Articles | Volume 11, issue 2
https://doi.org/10.5194/amt-11-1031-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-11-1031-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
22 Feb 2018
Research article |
| 22 Feb 2018
| 22 Feb 2018
An intercomparison of stratospheric gravity wave potential energy densities from METOP GPS radio occultation measurements and ECMWF model data
Deutsches Zentrum für Luft- und Raumfahrt, Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
Meteorologisches Institut München, Ludwig-Maximilians-Universität München, Munich, Germany
Andreas Dörnbrack
Deutsches Zentrum für Luft- und Raumfahrt, Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
Bernd Kaifler
Deutsches Zentrum für Luft- und Raumfahrt, Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
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Cited
21 citations as recorded by crossref.
- Global analysis for periodic variations in gravity wave squared amplitudes and momentum fluxes in the middle atmosphere D. Chen et al. 10.5194/angeo-37-487-2019
- Large Midlatitude Stratospheric Temperature Variability Caused by Inertial Instability: A Potential Source of Bias for Gravity Wave Climatologies M. Rapp et al. 10.1029/2018GL079142
- Tropospheric Gravity Waves as Observed by the High‐Resolution China Radiosonde Network and Their Potential Sources J. Zhang et al. 10.1029/2022JD037174
- How does knowledge of atmospheric gravity waves guide their parameterizations? R. Plougonven et al. 10.1002/qj.3732
- Reconstruction of the Internal-Wave Parameters in the Atmosphere from Signal Amplitude Fluctuations in a Radio-Occultation Experiment V. Kan et al. 10.1134/S0001433820050072
- Tropical Temperature Variability in the UTLS: New Insights from GPS Radio Occultation Observations B. Scherllin-Pirscher et al. 10.1175/JCLI-D-20-0385.1
- The Study of Internal Gravity Waves in the Earth’s Atmosphere by Radio Occultations: A Review M. Gorbunov & V. Kan 10.3390/rs16020221
- Assessing middle atmosphere weather models using infrasound detections from microbaroms P. Hupe et al. 10.1093/gji/ggy520
- High‐Cadence Lidar Observations of Middle Atmospheric Temperature and Gravity Waves at the Southern Andes Hot Spot R. Reichert et al. 10.1029/2021JD034683
- Latitudinal Distribution of the Parameters of Internal Gravity Waves in the Atmosphere Derived from Amplitude Fluctuations of Radio Occultation Signals V. Kan et al. 10.1134/S0001433820060055
- Temperature Profiles From Two Close Lidars and a Satellite to Infer the Structure of a Dominant Gravity Wave P. Alexander et al. 10.1029/2020EA001074
- How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements? P. Hupe et al. 10.3390/atmos10070399
- Removing spurious inertial instability signals from gravity wave temperature perturbations using spectral filtering methods C. Strube et al. 10.5194/amt-13-4927-2020
- Magnitudes of Gravity Wave Pseudomomentum Flux Derived by Combining COSMIC Radio Occultation and ERA-Interim Reanalysis Data X. Xu et al. 10.3390/atmos10100598
- Beware of Inertial Instability Masquerading as Gravity Waves in Stratospheric Temperature Perturbations V. Harvey & J. Knox 10.1029/2018GL081142
- Noise Floor and Signal-to-Noise Ratio of Radio Occultation Observations: A Cross-Mission Statistical Comparison M. Gorbunov et al. 10.3390/rs14030691
- Ionospheric Peak Parameters Retrieved from FY-3C Radio Occultation: A Statistical Comparison with Measurements from COSMIC RO and Digisondes Over the Globe H. Wang et al. 10.3390/rs11121419
- The parameters of internal gravity waves in the atmosphere from the amplitude fluctuations of radio occultation signals V. Kan et al. 10.1088/1755-1315/1040/1/012008
- Investigating the Spatio-Temporal Distribution of Gravity Wave Potential Energy over the Equatorial Region Using the ERA5 Reanalysis Data S. Yang et al. 10.3390/atmos12030311
- Stratospheric Gravity Wave Products from Satellite Infrared Nadir Radiances in the Planning, Execution, and Validation of Aircraft Measurements during DEEPWAVE S. Eckermann et al. 10.1175/JAMC-D-19-0015.1
- Assessment of FY-3E GNOS II Radio Occultation Data Using an Improved Three-Cornered Hat Method J. Liang et al. 10.3390/rs16203808
21 citations as recorded by crossref.
- Global analysis for periodic variations in gravity wave squared amplitudes and momentum fluxes in the middle atmosphere D. Chen et al. 10.5194/angeo-37-487-2019
- Large Midlatitude Stratospheric Temperature Variability Caused by Inertial Instability: A Potential Source of Bias for Gravity Wave Climatologies M. Rapp et al. 10.1029/2018GL079142
- Tropospheric Gravity Waves as Observed by the High‐Resolution China Radiosonde Network and Their Potential Sources J. Zhang et al. 10.1029/2022JD037174
- How does knowledge of atmospheric gravity waves guide their parameterizations? R. Plougonven et al. 10.1002/qj.3732
- Reconstruction of the Internal-Wave Parameters in the Atmosphere from Signal Amplitude Fluctuations in a Radio-Occultation Experiment V. Kan et al. 10.1134/S0001433820050072
- Tropical Temperature Variability in the UTLS: New Insights from GPS Radio Occultation Observations B. Scherllin-Pirscher et al. 10.1175/JCLI-D-20-0385.1
- The Study of Internal Gravity Waves in the Earth’s Atmosphere by Radio Occultations: A Review M. Gorbunov & V. Kan 10.3390/rs16020221
- Assessing middle atmosphere weather models using infrasound detections from microbaroms P. Hupe et al. 10.1093/gji/ggy520
- High‐Cadence Lidar Observations of Middle Atmospheric Temperature and Gravity Waves at the Southern Andes Hot Spot R. Reichert et al. 10.1029/2021JD034683
- Latitudinal Distribution of the Parameters of Internal Gravity Waves in the Atmosphere Derived from Amplitude Fluctuations of Radio Occultation Signals V. Kan et al. 10.1134/S0001433820060055
- Temperature Profiles From Two Close Lidars and a Satellite to Infer the Structure of a Dominant Gravity Wave P. Alexander et al. 10.1029/2020EA001074
- How Can the International Monitoring System Infrasound Network Contribute to Gravity Wave Measurements? P. Hupe et al. 10.3390/atmos10070399
- Removing spurious inertial instability signals from gravity wave temperature perturbations using spectral filtering methods C. Strube et al. 10.5194/amt-13-4927-2020
- Magnitudes of Gravity Wave Pseudomomentum Flux Derived by Combining COSMIC Radio Occultation and ERA-Interim Reanalysis Data X. Xu et al. 10.3390/atmos10100598
- Beware of Inertial Instability Masquerading as Gravity Waves in Stratospheric Temperature Perturbations V. Harvey & J. Knox 10.1029/2018GL081142
- Noise Floor and Signal-to-Noise Ratio of Radio Occultation Observations: A Cross-Mission Statistical Comparison M. Gorbunov et al. 10.3390/rs14030691
- Ionospheric Peak Parameters Retrieved from FY-3C Radio Occultation: A Statistical Comparison with Measurements from COSMIC RO and Digisondes Over the Globe H. Wang et al. 10.3390/rs11121419
- The parameters of internal gravity waves in the atmosphere from the amplitude fluctuations of radio occultation signals V. Kan et al. 10.1088/1755-1315/1040/1/012008
- Investigating the Spatio-Temporal Distribution of Gravity Wave Potential Energy over the Equatorial Region Using the ERA5 Reanalysis Data S. Yang et al. 10.3390/atmos12030311
- Stratospheric Gravity Wave Products from Satellite Infrared Nadir Radiances in the Planning, Execution, and Validation of Aircraft Measurements during DEEPWAVE S. Eckermann et al. 10.1175/JAMC-D-19-0015.1
- Assessment of FY-3E GNOS II Radio Occultation Data Using an Improved Three-Cornered Hat Method J. Liang et al. 10.3390/rs16203808
Latest update: 20 Nov 2024
Short summary
Temperature profiles from operational weather satellites are used to determine the global distribution of gravity wave activity. This is an important information to constrain global climate models. The quality of this data set is assessed by
systematic comparison to model fields from ECMWF which are considered very high quality. This reveals good agreement between model and observations, albeit the model misses localized centers of wave activity if model resolution is too low.
Temperature profiles from operational weather satellites are used to determine the global...
