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210512 ||| eng |
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|a 9783038976288
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|a books978-3-03897-629-5
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|a McGonigle, Andrew
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|a Volcanic Plumes.Impacts on the Atmosphere and Insights into Volcanic Processes
|h Elektronische Ressource
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260 |
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|b MDPI - Multidisciplinary Digital Publishing Institute
|c 2019
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300 |
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|a 1 electronic resource (252 p.)
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653 |
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|a UV cameras
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|a satellite remote sensing
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653 |
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|a Taylor bubble
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653 |
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|a volcanic geochemistry
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653 |
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|a puffing
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653 |
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|a degassing processes
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653 |
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|a Python 2.7
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653 |
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|a Holuhraun
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653 |
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|a volcanic emissions
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653 |
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|a interdisciplinary volcanology
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653 |
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|a image processing
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|a n/a
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|a eruption start and duration
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653 |
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|a portable photometry
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|a gas slug
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|a Differential Absorption Lidar (DIAL)
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653 |
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|a geochemical modelling
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|a SO2
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|a SEVIRI data
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|a volcanology
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|a analysis software
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|a volcanic gases
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|a fissure eruption
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|a gas
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|a hyperspectral remote sensing
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|a Mount Etna
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|a 2011-2015 Etna lava fountains
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|a atmospheric chemistry
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|a plume
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|a oxygen and sulfur multi-isotopes
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|a O3
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|a volcanic sulfate aerosols
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|a SSA
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|a volcanic CO2 flux
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|a volcanic plume top height
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|a BrO
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|a spherical-cap bubble
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|a Bárðarbunga
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|a aerosol optical properties
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|a nonlinear PCA
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|a eruption monitoring
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653 |
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|a remote sensing
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653 |
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|a ultraviolet cameras
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653 |
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|a radiative transfer
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|a radioactive disequilibria 210Pb-210Bi-210Po
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|a cloud height
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|a reactive halogen
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|a radiative forcing
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|a basaltic volcanism
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|a volcanic plumes
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|a time averaged discharge rate
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|a atmospheric remote sensing
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|a gases
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|a Etna volcano
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|a nonlinear spectral unmixing
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|a volcanic aerosols
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|a strombolian
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700 |
1 |
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|a Salerno, Giuseppe
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1 |
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|a Sellitto, Pasquale
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041 |
0 |
7 |
|a eng
|2 ISO 639-2
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|b DOAB
|a Directory of Open Access Books
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500 |
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|a Creative Commons (cc), https://creativecommons.org/licenses/by-nc-nd/4.0/
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024 |
8 |
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|a 10.3390/books978-3-03897-629-5
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856 |
4 |
2 |
|u https://directory.doabooks.org/handle/20.500.12854/62371
|z DOAB: description of the publication
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856 |
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|u https://www.mdpi.com/books/pdfview/book/1179
|7 0
|x Verlag
|3 Volltext
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082 |
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|a 540
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|a 700
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|a Volcanoes release plumes of gas and ash to the atmosphere during episodes of passive and explosive behavior. These ejecta have important implications for the chemistry and composition of the troposphere and stratosphere, with the capacity to alter Earth's radiation budget and climate system over a range of temporal and spatial scales. Volcanogenic sulphur dioxide reacts to form sulphate aerosols, which increase global albedo, e.g., by reducing surface temperatures, in addition to perturbing the formation processes and optical properties of clouds. Released halogen species can also deplete stratospheric and tropospheric ozone. Volcanic degassing, furthermore, played a key role in the formation of Earth's atmosphere, and volcanic plumes can affect air quality, pose hazards to aviation and human health, as well as damage ecosystems. The chemical compositions and emission rates of volcanic plumes are also monitored via a range of direct-sampling and remote-sensing instrumentation, in order to gain insights into subterranean processes, in the respect of the magmatic bodies these volatiles exsolve from. Given the significant role these gases play in driving volcanic activity, e.g., via pressurisation, the study of volcanic plumes is proving to be an increasingly fruitful means of improving our understanding of volcanic systems, potentially in concert with observations from geophysics and contributions from fluid dynamical modelling of conduit dynamics.
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