, and Mat Owens. "Cosmic meteorology." Astronomy & Geophysics 62, no. 3 (June 1, 2021): 3.12–3.19. http://dx.doi.org/10.1093/astrogeo/atab065.

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6

Crenner, Jim. "Hammock Meteorology." Iowa Review 40, no. 1 (April 2010): 80. http://dx.doi.org/10.17077/0021-065x.6851.

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7

MANNOJI, Nobutaka. "GPS Meteorology." Journal of the Visualization Society of Japan 16, no. 61 (1996): 107–11. http://dx.doi.org/10.3154/jvs.16.61_107.

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8

NAITO, Isao. "GPS Meteorology." Journal of Geography (Chigaku Zasshi) 109, no. 6 (2000): 964–70. http://dx.doi.org/10.5026/jgeography.109.6_964.

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9

Esau, Igor, Stefania Argentini, Rajmund Przybylak, Irina Repina, and Anna Sjöblom. "Svalbard Meteorology." Advances in Meteorology 2012 (2012): 1–3. http://dx.doi.org/10.1155/2012/818473.

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10

Etling, D. "Dynamic Meteorology." Eos, Transactions American Geophysical Union 68, no. 46 (1987): 1595. http://dx.doi.org/10.1029/eo068i046p01595-01.

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Дисертації з теми "Meteorology"

1

Johansson, Cecilia. "Influence of External Factors on the Turbulence Structure in the Atmospheric Boundary Layer." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2003. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-3221.

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The theory used in today’s weather- and climate models to describe processes near the earth’s surface, i.e. transport of heat, moisture and momentum between the ground and the atmosphere, is based on the idea that only local factors are important, such as temperature and wind speed near the ground. However, from measurements made at two sites, one agricultural and one marine, it has been found that large eddies, which are related to the convective boundary layer height, influence the turbulence structure near the ground during unstable conditions more than previously realized. Especially the momentum transport is affected. The large eddies have similar size over land and over the sea, typically 1000 m. The important difference being that over land diurnal variation plays a fundamental role; over the sea such variations are typically absent.

From the marine site it has also been found that the turbulence structure of the temperature field over the Baltic Sea is very different from over land. Instead of having a height dependence as expected from theory, the temperature structure seems to be constant with height within the surface layer.

Typically, the heat flux over the sea is smaller than over land during convective conditions. This gives rise to a turbulence transport regime which is fundamentally different from that observed during daytime convective conditions over land.

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2

Collins, Matthew. "The meteorology of Mars." Thesis, University of Reading, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.359043.

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3

Larson, Ellis, and Nelly Åkerblom. "Spectral clustering for Meteorology." Thesis, KTH, Skolan för teknikvetenskap (SCI), 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-297760.

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Climate is a tremendously complex topic, affecting many aspects of human activity and constantly changing. Defining some structures and rules for how it works is thereof of the utmost importance even though it might only cover a small part of the complexity. Cluster analysis is a tool developed in data analysis that is able to categorize data into groups of similar type. In this paper data from the Swedish Meteorological and Hydrological Institute (SMHI) is clustered to find a partitioning. The cluster analysis used is called Spectral clustering which is a family of methods making use of the spectral properties of graphs. Concrete results over different groupings of climate over Sweden were found.
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4

Björklund, Elin. "Observed Ice Supersaturated Layers over Sweden and Implications for Aviation Induced Contrails over the Baltic Sea." Thesis, Uppsala universitet, Luft-, vatten och landskapslära, 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-153694.

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In the atmosphere vertical extended layers that are in the state of super saturation with respect to ice can appear; these layers have been termed ice-supersaturated layers (ISSL). If an aircraft passes through an ISSL, persistent condensation trails can form. These contrails absorb the long wave radiation from the earth and reflect the incoming short wave radiation from space. The absorbing effect of the long wave radiation is although greater than the reflecting effect of the short wave radiation and therefore these contrails increase the greenhouse effect.This study contain statistics of when ice-supersaturated layers occur in the Swedish airspace, based on data from balloon soundings that take place each day at four locations in Sweden. The soundings that are used in this report were carried out from January 2006 to December of 2010. The results show that ISSL are more common in the Swedish airspace than expected. The layers are by average 42 hPa thick, located at the height of 339 hPa and are present in 44 % of the soundings.
I atmosfären kan det uppkomma vertikalt utsträckta skikt som är övermättade med avseende på is; dessa lager har blivit benämnda som ice-supersaturated layers (ISSL). Om ett flygplan flyger igenom dessa ISSL luftmassor kan permanenta kondensationsstrimmor bildas.Dessa kondensationsstrimmor absorberar den långvågiga strålningen från jorden och reflekterar den inkommande kortvågiga strålningen från rymden. Den absorberande effekten är större än den reflekterande effekten, vilket bidrar till en förstärkning av växthuseffekten. Den här studien innehåller statistik för när dessa ISSL uppkommer i det Svenska luftrummet, baserat på data från ballongsonderingar som var utförda från Januari 2006 till December 2010. Resultatet från denna statistik visar att ISSL är mer vanliga i det Svenska luftrummet än förväntat. Lagren är i medeltal 42 hPa tjocka, placerade på 339 hPa höjd och förekommer i 44 % av sonderingarna.
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5

Lindskog, Magnus. "On errors in meteorological data assimilation." Doctoral thesis, Stockholm : Department of Meteorology, Stockholm university, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-7258.

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6

Engström, Malin. "En studie av Uppsala stads värmeö." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-203057.

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The urban heat island is an area restricted to a city center where the temperatureis higher than its surrounding environment. The greatest temperature difference isfound at night when the weather is calm and the sky is clear of clouds. There are twomajor causes behind this phenomena and the first one is the use of energy forheating of houses. The heat leaks through the walls of the buildings and warms upthe surrounding mass of air. The second one is the use of building material whichstore the suns radiation on daytime and releases the heat during night. The heatisland leads to larger costs for cooling buildings. It also has an effect on humanhealth, since increased temperatures lead to heat stress which may be fatal. Thisreport aims to investigate if there is an urban heat island located over Uppsala cityand how it can affect daily life for the citizens. To find out how big the urban heatisland effect is in Uppsala city, a number of temperature measurements whereconducted. The results show that there is a visible temperature difference betweenurban and rural areas.
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7

Söder, Mats. "Growth and removal of inclusions during ladle refining." Doctoral thesis, KTH, Materials Science and Engineering, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-45.

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The overall purpose of this thesis work has been to further our understanding of the growth and removal of inclusions in gas- and induction-stirred ladles. The primary focus has been on alumina inclusions.

Growth mechanisms were studied using data from fundamental mathematical models of gas- and induction-stirred ladles. The results showed the turbulence mechanism to be the most dominant in alumina inclusion growth. The dynamic growth and removal of inclusions in a gas-stirred ladle was studied using mathematical modelling. The model results showed concentration gradients of inclusions. The effect was most obvious in the steel flow past the removal sites: top slag, ladle refractory, and gas plume (bubble flotation). A new removal model was developed for large spherical caps bubbles.

In order to verify the predicted concentration gradients for the size population of inclusions, three experiments were carried out in production. The sampling equipment enabled sampling at five different positions and different locations at the same time. The results showed that concentration gradients of inclusions do exist both in induction-stirred and gas-stirred ladles. A theoretical analysis showed that the drag force on the inclusions to be the dominating force and that therefore inclusions follow the fluid flow.

The cluster behaviour of alumina inclusions were examined on steel samples taken in an industrial-scale deoxidation experiment in a ladle. The samples were examined by microscope and the results used to study cluster growth. It was found that there was rapid cluster growth due to collision during stirring and that at the end of the deoxidation experiment a majority of the small inclusions were bound in clusters. The cluster growth data determined using the microscopic results were compared with predicted cluster-growth data. A method was developed for converting the experimental data observed per unit area into data given per unit volume and vice versa. An expression for the collision diameter of the cluster was also developed. The results showed that the predicted cluster growth agreed well with the microscopic observations for the assumptions made in the growth model.

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8

Tunved, Peter. "On the lifecycle of aerosol particles : Sources and dispersion over Scandinavia." Doctoral thesis, Stockholm : Meteorologiska institutionen (MISU), Univ, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-223.

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9

Sjöström, Stina. "Numerical exploration of radiative-dynamic interactions in cirrus." Thesis, Uppsala University, Department of Earth Sciences, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-8201.

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An important factor in forecast models today is cirrus clouds, but not much are known about their dynamics which makes them hard to parameterize. In this study a new theory was derived to enable a more correct way to describe the interplay between radiative heating and dynamical motions in these clouds. This hypothesis was tested by performing three dimensional simulations of cirrus clouds, using the University of Utah Large Eddy Simulator (UULES). Eleven clouds of varying initial radius and ice water mixing ratio were examined, with the aim of finding a pattern in their dynamical features. The model was set up without short wave radiation from the sun, and without any precipitation affecting the clouds, leaving only terrestrial heating and atmospheric cooling to create motions in the clouds. Two categories of initial dynamics could be seen:

• Isentropic adjustment: The isentropes within the cloud are adjusting to the environment due to rising of the cloud. Causes horizontal spreading through continuity.

• Density current: A dominating initial feature is spreading in small mixed layers at the cloud top and bottom. Caused by the density difference between the cloud and its environment.

An interesting phenomenon showing up in the simulations was mammatus clouds, which were visible in two of the cases. The only instability available to create these clouds was the radiative heating difference, which does not agree with present theories for how they form.

Two dimensionless numbers S and C were derived to describe the nature of the spreading motions and convection in the cloud. Both these numbers agreed with results.


Cirrusmoln har en viktig roll i dagens prognosmodeller, men är svåra att parametrisera på ett bra sätt eftersom man inte har tillräcklig kunskap om deras dynamik och utveckling. I denna studie togs en ny teori fram för att göra det möjligt att på ett mer korrekt sätt beskriva samspelet mellan strålningsuppvärmning och dynamiska rörelser i dessa moln. Hypotesen testades sedan genom att utföra tredimensionella simuleringar av cirrus moln med hjälp av University of Utah Large Eddy Simulator (UULES). Elva moln med varierande initiella radier och isvatteninnehåll undersöktes, med målet att finna ett mönster i dynamik och utveckling. UULES ställdes in så att miljön där molnen simulerades varken innehöll kortvågsstrålning från solen eller nederbörd. Således fanns det bara en resterande faktor för att skapa rörelser i molnen; skillnaden i den infraröda strålningsuppvärmningen mellan molntopp och molnbas. Två kategorier av initiella rörelser uppstod i molnen:

• Justering av isotroper: Molnen stiger i höjd vilket gör att isotroperna inuti dem justeras till omgivningen. Detta orsakar horisontell spridning genom kontinuitet.

• Densitets ström: Horisontell spridning av molnen koncentrerad till mixade skikt i de övre och undre delarna. Orsakas av skillnad i densitet mellan moln och omgivning.

Ett intressant fenomen som visade sig i två av simuleringarna var mammatusmoln. Den enda instabiliteten tillgänglig för att skapa dessa moln var skillnaden i strålningsuppvärmning mellan molntopp och -bas. Detta stämmer inte överrens med nuvarande teorier för hur dessa moln skapas.

Två dimensionslösa tal, S och C togs fram för att indikera vilken av de initiella rörelserna som dominerar i molnet, samt vilken typ av konvektion som dominerar. Båda dessa tal stämde väl överrens med resultat.

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10

Webber, Chris Paul. "Linking pollution, meteorology and climate change." Thesis, University of Reading, 2017. http://centaur.reading.ac.uk/73249/.

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This thesis examines the relationship between synoptic meteorology and particulate matter (PM10). PM10 is a pollutant of high interest to UK health policy (DEFRA, 2016) and this study evaluates the importance of Rossby wave breaking (RWB) on UK PM10 concentration ([PM10]). RWB can result in atmospheric blocking, which is one extreme of mid-latitude synoptic meteorological variability that favours the accumulation of PM10. This study finds significant increases (p < 0.01) in UK Midlands [PM10] resulting from winter-time northeast Atlantic/ European RWB. Furthermore, this study shows that northeast Atlantic/ European RWB increases the probability of exceeding a hazardous [PM10] threshold. We have identified the Omega block as the most hazardous RWB subset, with a probability of exceeding a hazardous [PM10] threshold (0.383) over three times that for days without RWB (0.129). We have implemented a tracer framework within a Hadley centre Met-Office climate model (HADGEM3-GA4) to identify flow regimes influencing the UK throughout northeast Atlantic/European RWB events. A present-day HADGEM3-GA4 simulation, nudged to ERA-Interim reanalysis data, is used to verify the tracer framework and to identify the flow regimes influencing Omega block events. This study finds that the advection of European tracer and the accumulation of locally sourced tracer contribute to hazardous [PM10] throughout Omega block events. This study’s principal aim is to determine climatic shifts in both the frequency of synoptic meteorological conditions conducive to UK PM10 accumulation and in the corresponding flow regimes. Using a further two HADGEM3-GA4 simulations, we find a north-eastward climate shift in northeast Atlantic/European RWB, with an overall reduction in events. Additionally, we find that uture RWB events result in significantly (p<0.01) increased European and reduced stagnant air masses within the UK. This result indicates a reduced frequency of UK [PM10] exceedances, however a tendency for increased transport of toxic particles from Europe.
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Книги з теми "Meteorology"

1

Ahrens, C. Donald. Essentials of meteorology: An invitation to the atmosphere. 4th ed. Belmont, CA: Thomson Brooks/Cole, 2005.

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2

Ahrens, C. Donald. Meteorology today: An introduction to weather, climate, and the environment. 2nd ed. St. Paul: West Pub. Co., 1985.

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3

Danielson, Eric William. Meteorology. 2nd ed. Boston: McGraw-Hill, 2003.

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4

1946-, Levin James, and Abrams Elliot 1947-, eds. Meteorology. Dubuque, IA: WCB/McGraw-Hill, 1998.

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5

Anthes, Richard A. Meteorology. 6th ed. New York: Macmillan Pub. Co., 1992.

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6

Panchev, S. Dynamic Meteorology. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5221-8.

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7

Grefen, K., and J. Löbel, eds. Environmental Meteorology. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2939-5.

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8

Raghavan, S. Radar Meteorology. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-017-0201-0.

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9

Rauber, Robert M., and Stephen W. Nesbitt. Radar Meteorology. Chichester, UK: John Wiley & Sons Ltd, 2018. http://dx.doi.org/10.1002/9781118432662.

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10

Krishnamurti, T. N., Lydia Stefanova, and Vasubandhu Misra. Tropical Meteorology. New York, NY: Springer New York, 2013. http://dx.doi.org/10.1007/978-1-4614-7409-8.

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Частини книг з теми "Meteorology"

1

Taub, Liba. "Meteorology." In A Companion to Science, Technology, and Medicine in Ancient Greece and Rome, 232–46. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2016. http://dx.doi.org/10.1002/9781118373057.ch14.

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2

Ziv, Baruch, Elad Shilo, Yury Lechinsky, and Alon Rimmer. "Meteorology." In Lake Kinneret, 81–96. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-017-8944-8_6.

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3

Wiin-Nielsen, Aksel C. "Meteorology." In Environmental Concerns, 91–107. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-2904-6_7.

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4

Nagarajan, R. "Meteorology." In Drought Assessment, 28–76. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-2500-5_2.

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5

Şen, Zekâi. "Meteorology." In Earth Systems Data Processing and Visualization Using MATLAB, 7–52. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01542-8_2.

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6

Pollitt, Christopher, Colin Talbot, Janice Caulfield, and Amanda Smullen. "Meteorology." In Agencies, 147–82. London: Palgrave Macmillan UK, 2005. http://dx.doi.org/10.1057/9780230504868_8.

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7

House, David. "Meteorology." In Seamanship Techniques, 425–75. 5th edition. | New York : Routledge, [2018]: Routledge, 2018. http://dx.doi.org/10.4324/9781315560250-12.

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8

Seshadri, V. "Meteorology." In The Inverse Gaussian Distribution, 230–31. New York, NY: Springer New York, 1999. http://dx.doi.org/10.1007/978-1-4612-1456-4_16.

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9

Foken, Thomas. "Applied Meteorology." In Micrometeorology, 315–26. Berlin, Heidelberg: Springer Berlin Heidelberg, 2017. http://dx.doi.org/10.1007/978-3-642-25440-6_8.

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10

Ahmad, Latief, Raihana Habib Kanth, Sabah Parvaze, and Syed Sheraz Mahdi. "Synoptic Meteorology." In Experimental Agrometeorology: A Practical Manual, 119–21. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-69185-5_16.

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Тези доповідей конференцій з теми "Meteorology"

1

Mazurkin, Petr. "QUANTUM METEOROLOGY." In 19th SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings. STEF92 Technology, 2019. http://dx.doi.org/10.5593/sgem2019/5.1/s20.077.

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2

Singh, Ram Chandra, and Rajeev Bhatla. "Wavelets in meteorology." In EMERGING APPLICATIONS OF WAVELET METHODS: 7th International Congress on Industrial and Applied Mathematics - Thematic Minisymposia. AIP, 2012. http://dx.doi.org/10.1063/1.4740045.

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3

HOFFMANN, GEERD-R. "GRID COMPUTING FOR METEOROLOGY." In Proceedings of the Ninth ECMWF Workshop on the Use of High Performance Computing in Meteorology. WORLD SCIENTIFIC, 2001. http://dx.doi.org/10.1142/9789812799685_0012.

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4

Guzzi, Rodolfo, Antonio Navarra, and Jagadish Shukla. "Meteorology and Environmental Sciences." In Course on Physical Climatology and Meteorology for Environmental Application. WORLD SCIENTIFIC, 1990. http://dx.doi.org/10.1142/9789814539722.

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5

Pries, Thomas H. "High-energy laser meteorology." In OE/LASE '90, 14-19 Jan., Los Angeles, CA, edited by Peter B. Ulrich and LeRoy E. Wilson. SPIE, 1990. http://dx.doi.org/10.1117/12.18347.

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6

Semenova, Nataliya V., Maksim Y. Chervyakov, Nadezhda V. Korotkova, and Elena V. Demidova. "ADDITIONAL EDUCATION IN METEOROLOGY." In Treshnikov readings – 2022 Modern geographical global picture and technology of geographic education. Ulyanovsk State Pedagogical University named after I. N. Ulyanov, 2022. http://dx.doi.org/10.33065/978-5-907216-88-4-2022-135-136.

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7

Bokal, Zhanna M., and Rustem B. Sinitsyn. "Random signal sodar for meteorology." In Photonics Applications in Astronomy, Communications, Industry, and High-Energy Physics Experiments 2009, edited by Ryszard S. Romaniuk and Krzysztof S. Kulpa. SPIE, 2009. http://dx.doi.org/10.1117/12.837997.

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8

Páta, Petr, Petr Janout, and Martin Blažek. "New generation of meteorology cameras." In Photonics Prague 2017, edited by Petr Páta and Karel Fliegel. SPIE, 2017. http://dx.doi.org/10.1117/12.2296846.

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9

Sand, Wayne, and Cleon Biter. "Meteorology surrounding the Roselawn accident." In 37th Aerospace Sciences Meeting and Exhibit. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1999. http://dx.doi.org/10.2514/6.1999-496.

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10

Dinoev, Todor, Alexander Hafele, Giovanni Martucci, Valentin B. Simeonov, Bertrand Calpini, Ilya Serikov, Sergei Bobrovnikov, and Daniel Leuenbergerd. "Raman lidar in operational meteorology." In Lidar Remote Sensing for Environmental Monitoring XVI, edited by Nobuo Sugimoto and Upendra N. Singh. SPIE, 2018. http://dx.doi.org/10.1117/12.2501987.

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Звіти організацій з теми "Meteorology"

1

Bruggeman, David, Marjorie Stockton, Kenneth Waight, Gregory Stanton, Melissa Coronado, and Jerome Quintana. Meteorology Program. Office of Scientific and Technical Information (OSTI), May 2022. http://dx.doi.org/10.2172/1868208.

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2

Hoitink, D. J. Climate and meteorology. Office of Scientific and Technical Information (OSTI), June 1995. http://dx.doi.org/10.2172/433025.

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3

Bruggeman, David Alan. LANL Meteorology Program. Office of Scientific and Technical Information (OSTI), August 2017. http://dx.doi.org/10.2172/1373533.

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4

Dewart, Jean Marie. LANL Meteorology Program. Office of Scientific and Technical Information (OSTI), February 2015. http://dx.doi.org/10.2172/1169672.

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5

Bruggeman, David, Kenneth Waight, Gregory Stanton, and Melissa Coronado. LANL Meteorology Program. Office of Scientific and Technical Information (OSTI), April 2021. http://dx.doi.org/10.2172/1776737.

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6

Dewart, Jean Marie. LANL Meteorology Program FY15. Office of Scientific and Technical Information (OSTI), August 2015. http://dx.doi.org/10.2172/1211602.

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7

Bruggeman, David Alan. Meteorology Tower Site Inspections. Office of Scientific and Technical Information (OSTI), August 2018. http://dx.doi.org/10.2172/1467188.

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8

Kane, D. L. Arctic hydrology and meteorology. Office of Scientific and Technical Information (OSTI), January 1989. http://dx.doi.org/10.2172/5118378.

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Kane, D. L. Arctic hydrology and meteorology. Office of Scientific and Technical Information (OSTI), January 1988. http://dx.doi.org/10.2172/5118405.

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10

Kane, D. L. Arctic hydrology and meteorology. Office of Scientific and Technical Information (OSTI), January 1990. http://dx.doi.org/10.2172/5142270.

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