Determination of the emission rates of CO<sub>2</sub> point sources with airborne lidar

<p>Anthropogenic point sources, such as coal-fired power plants, produce a major share of global <span class="inline-formula">CO<sub>2</sub></span> emissions. International climate agreements demand their independent monitoring. Due to the large number of poin...

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Main Authors: S. Wolff, G. Ehret, C. Kiemle, A. Amediek, M. Quatrevalet, M. Wirth, A. Fix
Format: Article
Language:English
Published: Copernicus Publications 2021-04-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/14/2717/2021/amt-14-2717-2021.pdf
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spelling doaj-815a6ac8d5d64c0e8f83c4ebd88480e82021-04-08T09:46:08ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482021-04-01142717273610.5194/amt-14-2717-2021Determination of the emission rates of CO<sub>2</sub> point sources with airborne lidarS. Wolff0G. Ehret1C. Kiemle2A. Amediek3M. Quatrevalet4M. Wirth5A. Fix6Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, GermanyDeutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, GermanyDeutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, GermanyDeutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, GermanyDeutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, GermanyDeutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, GermanyDeutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany<p>Anthropogenic point sources, such as coal-fired power plants, produce a major share of global <span class="inline-formula">CO<sub>2</sub></span> emissions. International climate agreements demand their independent monitoring. Due to the large number of point sources and their global spatial distribution, the implementation of a satellite-based observation system is convenient. Airborne active remote sensing measurements demonstrate that the deployment of lidar is promising in this respect. The integrated path differential absorption lidar CHARM-F is installed on board an aircraft in order to detect weighted column-integrated dry-air mixing ratios of <span class="inline-formula">CO<sub>2</sub></span> below the aircraft along its flight track. During the Carbon Dioxide and Methane Mission (CoMet) in spring 2018, airborne greenhouse gas measurements were performed, focusing on the major European sources of anthropogenic <span class="inline-formula">CO<sub>2</sub></span> emissions, i.e., large coal-fired power plants. The flights were designed to transect isolated exhaust plumes. From the resulting enhancement in the <span class="inline-formula">CO<sub>2</sub></span> mixing ratios, emission rates can be derived via the cross-sectional flux method. On average, our results roughly correspond to reported annual emission rates, with wind speed uncertainties being the major source of error. We observe significant variations between individual overflights, ranging up to a factor of 2. We hypothesize that these variations are mostly driven by turbulence. This is confirmed by a high-resolution large eddy simulation that enables us to give a qualitative assessment of the influence of plume inhomogeneity on the cross-sectional flux method. Our findings suggest avoiding periods of strong turbulence, e.g., midday and afternoon. More favorable measurement conditions prevail during nighttime and morning. Since lidars are intrinsically independent of sunlight, they have a significant advantage in this regard.</p>https://amt.copernicus.org/articles/14/2717/2021/amt-14-2717-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Wolff
G. Ehret
C. Kiemle
A. Amediek
M. Quatrevalet
M. Wirth
A. Fix
spellingShingle S. Wolff
G. Ehret
C. Kiemle
A. Amediek
M. Quatrevalet
M. Wirth
A. Fix
Determination of the emission rates of CO<sub>2</sub> point sources with airborne lidar
Atmospheric Measurement Techniques
author_facet S. Wolff
G. Ehret
C. Kiemle
A. Amediek
M. Quatrevalet
M. Wirth
A. Fix
author_sort S. Wolff
title Determination of the emission rates of CO<sub>2</sub> point sources with airborne lidar
title_short Determination of the emission rates of CO<sub>2</sub> point sources with airborne lidar
title_full Determination of the emission rates of CO<sub>2</sub> point sources with airborne lidar
title_fullStr Determination of the emission rates of CO<sub>2</sub> point sources with airborne lidar
title_full_unstemmed Determination of the emission rates of CO<sub>2</sub> point sources with airborne lidar
title_sort determination of the emission rates of co<sub>2</sub> point sources with airborne lidar
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2021-04-01
description <p>Anthropogenic point sources, such as coal-fired power plants, produce a major share of global <span class="inline-formula">CO<sub>2</sub></span> emissions. International climate agreements demand their independent monitoring. Due to the large number of point sources and their global spatial distribution, the implementation of a satellite-based observation system is convenient. Airborne active remote sensing measurements demonstrate that the deployment of lidar is promising in this respect. The integrated path differential absorption lidar CHARM-F is installed on board an aircraft in order to detect weighted column-integrated dry-air mixing ratios of <span class="inline-formula">CO<sub>2</sub></span> below the aircraft along its flight track. During the Carbon Dioxide and Methane Mission (CoMet) in spring 2018, airborne greenhouse gas measurements were performed, focusing on the major European sources of anthropogenic <span class="inline-formula">CO<sub>2</sub></span> emissions, i.e., large coal-fired power plants. The flights were designed to transect isolated exhaust plumes. From the resulting enhancement in the <span class="inline-formula">CO<sub>2</sub></span> mixing ratios, emission rates can be derived via the cross-sectional flux method. On average, our results roughly correspond to reported annual emission rates, with wind speed uncertainties being the major source of error. We observe significant variations between individual overflights, ranging up to a factor of 2. We hypothesize that these variations are mostly driven by turbulence. This is confirmed by a high-resolution large eddy simulation that enables us to give a qualitative assessment of the influence of plume inhomogeneity on the cross-sectional flux method. Our findings suggest avoiding periods of strong turbulence, e.g., midday and afternoon. More favorable measurement conditions prevail during nighttime and morning. Since lidars are intrinsically independent of sunlight, they have a significant advantage in this regard.</p>
url https://amt.copernicus.org/articles/14/2717/2021/amt-14-2717-2021.pdf
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