Gravity waves above the northern Atlantic and Europe during streamer events using Aeolus
<p>Information about the energy density of gravity waves (GWs) is crucial for improving atmosphere models. So far, most space-based studies report the potential energy, <span class="inline-formula"><i>E</i><sub>pot</sub></span>, of GWs, as temperat...
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Copernicus Publications
2025-04-01
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| Series: | Atmospheric Measurement Techniques |
| Online Access: | https://amt.copernicus.org/articles/18/1591/2025/amt-18-1591-2025.pdf |
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| author | S. Wüst L. Küchelbacher F. Trinkl F. Trinkl M. Bittner M. Bittner |
| author_facet | S. Wüst L. Küchelbacher F. Trinkl F. Trinkl M. Bittner M. Bittner |
| author_sort | S. Wüst |
| collection | DOAJ |
| description | <p>Information about the energy density of gravity waves (GWs) is crucial for improving atmosphere models. So far, most space-based studies report the potential energy, <span class="inline-formula"><i>E</i><sub>pot</sub></span>, of GWs, as temperature measurements from satellites are more common.</p>
<p>We use Aeolus wind data to derive the kinetic energy density, <span class="inline-formula"><i>E</i><sub>kin</sub></span>, of GWs above the northern Atlantic and Europe. Assuming perfect instrument performance, this would be a lower limit for the kinetic energy density, as Aeolus only measures the horizontal line-of-sight wind. Aeolus, the European Space Agency's (ESA's) fourth Earth Explorer Mission, was the first Doppler wind lidar in space and measured vertical profiles of the horizontal line-of-sight wind from the ground to an altitude of <span class="inline-formula">∼</span> 20–30 km between 2018 and 2023. With a vertical resolution of 0.25–2 km, Aeolus measurements are in principle well suited for the analysis of GWs. However, the data quality is a challenge for such analyses, as the error in the data is in the range of typical GW amplitudes in the troposphere and stratosphere.</p>
<p>In this study, we derive daily resolved time series of <span class="inline-formula"><i>E</i><sub>kin</sub></span> before, during, and after two streamer events above the northern Atlantic and Europe. Streamers are large-scale tongue-like structures of meridionally deflected air masses, which are caused by enhanced planetary wave activity. They are linked to vertical shear of horizontal wind and a pressure system, two possible GW generation mechanisms. We find that there is a temporal coincidence between the enhanced daily averaged <span class="inline-formula"><i>E</i><sub>kin</sub></span> and occurrence of the streamer events, which we identified in total column ozone measurements. The derivation of GW signals based on Aeolus data is possible, however: we collected about 100 profiles to statistically reduce the uncertainty in the daily averaged <span class="inline-formula"><i>E</i><sub>kin</sub></span>. Compared to non-satellite measurements, those daily averaged values are at the upper border.</p> |
| format | Article |
| id | doaj-art-4517a3925e39468eadce2a45ba9fdc8c |
| institution | OA Journals |
| issn | 1867-1381 1867-8548 |
| language | English |
| publishDate | 2025-04-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Atmospheric Measurement Techniques |
| spelling | doaj-art-4517a3925e39468eadce2a45ba9fdc8c2025-08-20T01:51:36ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482025-04-01181591160710.5194/amt-18-1591-2025Gravity waves above the northern Atlantic and Europe during streamer events using AeolusS. Wüst0L. Küchelbacher1F. Trinkl2F. Trinkl3M. Bittner4M. Bittner5Erdbeobachtungszentrum, Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen, 82234 Wessling, GermanyErdbeobachtungszentrum, Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen, 82234 Wessling, Germanynow at: Institute of Meteorology and Climate Research - Atmospheric Trace Gases and Remote Sensing, Karlsruhe Institute of Technology, 76131 Karlsruhe, Germanyformerly at: Erdbeobachtungszentrum, Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen, 82234 Wessling, GermanyErdbeobachtungszentrum, Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen, 82234 Wessling, GermanyInstitut für Physik, Universität Augsburg, 86159 Augsburg, Germany<p>Information about the energy density of gravity waves (GWs) is crucial for improving atmosphere models. So far, most space-based studies report the potential energy, <span class="inline-formula"><i>E</i><sub>pot</sub></span>, of GWs, as temperature measurements from satellites are more common.</p> <p>We use Aeolus wind data to derive the kinetic energy density, <span class="inline-formula"><i>E</i><sub>kin</sub></span>, of GWs above the northern Atlantic and Europe. Assuming perfect instrument performance, this would be a lower limit for the kinetic energy density, as Aeolus only measures the horizontal line-of-sight wind. Aeolus, the European Space Agency's (ESA's) fourth Earth Explorer Mission, was the first Doppler wind lidar in space and measured vertical profiles of the horizontal line-of-sight wind from the ground to an altitude of <span class="inline-formula">∼</span> 20–30 km between 2018 and 2023. With a vertical resolution of 0.25–2 km, Aeolus measurements are in principle well suited for the analysis of GWs. However, the data quality is a challenge for such analyses, as the error in the data is in the range of typical GW amplitudes in the troposphere and stratosphere.</p> <p>In this study, we derive daily resolved time series of <span class="inline-formula"><i>E</i><sub>kin</sub></span> before, during, and after two streamer events above the northern Atlantic and Europe. Streamers are large-scale tongue-like structures of meridionally deflected air masses, which are caused by enhanced planetary wave activity. They are linked to vertical shear of horizontal wind and a pressure system, two possible GW generation mechanisms. We find that there is a temporal coincidence between the enhanced daily averaged <span class="inline-formula"><i>E</i><sub>kin</sub></span> and occurrence of the streamer events, which we identified in total column ozone measurements. The derivation of GW signals based on Aeolus data is possible, however: we collected about 100 profiles to statistically reduce the uncertainty in the daily averaged <span class="inline-formula"><i>E</i><sub>kin</sub></span>. Compared to non-satellite measurements, those daily averaged values are at the upper border.</p>https://amt.copernicus.org/articles/18/1591/2025/amt-18-1591-2025.pdf |
| spellingShingle | S. Wüst L. Küchelbacher F. Trinkl F. Trinkl M. Bittner M. Bittner Gravity waves above the northern Atlantic and Europe during streamer events using Aeolus Atmospheric Measurement Techniques |
| title | Gravity waves above the northern Atlantic and Europe during streamer events using Aeolus |
| title_full | Gravity waves above the northern Atlantic and Europe during streamer events using Aeolus |
| title_fullStr | Gravity waves above the northern Atlantic and Europe during streamer events using Aeolus |
| title_full_unstemmed | Gravity waves above the northern Atlantic and Europe during streamer events using Aeolus |
| title_short | Gravity waves above the northern Atlantic and Europe during streamer events using Aeolus |
| title_sort | gravity waves above the northern atlantic and europe during streamer events using aeolus |
| url | https://amt.copernicus.org/articles/18/1591/2025/amt-18-1591-2025.pdf |
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