scholarly journals Sodium fluorescence Doppler lidar to measure atmospheric temperature in the mesopause region

2011 ◽  
Vol 56 (4-5) ◽  
pp. 417-423 ◽  
Author(s):  
Xiong Hu ◽  
ZhaoAi Yan ◽  
ShangYong Guo ◽  
YongQiang Cheng ◽  
JianCun Gong
Author(s):  
Bhupal Shrestha ◽  
J. A. Brotzge ◽  
J. Wang ◽  
N. Bain ◽  
C. D. Thorncroft ◽  
...  

AbstractVertical profiles of atmospheric temperature, moisture, wind, and aerosols are essential information for weather monitoring and prediction. Their availability, however, is limited in space and time due to the significant resources required to observe them. To fill this gap, the New York State Mesonet (NYSM) Profiler Network has been deployed as a national testbed to facilitate the research, development and evaluation of ground-based profiling technologies and applications. The testbed comprises 17 profiler stations across the state, forming a long-term regional observational network. Each Profiler station is comprised of a ground-based Doppler lidar, a microwave radiometer (MWR) and an environmental Sky Imaging Radiometer (eSIR). Thermodynamic profiles (temperature and humidity) from the MWR; wind and aerosol profiles from the Doppler lidar; and solar radiance and optical depth parameters from the eSIR are collected, processed, disseminated, and archived every 10 minutes. This paper introduces the NYSM Profiler Network and reviews the network design and siting, instrumentation, network operations and maintenance, data and products, and some example applications highlighting the benefits of the network. Some sample applications include improved situational awareness and monitoring of the sea/land breeze, long-range wildfire smoke transport, air quality (PM2.5 and AOD) and boundary layer height. Ground-based profiling systems promise a path forward for filling a critical gap in the nation’s observing system with the potential to improve analysis and prediction for many weather-sensitive sectors, such as aviation, ground transportation, health, and wind energy.


2017 ◽  
Vol 46 (5) ◽  
pp. 506002
Author(s):  
王 博 Wang Bo ◽  
胡 雄 Hu Xiong ◽  
闫召爱 Yan Zhaoai ◽  
肖存英 Xiao Cunying ◽  
郭商勇 Guo Shangyong ◽  
...  

2020 ◽  
Vol 20 (1) ◽  
pp. 333-343
Author(s):  
Christoph Franzen ◽  
Patrick Joseph Espy ◽  
Robert Edward Hibbins

Abstract. Spectroscopy of the hydroxyl (OH) airglow has been a commonly used way to remotely sense temperatures in the mesopause region for many decades. This technique relies on the OH rotational state populations to be thermalized through collisions with the surrounding gas into a Boltzmann distribution characterized by the local temperature. However, deviations of the rotational populations from a Boltzmann distribution characterized by a single temperature have been observed and attributed to an incomplete thermalization of the OH from its initial, non-thermodynamic-equilibrium distribution. Here we address an additional cause for the apparent amount of excess population in the higher rotational levels of the OH airglow brought about by integrating these OH emissions through vertical gradients in the atmospheric temperature. We find that up to 40 % of the apparent excess population, currently attributed to incomplete thermalization, can be due to the vertical temperature gradients created by waves. Additionally, we find that the populations of the different upper vibrational levels are affected differently. These effects need to be taken into account in order to assess the true extent of non-thermodynamic-equilibrium effects on the OH rotational populations.


2019 ◽  
Author(s):  
Christoph Franzen ◽  
Patrick Joseph Espy ◽  
Robert Edward Hibbins

Abstract. Spectroscopy of the hydroxyl (OH) airglow has been a commonly used way to remotely sense temperatures in the mesopause region for many decades. This technique relies on the OH rotational state populations to be thermalised through collisions with the surrounding gas into a Boltzmann distribution characterised by the local temperature. However, deviations of the rotational populations from a Boltzmann distribution characterised by a single temperature have been observed and attributed to an incomplete thermalisation of the OH from its initial, non-thermodynamic equilibrium distribution. Here we address an additional cause for the apparent amount of excess population in the higher rotational levels of the OH airglow brought about by integrating these OH emissions through vertical gradients in the atmospheric temperature. We find that up to 40 % of the apparent excess population, currently attributed to incomplete thermalisation, can be due to the vertical temperature gradients created by waves. Additionally, we find that the populations of the different upper vibrational levels are affected differently. These effects need to be taken into account in order to assess the true extent of non-thermodynamic equilibrium effects on the OH rotational populations.


2015 ◽  
Vol 24 (9) ◽  
pp. 094212 ◽  
Author(s):  
Ming-Jia Shangguan ◽  
Hai-Yun Xia ◽  
Xian-Kang Dou ◽  
Chong Wang ◽  
Jia-Wei Qiu ◽  
...  

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