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Open AccessJournal ArticleDOI

A mobile differential absorption lidar for simultaneous observations of tropospheric and stratospheric ozone over Tibet.

TLDR
A mobile ozone differential absorption lidar system to simultaneously measure the vertical profiles of tropospheric and stratospheric ozone from an altitude of ~5 to 50 km and results agree very well with those observed by the Aura/MLS satellite.
Abstract
We developed a mobile ozone differential absorption lidar system to simultaneously measure the vertical profiles of tropospheric and stratospheric ozone from an altitude of ~5 to 50 km. The system emits four laser beams at wavelength of 289 nm, 299 nm, 308 nm and 355 nm and receives their corresponding Mie/Rayleigh backscattering return signals, and two N2 Raman return signals at 332 nm and 387 nm shifted from 308 nm and 355 nm, respectively. An assembled telescope array with four 1.25-m telescopes (effective diameter > 2 m) collects the Rayleigh and Raman backscattering signals at 308/332 and 355/387 nm. This system is currently deployed at the Yangbajing Observatory in Tibet (~4300 m elevation) and has begun observations in regular campaign mode since October 2017. The lidar results agree very well with those observed by the Aura/MLS satellite. This novel ozone lidar system operates at the highest elevation of any such system in the world. The higher elevation and larger receiver aperture of this system yield a higher signal-to-noise ratio and lower statistical uncertainty.

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Citations
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Ground-based laser DIAL system for long-term measurements of stratospheric ozone. [differential absorption lidar system

TL;DR: A ground-based differential absorption lidar system has been implemented to make long-term, precise measurements of stratospheric ozone concentration profiles from ~20 to 50 km altitude.
Journal ArticleDOI

Measurements of Ozone Vertical Profiles in the Upper Troposphere–Stratosphere over Western Siberia by DIAL, MLS, and IASI

TL;DR: In this article, the authors measured the ozone vertical distribution (OVD) in the upper troposphere-stratosphere by differential absorption lidar (DIAL) at 299/341 nm and 308/353 nm and compared and analyzed the results against satellite data.
Journal ArticleDOI

Comparison of ozone vertical profiles in the upper troposphere–stratosphere measured over Tomsk, Russia (56.5° N, 85.0° E) with DIAL, MLS, and IASI

TL;DR: In this article, a laser ranging method employing light detection and ranging (LiDAR) technology is used for studying the atmosphere and monitoring its state and the purpose of this work is to measure the ozone.
Journal ArticleDOI

Rayleigh and sodium lidar system incorporating time-division and wavelength-division multiplexing

TL;DR: In this article, a Rayleigh and sodium lidar system was recently upgraded at the University of Science and Technology of China (USTC) in Hefei, China (31.5 ∘ N, 117 ∘ E).
Journal ArticleDOI

Temperature Correction of the Vertical Ozone Distribution Retrieval at the Siberian Lidar Station Using the MetOp and Aura Data

TL;DR: In this paper, the authors analyzed the influence of temperature correction on ozone vertical distribution (OVD) in the upper troposphere-stratosphere in the altitude range of 5-45 km using differential absorption lidar (DIAL), operating at the sensing wavelengths 299/341 nm and 308/353 nm.
References
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TL;DR: The Ozone Monitoring Instrument is a ultraviolet/visible nadir solar backscatter spectrometer, which provides nearly global coverage in one day with a spatial resolution of 13 km/spl times/24 km and will enable detection of air pollution on urban scale resolution.
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High spectral resolution ozone absorption cross-sections - Part 2: Temperature dependence

TL;DR: In this paper, the temperature dependence of ozone absorption cross-sections measured in a laboratory in the broad spectral range 213-1100 nm with a spectral resolution of 0.02-0.24 nm (full width at half maximum, FWHM) in the atmosphereherically relevant temperature range from 193 K to 293 K.
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