A summary of the linear trends estimated from the USU Rayleigh Lidar (41.74º N, 118ºW) temperature data set. The data set covers a time span from September, 1993 to August, 2003 and an altitude range of 45 to 80 km. The data set includes 584 data points at 45 km to 580 data points at 80 km. Cooling trend profiles are calculated and compared to results from other researchers. Collinearity and bias are also considered as issues that could affect the regression results. Also considered is the possibility that the Mt. Pinatubo eruption has influenced temperature trend estimates. This is important because the Pinatubo-related mesosphere temperature response occurred about the time the USU lidar came on line, which could be affecting our trend es...
Lidars have been used extensively to derive temperatures, but not absolute densities, in the mesosph...
The mesopause, a boundary between mesosphere and thermosphere with the coldest atmospheric temperatu...
From Aug. 1993 to Feb. 1996, regular Rayleigh-scatter observations of the stratosphere and mesospher...
The long-term midlatitude temperature trend between 85 and 105 km is deduced from 25 years (March 19...
Rayleigh lidar technology opened the middle atmosphere (from 30–90 km) to ground-based observations....
In June–July 2012, observations were carried out using the recently upgraded, large-aperture, Raylei...
International audienceThe long-term temperature profile data sets obtained by Rayleigh lidars at thr...
We present midlatitude solar response and linear trend from Colorado State University/Utah State Uni...
The Earth\u27s atmosphere is typically characterized by its temperature structure, which naturally d...
A Rayleigh-scatter lidar has been operated by the Center for Atmospheric and Space Sciences (CASS) a...
In June–July 2012, observations were carried out using the recently upgraded, large-aperture, Raylei...
As the impetus for extended observational measurements throughout the middle atmosphere has increase...
Temperature observations of the middle atmosphere have been carried out from September 1993 through ...
The Center for Atmospheric and Space Sciences (CASS) at Utah State University (USU) operates the ALO...
During 1990-2007, there were 894 lidar observations of nocturnal mesopause region temperatures over ...
Lidars have been used extensively to derive temperatures, but not absolute densities, in the mesosph...
The mesopause, a boundary between mesosphere and thermosphere with the coldest atmospheric temperatu...
From Aug. 1993 to Feb. 1996, regular Rayleigh-scatter observations of the stratosphere and mesospher...
The long-term midlatitude temperature trend between 85 and 105 km is deduced from 25 years (March 19...
Rayleigh lidar technology opened the middle atmosphere (from 30–90 km) to ground-based observations....
In June–July 2012, observations were carried out using the recently upgraded, large-aperture, Raylei...
International audienceThe long-term temperature profile data sets obtained by Rayleigh lidars at thr...
We present midlatitude solar response and linear trend from Colorado State University/Utah State Uni...
The Earth\u27s atmosphere is typically characterized by its temperature structure, which naturally d...
A Rayleigh-scatter lidar has been operated by the Center for Atmospheric and Space Sciences (CASS) a...
In June–July 2012, observations were carried out using the recently upgraded, large-aperture, Raylei...
As the impetus for extended observational measurements throughout the middle atmosphere has increase...
Temperature observations of the middle atmosphere have been carried out from September 1993 through ...
The Center for Atmospheric and Space Sciences (CASS) at Utah State University (USU) operates the ALO...
During 1990-2007, there were 894 lidar observations of nocturnal mesopause region temperatures over ...
Lidars have been used extensively to derive temperatures, but not absolute densities, in the mesosph...
The mesopause, a boundary between mesosphere and thermosphere with the coldest atmospheric temperatu...
From Aug. 1993 to Feb. 1996, regular Rayleigh-scatter observations of the stratosphere and mesospher...