Impact Factor 2.892 | CiteScore 2.74
More on impact ›

Original Research ARTICLE Provisionally accepted The full-text will be published soon. Notify me

Front. Earth Sci. | doi: 10.3389/feart.2019.00308

Mixing layer height retrievals from MiniMPL measurements in the Chiang Mai valley: implications for particulate matter pollution

 RAMAN SOLANKI1*, Ronald Macatangay1, 2, Vichawan Sakulsupich1, Thiranan Sonkaew3 and  Parth S. Mahapatra4
  • 1National Astronomical Research Institute of Thailand, Thailand
  • 2Institute of Environmental Science and Meteorology, College of Science, University of the Philippines Diliman, Philippines
  • 3Science Faculty, Lampang Rajabhat University, Thailand
  • 4International Centre for Integrated Mountain Development, Nepal

Urbanized mountain valleys are usually prone to episodes of high concentrations of air pollutants due to the strong interplay between mountain meteorology and synoptic weather conditions. The mountain valley of Chiang Mai is engulfed by air pollutants with particulate matter (PM) concentration remaining above 50 µg m-3 (PM2.5, 24-hour average) during approximately 13 % days every year (mostly during February to April). This study presents the first time continuous measurements of mini- micro pulse LiDAR (MiniMPL) installed on the valley floor of Chiang Mai, providing vertical backscatter profile of aerosols and clouds from April 2017 onwards. This paper analyzes unique dataset of mixing layer (ML) height measurements made during April 2017 to June 2018 with a temporal resolution of 15 minutes. The ML height derived from the backscatter profile measurements are analyzed to understand the annual, monthly and diurnal variations. The ML height depicts distinct diurnal variations for all months of the year, evolving up to < 3.0 km during April to September. From October onwards the ML evolution is gradually inhibited, reducing to < 2.0 km during October to December and < 1.5 km during January to March. The variations in the concentration of PM were found to be partly modulated by the ML variations (Pearson coefficient ≈ −0.50) during dry season (February, March and April), possibly triggering the aerosol-boundary layer feedback mechanism for high concentrations (100 µg m-3) of PM and low ventilation in the valley. The inhibition of ML evolution due to feedback mechanism further escalates the high concentrations of PM, resulting in severe haze conditions on many days during the dry season.

Keywords: Aerosols, MiniMPL, Mixing layer height, aerosol layer height, Particulate Matter, Mountain valley

Received: 27 Aug 2019; Accepted: 05 Nov 2019.

Copyright: © 2019 SOLANKI, Macatangay, Sakulsupich, Sonkaew and Mahapatra. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

* Correspondence: Dr. RAMAN SOLANKI, National Astronomical Research Institute of Thailand, Chiang Mai, Thailand, raman@narit.or.th