Relevant bibliographies by topics / Global atmospheric changes

Contents

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

Academic literature on the topic 'Global atmospheric changes'

Author: Grafiati
Published: 28 July 2024
Last updated: 31 July 2025

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Journal articles on the topic "Global atmospheric changes"

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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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Koval, Andrey, Nikolay Gavrilov, Anastasiya Golovko, Kseniia Didenko, and Tatiana Ermakova. "Modeling the impact of solar activity variations on global atmospheric circulation." Solar-Terrestrial Physics 10, no. 2 (2024): 111–18. http://dx.doi.org/10.12737/stp-102202411.

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In this study, we continue a series of works devoted to modeling and studying the sensitivity of global atmospheric dynamic processes to variations in solar emissions during the 11-year solar activity (SA) cycle. We focus on studying the response of meridional atmospheric circulation in the middle atmosphere to changes in thermosphere characteristics with changes in SA. For this purpose, numerical simulations of the general atmospheric circulation were carried out using the nonlinear numerical circulation model of the middle and upper atmosphere MUAM. The main mechanism of the influence of the
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Stephens, Graeme L., and Todd D. Ellis. "Controls of Global-Mean Precipitation Increases in Global Warming GCM Experiments." Journal of Climate 21, no. 23 (2008): 6141–55. http://dx.doi.org/10.1175/2008jcli2144.1.

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Abstract This paper examines the controls on global precipitation that are evident in the transient experiments conducted using coupled climate models collected for the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4). The change in precipitation, water vapor, clouds, and radiative heating of the atmosphere evident in the 1% increase in carbon dioxide until doubled (1pctto2x) scenario is examined. As noted in other studies, the ensemble-mean changes in water vapor as carbon dioxide is doubled occur at a rate similar to that predicted by the Clausius–Clapeyron rel
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Koval, Andrey, Nikolay Gavrilov, Anastasiya Golovko, Kseniia Didenko, and Tatiana Ermakova. "Modeling the impact of solar activity variations on global atmospheric circulation." Solnechno-Zemnaya Fizika 10, no. 2 (2024): 119–26. http://dx.doi.org/10.12737/szf-102202411.

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In this study, we continue a series of works devoted to modeling and studying the sensitivity of global atmospheric dynamic processes to variations in solar emissions during the 11-year solar activity (SA) cycle. We focus on studying the response of meridional atmospheric circulation in the middle atmosphere to changes in thermosphere characteristics with changes in SA. For this purpose, numerical simulations of the general atmospheric circulation were carried out using the nonlinear numerical circulation model of the middle and upper atmosphere MUAM. The main mechanism of the influence of the
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Pendergrass, Angeline G., and Dennis L. Hartmann. "The Atmospheric Energy Constraint on Global-Mean Precipitation Change." Journal of Climate 27, no. 2 (2014): 757–68. http://dx.doi.org/10.1175/jcli-d-13-00163.1.

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Abstract Models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) robustly predict that the rate of increase in global-mean precipitation with global-mean surface temperature increase is much less than the rate of increase of water vapor. The goal of this paper is to explain in detail the mechanisms by which precipitation increase is constrained by radiative cooling. Changes in clear-sky atmospheric radiative cooling resulting from changes in temperature and humidity in global warming simulations are in good agreement with the multimodel, global-mean precipitation increase proj
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Dlugokencky, Edward J., Euan G. Nisbet, Rebecca Fisher, and David Lowry. "Global atmospheric methane: budget, changes and dangers." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 369, no. 1943 (2011): 2058–72. http://dx.doi.org/10.1098/rsta.2010.0341.

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A factor of 2.5 increase in the global abundance of atmospheric methane (CH 4 ) since 1750 contributes 0.5 Wm −2 to total direct radiative forcing by long-lived greenhouse gases (2.77 Wm −2 in 2009), while its role in atmospheric chemistry adds another approximately 0.2 Wm −2 of indirect forcing. Since CH 4 has a relatively short lifetime and it is very close to a steady state, reductions in its emissions would quickly benefit climate. Sensible emission mitigation strategies require quantitative understanding of CH 4 ’s budget of emissions and sinks. Atmospheric observations of CH 4 abundance
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Trenberth, Kevin E. "Atmospheric circulation climate changes." Climatic Change 31, no. 2-4 (1995): 427–53. http://dx.doi.org/10.1007/bf01095156.

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Akιn, C., K. Heng, J. M. Mendonça, R. Deitrick, and L. Gkouvelis. "Global flow regimes of hot Jupiters." Astronomy & Astrophysics 699 (July 2025): A74. https://doi.org/10.1051/0004-6361/202453597.

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Context. The atmospheric dynamics of hot and ultrahot Jupiters are influenced by the stellar irradiation they receive, which shapes their atmospheric circulation and the underlying wave structures. Aims. We aim to investigate how variations in radiative and dynamical timescales influence global flow regimes, atmospheric circulation efficiency, and the interplay of wave structures across a curated sample of hot Jupiters. In particular, we explore a previously predicted transition in the global flow regime, where enhanced stellar irradiation suppresses the smaller-scale wave and eddy features th
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Ackerley, Duncan, Eleanor J. Highwood, David J. Frame, and Ben B. B. Booth. "Changes in the Global Sulfate Burden due to Perturbations in Global CO2 Concentrations." Journal of Climate 22, no. 20 (2009): 5421–32. http://dx.doi.org/10.1175/2009jcli2536.1.

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Abstract A large ensemble of general circulation model (GCM) integrations coupled to a fully interactive sulfur cycle scheme were run on the climateprediction.net platform to investigate the uncertainty in the climate response to sulfate aerosol and carbon dioxide (CO2) forcing. The sulfate burden within the model (and the atmosphere) depends on the balance between formation processes and deposition (wet and dry). The wet removal processes for sulfate aerosol are much faster than dry removal and so any changes in atmospheric circulation, cloud cover, and precipitation will feed back on the sul
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Liu, Chaoyu, Zizheng Meng, and Tangzihan Xia. "A Categorization of the Global Fair-weather Electric Field According to Position and Weather Conditions." E3S Web of Conferences 553 (2024): 03014. http://dx.doi.org/10.1051/e3sconf/202455303014.

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Atmospheric electricity is an important branch of physics, which mainly studies various electrical phenomena occurring in the atmosphere and the action process of various parameters in the atmosphere. This paper categorizes and integrates research literature based on different spaces and weather conditions. It focuses on analyzing specific regions and meteorological activities and obtains important conclusions. There is a certain correlation between atmospheric electric field and geological conditions, aerosol concentration, and atmospheric particle concentration, among other influencing facto
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Dissertations / Theses on the topic "Global atmospheric changes"

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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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Rosa, José Wilson Corrêa. "Global plate reconstructions, the area-age relationship, and global changes in sea level." Thesis, Massachusetts Institute of Technology, 1989. http://hdl.handle.net/1721.1/60421.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1990.<br>Archives copy lacks leaf 247.<br>15 folded maps in pocket.<br>Includes bibliographical references (leaves 120-140).<br>by José Wilson Corrêa Rosa.<br>Ph.D.
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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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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.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (p. 59-60).<br>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) a
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Braganza, Karl 1971. "Climate change detection and attribution using simple global indices." Monash University, School of Mathematical Sciences, 2002. http://arrow.monash.edu.au/hdl/1959.1/7783.

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Otto, James. "A Search for Periodic and Quasi-Periodic Patterns in Select Proxy Data with a Goal to Understanding Temperature Variation." Thesis, University of North Texas, 2005. https://digital.library.unt.edu/ark:/67531/metadc849601/.

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In this work over 200 temperature proxy data sets have been analyzed to determine if periodic and or quasi-periodic patterns exist in the data sets. References to the journal articles where data are recorded are provided. Chapter 1 serves an introduction to the problem of temperature determination in providing information on how various proxy data sources are derived. Examples are given of the techniques followed in producing proxy data that predict temperature for each method used. In chapter 2 temperature proxy data spanning the last 4000 years, from 2,000 BCE to 2,000 CE, are analyzed to
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Otto, James (James Robert). "A Search for Periodic and Quasi-Periodic Patterns in Select Proxy Data with a Goal to Understanding Temperature Variation." Thesis, University of North Texas, 2016. https://digital.library.unt.edu/ark:/67531/metadc849601/.

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In this work over 200 temperature proxy data sets have been analyzed to determine if periodic and or quasi-periodic patterns exist in the data sets. References to the journal articles where data are recorded are provided. Chapter 1 serves an introduction to the problem of temperature determination in providing information on how various proxy data sources are derived. Examples are given of the techniques followed in producing proxy data that predict temperature for each method used. In chapter 2 temperature proxy data spanning the last 4000 years, from 2,000 BCE to 2,000 CE, are analyzed to
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Leung, Wai-hung. "Global climate change : environmental implications for Hong Kong /." Hong Kong : University of Hong Kong, 1996. http://sunzi.lib.hku.hk/hkuto/record.jsp?B17457294.

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Nettleton, Stuart John. "Benchmarking climate change strategies under constrained resource usage /." Electronic version, 2009. http://utsescholarship.lib.uts.edu.au/iresearch/scholarly-works/handle/2100/1012.

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Benjamin, Jordan T. "Analyzing recent latitudinal and seasonal changes in simulated atmospheric temperatures from a global chemistry-climate model." Thesis, Massachusetts Institute of Technology, 2019. https://hdl.handle.net/1721.1/122235.

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Thesis: S.B., Massachusetts Institute of Technology, Department of Physics, 2019<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (pages 28-29).<br>Recent work by Santer et al. (2018) in Science examined the usefulness of the latitudinal structure and seasonal behavior of warming for fingerprinting anthropogenic climate change using satellite data and the CMIP5 multi-model ensemble over 1979-2016. They identify the first seasonal fingerprint in the northern hemisphere annual cycle and structure of warming, but do not specify what forcing agent (e.g. ozone, soot,
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Books on the topic "Global atmospheric changes"

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Williamson, Phillip. Global change: Reducing uncertainties. International Geosphere-Biosphere Programme, the Royal Swedish Academy of Sciences, 1992.

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Tricker, A. S. Global climate: Possible contemporary change. Dept. of Geography, University of Dundee, 1992.

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National Agricultural Library (U.S.), ed. Global change information packet. 2nd ed. National Agricultural Library, U.S. Dept. of Agriculture, 1992.

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National Agricultural Library (U.S.). Global change information packet. 2nd ed. National Agricultural Library, U.S. Department of Agriculture, 1992.

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E, Abrahamson Dean, ed. The Challenge of global warming. Island Press, 1989.

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van, Ierland E., Górka Kazimierz, North Atlantic Treaty Organization. Scientific Affairs Division., and NATO Advanced Research Workshop "The Economics of Atmospheric Pollution, Theories, Applied Models and Implications for International Policy Making" (1994 : Wageningen, Netherlands), eds. Economics of atmospheric pollution. Springer, 1996.

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John, Firor, ed. Global warming: Selected reprints. American Association of Physics Teachers, 1995.

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Singer, S. Fred. Unstoppable global warming: Every 1,500 years. Rowman & Littlefield, 2008.

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Singer, S. Fred. Hot talk, cold science: Global warming's unfinished debate. Independent Institute, 1998.

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United States. Dept. of Energy. Atmospheric and Climate Research Division and Atmospheric Radiation Measurement Program (U.S.), eds. Identification, recommendation, and justification of potential locales for ARM sites. The Division, 1991.

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Book chapters on the topic "Global atmospheric changes"

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

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

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

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Warneck, Peter. "Chemical Changes of the Atmosphere on Geological and Recent Time Scales." In Global Atmospheric Chemical Change. Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1864-4_1.

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Warneck, Peter. "Chemical Changes of the Atmosphere on Geological and Recent Time Scales." In Global Atmospheric Chemical Change. Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-015-3714-8_1.

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Jayaraman, A., G. Beig, U. C. Kulshrestha, et al. "Atmospheric Composition Change and Air Quality." In Global Environmental Changes in South Asia. Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-9913-7_5.

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

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Keller, Michael, and Pamela A. Matson. "Biosphere-Atmosphere Exchange of Trace Gases in the Tropics: Evaluating the Effects of Land Use Changes." In Global Atmospheric-Biospheric Chemistry. Springer US, 1994. http://dx.doi.org/10.1007/978-1-4615-2524-0_7.

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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. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5313-0_110.

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Randel, William J., Fei Wu, J. M. Russell, J. M. Zawodny, and John Nash. "Interannual changes in stratospheric constituents and global circulation derived from satellite data." In Atmospheric Science Across the Stratopause. American Geophysical Union, 2000. http://dx.doi.org/10.1029/gm123p0271.

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Conference papers on the topic "Global atmospheric changes"

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Valujeva, Kristine, Jovita Pilecka-Ulcugaceva, Kristaps Siltumens, Olga Skiste, and Inga Grinfelde. "EFFECTS OF TILLAGE SYSTEMS ON METHANE ASSIMILATION IN CAMBIC CALCISOL AND IMPLICATIONS FOR CLIMATE CHANGE MITIGATION." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024v/4.2/s18.27.

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Well-aerated soils are essential for methane (CH4) uptake from the atmosphere, acting as significant sinks for this greenhouse gas, which has a global warming potential 25 times greater than that of carbon dioxide (CO2). These soils contain methanotrophic bacteria, which oxidize CH4 and thereby reduce atmospheric methane concentrations. The potential of soils to assimilate CH4 depends on factors such as soil type and moisture regime. This study investigates the ability of clay soil Cambic Calcisol to assimilate CH4. Measurements were conducted at an experimental site with two tillage systems a
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Suslin, Vyacheslav. "OCEAN'S VIOLET BREATH AS AN INDICATOR OF GLOBAL AND REGIONAL CHANGES IN THE EARTH'S ECOSYSTEM." In The XXXI International Symposium "Atmospheric and Ocean Optics. Atmospheric Physics". V.E. Zuev Institute of Atmospheric Optics, Siberian Branch of the Russian Academy of Sciences, 2025. https://doi.org/10.56820/conferencearticle_685be465f1b580.17385103.

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The paper considers the long-term variability of remote sensing reflectance at 412 nm RRS(412) in several fixed subtropical regions of the World Ocean. For a separate region, the area occupied by waters with a high RRS(412) value is maximum for the local summer and minimum for the local winter. This behavior of the marine ecosystem is called "the violet breath of the ocean". The significance of this phenomenon is that its anomalies on different time scales reflect the ocean's response to global changes in the Earth's ecosystem, occurring both in individual regions of the planet and as a whole.
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Ganagina, Irina, Vadim Kanushin, Denis Goldobin, Inna Dorogova, Aleksander Elagin, and Lyudmila Shebyreva. "The impact of the nonuniform distribution of atmospheric pressure to changes in the Earth’s global gravity field." 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/10.1117/12.2540688.

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Postiglione, Alessia. "A Nature-Based Tool to design vegetation barriers along road infrastructure to contain anthropogenic atmospheric Particulate Matter: characterization of leaf functional traits." In Global Meet on Climate Changes and Sustainability. United Research Forum, 2024. https://doi.org/10.51219/urforum.2024.alessia-postiglione.

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Muryshev, Kirill, Alexey Eliseev, Igor Mokhov, Maxim Arzhanov, Alexandr Timazhev, and Sergey Denisov. "Time lag between changes in global temperature and atmospheric CO2 content according to the results of numerical experiments with Earth system models." 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/10.1117/12.2540793.

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Zander, R., and Ph Demoulin. "Atmospheric Changes above ISSJ from Infrared Solar Observations." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1990. http://dx.doi.org/10.1364/orsa.1990.thc1.

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Despite the outstanding progress made during the last decade in observational methods such as passive emission spectrometry and active Lidar applications, infrared remote sensors using the sun as source of radiation remain among the most powerful tools for atmospheric investigations. The quality and quantity of such solar observations have reflected the progress made in detector sensitivities, in new instrumental techniques and modes of operation, as well as the power of analytical algorithms based on modern computers. Infrared spectrometers have been adapted and proven suitable for measuremen
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Wu, Sifan, and Congying Li. "Global atmospheric pCO2 changes during the Early Aptian OAE 1a." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.19059.

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Conkol, Gary K. "Climate Change and Global Warming - The Forgotten Factors." In ASME 2021 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2021. http://dx.doi.org/10.1115/imece2021-70096.

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Abstract The recent global pandemic has provided an unparalleled opportunity to examine and potentially calibrate our responses to Global Warming. Since 1992 there has been much debate but also vast deployment of technology from satellites to atmospheric monitoring stations to study climate change and, specifically, global warming. Copious amounts of atmospheric temperature and Greenhouse Gas (GHG) data have been continuously recorded. Data throughout the 2019 pandemic to present, now provide the rare opportunity to test understanding of Global Warming and resulting Climate Change. Herein, cha
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Bick, Jay A., and Keith E. Holbert. "An analysis of atmospheric carbon dioxide content and impacts of global generation supply changes." In 2012 North American Power Symposium (NAPS 2012). IEEE, 2012. http://dx.doi.org/10.1109/naps.2012.6336349.

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Molodykh, Sergey, and Ashkhen Karakhanyan. "ASSESSING THE INFLUENCE OF SOLAR ACTIVITY ON THE TRANSMISSION OF LONGWAVE RADIATION IN THE TROPOSPHERE." In The XXXI International Symposium "Atmospheric and Ocean Optics. Atmospheric Physics". V.E. Zuev Institute of Atmospheric Optics, Siberian Branch of the Russian Academy of Sciences, 2025. https://doi.org/10.56820/conferencearticle_685be4659979a0.80521055.

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The rapid increase in global near-surface temperature in recent decades has intensified research into various mechanisms of influence on the Earth's climate system. The paper proposes a parameterization of the mechanism of solar activity influence on the troposphere that has been developed at the ISTP SB RAS. A modification of the spectral radiation block used in general atmospheric circulation models has been carried out, allowing the influence of solar activity on the transmission of longwave radiation in the atmosphere to be taken into account. The variants for calculating changes in the ra
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Reports on the topic "Global atmospheric changes"

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Matchaya, G. Brief: wetlands for hydrological resilience. International Water Management Institute (IWMI), 2025. https://doi.org/10.5337/2025.222.

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Human-driven changes to blue (surface water and groundwater) and green (soil moisture and atmospheric) water flows are intensifying risks such as floods, droughts, and biodiversity loss. The Global Commission on the Economics of Water (GCEW) calls for water to be treated as a global common good—placing ecosystems such as wetlands at the center of resilience strategies. Wetlands are critical natural infrastructure: they buffer climate extremes, recharge aquifers, purify water, and sustain atmospheric moisture cycles. Yet, they remain undervalued, degraded, and lost at alarming rates. This brief
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Xavier, Prince, Martin Willett, Tim Graham, et al. Assessment of the Met Office Global Coupled model version 4 (GC4) configurations. Met Office, 2024. http://dx.doi.org/10.62998/uzui3766.

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The Global Coupled model version 4 (GC4) is an upgraded configuration of the MetUM system, building upon its predecessor, GC3.0/3.1. It incorporates various improvements and changes in the atmospheric and land components (Global Atmosphere 8 and Global Land 9 - GA8GL9) while keeping the ocean component (Global Ocean 6 - GO6) unchanged, except for minor bug fixes. The GC4 model introduces several enhancements, such as the drag package for land surface and hydrology, improvements in radiation and large-scale precipitation parametrisations, advancements in the boundary layer and convection repres
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Seifert, Miriam, Claudia Hinrichs, Judith Hauck, and Christoph Völker. New / improved model parametrizations for responses in phytoplankton growth and calcification to changes in alkalinity implemented. OceanNets, 2023. http://dx.doi.org/10.3289/oceannets_d4.5.

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Global biogeochemical ocean models that are currently in place to investigate alkalinity enhancement at a global scale do usually not consider the effects of a changing carbonate system on phytoplankton. We introduce new and modified parameterizations of phytoplankton carbonate systems sensitivities into the biogeochemistry model REcoM. We then compare phytoplankton biomass and net primary production at different atmospheric CO2 concentrations to results from other deliverables (D5.3, 5.6, 5.7) based on experiments and models. The resilience of phytoplankton biomass towards low CO2 concentrati
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Felix, Meier, Wilfried Rickels, Christian Traeger, and Martin Quaas. Working paper published on NETs in strategically interacting regions based on simulation and analysis in an extended ACE model. OceanNets, 2022. http://dx.doi.org/10.3289/oceannets_d1.5.

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Net-zero climate policies foresee deployment of atmospheric carbon dioxide removal wit geological, terrestrial, or marine carbon storage. While terrestrial and geological storage would be governed under the framework of national property rights, marine storage implies that carbon is transferred from one global common, the atmosphere, to another global common, the ocean, in particular if storage exceeds beyond coastal applications. This paper investigates the option of carbon dioxide removal (CDR) and storage in different (marine) reservoir types in an analytic climate-economy model, and derive
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Meier, Felix, Wilfried Rickels, Christian Traeger, and Martin Quaas. Working paper published on NETs in strategically interacting regions based on simulation and analysis in an extended ACE model. OceanNets, 2023. http://dx.doi.org/10.3289/oceannets_d1.5_v2.

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Net-zero climate policies foresee deployment of atmospheric carbon dioxide removal wit geological, terrestrial, or marine carbon storage. While terrestrial and geological storage would be governed under the framework of national property rights, marine storage implies that carbon is transferred from one global common, the atmosphere, to another global common, the ocean, in particular if storage exceeds beyond coastal applications. This paper investigates the option of carbon dioxide removal (CDR) and storage in different (marine) reservoir types in an analytic climate-economy model, and derive
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Eick, Ryan, James Gibbs, P. McPhearson, and William Schlesinger. The Global Carbon Cycle: The Chemistry of Climate Change. American Museum of Natural History, 2009. http://dx.doi.org/10.5531/cbc.ncep.0159.

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Over the past century or so, human activities have altered the atmospheric balance, affecting processes such as the global carbon cycle—with environmental consequences. The global carbon cycle is a complex series of both abiotic and biotic processes. While atmospheric carbon levels have varied in the past, humans have definitively altered the global carbon cycle through fossil fuel use and forest destruction. Recent attempts at managing the carbon cycle include reforestation and geologic/oceanic sequestration. At current rates of human activity, atmospheric carbon levels will continue to rise
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7

Moraes, Jr., Francis Perry. The global change research center atmospheric chemistry model. Office of Scientific and Technical Information (OSTI), 1995. http://dx.doi.org/10.2172/576052.

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8

Buesseler, Ken O., Di Jin, Melina Kourantidou, David S. Levin, Kilaparti Ramakrishna, and Philip Renaud. The ocean twilight zone’s role in climate change. Woods Hole Oceanographic Institution, 2022. http://dx.doi.org/10.1575/1912/28074.

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The ocean twilight zone (more formally known as the mesopelagic zone) plays a fundamental role in global climate. It is the mid-ocean region roughly 100 to 1000 meters below the surface, encompassing a half-mile deep belt of water that spans more than two-thirds of our planet. The top of the ocean twilight zone only receives 1% of incident sunlight and the bottom level is void of sunlight. Life in the ocean twilight zone helps to transport billions of metric tons (gigatonnes) of carbon annually from the upper ocean into the deep sea, due in part to processes known as the biological carbon pump
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Noronha, S. Climate Change and Generation Zero – Analysing the 50/50 Campaign: A Communication for Social Change Approach. Unitec ePress, 2012. http://dx.doi.org/10.34074/ocds.12013.

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Climate change does not respect national boundaries or distinguish between big and small polluters. It is one of the truly global problems humanity faces today. In spite of this, there is a reluctance to believe in the existence of climate change even though the scientific consensus is that human influence bears much of the responsibility. In less than 200 years, human activity has increased the atmospheric concentration of greenhouse gases by some 50 percent relative to pre-industrial levels, leading to an increase in global temperatures. 1 Yet contrarian perspectives abound, given prominence
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10

Noronha, S. Climate Change and Generation Zero – Analysing the 50/50 Campaign: A Communication for Social Change Approach. Unitec ePress, 2012. http://dx.doi.org/10.34074/ocds.12013.

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Abstract:
Climate change does not respect national boundaries or distinguish between big and small polluters. It is one of the truly global problems humanity faces today. In spite of this, there is a reluctance to believe in the existence of climate change even though the scientific consensus is that human influence bears much of the responsibility. In less than 200 years, human activity has increased the atmospheric concentration of greenhouse gases by some 50 percent relative to pre-industrial levels, leading to an increase in global temperatures. 1 Yet contrarian perspectives abound, given prominence
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