scholarly journals Mean thermal structure of the low-latitude middle atmosphere studied using Gadanki Rayleigh lidar, Rocket, and SABER/TIMED observations

2008 ◽  
Vol 113 (D23) ◽  
Author(s):  
G. Kishore Kumar ◽  
M. Venkat Ratnam ◽  
A. K. Patra ◽  
S. Vijaya Bhaskara Rao ◽  
James Russell
2011 ◽  
Vol 29 (4) ◽  
pp. 649-662 ◽  
Author(s):  
V. Sivakumar ◽  
P. Vishnu Prasanth ◽  
P. Kishore ◽  
H. Bencherif ◽  
P. Keckhut

Abstract. For the first time, climatology of the middle atmosphere thermal structure is presented, based on 14 years of LIDAR and satellite (HALOE, SABER, CHAMP and COSMIC) temperature measurements. The data is collected over a southern sub-tropical site, Reunion Island (20.8° S; 55.5° E), for the height range between 30 and 60 km. The overall monthly mean temperature shows a maximum of 265–270 K at the stratopause height region from ~44–52 km and peaks during the months of March and November. Furthermore, the temperature profiles are compared with different satellite datasets (HALOE, CHAMP, COSMIC and SABER) and the results are found to be in reasonable agreement with each other, although a relative difference in temperature of ± 5 to 6 K is noticed. In comparison, LIDAR shows higher/lower temperatures for the lower mesosphere/upper stratosphere height region. The differences in temperature measured by the LIDAR and satellite measurements are analogous with previous results available elsewhere. Long-term temperature measurements are used to further study seasonal oscillations, especially annual, semi-annual and quasi-biennial oscillations. In comparison with SAO, the measured spectral amplitudes of AO shows dominant amplitudes in both the upper stratosphere and lower mesosphere height regions. Using LIDAR and the other satellite measurements, the quasi-biennial oscillation was found to be approximately 26 months. The spectral amplitudes are comparable to the results reported earlier by other researchers.


2012 ◽  
Vol 108 (1/2) ◽  
Author(s):  
Nkanyiso Mbatha ◽  
Venkataraman Sivakumar ◽  
Hassan Bencherif ◽  
Sandile B. Malinga ◽  
Sadhasivan R. Pillay ◽  
...  

1991 ◽  
Vol 96 (D3) ◽  
pp. 5169 ◽  
Author(s):  
R. Wilson ◽  
M. L. Chanin ◽  
A. Hauchecorne

2011 ◽  
Vol 29 (9) ◽  
pp. 1647-1654 ◽  
Author(s):  
S. K. Das ◽  
A. Taori ◽  
A. Jayaraman

Abstract. Lower atmospheric perturbations often produce measurable effects in the middle and upper atmosphere. The present study demonstrates the response of the middle atmospheric thermal structure to the significant enhancement of the lower atmospheric heating effect caused by dust storms observed over the Thar Desert, India. Our study from multi-satellite observations of two dust storm events that occurred on 3 and 8 May 2007 suggests that dust storm events produce substantial changes in the lower atmospheric temperatures as hot spots which can become sources for gravity waves observed in the middle atmosphere.


Author(s):  
Alain Hauchecorne ◽  
Sergey Khaykin ◽  
Philippe Keckhut ◽  
Nahoudha Mzé ◽  
Guillaume Angot ◽  
...  

2012 ◽  
Vol 63-64 ◽  
pp. 36-48 ◽  
Author(s):  
Som Sharma ◽  
S. Sridharan ◽  
H. Chandra ◽  
S. Lal ◽  
Y.B. Acharya

1999 ◽  
Vol 51 (7-8) ◽  
pp. 825-832 ◽  
Author(s):  
S. P. Namboothiri ◽  
N. Sugimoto ◽  
H. Nakane ◽  
I. Matsui ◽  
Y. Murayama

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