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Study on the impact of sudden stratosphere warming in the upper mesosphere-lower thermosphere regions using satellite and HF radar - [Article]

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dc.contributor.author Mbatha, N
dc.contributor.author Sivakumar, V
dc.contributor.author Malinga, SB
dc.contributor.author Bencherif, H
dc.contributor.author Pillay, SR
dc.date.accessioned 2009-11-17T09:54:38Z
dc.date.available 2009-11-17T09:54:38Z
dc.date.issued 2010
dc.identifier.citation Mbatha, N, Venkataraman, S, Malinga, SB et al. 2010. Study on the impact of sudden stratosphere warming in the upper mesosphere-lower thermosphere regions using satellite and HF radar measurements. Atmospheric Chemistry and Physics Duscussions, Vol. 10, pp 3397–3404 en
dc.identifier.uri http://hdl.handle.net/10204/3737
dc.identifier.uri http://www.atmos-chem-phys.net/10/3397/2010/acp-10-3397-2010.pdf en
dc.description This work is distributed under the Creative Commons Attribution 3.0 License. en
dc.description.abstract The occurrence of sudden stratospheric warming (SSW) excites disturbances in the mesosphere-lower thermospheric (MLT) wind and temperature. Here, researchers have examined the high frequency (HF) radar wind data from the South African National Antarctic Expedition, SANAE (72° S, 5 3° W), a radar which is part of the Super Dual Auroral Radar Network (SuperDARN). Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) on board the Thermosphere-Ionosphere-Mesosphere-Energetics and Dynamics (TIMED) satellite temperature data and National Centre for Environmental Prediction (NCEP) temperature and wind data were use to investigate the dynamical 10 effects of the unprecedented September 2002 SSW in the Antarctica stratosphere and MLT. The mean zonal wind (from SANAE HF radar) at the MLT shows reversal in approximately 7 days before the reversal at 10 hPa (from NCEP). This indicates that there was a downwards propagation of circulation disturbance. Westerly zonal winds dominate the winter MLT, but during the 2002 winter there were many periods of westward 15 winds observed compared to other years. The dynamic spectrums of both meridional and zonal winds show presence of planetary waves (of ~14-day period) before the occurrence of the SSW. The SABER vertical temperature profiles indicated the cooling of the MLT region before the SSW event. en
dc.language.iso en en
dc.publisher Copernicus Publications & European Geosciences Union en
dc.subject Stratosphere warming en
dc.subject Mesosphere en
dc.subject Thermosphere en
dc.subject High frequency radar en
dc.subject Satellite measurements en
dc.subject Mesosphere-lower thermospheric en
dc.subject Temperature en
dc.subject Atmospheric chemistry en
dc.subject Physics en
dc.subject Super dual auroral radar network en
dc.subject South African National Antarctic Expedition en
dc.subject Broadband Emission Radiometry en
dc.subject SABER en
dc.title Study on the impact of sudden stratosphere warming in the upper mesosphere-lower thermosphere regions using satellite and HF radar - [Article] en
dc.type Article en
dc.identifier.apacitation Mbatha, N., Sivakumar, V., Malinga, S., Bencherif, H., & Pillay, S. (2010). Study on the impact of sudden stratosphere warming in the upper mesosphere-lower thermosphere regions using satellite and HF radar - [Article]. http://hdl.handle.net/10204/3737 en_ZA
dc.identifier.chicagocitation Mbatha, N, V Sivakumar, SB Malinga, H Bencherif, and SR Pillay "Study on the impact of sudden stratosphere warming in the upper mesosphere-lower thermosphere regions using satellite and HF radar - [Article]." (2010) http://hdl.handle.net/10204/3737 en_ZA
dc.identifier.vancouvercitation Mbatha N, Sivakumar V, Malinga S, Bencherif H, Pillay S. Study on the impact of sudden stratosphere warming in the upper mesosphere-lower thermosphere regions using satellite and HF radar - [Article]. 2010; http://hdl.handle.net/10204/3737. en_ZA
dc.identifier.ris TY - Article AU - Mbatha, N AU - Sivakumar, V AU - Malinga, SB AU - Bencherif, H AU - Pillay, SR AB - The occurrence of sudden stratospheric warming (SSW) excites disturbances in the mesosphere-lower thermospheric (MLT) wind and temperature. Here, researchers have examined the high frequency (HF) radar wind data from the South African National Antarctic Expedition, SANAE (72° S, 5 3° W), a radar which is part of the Super Dual Auroral Radar Network (SuperDARN). Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) on board the Thermosphere-Ionosphere-Mesosphere-Energetics and Dynamics (TIMED) satellite temperature data and National Centre for Environmental Prediction (NCEP) temperature and wind data were use to investigate the dynamical 10 effects of the unprecedented September 2002 SSW in the Antarctica stratosphere and MLT. The mean zonal wind (from SANAE HF radar) at the MLT shows reversal in approximately 7 days before the reversal at 10 hPa (from NCEP). This indicates that there was a downwards propagation of circulation disturbance. Westerly zonal winds dominate the winter MLT, but during the 2002 winter there were many periods of westward 15 winds observed compared to other years. The dynamic spectrums of both meridional and zonal winds show presence of planetary waves (of ~14-day period) before the occurrence of the SSW. The SABER vertical temperature profiles indicated the cooling of the MLT region before the SSW event. DA - 2010 DB - ResearchSpace DP - CSIR KW - Stratosphere warming KW - Mesosphere KW - Thermosphere KW - High frequency radar KW - Satellite measurements KW - Mesosphere-lower thermospheric KW - Temperature KW - Atmospheric chemistry KW - Physics KW - Super dual auroral radar network KW - South African National Antarctic Expedition KW - Broadband Emission Radiometry KW - SABER LK - https://researchspace.csir.co.za PY - 2010 T1 - Study on the impact of sudden stratosphere warming in the upper mesosphere-lower thermosphere regions using satellite and HF radar - [Article] TI - Study on the impact of sudden stratosphere warming in the upper mesosphere-lower thermosphere regions using satellite and HF radar - [Article] UR - http://hdl.handle.net/10204/3737 ER - en_ZA


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