Offline estimates and tuning of mesospheric gravity‐wave forcing using Met Office analyses
Estimates of small‐scale non‐orographic gravity‐wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such estimates are obtained using the ultrasimple spectral parametrization (USSP) gravity‐wave scheme, currently employed operationally by the Met Office. A c...
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| Published in | Quarterly journal of the Royal Meteorological Society Vol. 140; no. 680; pp. 1025 - 1038 |
|---|---|
| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
Chichester, UK
John Wiley & Sons, Ltd
01.04.2014
Wiley Wiley Subscription Services, Inc |
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| Online Access | Get full text |
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| Abstract | Estimates of small‐scale non‐orographic gravity‐wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such estimates are obtained using the ultrasimple spectral parametrization (USSP) gravity‐wave scheme, currently employed operationally by the Met Office. A climatology of monthly zonal mean gravity‐wave forcing from January 2005–December 2010 is presented, along with a discussion of estimated uncertainties and comparison with previous studies. Mesospheric gravity‐wave forcing is found to be underestimated, consistent with the known seasonal evolution of extratropical mesospheric temperature biases within the Met Office assimilated dataset. The sensitivity of gravity‐wave forcing to various parameters within the USSP scheme is investigated. Subsequent experiments diagnose the temperature response in a free‐running version of the Unified Model when mesospheric gravity‐wave forcing is increased through perturbing the energy scalefactor parameter within the USSP scheme and imposing momentum‐flux conservation at the model lid. For physically justifiable perturbations to the USSP scheme, significant temperature responses of ∼10–25 K are seen for mesospheric polar regions under solstice conditions, highlighting the positive impact such changes could possibly have on known temperature biases within the Met Office assimilated dataset. |
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| AbstractList | Estimates of small-scale non-orographic gravity-wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such estimates are obtained using the ultrasimple spectral parametrization (USSP) gravity-wave scheme, currently employed operationally by the Met Office. A climatology of monthly zonal mean gravity-wave forcing from January 2005-December 2010 is presented, along with a discussion of estimated uncertainties and comparison with previous studies. Mesospheric gravity-wave forcing is found to be underestimated, consistent with the known seasonal evolution of extratropical mesospheric temperature biases within the Met Office assimilated dataset. The sensitivity of gravity-wave forcing to various parameters within the USSP scheme is investigated. Subsequent experiments diagnose the temperature response in a free-running version of the Unified Model when mesospheric gravity-wave forcing is increased through perturbing the energy scalefactor parameter within the USSP scheme and imposing momentum-flux conservation at the model lid. For physically justifiable perturbations to the USSP scheme, significant temperature responses of 10-25 K are seen for mesospheric polar regions under solstice conditions, highlighting the positive impact such changes could possibly have on known temperature biases within the Met Office assimilated dataset. [PUBLICATION ABSTRACT] Abstract Estimates of small‐scale non‐orographic gravity‐wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such estimates are obtained using the ultrasimple spectral parametrization ( USSP ) gravity‐wave scheme, currently employed operationally by the Met Office. A climatology of monthly zonal mean gravity‐wave forcing from January 2005–December 2010 is presented, along with a discussion of estimated uncertainties and comparison with previous studies. Mesospheric gravity‐wave forcing is found to be underestimated, consistent with the known seasonal evolution of extratropical mesospheric temperature biases within the Met Office assimilated dataset. The sensitivity of gravity‐wave forcing to various parameters within the USSP scheme is investigated. Subsequent experiments diagnose the temperature response in a free‐running version of the Unified Model when mesospheric gravity‐wave forcing is increased through perturbing the energy scalefactor parameter within the USSP scheme and imposing momentum‐flux conservation at the model lid. For physically justifiable perturbations to the USSP scheme, significant temperature responses of ∼10–25 K are seen for mesospheric polar regions under solstice conditions, highlighting the positive impact such changes could possibly have on known temperature biases within the Met Office assimilated dataset. Estimates of small-scale non-orographic gravity-wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such estimates are obtained using the ultrasimple spectral parametrization (USSP) gravity-wave scheme, currently employed operationally by the Met Office. A climatology of monthly zonal mean gravity-wave forcing from January 2005-December 2010 is presented, along with a discussion of estimated uncertainties and comparison with previous studies. Mesospheric gravity-wave forcing is found to be underestimated, consistent with the known seasonal evolution of extratropical mesospheric temperature biases within the Met Office assimilated dataset. The sensitivity of gravity-wave forcing to various parameters within the USSP scheme is investigated. Subsequent experiments diagnose the temperature response in a free-running version of the Unified Model when mesospheric gravity-wave forcing is increased through perturbing the energy scalefactor parameter within the USSP scheme and imposing momentum-flux conservation at the model lid. For physically justifiable perturbations to the USSP scheme, significant temperature responses of 10-25 K are seen for mesospheric polar regions under solstice conditions, highlighting the positive impact such changes could possibly have on known temperature biases within the Met Office assimilated dataset. Estimates of small‐scale non‐orographic gravity‐wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such estimates are obtained using the ultrasimple spectral parametrization (USSP) gravity‐wave scheme, currently employed operationally by the Met Office. A climatology of monthly zonal mean gravity‐wave forcing from January 2005–December 2010 is presented, along with a discussion of estimated uncertainties and comparison with previous studies. Mesospheric gravity‐wave forcing is found to be underestimated, consistent with the known seasonal evolution of extratropical mesospheric temperature biases within the Met Office assimilated dataset. The sensitivity of gravity‐wave forcing to various parameters within the USSP scheme is investigated. Subsequent experiments diagnose the temperature response in a free‐running version of the Unified Model when mesospheric gravity‐wave forcing is increased through perturbing the energy scalefactor parameter within the USSP scheme and imposing momentum‐flux conservation at the model lid. For physically justifiable perturbations to the USSP scheme, significant temperature responses of ∼10–25 K are seen for mesospheric polar regions under solstice conditions, highlighting the positive impact such changes could possibly have on known temperature biases within the Met Office assimilated dataset. |
| Author | Long, D. J. Jackson, D. R. Thuburn, J. |
| Author_xml | – sequence: 1 givenname: D. J. surname: Long fullname: Long, D. J. organization: University of Exeter – sequence: 2 givenname: D. R. surname: Jackson fullname: Jackson, D. R. organization: Met Office – sequence: 3 givenname: J. surname: Thuburn fullname: Thuburn, J. organization: University of Exeter |
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| Keywords | gravity-wave forcing Forcing Mesosphere Gravity wave USSP scheme |
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Monograph contributor: fullname: Holton J |
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| Snippet | Estimates of small‐scale non‐orographic gravity‐wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such estimates... Abstract Estimates of small‐scale non‐orographic gravity‐wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such... Estimates of small-scale non-orographic gravity-wave forcing in the mesosphere are investigated using Met Office middle atmospheric analyses. Such estimates... |
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| Title | Offline estimates and tuning of mesospheric gravity‐wave forcing using Met Office analyses |
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