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Relevant bibliographies by topics / Arctic clouds

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Academic literature on the topic 'Arctic clouds'

Author: Grafiati

Published: 30 June 2021

Last updated: 29 July 2025

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Journal articles on the topic "Arctic clouds"

1

Klingebiel, Marcus, André Ehrlich, Elena Ruiz-Donoso, et al. "Variability and properties of liquid-dominated clouds over the ice-free and sea-ice-covered Arctic Ocean." Atmospheric Chemistry and Physics 23, no. 24 (2023): 15289–304. http://dx.doi.org/10.5194/acp-23-15289-2023.

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Abstract. Due to their potential to either warm or cool the surface, liquid-phase clouds and their interaction with the ice-free and sea-ice-covered ocean largely determine the energy budget and surface temperature in the Arctic. Here, we use airborne measurements of solar spectral cloud reflectivity obtained during the Arctic CLoud Observations Using airborne measurements during polar Day (ACLOUD) campaign in summer 2017 and the Arctic Amplification: FLUXes in the Cloudy Atmospheric Boundary Layer (AFLUX) campaign in spring 2019 in the vicinity of Svalbard to retrieve microphysical properties

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Zamora, Lauren M., Ralph A. Kahn, Sabine Eckhardt, et al. "Aerosol indirect effects on the nighttime Arctic Ocean surface from thin, predominantly liquid clouds." Atmospheric Chemistry and Physics 17, no. 12 (2017): 7311–32. http://dx.doi.org/10.5194/acp-17-7311-2017.

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Abstract. Aerosol indirect effects have potentially large impacts on the Arctic Ocean surface energy budget, but model estimates of regional-scale aerosol indirect effects are highly uncertain and poorly validated by observations. Here we demonstrate a new way to quantitatively estimate aerosol indirect effects on a regional scale from remote sensing observations. In this study, we focus on nighttime, optically thin, predominantly liquid clouds. The method is based on differences in cloud physical and microphysical characteristics in carefully selected clean, average, and aerosol-impacted cond

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Sotiropoulou, G., J. Sedlar, M. Tjernström, M. D. Shupe, I. M. Brooks, and P. O. G. Persson. "The thermodynamic structure of summer Arctic stratocumulus and the dynamic coupling to the surface." Atmospheric Chemistry and Physics Discussions 14, no. 3 (2014): 3815–74. http://dx.doi.org/10.5194/acpd-14-3815-2014.

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Abstract. The vertical structure of Arctic low-level clouds and Arctic boundary layer is studied, using observations from ASCOS (Arctic Summer Cloud Ocean Study), in the central Arctic, in late summer 2008. Two general types of cloud structures are examined: the "neutrally-stratified" and "stably-stratified" clouds. Neutrally-stratified are mixed-phase clouds where radiative-cooling near cloud top produces turbulence that creates a cloud-driven mixed layer. When this layer mixes with the surface-generated turbulence, the cloud layer is coupled to the surface, whereas when such an interaction d

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Sotiropoulou, G., J. Sedlar, M. Tjernström, M. D. Shupe, I. M. Brooks, and P. O. G. Persson. "The thermodynamic structure of summer Arctic stratocumulus and the dynamic coupling to the surface." Atmospheric Chemistry and Physics 14, no. 22 (2014): 12573–92. http://dx.doi.org/10.5194/acp-14-12573-2014.

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Abstract. The vertical structure of Arctic low-level clouds and Arctic boundary layer is studied, using observations from ASCOS (Arctic Summer Cloud Ocean Study), in the central Arctic, in late summer 2008. Two general types of cloud structures are examined: the "neutrally stratified" and "stably stratified" clouds. Neutrally stratified are mixed-phase clouds where radiative-cooling near cloud top produces turbulence that generates a cloud-driven mixed layer. When this layer mixes with the surface-generated turbulence, the cloud layer is coupled to the surface, whereas when such an interaction

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Tjernström, Michael, Joseph Sedlar, and Matthew D. Shupe. "How Well Do Regional Climate Models Reproduce Radiation and Clouds in the Arctic? An Evaluation of ARCMIP Simulations." Journal of Applied Meteorology and Climatology 47, no. 9 (2008): 2405–22. http://dx.doi.org/10.1175/2008jamc1845.1.

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Abstract Downwelling radiation in six regional models from the Arctic Regional Climate Model Intercomparison (ARCMIP) project is systematically biased negative in comparison with observations from the Surface Heat Budget of the Arctic Ocean (SHEBA) experiment, although the correlations with observations are relatively good. In this paper, links between model errors and the representation of clouds in these models are investigated. Although some modeled cloud properties, such as the cloud water paths, are reasonable in a climatological sense, the temporal correlation of model cloud properties w

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Baek, Eun-Hyuk, Joo-Hong Kim, Sungsu Park, Baek-Min Kim, and Jee-Hoon Jeong. "Impact of poleward heat and moisture transports on Arctic clouds and climate simulation." Atmospheric Chemistry and Physics 20, no. 5 (2020): 2953–66. http://dx.doi.org/10.5194/acp-20-2953-2020.

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Abstract. Many general circulation models (GCMs) have difficulty simulating Arctic clouds and climate, causing substantial inter-model spread. To address this issue, two Atmospheric Model Intercomparison Project (AMIP) simulations from the Community Atmosphere Model version 5 (CAM5) and Seoul National University (SNU) Atmosphere Model version 0 (SAM0) with a unified convection scheme (UNICON) are employed to identify an effective mechanism for improving Arctic cloud and climate simulations. Over the Arctic, SAM0 produced a larger cloud fraction and cloud liquid mass than CAM5, reducing the neg

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Loewe, Katharina, Annica M. L. Ekman, Marco Paukert, Joseph Sedlar, Michael Tjernström, and Corinna Hoose. "Modelling micro- and macrophysical contributors to the dissipation of an Arctic mixed-phase cloud during the Arctic Summer Cloud Ocean Study (ASCOS)." Atmospheric Chemistry and Physics 17, no. 11 (2017): 6693–704. http://dx.doi.org/10.5194/acp-17-6693-2017.

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Abstract. The Arctic climate is changing; temperature changes in the Arctic are greater than at midlatitudes, and changing atmospheric conditions influence Arctic mixed-phase clouds, which are important for the Arctic surface energy budget. These low-level clouds are frequently observed across the Arctic. They impact the turbulent and radiative heating of the open water, snow, and sea-ice-covered surfaces and influence the boundary layer structure. Therefore the processes that affect mixed-phase cloud life cycles are extremely important, yet relatively poorly understood. In this study, we pres

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Xie, Shaocheng, Xiaohong Liu, Chuanfeng Zhao, and Yuying Zhang. "Sensitivity of CAM5-Simulated Arctic Clouds and Radiation to Ice Nucleation Parameterization." Journal of Climate 26, no. 16 (2013): 5981–99. http://dx.doi.org/10.1175/jcli-d-12-00517.1.

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Abstract Sensitivity of Arctic clouds and radiation in the Community Atmospheric Model, version 5, to the ice nucleation process is examined by testing a new physically based ice nucleation scheme that links the variation of ice nuclei (IN) number concentration to aerosol properties. The default scheme parameterizes the IN concentration simply as a function of ice supersaturation. The new scheme leads to a significant reduction in simulated IN concentration at all latitudes while changes in cloud amounts and properties are mainly seen at high- and midlatitude storm tracks. In the Arctic, there

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Stapf, Johannes, André Ehrlich, Evelyn Jäkel, Christof Lüpkes, and Manfred Wendisch. "Reassessment of shortwave surface cloud radiative forcing in the Arctic: consideration of surface-albedo–cloud interactions." Atmospheric Chemistry and Physics 20, no. 16 (2020): 9895–914. http://dx.doi.org/10.5194/acp-20-9895-2020.

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Abstract. The concept of cloud radiative forcing (CRF) is commonly applied to quantify the impact of clouds on the surface radiative energy budget (REB). In the Arctic, specific radiative interactions between microphysical and macrophysical properties of clouds and the surface strongly modify the warming or cooling effect of clouds, complicating the estimate of CRF obtained from observations or models. Clouds tend to increase the broadband surface albedo over snow or sea ice surfaces compared to cloud-free conditions. However, this effect is not adequately considered in the derivation of CRF i

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Sartori, Ernani. "The Arctic ice melting confirms the new theory." Journal of Water and Climate Change 10, no. 2 (2018): 321–43. http://dx.doi.org/10.2166/wcc.2018.153.

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Abstract The new theory shows that the global and the Arctic atmospheres behave as an open atmosphere (few clouds) or as a ‘closed’ atmosphere (fully cloudy), which explains the Arctic ice melting. Within the closed atmosphere the solar radiation, wind and evaporation are reduced while the water and air temperatures and the humidity increase. Real data confirm these effects for the planet and for the Arctic. Many authors did not understand these apparent inconsistencies, but this paper solves many intriguing problems, and provides solutions that led the present author to discover the new hydro

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Dissertations / Theses on the topic "Arctic clouds"

1

Beesley, John Anthony. "The climatic effects and requirements of arctic clouds /." Thesis, Connect to this title online; UW restricted, 1997. http://hdl.handle.net/1773/10056.

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Garrett, Timothy J. "Radiative properties of arctic clouds /." Thesis, Connect to this title online; UW restricted, 2000. http://hdl.handle.net/1773/10090.

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Zygmuntowska, Marta, Thorsten Mauritsen, Johannes Quaas, and Lars Kaleschke. "Arctic clouds and surface radiation." Universitätsbibliothek Leipzig, 2015. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-185357.

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Clouds regulate the Earth’s radiation budget, both by reflecting part of the incoming sunlight leading to cooling and by absorbing and emitting infrared radiation which tends to have a warming effect. Globally averaged, at the top of the atmosphere the cloud radiative effect is to cool the climate, while at the Arctic surface, clouds are thought to be warming. Here we compare a passive instrument, the AVHRR-based retrieval from CM-SAF, with recently launched active instruments onboard CloudSat and CALIPSO and the widely used ERA-Interim reanalysis. We find that in particular in winter months t

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Lampert, Astrid. "Airborne lidar observations of tropospheric arctic clouds." Phd thesis, Universität Potsdam, 2009. http://opus.kobv.de/ubp/volltexte/2010/4121/.

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Due to the unique environmental conditions and different feedback mechanisms, the Arctic region is especially sensitive to climate changes. The influence of clouds on the radiation budget is substantial, but difficult to quantify and parameterize in models. In the framework of the PhD, elastic backscatter and depolarization lidar observations of Arctic clouds were performed during the international Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR) from Svalbard in March and April 2007. Clouds were probed above the inaccessible Arctic Ocean with a combination of airborne inst

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Pleavin, Thomas Daniel. "Large eddy simulations of Arctic stratus clouds." Thesis, University of Leeds, 2013. http://etheses.whiterose.ac.uk/4934/.

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Mixed-phase Arctic stratocumulus clouds are ubiquitous to the region during the summer months. However, despite their prevalence, very little is known about the processes which maintain the cloud. Recent observations have shown that Arctic stratocumulus commonly extend into the temperature inversion which caps the Arctic boundary layer. This is atypical to sub-tropical stratocumulus where the cloud top is found in the vicinity of the inversion base, and unexpected as strong longwave radiative cooling would be expected to keep the cloud top and inversion base heights in equilibrium. Uniquely to

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Kanngießer, Franz, André Ehrlich, and Manfred Wendisch. "Observations of glories above arctic boundary layer clouds to identify cloud phase." Universität Leipzig, 2017. https://ul.qucosa.de/id/qucosa%3A16743.

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The glory is an optical phenomenon observed above liquid water clouds and consists of coloured rings around the anti-solar point. Since the glory is caused by scattering on spherical particles it can be used as a proxy to identify liquid water at the cloud top. Images taken with a CANON digital camera equipped with a fish-eye lens on board the research aircraft Polar 5 during the measurement campaign Radiation-Aerosol-Cloud Experiment in the Arctic Circle (RACEPAC) were analysed for glories. To identify glories an algorithm consisting of five criteria was developed by using simulations of the

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Poole, Lamont Rozelle. "Airborne lidar studies of Arctic polar stratospheric clouds." Diss., The University of Arizona, 1987. http://hdl.handle.net/10150/184277.

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Airborne lidar measurements of Arctic polar stratospheric clouds (PSCs) in January 1984 and January 1986 are reported. The locales and altitudes of the clouds coincided in both years with very cold ambient temperatures. During the 1984 experiment, PSCs were observed on three flights north of Thule, Greenland; peak backscatter occurred near 20 km (at temperatures below 193 K). A single PSC formation was seen between Iceland and Scotland during the 1986 experiment, with beak backscatter occurring near 22 km (at temperatures from 188-191 K). A sequence of observations in this same area by the SAM

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Lampert, Astrid [Verfasser]. "Airborne lidar observations of tropospheric Arctic clouds / Astrid Lampert." Bremerhaven : AWI, Alfred-Wegener-Institut für Polar- und Meeresforschung, 2010. http://d-nb.info/101019965X/34.

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Achtert, Peggy. "Lidar Measurements of Polar Stratospheric Clouds in the Arctic." Doctoral thesis, Stockholms universitet, Meteorologiska institutionen (MISU), 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-88054.

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Polar Stratospheric Clouds (PSCs) play a key role for ozone depletion in the polar stratosphere. Its magnitude depends on the type of PSC and its lifetime and extent. This thesis presents PSC observations conducted with the Esrange lidar and the space-borne CALIPSO lidar. PSCs are separated into three types according to their optical properties. The occurrence rate of the different types which are often observed simultaneously as well as their interaction and connection is not well understood. To better understand the processes that govern PSC formation, observations need to be combined with a

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Cremer, Roxana, Johannes Quaas, and Johannes Mülmenstädt. "Interactions between clouds and sea ice in the Arctic." Universität Leipzig, 2017. https://ul.qucosa.de/id/qucosa%3A16773.

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The feedback between clouds and sea ice got more importance in the last years, because of the declining Arctic sea ice extent. Previous observations show the formation of low clouds over newly formed open water. These low clouds are very important for the Arctic Energy Budget, because they warm the surface. This leads to increasing temperatures and stronger sea ice loss. To assess the relationship between sea ice cover and cloudiness, satellite observations by DARDAR were compared with both global climate reanalyses ERA–Interim and MACC. The analysis focuses on 2007 – 2010 and the relationship

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Books on the topic "Arctic clouds"

1

Yang, Ping (Professor in Atmospheric Sciences), author and Ehrlich André 1980 author, eds. Amplified climate changes in the Arctic: Role of clouds and atmospheric radiation. Hirzel, 2013.

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2

Smith, William L. The analysis of polar clouds from AVHRR satellite data using pattern recognition techniques: Final report. Space Science and Engineering Center, University of Wisconsin-Madison, 1990.

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3

Freese, Dietmar. Solare und terrestrische Strahlungswechselwirkung zwischen arktischen Eisflächen und Wolken =: Solar and terrestrial radiation interaction between arctic sea ice and clouds. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1999.

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4

Guest, Peter Staples. A numerical, analytical and observational study of the effect of clouds on surface wind and wind stress during the central Arctic winter. Naval Postgraduate School, 1992.

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5

Shiel, M. P. The purple cloud. Allison and Busby, 1986.

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Shiel, M. P. The purple cloud. University of Nebraska Press, 2000.

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7

Barron, John P. An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery. Naval Postgraduate School, 1988.

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8

Salvato, Gregory. Comparison between Arctic and subtropic ship exaust [i.e. exhaust] effects on cloud properties. Naval Postgraduate School, 1992.

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9

1953-, Willig Judith A., Aikens C. Melvin, and Fagan John Lee, eds. Early human occupation in far western North America: The Clovis-Archaic interface. Nevada State Museum, 1988.

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10

Loewe, Katharina. Arctic Mixed-phase Clouds: Macro- and Microphysical Insights With a Numerical Model. Saint Philip Street Press, 2020.

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Book chapters on the topic "Arctic clouds"

1

Herman, Gerald F. "Arctic Stratus Clouds." In The Geophysics of Sea Ice. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-5352-0_7.

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Herva, Vesa-Pekka, Aki Hakonen, Roger Norum, Oula Seitsonen, and Markus Fjellström. "The Fjell in the Cloud." In Arctic Encounters. Springer Nature Switzerland, 2025. https://doi.org/10.1007/978-3-031-85016-5_6.

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Abstract On the second day around noon, as the clouds had shifted just enough to provide fleeting glimpses of the world beyond them—enough to show that only the top of Ritničohkka was submerged—we ventured out to continue the survey. We first navigated in the cloud for some time, which made the fjell look and feel very peculiar. Unable to see the horizon in any direction, only the grey rocks and ground in our immediate vicinity offered points of reference, which disappeared as we walked further in the grey cloud. Occasional rock formations loomed in the mist. The scene was reminiscent, yet aga

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Ehrlich, André, Michael Schäfer, Elena Ruiz-Donoso, and Manfred Wendisch. "Airborne Remote Sensing of Arctic Clouds." In Springer Series in Light Scattering. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-38696-2_2.

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Devasthale, Abhay, Joseph Sedlar, Michael Tjernström, and Alexander Kokhanovsky. "A Climatological Overview of Arctic Clouds." In Physics and Chemistry of the Arctic Atmosphere. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-33566-3_5.

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Cairo, Francesco, and Tiziana Colavitto. "Polar Stratospheric Clouds in the Arctic." In Physics and Chemistry of the Arctic Atmosphere. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-33566-3_7.

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von Savigny, Christian, Gerd Baumgarten, and Franz-Josef Lübken. "Noctilucent Clouds: General Properties and Remote Sensing." In Physics and Chemistry of the Arctic Atmosphere. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-33566-3_8.

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Böckmann, Christine, and Christoph Ritter. "Properties of Polar Stratospheric Clouds over the European Arctic from Ground-Based Lidar." In Proceedings of the 30th International Laser Radar Conference. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-37818-8_43.

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Gong, Wanmin, Stephen Beagley, Roya Ghahreman, et al. "Modelling Arctic Atmospheric Aerosols: Representation of Aerosol Processing by Ice and Mixed-Phase Clouds." In Springer Proceedings in Complexity. Springer Nature Switzerland, 2025. https://doi.org/10.1007/978-3-031-70424-6_36.

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Gong, Wanmin, Stephen Beagley, Roya Ghahreman, Ayodeji Akingunola, and Paul A. Makar. "Modeling Atmospheric Composition in the Summertime Arctic: Transport of North American Biomass Burning Pollutants and Their Impact on the Arctic Marine Boundary Layer Clouds." In Springer Proceedings in Complexity. Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-63760-9_11.

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Key, Jeffrey R. "Classification of Arctic Cloud and Sea Ice Features in Multi-Spectral Satellite Data." In The GeoJournal Library. Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-1122-5_8.

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Conference papers on the topic "Arctic clouds"

1

Qian, Shen-En, Stephane Routhier, Tongxi Wu, et al. "GHG measurements using an imaging FTS on a stratospheric balloon: a tech demo for the Arctic observing mission." In Remote Sensing of Clouds and the Atmosphere XXIX, edited by Evgueni I. Kassianov and Simone Lolli. SPIE, 2024. http://dx.doi.org/10.1117/12.3030957.

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Zabolotskikh, E. V., E. V. Lvova, K. I. Yarusov, and S. M. Azarov. "Total Cloud Liquid Water Content Retrieval over the Arctic Sea Ice from the AMSR2 Data." In 2024 Photonics & Electromagnetics Research Symposium (PIERS). IEEE, 2024. http://dx.doi.org/10.1109/piers62282.2024.10618325.

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Li, Mo, and Hao Li. "Cloud-Based Intelligent Spoken English Learning System using GPT-4 and the L2-ARCTIC Corpus." In 2025 3rd International Conference on Data Science and Information System (ICDSIS). IEEE, 2025. https://doi.org/10.1109/icdsis65355.2025.11069435.

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Shaw, Joseph A., Erik Edqvist, Hector E. Bravo, Kohei Mizutani, and Brentha Thurairajah. "Measuring Arctic clouds with the infrared cloud imager." In International Symposium on Optical Science and Technology, edited by Joseph A. Shaw. SPIE, 2002. http://dx.doi.org/10.1117/12.482315.

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Eloranta, Edwin W., Taneil Uttal, and Matthew Shupe. "Cloud particle size measurements in Arctic clouds using lidar and radar data." In 2007 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2007. http://dx.doi.org/10.1109/igarss.2007.4423292.

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Taylor, Patrick C. "Does a relationship between Arctic low clouds and sea ice matter?" In RADIATION PROCESSES IN THE ATMOSPHERE AND OCEAN (IRS2016): Proceedings of the International Radiation Symposium (IRC/IAMAS). Author(s), 2017. http://dx.doi.org/10.1063/1.4975530.

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Yasui, Motoaki, Kohei Mizutani, Toshikazu Itabe, et al. "Observation of Polar Stratospheric Clouds (PSCs) in Canadian Arctic by Lidar and Balloonborne Optical Particle Counter." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1997. http://dx.doi.org/10.1364/orsa.1997.omb.4.

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PSCs play important roles not only in global climate change through its own effects on radiation budget of the earth but also in ozone depletion through heterogeneous chemical processes which occur on the surfaces of the PSCs. The mechanisms of the processes, however, have never clarified enough because of scarcity of data especially in arctic stratosphere. Japanese lidar group started operating Japan Arctic Lidar Network in arctic region in 1993, and plenty of lidar data have been obtained so far. The PSC lidar at Eureka station (80° N, 86° W) in Canadian arctic forms a link in the chain of t

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Rees, D., M. Vyssogorets, P.-E. Nilsen, I. Gandham, and David Rees. "High resolution observations of polar stratospheric clouds by the alomar doppler wind and temperature system." In The European Conference on Lasers and Electro-Optics. Optica Publishing Group, 1996. http://dx.doi.org/10.1364/cleo_europe.1996.cwj2.

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The Arctic Lidar Observatory for Middle Atmosphere Research (ALOMAR) at Andoya, Norway (69°N, 16°E, von Zahn and Rees, 1994), is a complex multi-instrument facility using lidars, radars and passive IR and Visible-wavelength instruments to study the complex behaviour of the Arctic Stratosphere and Mesosphere (von Cossart et al, 1995, 1996).

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Sikand, M., J. Koskulics, K. Stamnes, B. Hamre, J. J. Stamnes, and R. P. Lawson. "Mixed phase boundary layer clouds observed from a tethered balloon platform in the Arctic." In RADIATION PROCESSES IN THE ATMOSPHERE AND OCEAN (IRS2012): Proceedings of the International Radiation Symposium (IRC/IAMAS). AIP, 2013. http://dx.doi.org/10.1063/1.4804826.

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Browell, Edward V. "Recent Developments in Airborne Lidar Measurements of Ozone, Water Vapor, and Aerosols." In Laser Applications to Chemical Analysis. Optica Publishing Group, 1992. http://dx.doi.org/10.1364/laca.1992.tuc3.

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Major advances have taken place in the last 3 years in the development and application of airborne lidar systems in the measurement of ozone (O3), water vapor (H2O), and aerosols in various regions of the atmosphere. The first simultaneous measurements of O3 and aerosol distributions above and below an aircraft were made in tropospheric investigations in the Arctic during the summer of 1988 as part of the NASA Global Tropospheric Experiment (GTE), and this capability was subsequently used in the 1990 GTE field experiment over Canada. During the 1989 Airborne Arctic Stratospheric Experiment, th

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Reports on the topic "Arctic clouds"

1

Shaw, J. A. Arctic Clouds Infrared Imaging Field Campaign Report. Office of Scientific and Technical Information (OSTI), 2016. http://dx.doi.org/10.2172/1248496.

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Turner, David D. Microphysical Properties of Single and Mixed-Phase Arctic Clouds Derived from AERI Observations. Office of Scientific and Technical Information (OSTI), 2003. http://dx.doi.org/10.2172/1000181.

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Stephen J. Vavrus. Final Technical Report for Project "Improving the Simulation of Arctic Clouds in CCSM3". Office of Scientific and Technical Information (OSTI), 2008. http://dx.doi.org/10.2172/940966.

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Hobbs, Peter V. The Spectral Radiative Properties of Stratus Clouds and Ice Surfaces in the Arctic. Defense Technical Information Center, 1997. http://dx.doi.org/10.21236/ada627637.

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Igel, Adele. Dissipation of Mixed-Phase Arctic Clouds and Its Relationship to Aerosol Properties - Final Technical Report. Office of Scientific and Technical Information (OSTI), 2024. http://dx.doi.org/10.2172/2323558.

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Korolev, A., A. Shashkov, and H. Barker. Parameterization of the Extinction Coefficient in Ice and Mixed-Phase Arctic Clouds during the ISDAC Field Campaign. Office of Scientific and Technical Information (OSTI), 2012. http://dx.doi.org/10.2172/1035864.

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Verlinde, Johannes. Arctic Cloud Microphysical Processes. Final report. Office of Scientific and Technical Information (OSTI), 2019. http://dx.doi.org/10.2172/1578280.

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Kenneth Sassen. Improved Arctic Cloud and Aerosol Research and Model Parameterizations. Office of Scientific and Technical Information (OSTI), 2007. http://dx.doi.org/10.2172/900752.

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Hobbs, Peter V. Airborne Studies of Ocean-Particle-Cloud-Interactions in the Arctic. Defense Technical Information Center, 1993. http://dx.doi.org/10.21236/ada270752.

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Холошин, Ігор Віталійович, Ольга Володимирівна Бондаренко, Олена Вікторівна Ганчук, and Катерина Олегівна Шмельцер. Cloud ArcGIS Online as an innovative tool for developing geoinformation competence with future geography teachers. CEUR-WS.org, 2018. http://dx.doi.org/10.31812/123456789/3258.

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Abstract:

Abstract. The article dwells upon the scientifically relevant problem of using cloud-based GIS-technologies when training future geography teachers (based on ArcGIS Online application). The authors outline the basic principles for implementing ArcGIS Online in the educational process (interdisciplinary integration, the sequence of individualization in training, communicability, distance education and regional studies), and provide an example of an interactive map created with the help of the specified cloud GIS, since this kind of map is the most popular a form of research by geography student

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