4.3 Article

Planetary boundary layer height retrieval from a diode-laser-based high spectral resolution lidar

期刊

JOURNAL OF APPLIED REMOTE SENSING
卷 16, 期 2, 页码 -

出版社

SPIE-SOC PHOTO-OPTICAL INSTRUMENTATION ENGINEERS
DOI: 10.1117/1.JRS.16.024507

关键词

planetary boundary layer; atmospheric boundary layer; lidar; high spectral resolution lidar; remote sensing; atmospheric sensing

资金

  1. National Science Foundation [1917851]
  2. Div Atmospheric & Geospace Sciences
  3. Directorate For Geosciences [1917851] Funding Source: National Science Foundation

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The planetary boundary layer height (PBLH) is an important parameter for weather forecasting and climate modeling. This study presents a retrieval algorithm based on Haar wavelet transform (HWT) to determine the PBLH using lidar measurements of aerosol layers. The retrieved PBLH is compared with the PBLH determined from radiosonde measurements, showing good agreement between the two methods.
The planetary boundary layer height (PBLH) is an essential parameter for weather forecasting and climate modeling. The primary methods for obtaining the PBLH include radiosonde measurements of atmospheric parameters and lidar measurements, which track aerosol layers in the lower atmosphere. Radiosondes provide the parameters to determine the PBLH but cannot monitor changes over a diurnal cycle. Lidar instruments can track the temporal variability of the PBLH and account for spatial variability when operated in a network configuration. The networkable micropulse DIAL (MPD) instruments for thermodynamic profiling are based on diode-laser technology that is eye-safe and cost-effective and has demonstrated long-term autonomous operation. We present a retrieval algorithm for determining the PBLH from the quantitative aerosol profiling capability of the high spectral resolution channel of the MPD. The PBLH is determined using a Haar wavelet transform (HWT) method that tracks aerosol layers in the lower atmosphere. The PBLH from the lidar is compared with the PBLH determined from potential temperature profiles from radiosondes. In many cases, good agreement among the PBLH retrievals was seen. However, the radiosonde retrieval often missed the lowest inversion layer when several layers were present, while the HWT could track the lowest layer. (c) The Authors. Published by SPIE under a Creative Commons Attribution 4.0 International License. Distribution or reproduction of this work in whole or in part requires full attribution of the original publication, including its DOI.

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