Observed and Modeled Mountain Waves from the Surface to the Mesosphere near the Drake Passage

Four state-of-the-science numerical weather prediction (NWP) models were used to perform mountain wave (MW)-resolving hindcasts over the Drake Passage of a 10-day period in 2010 with numerous observed MW cases. The Integrated Forecast System (IFS) and the Icosahedral Nonhydrostatic (ICON) model were...

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Vydáno v:Journal of the atmospheric sciences Ročník 79; číslo 4; s. 909 - 932
Hlavní autoři: Kruse, Christopher G., Alexander, M. Joan, Hoffmann, Lars, van Niekerk, Annelize, Polichtchouk, Inna, Bacmeister, Julio T., Holt, Laura, Plougonven, Riwal, Šácha, Petr, Wright, Corwin, Sato, Kaoru, Shibuya, Ryosuke, Gisinger, Sonja, Ern, Manfred, Meyer, Catrin I., Stein, Olaf
Médium: Journal Article
Jazyk:angličtina
Vydáno: Boston American Meteorological Society 01.04.2022
Témata:
Amplitudes
Atmosphere
Atmospheric Infrared Sounder
Atmospheric models
Climate models
Direction
Domains
Drag
Fluxes
Fluxing
Global weather
Lee waves
Lower mantle
Mesosphere
Meteorological satellites
Middle atmosphere
Modelling
Momentum
Mountain waves
Mountains
Numerical prediction
Numerical weather forecasting
Radiative transfer
Resolution
Sciences of the Universe
Stratosphere
Temperature
Upper stratosphere
Weather
Weather forecasting
Winds
Zonal winds
Drake Passage
ISSN:0022-4928, 1520-0469
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Abstract Four state-of-the-science numerical weather prediction (NWP) models were used to perform mountain wave (MW)-resolving hindcasts over the Drake Passage of a 10-day period in 2010 with numerous observed MW cases. The Integrated Forecast System (IFS) and the Icosahedral Nonhydrostatic (ICON) model were run at Δ x ≈ 9 and 13 km globally. The Weather Research and Forecasting (WRF) Model and the Met Office Unified Model (UM) were both configured with a Δ x = 3-km regional domain. All domains had tops near 1 Pa ( z ≈ 80 km). These deep domains allowed quantitative validation against Atmospheric Infrared Sounder (AIRS) observations, accounting for observation time, viewing geometry, and radiative transfer. All models reproduced observed middle-atmosphere MWs with remarkable skill. Increased horizontal resolution improved validations. Still, all models underrepresented observed MW amplitudes, even after accounting for model effective resolution and instrument noise, suggesting even at Δ x ≈ 3-km resolution, small-scale MWs are underresolved and/or overdiffused. MW drag parameterizations are still necessary in NWP models at current operational resolutions of Δ x ≈ 10 km. Upper GW sponge layers in the operationally configured models significantly, artificially reduced MW amplitudes in the upper stratosphere and mesosphere. In the IFS, parameterized GW drags partly compensated this deficiency, but still, total drags were ≈6 times smaller than that resolved at Δ x ≈ 3 km. Meridionally propagating MWs significantly enhance zonal drag over the Drake Passage. Interestingly, drag associated with meridional fluxes of zonal momentum (i.e., ) were important; not accounting for these terms results in a drag in the wrong direction at and below the polar night jet.
AbstractList Four state-of-the-science numerical weather prediction (NWP) models were used to perform mountain wave (MW)-resolving hindcasts over the Drake Passage of a 10-day period in 2010 with numerous observed MW cases. The Integrated Forecast System (IFS) and the Icosahedral Nonhydrostatic (ICON) model were run at Δx ≈ 9 and 13 km globally. The Weather Research and Forecasting (WRF) Model and the Met Office Unified Model (UM) were both configured with a Δx = 3-km regional domain. All domains had tops near 1 Pa (z ≈ 80 km). These deep domains allowed quantitative validation against Atmospheric Infrared Sounder (AIRS) observations, accounting for observation time, viewing geometry, and radiative transfer. All models reproduced observed middle-atmosphere MWs with remarkable skill. Increased horizontal resolution improved validations. Still, all models underrepresented observed MW amplitudes, even after accounting for model effective resolution and instrument noise, suggesting even at Δx ≈ 3-km resolution, small-scale MWs are underresolved and/or overdiffused. MW drag parameterizations are still necessary in NWP models at current operational resolutions of Δx ≈ 10 km. Upper GW sponge layers in the operationally configured models significantly, artificially reduced MW amplitudes in the upper stratosphere and mesosphere. In the IFS, parameterized GW drags partly compensated this deficiency, but still, total drags were ≈6 times smaller than that resolved at Δx ≈ 3 km. Meridionally propagating MWs significantly enhance zonal drag over the Drake Passage. Interestingly, drag associated with meridional fluxes of zonal momentum (i.e., u'υ' ¯ ) were important; not accounting for these terms results in a drag in the wrong direction at and below the polar night jet.
Four state-of-the-science numerical weather prediction (NWP) models were used to perform mountain wave (MW)-resolving hindcasts over the Drake Passage of a 10-day period in 2010 with numerous observed MW cases. The Integrated Forecast System (IFS) and the Icosahedral Nonhydrostatic (ICON) model were run at Δ x ≈ 9 and 13 km globally. The Weather Research and Forecasting (WRF) Model and the Met Office Unified Model (UM) were both configured with a Δ x = 3-km regional domain. All domains had tops near 1 Pa ( z ≈ 80 km). These deep domains allowed quantitative validation against Atmospheric Infrared Sounder (AIRS) observations, accounting for observation time, viewing geometry, and radiative transfer. All models reproduced observed middle-atmosphere MWs with remarkable skill. Increased horizontal resolution improved validations. Still, all models underrepresented observed MW amplitudes, even after accounting for model effective resolution and instrument noise, suggesting even at Δ x ≈ 3-km resolution, small-scale MWs are underresolved and/or overdiffused. MW drag parameterizations are still necessary in NWP models at current operational resolutions of Δ x ≈ 10 km. Upper GW sponge layers in the operationally configured models significantly, artificially reduced MW amplitudes in the upper stratosphere and mesosphere. In the IFS, parameterized GW drags partly compensated this deficiency, but still, total drags were ≈6 times smaller than that resolved at Δ x ≈ 3 km. Meridionally propagating MWs significantly enhance zonal drag over the Drake Passage. Interestingly, drag associated with meridional fluxes of zonal momentum (i.e., ) were important; not accounting for these terms results in a drag in the wrong direction at and below the polar night jet.
Four state-of-the-science numerical weather prediction (NWP) models were used to perform mountain wave (MW)-resolving hindcasts over the Drake Passage of a 10-day period in 2010 with numerous observed MW cases. The Integrated Forecast System (IFS) and the Icosahedral Nonhydrostatic (ICON) model were run at Δx ≈ 9 and 13 km globally. The Weather Research and Forecasting (WRF) Model and the Met Office Unified Model (UM) were both configured with a Δx = 3-km regional domain. All domains had tops near 1 Pa (z ≈ 80 km). These deep domains allowed quantitative validation against Atmospheric Infrared Sounder (AIRS) observations, accounting for observation time, viewing geometry, and radiative transfer. All models reproduced observed middle-atmosphere MWs with remarkable skill. Increased horizontal resolution improved validations. Still, all models underrepresented observed MW amplitudes, even after accounting for model effective resolution and instrument noise, suggesting even at Δx ≈ 3-km resolution, small-scale MWs are underresolved and/or overdiffused. MW drag parameterizations are still necessary in NWP models at current operational resolutions of Δx ≈ 10 km. Upper GW sponge layers in the operationally configured models significantly, artificially reduced MW amplitudes in the upper stratosphere and mesosphere. In the IFS, parameterized GW drags partly compensated this deficiency, but still, total drags were ≈6 times smaller than that resolved at Δx ≈ 3 km. Meridionally propagating MWs significantly enhance zonal drag over the Drake Passage. Interestingly, drag associated with meridional fluxes of zonal momentum (i.e.,u′υ′¯ ) were important; not accounting for these terms results in a drag in the wrong direction at and below the polar night jet.Significance StatementThis study had three purposes: to quantitatively evaluate how well four state-of-the-science weather models could reproduce observed mountain waves (MWs) in the middle atmosphere, to compare the simulated MWs within the models, and to quantitatively evaluate two MW parameterizations in a widely used climate model. These models reproduced observed MWs with remarkable skill. Still, MW parameterizations are necessary in current Δx ≈ 10-km resolution global weather models. Even Δx ≈ 3-km resolution does not appear to be high enough to represent all momentum-fluxing MW scales. Meridionally propagating MWs can significantly influence zonal winds over the Drake Passage. Parameterizations that handle horizontal propagation may need to consider horizontal fluxes of horizontal momentum in order to get the direction of their forcing correct.
Author van Niekerk, Annelize
Bacmeister, Julio T.
Gisinger, Sonja
Plougonven, Riwal
Ern, Manfred
Sato, Kaoru
Alexander, M. Joan
Stein, Olaf
Polichtchouk, Inna
Šácha, Petr
Kruse, Christopher G.
Hoffmann, Lars
Holt, Laura
Wright, Corwin
Meyer, Catrin I.
Shibuya, Ryosuke
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PublicationTitle Journal of the atmospheric sciences
PublicationYear 2022
Publisher American Meteorological Society
Publisher_xml – name: American Meteorological Society
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Snippet Four state-of-the-science numerical weather prediction (NWP) models were used to perform mountain wave (MW)-resolving hindcasts over the Drake Passage of a...
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StartPage 909
SubjectTerms Amplitudes
Atmosphere
Atmospheric Infrared Sounder
Atmospheric models
Climate models
Direction
Domains
Drag
Fluxes
Fluxing
Global weather
Lee waves
Lower mantle
Mesosphere
Meteorological satellites
Middle atmosphere
Modelling
Momentum
Mountain waves
Mountains
Numerical prediction
Numerical weather forecasting
Radiative transfer
Resolution
Sciences of the Universe
Stratosphere
Temperature
Upper stratosphere
Weather
Weather forecasting
Winds
Zonal winds
Title Observed and Modeled Mountain Waves from the Surface to the Mesosphere near the Drake Passage
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https://insu.hal.science/insu-03726907
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