Probing the vertical structure of the lower atmosphere over Svalbard
This is chapter 9 of the State of Environmental Science in Svalbard (SESS) report 2019 (https://sios-svalbard.org/SESS_Issue2). Understanding the causes and mechanisms of climate change requires an enormous number of continuous and accurate measurements. To measure atmospheric parameters along the v...
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ftdatacite:10.5281/zenodo.4777710 2023-05-15T15:13:37+02:00 Probing the vertical structure of the lower atmosphere over Svalbard Mazzola, Mauro Viola, Angelo Pietro Cappelletti, David Michele Ritter, Christoph Storvold, Rune 2020 https://dx.doi.org/10.5281/zenodo.4777710 https://zenodo.org/record/4777710 en eng Zenodo https://zenodo.org/communities/sios https://dx.doi.org/10.5281/zenodo.4777711 https://zenodo.org/communities/sios Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY Atmospheric profiles meteorology aerosol clouds radiosonde tethered balloon remote sensing UAV drones Text Report report 2020 ftdatacite https://doi.org/10.5281/zenodo.4777710 https://doi.org/10.5281/zenodo.4777711 2021-11-05T12:55:41Z This is chapter 9 of the State of Environmental Science in Svalbard (SESS) report 2019 (https://sios-svalbard.org/SESS_Issue2). Understanding the causes and mechanisms of climate change requires an enormous number of continuous and accurate measurements. To measure atmospheric parameters along the vertical profile, one must either fly the instrumentation or infer such information at a distance from the emissions or reflections of components in the atmosphere (remote sensing). Techniques that use one of these approaches have been developed since the 1940s. However, both approaches suffer from limitations on the accuracy of the measurements and the amount of information that can be obtained. Recent technological development has enabled production of small, low-cost sensors with capabilities similar to those used in the laboratory. These sensors can be installed on balloons or small unmanned aerial vehicles, allowing direct measurements in the lower atmosphere. With more accurate information on the status of the atmosphere, researchers can refine their mathematical data interpretation techniques. The research station in Ny-Ålesund is already well equipped for a number of standard vertical profile measurements. Fewer activities are performed at other stations in Svalbard. This is clear from the studies we cited in our contribution: about 60 papers. Half were based on remote sensing, 22 on balloons (tethered or free), 5 on dropsondes and 5 on drones. Although we do not claim that this list is exhaustive, it may represent the status of activities in Svalbard. The limited air traffic in the Arctic means that carrying out measurements with balloons and small radio-controlled airplanes is easier than elsewhere. Report Arctic Climate change Ny Ålesund Ny-Ålesund Svalbard DataCite Metadata Store (German National Library of Science and Technology) Arctic Svalbard Ny-Ålesund |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Atmospheric profiles meteorology aerosol clouds radiosonde tethered balloon remote sensing UAV drones |
spellingShingle |
Atmospheric profiles meteorology aerosol clouds radiosonde tethered balloon remote sensing UAV drones Mazzola, Mauro Viola, Angelo Pietro Cappelletti, David Michele Ritter, Christoph Storvold, Rune Probing the vertical structure of the lower atmosphere over Svalbard |
topic_facet |
Atmospheric profiles meteorology aerosol clouds radiosonde tethered balloon remote sensing UAV drones |
description |
This is chapter 9 of the State of Environmental Science in Svalbard (SESS) report 2019 (https://sios-svalbard.org/SESS_Issue2). Understanding the causes and mechanisms of climate change requires an enormous number of continuous and accurate measurements. To measure atmospheric parameters along the vertical profile, one must either fly the instrumentation or infer such information at a distance from the emissions or reflections of components in the atmosphere (remote sensing). Techniques that use one of these approaches have been developed since the 1940s. However, both approaches suffer from limitations on the accuracy of the measurements and the amount of information that can be obtained. Recent technological development has enabled production of small, low-cost sensors with capabilities similar to those used in the laboratory. These sensors can be installed on balloons or small unmanned aerial vehicles, allowing direct measurements in the lower atmosphere. With more accurate information on the status of the atmosphere, researchers can refine their mathematical data interpretation techniques. The research station in Ny-Ålesund is already well equipped for a number of standard vertical profile measurements. Fewer activities are performed at other stations in Svalbard. This is clear from the studies we cited in our contribution: about 60 papers. Half were based on remote sensing, 22 on balloons (tethered or free), 5 on dropsondes and 5 on drones. Although we do not claim that this list is exhaustive, it may represent the status of activities in Svalbard. The limited air traffic in the Arctic means that carrying out measurements with balloons and small radio-controlled airplanes is easier than elsewhere. |
format |
Report |
author |
Mazzola, Mauro Viola, Angelo Pietro Cappelletti, David Michele Ritter, Christoph Storvold, Rune |
author_facet |
Mazzola, Mauro Viola, Angelo Pietro Cappelletti, David Michele Ritter, Christoph Storvold, Rune |
author_sort |
Mazzola, Mauro |
title |
Probing the vertical structure of the lower atmosphere over Svalbard |
title_short |
Probing the vertical structure of the lower atmosphere over Svalbard |
title_full |
Probing the vertical structure of the lower atmosphere over Svalbard |
title_fullStr |
Probing the vertical structure of the lower atmosphere over Svalbard |
title_full_unstemmed |
Probing the vertical structure of the lower atmosphere over Svalbard |
title_sort |
probing the vertical structure of the lower atmosphere over svalbard |
publisher |
Zenodo |
publishDate |
2020 |
url |
https://dx.doi.org/10.5281/zenodo.4777710 https://zenodo.org/record/4777710 |
geographic |
Arctic Svalbard Ny-Ålesund |
geographic_facet |
Arctic Svalbard Ny-Ålesund |
genre |
Arctic Climate change Ny Ålesund Ny-Ålesund Svalbard |
genre_facet |
Arctic Climate change Ny Ålesund Ny-Ålesund Svalbard |
op_relation |
https://zenodo.org/communities/sios https://dx.doi.org/10.5281/zenodo.4777711 https://zenodo.org/communities/sios |
op_rights |
Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5281/zenodo.4777710 https://doi.org/10.5281/zenodo.4777711 |
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1766344158302175232 |