ERA5 overviews complementing temperature measurements of ground-based Rayleigh lidars for the investigation of gravity waves generated by moving sources ...

ERA5 overviews to associate stratospheric gravity waves in temperature measurements from vertically staring (zenith-pointing) ground-based Rayleigh lidars with atmospheric processes. Animations are for a virtual lidar location over the Southern Ocean during research flight RF25 of the DEEPWAVE campa...

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Main Authors: Binder, Michael, Dörnbrack, Andreas
Format: Article in Journal/Newspaper
Language:unknown
Published: Zenodo 2024
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.10686792
https://zenodo.org/doi/10.5281/zenodo.10686792
id ftdatacite:10.5281/zenodo.10686792
record_format openpolar
spelling ftdatacite:10.5281/zenodo.10686792 2024-03-31T07:55:26+00:00 ERA5 overviews complementing temperature measurements of ground-based Rayleigh lidars for the investigation of gravity waves generated by moving sources ... Binder, Michael Dörnbrack, Andreas 2024 https://dx.doi.org/10.5281/zenodo.10686792 https://zenodo.org/doi/10.5281/zenodo.10686792 unknown Zenodo https://dx.doi.org/10.5281/zenodo.7674037 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 non-orographic gravity waves upper-level troughs Rayleigh lidar idealized numerical simulations ERA5 transient gravity wave source article Audiovisual MediaObject 2024 ftdatacite https://doi.org/10.5281/zenodo.1068679210.5281/zenodo.7674037 2024-03-04T13:51:13Z ERA5 overviews to associate stratospheric gravity waves in temperature measurements from vertically staring (zenith-pointing) ground-based Rayleigh lidars with atmospheric processes. Animations are for a virtual lidar location over the Southern Ocean during research flight RF25 of the DEEPWAVE campaign (July 17 to 19, 2014) and for the location of the COmpact Rayleigh Autonomous Lidar (CORAL) in the lee of the southern Andes. Here, the first overview is for the CORAL measurement from June 22 to 23, 2018. The second one is for the nightly measurements between August 7 and 9, 2020. (a) and (b) emulate the measurement of a vertically staring ground-based lidar and show temperature perturbations after subtracting a temporal running mean of 12h (a) and the mean absolute temperature profile (b). Panels (c) and (d) are vertical sections of stratospheric ????′ along sectors of the latitude circle (c) and meridian (d) of the virtual lidar location. (e) and (f) are corresponding vertical sections of thermal stability ????2 ... Article in Journal/Newspaper Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic non-orographic gravity waves
upper-level troughs
Rayleigh lidar
idealized numerical simulations
ERA5
transient gravity wave source
spellingShingle non-orographic gravity waves
upper-level troughs
Rayleigh lidar
idealized numerical simulations
ERA5
transient gravity wave source
Binder, Michael
Dörnbrack, Andreas
ERA5 overviews complementing temperature measurements of ground-based Rayleigh lidars for the investigation of gravity waves generated by moving sources ...
topic_facet non-orographic gravity waves
upper-level troughs
Rayleigh lidar
idealized numerical simulations
ERA5
transient gravity wave source
description ERA5 overviews to associate stratospheric gravity waves in temperature measurements from vertically staring (zenith-pointing) ground-based Rayleigh lidars with atmospheric processes. Animations are for a virtual lidar location over the Southern Ocean during research flight RF25 of the DEEPWAVE campaign (July 17 to 19, 2014) and for the location of the COmpact Rayleigh Autonomous Lidar (CORAL) in the lee of the southern Andes. Here, the first overview is for the CORAL measurement from June 22 to 23, 2018. The second one is for the nightly measurements between August 7 and 9, 2020. (a) and (b) emulate the measurement of a vertically staring ground-based lidar and show temperature perturbations after subtracting a temporal running mean of 12h (a) and the mean absolute temperature profile (b). Panels (c) and (d) are vertical sections of stratospheric ????′ along sectors of the latitude circle (c) and meridian (d) of the virtual lidar location. (e) and (f) are corresponding vertical sections of thermal stability ????2 ...
format Article in Journal/Newspaper
author Binder, Michael
Dörnbrack, Andreas
author_facet Binder, Michael
Dörnbrack, Andreas
author_sort Binder, Michael
title ERA5 overviews complementing temperature measurements of ground-based Rayleigh lidars for the investigation of gravity waves generated by moving sources ...
title_short ERA5 overviews complementing temperature measurements of ground-based Rayleigh lidars for the investigation of gravity waves generated by moving sources ...
title_full ERA5 overviews complementing temperature measurements of ground-based Rayleigh lidars for the investigation of gravity waves generated by moving sources ...
title_fullStr ERA5 overviews complementing temperature measurements of ground-based Rayleigh lidars for the investigation of gravity waves generated by moving sources ...
title_full_unstemmed ERA5 overviews complementing temperature measurements of ground-based Rayleigh lidars for the investigation of gravity waves generated by moving sources ...
title_sort era5 overviews complementing temperature measurements of ground-based rayleigh lidars for the investigation of gravity waves generated by moving sources ...
publisher Zenodo
publishDate 2024
url https://dx.doi.org/10.5281/zenodo.10686792
https://zenodo.org/doi/10.5281/zenodo.10686792
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation https://dx.doi.org/10.5281/zenodo.7674037
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.5281/zenodo.1068679210.5281/zenodo.7674037
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