How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements?

Gravity waves (GWs) propagate horizontally and vertically in the atmosphere. They transport energy and momentum, and therefore GWs can affect the atmospheric circulation at different altitude layers when dissipating. Thus knowledge about the occurrence of GWs is essential for Numerical Weather Predi...

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Main Authors: Patrick Hupe, Lars Ceranna, Alexis Le Pichon
Format: Article
Language:English
Published: MDPI AG 2019-07-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/10/7/399
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spelling doaj-415d0516e36c4dfab35c86e7b0f599132020-11-25T02:23:48ZengMDPI AGAtmosphere2073-44332019-07-0110739910.3390/atmos10070399atmos10070399How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements?Patrick Hupe0Lars Ceranna1Alexis Le Pichon2Federal Institute for Geosciences and Natural Resources (BGR), B4.3, 30655 Hannover, GermanyFederal Institute for Geosciences and Natural Resources (BGR), B4.3, 30655 Hannover, GermanyCommissariat à l’énergie atomique et aux énergies alternatives (CEA), DAM, DIF, 91297 Arpajon, FranceGravity waves (GWs) propagate horizontally and vertically in the atmosphere. They transport energy and momentum, and therefore GWs can affect the atmospheric circulation at different altitude layers when dissipating. Thus knowledge about the occurrence of GWs is essential for Numerical Weather Prediction (NWP). However, uniform networks for covering GW measurements globally are rare, especially in the troposphere. It has been shown that an infrasound station of the International Monitoring System (IMS) infrasound network is capable of measuring GWs at the Earth’s surface. The IMS was deployed for monitoring the atmosphere to verify compliance with the Comprehensive Nuclear-Test-Ban-Treaty. In this study, the Progressive Multi-Channel Correlation Method (PMCC) is used for re-processing up to 20 years of IMS infrasound recordings in order to derive GW detections. For this purpose, two alternative PMCC configurations are discussed, covering GW frequencies equivalent to periods of between 5 min and 150 min. These detections mainly reflect sources of deep convection, particularly in the tropics. At mid-latitudes, coherent wind noise more often produces spurious detections. Combining the results of both configurations provides a global dataset of ground-based GW measurements, which enables the calculation of GW parameters. These can be used for improving NWP models.https://www.mdpi.com/2073-4433/10/7/399International Monitoring System (IMS)infrasoundgravity wavesComprehensive Nuclear-Test-Ban Treaty (CTBT)atmospheric dynamicsARISEPMCC
collection DOAJ
language English
format Article
sources DOAJ
author Patrick Hupe
Lars Ceranna
Alexis Le Pichon
spellingShingle Patrick Hupe
Lars Ceranna
Alexis Le Pichon
How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements?
Atmosphere
International Monitoring System (IMS)
infrasound
gravity waves
Comprehensive Nuclear-Test-Ban Treaty (CTBT)
atmospheric dynamics
ARISE
PMCC
author_facet Patrick Hupe
Lars Ceranna
Alexis Le Pichon
author_sort Patrick Hupe
title How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements?
title_short How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements?
title_full How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements?
title_fullStr How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements?
title_full_unstemmed How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements?
title_sort how can the international monitoring system infrasound network contribute to gravity wave measurements?
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2019-07-01
description Gravity waves (GWs) propagate horizontally and vertically in the atmosphere. They transport energy and momentum, and therefore GWs can affect the atmospheric circulation at different altitude layers when dissipating. Thus knowledge about the occurrence of GWs is essential for Numerical Weather Prediction (NWP). However, uniform networks for covering GW measurements globally are rare, especially in the troposphere. It has been shown that an infrasound station of the International Monitoring System (IMS) infrasound network is capable of measuring GWs at the Earth’s surface. The IMS was deployed for monitoring the atmosphere to verify compliance with the Comprehensive Nuclear-Test-Ban-Treaty. In this study, the Progressive Multi-Channel Correlation Method (PMCC) is used for re-processing up to 20 years of IMS infrasound recordings in order to derive GW detections. For this purpose, two alternative PMCC configurations are discussed, covering GW frequencies equivalent to periods of between 5 min and 150 min. These detections mainly reflect sources of deep convection, particularly in the tropics. At mid-latitudes, coherent wind noise more often produces spurious detections. Combining the results of both configurations provides a global dataset of ground-based GW measurements, which enables the calculation of GW parameters. These can be used for improving NWP models.
topic International Monitoring System (IMS)
infrasound
gravity waves
Comprehensive Nuclear-Test-Ban Treaty (CTBT)
atmospheric dynamics
ARISE
PMCC
url https://www.mdpi.com/2073-4433/10/7/399
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