Satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere (MLT): feasibility and requirements

<p>In the recent decade it became evident that we need to revise our picture of how gravity waves (GWs) reach the mesosphere and lower thermosphere (MLT). This has consequences for our understanding not just of the properties of the GWs themselves, but in particular of the global circulation i...

Full description

Bibliographic Details
Main Authors: Q. Chen, K. Ntokas, B. Linder, L. Krasauskas, M. Ern, P. Preusse, J. Ungermann, E. Becker, M. Kaufmann, M. Riese
Format: Article
Language:English
Published: Copernicus Publications 2022-12-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/15/7071/2022/amt-15-7071-2022.pdf
_version_ 1811205935488565248
author Q. Chen
K. Ntokas
B. Linder
L. Krasauskas
M. Ern
P. Preusse
J. Ungermann
E. Becker
M. Kaufmann
M. Riese
author_facet Q. Chen
K. Ntokas
B. Linder
L. Krasauskas
M. Ern
P. Preusse
J. Ungermann
E. Becker
M. Kaufmann
M. Riese
author_sort Q. Chen
collection DOAJ
description <p>In the recent decade it became evident that we need to revise our picture of how gravity waves (GWs) reach the mesosphere and lower thermosphere (MLT). This has consequences for our understanding not just of the properties of the GWs themselves, but in particular of the global circulation in the MLT. Information on spectral distribution, direction, and zonal mean GW momentum flux is required to test the theoretical and modeling findings. In this study, we propose a constellation of two CubeSats for observing mesoscale GWs in the MLT region by means of temperature limb sounding in order to derive such constraints. Each CubeSat deploys a highly miniaturized spatial heterodyne interferometer (SHI) for the measurement of global oxygen atmospheric band emissions. From these emissions, the 3-D temperature structure can be inferred. We propose obtaining four independent observation tracks by splitting the interferograms in the center and thus gaining two observation tracks for each satellite. We present a feasibility study of this concept based on self-consistent, high-resolution global model data. This yields a full chain of end-to-end (E2E) simulations incorporating (1) orbit simulation, (2) airglow forward modeling, (3) tomographic temperature retrieval, (4) 3-D wave analysis, and (5) GW momentum flux (GWMF) calculation. The simulation performance is evaluated by comparing the retrieved zonal mean GWMF with that computed directly from the model wind data. A major question to be considered in our assessment is the minimum number of tracks required for the derivation of 3-D GW parameters. The main result from our simulations is that the GW polarization relations are still valid in the MLT region and can thus be employed for inferring GWMF from the 3-D temperature distributions. Based on the E2E simulations for gaining zonal mean climatologies of GW momentum flux, we demonstrate that our approach is robust and stable, given a four-track observation geometry and the expected instrument noise under nominal operation conditions. Using phase speed and direction spectra we show also that the properties of individual wave events are recovered when employing four tracks. Finally, we discuss the potential of the proposed observations to address current topics in the GW research. We outline for which investigations ancillary data are required to answer science questions.</p>
first_indexed 2024-04-12T03:38:37Z
format Article
id doaj.art-22f22add6d5b4f7db6cf912b5a7d6eec
institution Directory Open Access Journal
issn 1867-1381
1867-8548
language English
last_indexed 2024-04-12T03:38:37Z
publishDate 2022-12-01
publisher Copernicus Publications
record_format Article
series Atmospheric Measurement Techniques
spelling doaj.art-22f22add6d5b4f7db6cf912b5a7d6eec2022-12-22T03:49:20ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482022-12-01157071710310.5194/amt-15-7071-2022Satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere (MLT): feasibility and requirementsQ. Chen0K. Ntokas1B. Linder2L. Krasauskas3M. Ern4P. Preusse5J. Ungermann6E. Becker7M. Kaufmann8M. Riese9Institute of Energy and Climate Research (IEK-7: Stratosphere), Forschungszentrum Jülich, Jülich, GermanyInstitute of Energy and Climate Research (IEK-7: Stratosphere), Forschungszentrum Jülich, Jülich, GermanyDepartment of Meteorology, Stockholm University, Stockholm, SwedenInstitute of Energy and Climate Research (IEK-7: Stratosphere), Forschungszentrum Jülich, Jülich, GermanyInstitute of Energy and Climate Research (IEK-7: Stratosphere), Forschungszentrum Jülich, Jülich, GermanyInstitute of Energy and Climate Research (IEK-7: Stratosphere), Forschungszentrum Jülich, Jülich, GermanyInstitute of Energy and Climate Research (IEK-7: Stratosphere), Forschungszentrum Jülich, Jülich, GermanyNorthwest Research Associates Inc., Boulder, CO, USAInstitute of Energy and Climate Research (IEK-7: Stratosphere), Forschungszentrum Jülich, Jülich, GermanyInstitute of Energy and Climate Research (IEK-7: Stratosphere), Forschungszentrum Jülich, Jülich, Germany<p>In the recent decade it became evident that we need to revise our picture of how gravity waves (GWs) reach the mesosphere and lower thermosphere (MLT). This has consequences for our understanding not just of the properties of the GWs themselves, but in particular of the global circulation in the MLT. Information on spectral distribution, direction, and zonal mean GW momentum flux is required to test the theoretical and modeling findings. In this study, we propose a constellation of two CubeSats for observing mesoscale GWs in the MLT region by means of temperature limb sounding in order to derive such constraints. Each CubeSat deploys a highly miniaturized spatial heterodyne interferometer (SHI) for the measurement of global oxygen atmospheric band emissions. From these emissions, the 3-D temperature structure can be inferred. We propose obtaining four independent observation tracks by splitting the interferograms in the center and thus gaining two observation tracks for each satellite. We present a feasibility study of this concept based on self-consistent, high-resolution global model data. This yields a full chain of end-to-end (E2E) simulations incorporating (1) orbit simulation, (2) airglow forward modeling, (3) tomographic temperature retrieval, (4) 3-D wave analysis, and (5) GW momentum flux (GWMF) calculation. The simulation performance is evaluated by comparing the retrieved zonal mean GWMF with that computed directly from the model wind data. A major question to be considered in our assessment is the minimum number of tracks required for the derivation of 3-D GW parameters. The main result from our simulations is that the GW polarization relations are still valid in the MLT region and can thus be employed for inferring GWMF from the 3-D temperature distributions. Based on the E2E simulations for gaining zonal mean climatologies of GW momentum flux, we demonstrate that our approach is robust and stable, given a four-track observation geometry and the expected instrument noise under nominal operation conditions. Using phase speed and direction spectra we show also that the properties of individual wave events are recovered when employing four tracks. Finally, we discuss the potential of the proposed observations to address current topics in the GW research. We outline for which investigations ancillary data are required to answer science questions.</p>https://amt.copernicus.org/articles/15/7071/2022/amt-15-7071-2022.pdf
spellingShingle Q. Chen
K. Ntokas
B. Linder
L. Krasauskas
M. Ern
P. Preusse
J. Ungermann
E. Becker
M. Kaufmann
M. Riese
Satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere (MLT): feasibility and requirements
Atmospheric Measurement Techniques
title Satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere (MLT): feasibility and requirements
title_full Satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere (MLT): feasibility and requirements
title_fullStr Satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere (MLT): feasibility and requirements
title_full_unstemmed Satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere (MLT): feasibility and requirements
title_short Satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere (MLT): feasibility and requirements
title_sort satellite observations of gravity wave momentum flux in the mesosphere and lower thermosphere mlt feasibility and requirements
url https://amt.copernicus.org/articles/15/7071/2022/amt-15-7071-2022.pdf
work_keys_str_mv AT qchen satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT kntokas satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT blinder satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT lkrasauskas satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT mern satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT ppreusse satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT jungermann satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT ebecker satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT mkaufmann satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements
AT mriese satelliteobservationsofgravitywavemomentumfluxinthemesosphereandlowerthermospheremltfeasibilityandrequirements