Abstract

Abstract. The methodology of analysing the biomass burning events recorded in the database of the European Aerosol Research Lidar Network in the framework of the Aerosol, Clouds and Trace Gases Research Infrastructure is presented. The period of 2008–2017 was chosen to analyse all of the events stored in the database under the Forest Fire category for a total of 14 stations available. The data provided ranged from complete datasets (particle backscatter, extinction and linear depolarization ratio profiles) to single profiles (particle backscatter coefficient profile). Smoke layers geometry was evaluated and the mean optical properties within each layer were computed. The back-trajectory technique was used to double-check the source of all pollution layers. The biomass burning layers were identified by taking into account the presence of the fires along the back trajectory. The biomass burning events are analysed by the means of the intensive parameters. The analysis was structured in three directions: (I) common biomass burning source (fire) recorded by at least two stations, (II) long-range transport from North America, and (III) analysis over four geographical regions (south-eastern Europe, north-eastern Europe, central Europe, and south-western Europe). Based on back-trajectory calculations and fire locations, the lidar measurements can be labelled either as measurements of a “single fire” or “mixed fires” (case I), measurements of North American fires, or measurements of mixed North American and local fires (case II). The histogram of the fire locations reveals the smoke sources for each region. For each region, statistics on intensive parameters are performed. The source origin of the intensive parameters is categorized based on the continental origin of the air mass (European, African, Asian, North American, or a combination of them). The methodology presented here is meant to provide a perspective to explore a large number of lidar data and deliver novel approaches to analyse the intensive parameters based on the assigned biomass burning sources. A thorough consideration of all potential fire sources reveals that most of the time the lidar measurements characterize the smoke from a mixture of fires. A comprehensive discussion of all the results (based on the intensive parameters and the source locations) will be given in a companion paper submitted to the ACP EARLINET special issue.

Highlights

  • Biomass burning (BB) represents one of the major sources of atmospheric particles

  • Examples are given for the following research directions: (I) fire events as observed by two lidar systems, (II) long-range transport (LRT) from North America, and (III) study based on four geographical measurement regions including the histogram of the fire source locations for each region

  • The current study focuses on developing a methodology to analyse large amounts of biomass burning measurements by lidars

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Summary

Introduction

Biomass burning (BB) represents one of the major sources of atmospheric particles (aerosols). Fiebig et al, 2002; Lolli et al, 2019; Markowicz et al, 2016) Within these applications, the EARLINET (European Aerosol Research Lidar Network) can provide spatial and temporal coverage of the BB transport over Europe. The current study shows the research on biomass burning aerosol as measured by 14 stations in EARLINET over the period 2008–2017. Examples are given for the following research directions: (I) fire events (same source) as observed by two lidar systems, (II) long-range transport (LRT) from North America, and (III) study based on four geographical measurement regions including the histogram of the fire source locations for each region. For systems with depolarization capability, the retrieval of the particle linear depolarization ratio (PDR) is recorded in b-files except Warsaw, which records it in both b-files and e-files

EARLINET Forest Fire category
Overview of the metadata
Calculation of the aerosol layer boundaries
Calculation of the back trajectories
Layer identification based on back trajectories and fire emissions
Smoke event recorded on 13 July 2017
Geographical regions
Intensive parameters by geographical regions
Findings
Summary and conclusions
Full Text
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