dc.contributor.author |
Kalapureddy, MCR
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dc.contributor.author |
Kumar, KK
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dc.contributor.author |
Sivakumar, V
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dc.contributor.author |
Ghosh, AK
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dc.contributor.author |
Jain, AR
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dc.contributor.author |
Reddy, KK
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dc.date.accessioned |
2007-06-29T07:56:48Z |
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dc.date.available |
2007-06-29T07:56:48Z |
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dc.date.issued |
2007-04 |
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dc.identifier.citation |
Kalapureddy, MCR et al. 2007. Diurnal and seasonal variability of TKE dissipation rate in the ABL over a tropical station using UHF wind profiler. Journal of Atmospheric and Solar-Terrestrial Physics, Vol. 69 pp 419-430 |
en |
dc.identifier.issn |
1364-6826 |
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dc.identifier.uri |
http://hdl.handle.net/10204/757
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dc.description |
http://www.sciencedirect.com/science/journal/13646826 |
en |
dc.description.abstract |
This paper presents the diurnal and seasonal variation of Turbulence Kinetic Energy (TKE) dissipation rate (ε) in the Atmospheric Boundary-Layer (ABL) over a tropical station, Gadanki (13.5° N, 79.2° E) in India. Doppler spectral width measurements made by Lower Atmospheric Wind Profiler (LAWP) operating at 1357 MHz are utilized to estimate ε in the height region of 0.5–4.0 km on clear air days. Various non-turbulent spectral broadenings are calculated and separated out from the observed spectral width before estimating ε. It is found that in the lower tropospheric height region ε is in the range from 10−5.0 to 10−1.0 m2 s−3. ε showed significant diurnal variation in the boundary-layer. The larger values of ε, 10–2.7 m2 s−3, are noted to be associated with the Convective Boundary-Layer (CBL). The parameter ε is also showing significant seasonal variation. In summer and monsoon seasons the boundary-layer depths are observed up to a height of 4.0 km while the same are confined to below 2.0 km in post-monsoon and winter seasons. |
en |
dc.language.iso |
en |
en |
dc.publisher |
Pergamon-Elsevier Science Ltd |
en |
dc.subject |
ABL |
en |
dc.subject |
Atmospheric boundary-layer |
en |
dc.subject |
Turbulence energy dissipation rate |
en |
dc.subject |
Radar doppler spectral width |
en |
dc.subject |
UHF wind profiler |
en |
dc.title |
Diurnal and seasonal variability of TKE dissipation rate in the ABL over a tropical station using UHF wind profiler |
en |
dc.type |
Article |
en |
dc.identifier.apacitation |
Kalapureddy, M., Kumar, K., Sivakumar, V., Ghosh, A., Jain, A., & Reddy, K. (2007). Diurnal and seasonal variability of TKE dissipation rate in the ABL over a tropical station using UHF wind profiler. http://hdl.handle.net/10204/757 |
en_ZA |
dc.identifier.chicagocitation |
Kalapureddy, MCR, KK Kumar, V Sivakumar, AK Ghosh, AR Jain, and KK Reddy "Diurnal and seasonal variability of TKE dissipation rate in the ABL over a tropical station using UHF wind profiler." (2007) http://hdl.handle.net/10204/757 |
en_ZA |
dc.identifier.vancouvercitation |
Kalapureddy M, Kumar K, Sivakumar V, Ghosh A, Jain A, Reddy K. Diurnal and seasonal variability of TKE dissipation rate in the ABL over a tropical station using UHF wind profiler. 2007; http://hdl.handle.net/10204/757. |
en_ZA |
dc.identifier.ris |
TY - Article
AU - Kalapureddy, MCR
AU - Kumar, KK
AU - Sivakumar, V
AU - Ghosh, AK
AU - Jain, AR
AU - Reddy, KK
AB - This paper presents the diurnal and seasonal variation of Turbulence Kinetic Energy (TKE) dissipation rate (ε) in the Atmospheric Boundary-Layer (ABL) over a tropical station, Gadanki (13.5° N, 79.2° E) in India. Doppler spectral width measurements made by Lower Atmospheric Wind Profiler (LAWP) operating at 1357 MHz are utilized to estimate ε in the height region of 0.5–4.0 km on clear air days. Various non-turbulent spectral broadenings are calculated and separated out from the observed spectral width before estimating ε. It is found that in the lower tropospheric height region ε is in the range from 10−5.0 to 10−1.0 m2 s−3. ε showed significant diurnal variation in the boundary-layer. The larger values of ε, 10–2.7 m2 s−3, are noted to be associated with the Convective Boundary-Layer (CBL). The parameter ε is also showing significant seasonal variation. In summer and monsoon seasons the boundary-layer depths are observed up to a height of 4.0 km while the same are confined to below 2.0 km in post-monsoon and winter seasons.
DA - 2007-04
DB - ResearchSpace
DP - CSIR
KW - ABL
KW - Atmospheric boundary-layer
KW - Turbulence energy dissipation rate
KW - Radar doppler spectral width
KW - UHF wind profiler
LK - https://researchspace.csir.co.za
PY - 2007
SM - 1364-6826
T1 - Diurnal and seasonal variability of TKE dissipation rate in the ABL over a tropical station using UHF wind profiler
TI - Diurnal and seasonal variability of TKE dissipation rate in the ABL over a tropical station using UHF wind profiler
UR - http://hdl.handle.net/10204/757
ER -
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en_ZA |