dc.contributor.author |
Sivakumar, V
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|
dc.contributor.author |
Bencherif, H
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|
dc.contributor.author |
Acharyulu, DV
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dc.contributor.author |
Hauchecorne, A
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dc.contributor.author |
Rao, DN
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dc.contributor.author |
Sharma, S
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dc.contributor.author |
Rao, PB
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|
dc.date.accessioned |
2009-01-23T09:59:04Z |
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dc.date.available |
2009-01-23T09:59:04Z |
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dc.date.issued |
2006-07 |
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dc.identifier.citation |
Sivakumar, V, Bencherif, H, Acharyulu, DV et al. 2006. Rayleigh lidar investigation of sudden stratospheric warming observed over northern and southern hemisphere stations. Western Pacific Geophysics Meeting, Beijing, China, 24-27 July 2006, pp 24 |
en |
dc.identifier.uri |
http://hdl.handle.net/10204/2891
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|
dc.description |
Western Pacific Geophysics Meeting held in Beijing, China, July 2006 |
en |
dc.description.abstract |
First observation of the Stratospheric Sudden Warming (SSW) was made by Scherhag in 1952, using radiosonde measurements over Berlin. Schoeberl (1978) provided a review on theory and observations of stratospheric warming using results reported from different places. The results were suggested that the warming is confined to the Northern Hemisphere, especially during winter over the polar region. Similarly, there is also some evidence of SSW occurrence in Southern Hemisphere and reported in many research papers. The causes for such warmings were attributed mainly due to planetary wave and /or Gravity wave propagation. There are many results reported for high latitude and very rarely for mid and low latitudes |
en |
dc.language.iso |
en |
en |
dc.subject |
Stratospheric sudden warming |
en |
dc.subject |
Rayleigh lidar |
en |
dc.subject |
Radiosonde measurements |
en |
dc.subject |
SSW |
|
dc.title |
Rayleigh lidar investigation of sudden stratospheric warming observed over northern and southern hemisphere stations |
en |
dc.type |
Conference Presentation |
en |
dc.identifier.apacitation |
Sivakumar, V., Bencherif, H., Acharyulu, D., Hauchecorne, A., Rao, D., Sharma, S., & Rao, P. (2006). Rayleigh lidar investigation of sudden stratospheric warming observed over northern and southern hemisphere stations. http://hdl.handle.net/10204/2891 |
en_ZA |
dc.identifier.chicagocitation |
Sivakumar, V, H Bencherif, DV Acharyulu, A Hauchecorne, DN Rao, S Sharma, and PB Rao. "Rayleigh lidar investigation of sudden stratospheric warming observed over northern and southern hemisphere stations." (2006): http://hdl.handle.net/10204/2891 |
en_ZA |
dc.identifier.vancouvercitation |
Sivakumar V, Bencherif H, Acharyulu D, Hauchecorne A, Rao D, Sharma S, et al, Rayleigh lidar investigation of sudden stratospheric warming observed over northern and southern hemisphere stations; 2006. http://hdl.handle.net/10204/2891 . |
en_ZA |
dc.identifier.ris |
TY - Conference Presentation
AU - Sivakumar, V
AU - Bencherif, H
AU - Acharyulu, DV
AU - Hauchecorne, A
AU - Rao, DN
AU - Sharma, S
AU - Rao, PB
AB - First observation of the Stratospheric Sudden Warming (SSW) was made by Scherhag in 1952, using radiosonde measurements over Berlin. Schoeberl (1978) provided a review on theory and observations of stratospheric warming using results reported from different places. The results were suggested that the warming is confined to the Northern Hemisphere, especially during winter over the polar region. Similarly, there is also some evidence of SSW occurrence in Southern Hemisphere and reported in many research papers. The causes for such warmings were attributed mainly due to planetary wave and /or Gravity wave propagation. There are many results reported for high latitude and very rarely for mid and low latitudes
DA - 2006-07
DB - ResearchSpace
DP - CSIR
KW - Stratospheric sudden warming
KW - Rayleigh lidar
KW - Radiosonde measurements
KW - SSW
LK - https://researchspace.csir.co.za
PY - 2006
T1 - Rayleigh lidar investigation of sudden stratospheric warming observed over northern and southern hemisphere stations
TI - Rayleigh lidar investigation of sudden stratospheric warming observed over northern and southern hemisphere stations
UR - http://hdl.handle.net/10204/2891
ER -
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en_ZA |