elib
DLR-Header
DLR-Logo -> http://www.dlr.de
DLR Portal Home | Imprint | Privacy Policy | Contact | Deutsch
Fontsize: [-] Text [+]

Insights into the role of soot aerosols in cirrus cloud formation

Kärcher, Bernd and Möhler, Ottmar and DeMott, Paul J. and Pechtl, Susanne and Yu, Fangqun (2007) Insights into the role of soot aerosols in cirrus cloud formation. Atmospheric Chemistry and Physics, 7, pp. 4203-4227. Copernicus Publications.

[img]
Preview
PDF
680kB

Official URL: http://www.atmos-chem-phys.net/7/4203/2007/acp-7-4203-2007.pdf

Abstract

Cirrus cloud formation is believed to be domi-nated by homogeneous freezing of supercooled liquid aerosols in many instances. Heterogeneous ice nuclei such as mineral dust, metallic, and soot particles, and some crystalline solids within partially soluble aerosols are suspected to modulate cirrus properties. Among those, the role of ubiqui-tous soot particles is perhaps the least understood. Because aviation is a major source of upper tropospheric soot particles, we put emphasis on ice formation in dispersing aircraft plumes. The effect of aircraft soot on cirrus formation in the absence of contrails is highly complex and depends on a wide array of emission and environmental parameters. We use a microphysical-chemical model predicting the formation of internally mixed, soot-containing particles up to two days after emission, and suggest two principal scenarios: high concentrations of original soot emissions could slightly increase the number of ice crystals; low concentrations of particles originating from coagulation of emitted soot with background aerosols could lead to a significant reduction in ice crystal number. Both scenarios assume soot particles to be moderate ice nuclei relative to cirrus formation by homogeneous freezing in the presence of few efficient dust ice nuclei. A critical discussion of laboratory experiments reveals that the ice nucleation efficiency of soot particles depends strongly on their source, and, by inference, on atmospheric aging processes. Mass and chemistry of soluble surface coatings appear to be crucial factors. Immersed soot particles tend to be poor ice nuclei, some bare ones nucleate ice at low supersaturations. However, a fundamental understanding of these studies is lacking, rendering extrapolations to atmospheric conditions speculative. In particular, we cannot yet decide which indirect aircraft effect scenario is more plausible, and options suggested to mitigate the problem remain uncertain.

Item URL in elib:https://elib.dlr.de/50943/
Document Type:Article
Title:Insights into the role of soot aerosols in cirrus cloud formation
Authors:
AuthorsInstitution or Email of AuthorsAuthors ORCID iD
Kärcher, BerndUNSPECIFIEDUNSPECIFIED
Möhler, OttmarIMK-AAF, FZ KarlsruheUNSPECIFIED
DeMott, Paul J.Colorado State University, CO, USAUNSPECIFIED
Pechtl, SusanneUniv. Heidelberg, HeidelbergUNSPECIFIED
Yu, FangqunSUNY at Albany, NY, USAUNSPECIFIED
Date:17 August 2007
Journal or Publication Title:Atmospheric Chemistry and Physics
Refereed publication:Yes
Open Access:Yes
Gold Open Access:Yes
In SCOPUS:Yes
In ISI Web of Science:Yes
Volume:7
Page Range:pp. 4203-4227
Publisher:Copernicus Publications
Status:Published
Keywords:soot, cirrus, aviation
HGF - Research field:Aeronautics, Space and Transport
HGF - Program:Aeronautics
HGF - Program Themes:L VU - Air Traffic and Environment (old)
DLR - Research area:Aeronautics
DLR - Program:L VU - Air Traffic and Environment
DLR - Research theme (Project):L - Low-Emission Air Traffic (old)
Location: Oberpfaffenhofen
Institutes and Institutions:Institute of Atmospheric Physics > Atmospheric Trace Species
Deposited By: Kärcher, Prof. Bernd
Deposited On:22 Aug 2007
Last Modified:02 May 2019 14:03

Repository Staff Only: item control page

Browse
Search
Help & Contact
Information
electronic library is running on EPrints 3.3.12
Copyright © 2008-2017 German Aerospace Center (DLR). All rights reserved.