28 June 2015 to 3 July 2015
Africa/Johannesburg timezone
SAIP2015 Proceeding published on 17 July 2016

The study on the short term planetary wave activity in the MLT region over Southern Hemisphere using SuperDARN HF radar

2 Jul 2015, 11:30
20m
Oral Presentation Track D2 - Space Science Space

Speaker

Mr Ntlakanipho Ngwane (Student)

Main supervisor (name and email)<br>and his / her institution

Prof. Sivakumar Venkataraman

Apply to be<br> considered for a student <br> &nbsp; award (Yes / No)?

Yes

Would you like to <br> submit a short paper <br> for the Conference <br> Proceedings (Yes / No)?

Yes

Level for award<br>&nbsp;(Hons, MSc, <br> &nbsp; PhD, N/A)?

MSc

Abstract content <br> &nbsp; (Max 300 words)<br><a href="http://events.saip.org.za/getFile.py/access?resId=0&materialId=0&confId=34" target="_blank">Formatting &<br>Special chars</a>

The mesosphere lower thermosphere (MLT) region connects the middle atmosphere to the thermosphere. It is therefore a combination of physical dynamics due to forced waves from lower atmospheric layers and photochemical reactions enhanced by solar radiation. This work focuses on the influence that forced atmospheric waves (for e-g planetary waves and atmospheric tides) from lower layers have on the MLT dynamics. SuperDARN HF radar is used to study short term planetary wave activity in the MLT over southern hemisphere. The emphasis on the “short term” behaviour is motivated by the substantial work conducted on the relatively large period planetary waves (e-g 14, 16, 20, 23 and 27 day waves). Short period planetary waves in this work refer to waves ranging from quasi 2 to 6 day waves. This work will also study interactions between tides and planetary waves during minor sudden stratospheric warming (SSW) events. SSW is characterized by a rapid enhancement of stratospheric temperature that takes place, within few days, poleward from 60° latitude and at 10 hPa pressure level or below, and is followed by a deceleration and/or reversal of eastward winter winds.

We have thus far identified the years and days of interests, where minor warming events occurred. We have produced wind dynamic spectra for those years. From the dynamic spectra, extracted the wind speed amplitudes corresponding to minor warming days. The analysis that is still pending is the wavelet spectral representation of short term planetary waves and the bi-spectra plots comprising of the planetary waves and atmospheric tides so as to study the interactions. The obtained and planned results shall be presented in the conference.

Please indicate whether<br>this abstract may be<br>published online<br>(Yes / No)

Yes

Primary author

Co-authors

Dr Sibusiso Mthembu (University of KwaZulu Natal) Prof. Venkataraman Sivakumar (University of KwaZulu Natal)

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