Relevant bibliographies by topics / Atmospheric changes

Contents

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

Academic literature on the topic 'Atmospheric changes'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Atmospheric changes"

1

Piver, W. T. "Global atmospheric changes." Environmental Health Perspectives 96 (December 1991): 131–37. http://dx.doi.org/10.1289/ehp.9196131.

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Johnstone, C. P., M. Güdel, H. Lammer, and K. G. Kislyakova. "Upper atmospheres of terrestrial planets: Carbon dioxide cooling and the Earth’s thermospheric evolution." Astronomy & Astrophysics 617 (September 2018): A107. http://dx.doi.org/10.1051/0004-6361/201832776.

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Context.The thermal and chemical structures of the upper atmospheres of planets crucially influence losses to space and must be understood to constrain the effects of losses on atmospheric evolution.Aims.We develop a 1D first-principles hydrodynamic atmosphere model that calculates atmospheric thermal and chemical structures for arbitrary planetary parameters, chemical compositions, and stellar inputs. We apply the model to study the reaction of the Earth’s upper atmosphere to large changes in the CO2abundance and to changes in the input solar XUV field due to the Sun’s activity evolution from 3 Gyr in the past to 2.5 Gyr in the future.Methods.For the thermal atmosphere structure, we considered heating from the absorption of stellar X-ray, UV, and IR radiation, heating from exothermic chemical reactions, electron heating from collisions with non-thermal photoelectrons, Joule heating, cooling from IR emission by several species, thermal conduction, and energy exchanges between the neutral, ion, and electron gases. For the chemical structure, we considered ~500 chemical reactions, including 56 photoreactions, eddy and molecular diffusion, and advection. In addition, we calculated the atmospheric structure by solving the hydrodynamic equations. To solve the equations in our model, we developed the Kompot code and have provided detailed descriptions of the numerical methods used in the appendices.Results.We verify our model by calculating the structures of the upper atmospheres of the modern Earth and Venus. By varying the CO2abundances at the lower boundary (65 km) of our Earth model, we show that the atmospheric thermal structure is significantly altered. Increasing the CO2abundances leads to massive reduction in thermospheric temperature, contraction of the atmosphere, and reductions in the ion densities indicating that CO2can significantly influence atmospheric erosion. Our models for the evolution of the Earth’s upper atmosphere indicate that the thermospheric structure has not changed significantly in the last 2 Gyr and is unlikely to change signficantly in the next few Gyr. The largest changes that we see take place between 3 and 2 Gyr ago, with even larger changes expected at even earlier times.
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Aplin, K. L., C. J. Scott, and S. L. Gray. "Atmospheric changes from solar eclipses." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 374, no. 2077 (September 28, 2016): 20150217. http://dx.doi.org/10.1098/rsta.2015.0217.

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This article reviews atmospheric changes associated with 44 solar eclipses, beginning with the first quantitative results available, from 1834 (earlier qualitative accounts also exist). Eclipse meteorology attracted relatively few publications until the total solar eclipse of 16 February 1980, with the 11 August 1999 eclipse producing the most papers. Eclipses passing over populated areas such as Europe, China and India now regularly attract scientific attention, whereas atmospheric measurements of eclipses at remote locations remain rare. Many measurements and models have been used to exploit the uniquely predictable solar forcing provided by an eclipse. In this paper, we compile the available publications and review a subset of them chosen on the basis of importance and novelty. Beyond the obvious reduction in incoming solar radiation, atmospheric cooling from eclipses can induce dynamical changes. Observations and meteorological modelling provide evidence for the generation of a local eclipse circulation that may be the origin of the ‘eclipse wind’. Gravity waves set up by the eclipse can, in principle, be detected as atmospheric pressure fluctuations, though theoretical predictions are limited, and many of the data are inconclusive. Eclipse events providing important early insights into the ionization of the upper atmosphere are also briefly reviewed. This article is part of the themed issue ‘Atmospheric effects of solar eclipses stimulated by the 2015 UK eclipse’.
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Trenberth, Kevin E. "Atmospheric circulation climate changes." Climatic Change 31, no. 2-4 (December 1995): 427–53. http://dx.doi.org/10.1007/bf01095156.

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Lee, Ariel, Mehdi Abouzari, and Hamid Djalilian. "Symptom: Dizziness with Atmospheric Changes." Hearing Journal 73, no. 10 (October 2020): 30,32,33. http://dx.doi.org/10.1097/01.hj.0000719812.50617.36.

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Choi, Nakbin, Myong-In Lee, Dong-Hyun Cha, Young-Kwon Lim, and Kyu-Myong Kim. "Decadal Changes in the Interannual Variability of Heat Waves in East Asia Caused by Atmospheric Teleconnection Changes." Journal of Climate 33, no. 4 (February 15, 2020): 1505–22. http://dx.doi.org/10.1175/jcli-d-19-0222.1.

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AbstractThe heat wave in East Asia is examined by using empirical orthogonal function analysis to isolate dominant heat-wave patterns in the ground-based temperature observations over the Korean Peninsula and China and related large-scale atmospheric circulations obtained from the National Centers for Environmental Prediction–National Center for Atmospheric Research Reanalysis 1 during 1973–2012. This study focuses particularly on the interannual variability of heat waves and its decadal change. The analysis identifies two major atmospheric teleconnection patterns playing an important role in developing typical heat-wave patterns in East Asia—the Scandinavian (SCAND) and the circumglobal teleconnection (CGT) patterns, which exhibit a significant decadal change in the interannual variability in the mid-1990s. Before the mid-1990s, heat-wave occurrence was closely related to the CGT pattern, whereas the SCAND pattern is more crucial to explain heat-wave variability in the recent period. The stationary wave model experiments suggest an intensification of the SCAND pattern in the recent period driven by an increase in land–atmosphere interaction over Eurasia and decadal change in the dominant heat-wave patterns in East Asia.
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Kubát, Jiří. "NLTE Model Atmospheres of Irradiated Stars in B Binaries." International Astronomical Union Colloquium 175 (2000): 705–8. http://dx.doi.org/10.1017/s0252921100056797.

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AbstractModel atmospheres of B stars irradiated by their companion are calculated using our model atmosphere computer code under the assumption of hydrostatic, radiative, and statistical equilibrium (NLTE). The external source of radiation (a hot white dwarf) is able to change the temperature structure of the outer atmospheric layers of B stars significantly. The changes of the temperature structure cause changes in the profiles of some lines, especially in those of hydrogen.
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Laguë, Marysa M., Gordon B. Bonan, and Abigail L. S. Swann. "Separating the Impact of Individual Land Surface Properties on the Terrestrial Surface Energy Budget in both the Coupled and Uncoupled Land–Atmosphere System." Journal of Climate 32, no. 18 (August 12, 2019): 5725–44. http://dx.doi.org/10.1175/jcli-d-18-0812.1.

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Abstract Changes in the land surface can drive large responses in the atmosphere on local, regional, and global scales. Surface properties control the partitioning of energy within the surface energy budget to fluxes of shortwave and longwave radiation, sensible and latent heat, and ground heat storage. Changes in surface energy fluxes can impact the atmosphere across scales through changes in temperature, cloud cover, and large-scale atmospheric circulation. We test the sensitivity of the atmosphere to global changes in three land surface properties: albedo, evaporative resistance, and surface roughness. We show the impact of changing these surface properties differs drastically between simulations run with an offline land model, compared to coupled land–atmosphere simulations that allow for atmospheric feedbacks associated with land–atmosphere coupling. Atmospheric feedbacks play a critical role in defining the temperature response to changes in albedo and evaporative resistance, particularly in the extratropics. More than 50% of the surface temperature response to changing albedo comes from atmospheric feedbacks in over 80% of land areas. In some regions, cloud feedbacks in response to increased evaporative resistance result in nearly 1 K of additional surface warming. In contrast, the magnitude of surface temperature responses to changes in vegetation height are comparable between offline and coupled simulations. We improve our fundamental understanding of how and why changes in vegetation cover drive responses in the atmosphere, and develop understanding of the role of individual land surface properties in controlling climate across spatial scales—critical to understanding the effects of land-use change on Earth’s climate.
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Stauffer, B., H. Oeschger, and J. Schwander. "Changes Of Atmospheric Methane Concentration Parallel To Climatic Changes." Annals of Glaciology 14 (1990): 359. http://dx.doi.org/10.1017/s0260305500009368.

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Measurements on ice-core samples showed that atmospheric methane concentration changed with the large climatic cycles during the last two glaciations (Stauffer and others, 1988; Raynaud and others, 1988). The methane concentration is lower in cold periods and higher in warm periods. In this paper we discuss the results of CH4 measurements of samples from periods of minor climatic change, like the climatic optimum 8000 years B.P. and the Younger Dryas period about 10 000 to 11 000 years B.P.. The data are interpreted in terms of the present understanding of methane sources and sinks.
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Stauffer, B., H. Oeschger, and J. Schwander. "Changes Of Atmospheric Methane Concentration Parallel To Climatic Changes." Annals of Glaciology 14 (1990): 359. http://dx.doi.org/10.3189/s0260305500009368.

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Measurements on ice-core samples showed that atmospheric methane concentration changed with the large climatic cycles during the last two glaciations (Stauffer and others, 1988; Raynaud and others, 1988). The methane concentration is lower in cold periods and higher in warm periods. In this paper we discuss the results of CH4 measurements of samples from periods of minor climatic change, like the climatic optimum 8000 years B.P. and the Younger Dryas period about 10 000 to 11 000 years B.P.. The data are interpreted in terms of the present understanding of methane sources and sinks.
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Dissertations / Theses on the topic "Atmospheric changes"

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Doi, Koichiro. "Study on Gravity Changes Induced by Atmospheric Loading." 京都大学 (Kyoto University), 1992. http://hdl.handle.net/2433/168819.

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本文データは平成22年度国立国会図書館の学位論文(博士)のデジタル化実施により作成された画像ファイルを基にpdf変換したものである
Kyoto University (京都大学)
0048
新制・課程博士
博士(理学)
甲第4973号
理博第1370号
新制||理||765(附属図書館)
UT51-92-J20
京都大学大学院理学研究科地球物理学専攻
(主査)教授 中川 一郎, 教授 田中 寅夫, 教授 住友 則彦
学位規則第4条第1項該当
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Thompson, David W. J. "Annular modes in the atmospheric general circulation /." Thesis, Connect to this title online; UW restricted, 2000. http://hdl.handle.net/1773/10057.

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Bayr, Tobias [Verfasser]. "Tropical atmospheric circulation changes under global warming / Tobias Bayr." Kiel : Universitätsbibliothek Kiel, 2013. http://d-nb.info/1045194751/34.

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Rennert, Kevin J. "Relationships between wintertime modes of atmospheric variability on intermediate and long timescales /." Thesis, Connect to this title online; UW restricted, 2007. http://hdl.handle.net/1773/10089.

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Osterberg, Erich Christian. "North Pacific Late Holocene Climate Variability and Atmospheric Composition." Fogler Library, University of Maine, 2007. http://www.library.umaine.edu/theses/pdf/OsterbergEC2007.pdf.

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Manning, Amanda J. L. "Radiative transfer in the middle atmosphere." Thesis, University of Oxford, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.279907.

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Avise, Jeremy Charles. "Global change and regional air quality impacts of climate, land-use, and emissions changes /." Online access for everyone, 2007. http://www.dissertations.wsu.edu/Dissertations/Fall2007/J_Avise_120907.pdf.

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Gottschalk, Julia. "The role of the Southern Ocean in millennial-scale atmospheric CO₂ changes." Thesis, University of Cambridge, 2015. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.709208.

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Mooring, Todd A. "Changes in atmospheric eddy length with the seasonal cycle and global warming." Thesis, Massachusetts Institute of Technology, 2011. http://hdl.handle.net/1721.1/65599.

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Thesis (S.B.)--Massachusetts Institute of Technology, Dept. of Physics; and, (S.B.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2011.
Cataloged from PDF version of thesis.
Includes bibliographical references (p. 59-60).
A recent article by Kidston et al. [8] demonstrates that the length of atmospheric eddies increases in simulations of future global warming. This thesis expands on Kidston et al.'s work with additional studies of eddy length in the NCEP2 reanalysis (a model-data synthesis that reconstructs past atmospheric circulation) and general circulation models (GCMs) from the Coupled Model Intercomparison Project phase 3. Eddy lengths are compared to computed values of the Rossby radius and the Rhines scale, which have been hypothesized to set the eddy length. The GCMs reproduce the seasonal variation in the eddy lengths seen in the reanalysis. To explore the effect of latent heating on the eddies, a modification to the static stability is used to calculate an effective Rossby radius. The effective Rossby radius is an improvement over the traditional dry Rossby radius in predicting the seasonal cycle of northern hemisphere eddy length, if the height scale used for calculation of the Rossby radius is the depth of the free troposphere. There is no improvement if the scale height is used instead of the free troposphere depth. However, both Rossby radii and the Rhines scale fail to explain the weaker seasonal cycle in southern hemisphere eddy length. In agreement with Kidson et al., the GCMs robustly project an increase in eddy length as the climate warms. The Rossby radii and Rhines scale are also generally projected to increase. Although it is not possible to state with confidence what process ultimately controls atmospheric eddy lengths, taken as a whole the results of this study increase confidence in the projection of future increases in eddy length.
by Todd A. Mooring.
S.B.
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Quadrelli, Roberta. "Patterns of climate variability of the Northern Hemisphere wintertime circulation /." Thesis, Connect to this title online; UW restricted, 2004. http://hdl.handle.net/1773/10058.

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Books on the topic "Atmospheric changes"

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Global and regional changes in atmospheric composition. Boca Raton, FL: Lewis Publishers, 1993.

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Budyko, M. I. Istorii͡a︡ atmosfery. Leningrad: Gidrometeoizdat, 1985.

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Borisovich, Ronov Aleksandr, and I͡A︡nshin Aleksandr Leonidovich 1911-, eds. History of the Earth's atmosphere. Berlin: Springer-Verlag, 1987.

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W, Johnson R. Volcanic eruptions & atmospheric change. Canberra: Australian Geological Survey Organisation, Dept. of Primary Industries and Energy, 1993.

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Graedel, T. E. Atmospheric change: An Earth system perspective. New York: W.H. Freeman, 1993.

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The atmosphere and climate change: An introduction. Dubuque, Iowa: Kendall/Hunt Pub. Co., 1994.

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Fiduciary duty and the atmospheric trust. Farnham, Surrey, England: Ashgate Pub. Company, 2011.

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Fiduciary duty and the atmospheric trust. Farnham, Surrey, England: Ashgate Pub. Company, 2011.

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H, Baker Samantha M., Reis Stefan, and SpringerLink (Online service), eds. Atmospheric Ammonia: Detecting emission changes and environmental impacts. Dordrecht: Springer Netherlands, 2009.

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Natty, Urquizo, Auld H, and Canada Environment Canada, eds. Atmospheric change in Canada: An integrated overview. [Ottawa]: Environment Canada, 1999.

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Book chapters on the topic "Atmospheric changes"

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Jin, Shuanggen, R. Jin, and X. Liu. "Atmospheric Changes and Observations." In GNSS Atmospheric Seismology, 15–29. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-10-3178-6_2.

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Kumar, Har Darshan, and Donat-P. Häder. "Ozone Changes." In Global Aquatic and Atmospheric Environment, 257–340. Berlin, Heidelberg: Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-642-60070-8_4.

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Trenberth, Kevin E. "Atmospheric Circulation Climate Changes." In Long-Term Climate Monitoring by the Global Climate Observing System, 297–323. Dordrecht: Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-011-0323-7_16.

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Lin, Hua. "Changes in Atmospheric Carbon Dioxide." In Global Environmental Change, 61–67. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-5784-4_48.

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Roscoe, H. K., B. J. Kerridge, L. J. Gray, R. J. Wells, and J. A. Pyle. "Comparisons of Measured and Predicted Diurnal Changes in Stratospheric NO and NO2." In Atmospheric Ozone, 173–74. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5313-0_35.

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Micu, Dana Magdalena, Alexandru Dumitrescu, Sorin Cheval, and Marius-Victor Birsan. "Projections of Future Changes in Climate of the Romanian Carpathians." In Springer Atmospheric Sciences, 199–205. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-02886-6_10.

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Vogel, G., U. Schubert, and D. Spänkuch. "Regional Distribution of Total Column Ozone Changes in Central Europe." In Atmospheric Ozone Dynamics, 311–25. Berlin, Heidelberg: Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60797-4_26.

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Simon, Paul C. "Atmospheric Changes and UV-B Monitoring." In The Role of the Stratosphere in Global Change, 403–23. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-78306-7_20.

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Jucks, K. W., and R. J. Salawitch. "Future changes in upper stratospheric ozone." In Atmospheric Science Across the Stratopause, 241–55. Washington, D. C.: American Geophysical Union, 2000. http://dx.doi.org/10.1029/gm123p0241.

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Hasebe, Fumio. "The Interannual Variations of the Global Total Ozone as a Reflection of the General Circulation Changes in the Stratosphere." In Atmospheric Ozone, 553–57. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5313-0_110.

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Conference papers on the topic "Atmospheric changes"

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Vasil'ev, Denis Y., Vladimir Semenov, and Vladimir Vodopyanov. "Climatic changes on the Southern Urals." In XXV International Symposium, Atmospheric and Ocean Optics, Atmospheric Physics, edited by Gennadii G. Matvienko and Oleg A. Romanovskii. SPIE, 2019. http://dx.doi.org/10.1117/12.2539064.

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MEASE, KENNETH, and NGUYEN VINH. "Orbital changes during hypersonic aerocruise." In 14th Atmospheric Flight Mechanics Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1987. http://dx.doi.org/10.2514/6.1987-2564.

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Karakhanyan, Ashkhen, and Sergey Molodykh. "Changes in temperature field under external impact considering humidity." In XXIV International Symposium, Atmospheric and Ocean Optics, Atmospheric Physics, edited by Oleg A. Romanovskii and Gennadii G. Matvienko. SPIE, 2018. http://dx.doi.org/10.1117/12.2504444.

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Dyukarev, E. A., and Victor I. Shishlov. "Analysis of climatic changes using phase portraits." In Eighth Joint International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, edited by Gelii A. Zherebtsov, Gennadii G. Matvienko, Viktor A. Banakh, and Vladimir V. Koshelev. SPIE, 2002. http://dx.doi.org/10.1117/12.458514.

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Dyukarev, E. A., and Victor I. Shishlov. "Estimation of aperiodic changes of climate parameters." In Eighth Joint International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, edited by Gelii A. Zherebtsov, Gennadii G. Matvienko, Viktor A. Banakh, and Vladimir V. Koshelev. SPIE, 2002. http://dx.doi.org/10.1117/12.458515.

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Sidorenkov, N. S. "The geodynamic reasons of decade changes of climate." In Eighteenth International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, edited by Oleg A. Romanovskii. SPIE, 2012. http://dx.doi.org/10.1117/12.2008803.

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Ganagina, Irina, Vadim Kanushin, Denis Goldobin, Elena Gienko, and Inna Dorogova. "Seasonal changes of Earth’s gravitational field due to solid precipitation." In XXV International Symposium, Atmospheric and Ocean Optics, Atmospheric Physics, edited by Gennadii G. Matvienko and Oleg A. Romanovskii. SPIE, 2019. http://dx.doi.org/10.1117/12.2540317.

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Lomakina, N. Ya, V. S. Komarov, S. N. Il'in, and A. V. Lavrinenko. "Long-term changes of low stratiform clouds over the Siberian region." In XXI International Symposium Atmospheric and Ocean Optics. Atmospheric Physics, edited by Oleg A. Romanovskii. SPIE, 2015. http://dx.doi.org/10.1117/12.2203350.

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Lomakina, N. Ya, V. S. Komarov, S. N. Il'in, and A. V. Lavrinenko. "Long-term changes in average seasonal surface air temperature over Siberia." In XXII International Symposium Atmospheric and Ocean Optics. Atmospheric Physics, edited by Gennadii G. Matvienko and Oleg A. Romanovskii. SPIE, 2016. http://dx.doi.org/10.1117/12.2248531.

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Kuzin, Viktor I., and Natalya A. Lapteva. "Assessment of changes in hydrology of Siberia in the XXIst century." In XXII International Symposium Atmospheric and Ocean Optics. Atmospheric Physics, edited by Gennadii G. Matvienko and Oleg A. Romanovskii. SPIE, 2016. http://dx.doi.org/10.1117/12.2249037.

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Reports on the topic "Atmospheric changes"

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Zdanowicz, C. Ice-core based studies of climate and atmospheric changes. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/290196.

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Reck, R. A., R. M. Bornick, G. Wen, J. E. Frederick, and B. L. Weinberg. A new approach to the characterization of long-term changes in total atmospheric ozone: Applications of frequency and extreme value statistics. Office of Scientific and Technical Information (OSTI), February 1996. http://dx.doi.org/10.2172/207600.

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McCoy, Kelly, Michael Bell, and Emmi Felker-Quinn. Risk to epiphytic lichen communities in NPS units from atmospheric nitrogen and sulfur pollution: Changes in critical load exceedances from 2001‒2016. National Park Service, August 2021. http://dx.doi.org/10.36967/nrr-2287254.

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Douglas, Thomas, Matthew Sturm, Joel Blum, Christopher Polashenski, Svetlana Stuefer, Christopher Hiemstra, Alexandra Steffen, Simon Filhol, and Romain Prevost. A pulse of mercury and major ions in snowmelt runoff from a small Arctic Alaska watershed. Engineer Research and Development Center (U.S.), July 2021. http://dx.doi.org/10.21079/11681/41203.

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Atmospheric mercury (Hg) is deposited to Polar Regions during springtime atmospheric mercury depletion events (AMDEs) that require halogens and snow or ice surfaces. The fate of this Hg during and following snowmelt is largely unknown. We measured Hg, major ions, and stable water isotopes from the snowpack through the entire spring melt runoff period for two years. Our small (2.5 ha) watershed is near Barrow (now Utqiaġvik), Alaska. We measured discharge, made 10 000 snow depths, and collected over 100 samples of snow and meltwater for chemical analysis in 2008 and 2009 from the watershed snowpack and ephemeral stream channel. Our results suggest AMDE Hg complexed with Cl⁻ or Br⁻ may be less likely to be photochemically reduced and re-emitted to the atmosphere prior to snowmelt, and we estimate that roughly 25% of the Hg in snowmelt is attributable to AMDEs. Projected Arctic warming, with more open sea ice leads providing halogen sources that promote AMDEs, may provide enhanced Hg deposition, reduced Hg emission and, ultimately, an increase in snowpack and snowmelt runoff Hg concentrations.
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Moraes, Jr., Francis Perry. The global change research center atmospheric chemistry model. Office of Scientific and Technical Information (OSTI), January 1995. http://dx.doi.org/10.2172/576052.

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Smith, J., and H. G. Hughes. Atmospheric Transmittance Determination from a Two-Angle Measurement of Radiance Change. Fort Belvoir, VA: Defense Technical Information Center, September 1989. http://dx.doi.org/10.21236/ada213847.

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Skyllingstad, Eric D. Modeling of the Atmospheric Circulation in the Santa Barbara Channel. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada613938.

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8

Gadwall, V. M., D. J. Belanger, A. E. Barrios, S. Ramlall, and B. C. Hobson. Wideband Channel Modeling in Real Atmospheric Environments with Experimental Evaluation. Fort Belvoir, VA: Defense Technical Information Center, April 2013. http://dx.doi.org/10.21236/ada585590.

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9

Peng, Tsung-Hung. (The cause of the glacial to interglacial atmospheric CO sub 2 change). Office of Scientific and Technical Information (OSTI), October 1989. http://dx.doi.org/10.2172/5415298.

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10

Houghton, R. A. Carbon Flux to the Atmosphere from Land-Use Changes: 1850 to 1990. Office of Scientific and Technical Information (OSTI), February 2001. http://dx.doi.org/10.2172/775411.

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