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		<id>http://atmoschem.org.cn/index.php?action=history&amp;feed=atom&amp;title=Papers%3AFu_et_al_2008</id>
		<title>Papers:Fu et al 2008 - Revision history</title>
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		<updated>2026-05-13T18:48:13Z</updated>
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	<entry>
		<id>http://atmoschem.org.cn/index.php?title=Papers:Fu_et_al_2008&amp;diff=2700&amp;oldid=prev</id>
		<title>Atomoschem at 06:57, 8 October 2023</title>
		<link rel="alternate" type="text/html" href="http://atmoschem.org.cn/index.php?title=Papers:Fu_et_al_2008&amp;diff=2700&amp;oldid=prev"/>
				<updated>2023-10-08T06:57:35Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class='diff diff-contentalign-left'&gt;
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				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 06:57, 8 October 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 24:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 24:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Publication |''' '''Fu, T.-M.*''', D. J. Jacob, F. Wittrock, J. P. Burrows, M. Vrekoussis, and D. K. Henze (2008), Global budgets of atmospheric glyoxal and methylglyoxal, and implications for formation of secondary organic aerosols, ''J. Geophys. Res.'', 113, D15303, doi:10.1026/2007JD009505. [http://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;162&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;105&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;245.3/~tmfu/web&lt;/del&gt;/papers/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Fu_et_al_2008&lt;/del&gt;.pdf PDF]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Publication |''' '''Fu, T.-M.*''', D. J. Jacob, F. Wittrock, J. P. Burrows, M. Vrekoussis, and D. K. Henze (2008), Global budgets of atmospheric glyoxal and methylglyoxal, and implications for formation of secondary organic aerosols, ''J. Geophys. Res.'', 113, D15303, doi:10.1026/2007JD009505. [http://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;atmoschem&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;org&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cn&lt;/ins&gt;/papers/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Fu_et_al_2008_Journal_of_Geophysical_Research&lt;/ins&gt;.pdf PDF]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Atomoschem</name></author>	</entry>

	<entry>
		<id>http://atmoschem.org.cn/index.php?title=Papers:Fu_et_al_2008&amp;diff=372&amp;oldid=prev</id>
		<title>Atmoschem: Created page with &quot;'''Abstract |''' We construct global budgets of atmospheric glyoxal and methylglyoxal with the goal of quantifying their potential for global secondary organic aerosol (SOA) f...&quot;</title>
		<link rel="alternate" type="text/html" href="http://atmoschem.org.cn/index.php?title=Papers:Fu_et_al_2008&amp;diff=372&amp;oldid=prev"/>
				<updated>2014-05-06T01:19:38Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot;&amp;#039;&amp;#039;&amp;#039;Abstract |&amp;#039;&amp;#039;&amp;#039; We construct global budgets of atmospheric glyoxal and methylglyoxal with the goal of quantifying their potential for global secondary organic aerosol (SOA) f...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;'''Abstract |''' We construct global budgets of atmospheric glyoxal and methylglyoxal with the goal&lt;br /&gt;
of quantifying their potential for global secondary organic aerosol (SOA) formation via&lt;br /&gt;
irreversible uptake by aqueous aerosols and clouds. We conduct a detailed simulation of&lt;br /&gt;
glyoxal and methylglyoxal in the GEOS-Chem global 3-D chemical transport model&lt;br /&gt;
including our best knowledge of source and sink processes. Our resulting best estimates of&lt;br /&gt;
the global sources of glyoxal and methylglyoxal are 45 Tg/a and 140 Tg/a,&lt;br /&gt;
respectively. Oxidation of biogenic isoprene contributes globally 47% of glyoxal and 79%&lt;br /&gt;
of methylglyoxal. The second most important precursors are acetylene (mostly&lt;br /&gt;
anthropogenic) for glyoxal and acetone (mostly biogenic) for methylglyoxal. Both&lt;br /&gt;
acetylene and acetone have long lifetimes and provide a source of dicarbonyls in the free&lt;br /&gt;
troposphere. Atmospheric lifetimes of glyoxal and methylglyoxal in the model are 2.9 h&lt;br /&gt;
and 1.6 h, respectively, mostly determined by photolysis. Simulated dicarbonyl&lt;br /&gt;
concentrations in continental surface air at northern midlatitudes are in the range&lt;br /&gt;
10–100 ppt, consistent with in situ measurements. On a global scale, the highest&lt;br /&gt;
concentrations are over biomass burning regions, in agreement with glyoxal column&lt;br /&gt;
observations from the SCIAMACHY satellite instrument. SCIAMACHY and a few&lt;br /&gt;
ship cruises also suggest a large marine source of dicarbonyls missing from our&lt;br /&gt;
model. The global source of SOA from the irreversible uptake of dicarbonyls in&lt;br /&gt;
GEOS-Chem is 11 Tg C/a, including 2.6 Tg C/a from glyoxal and 8 Tg C/a&lt;br /&gt;
from methylglyoxal; 90% of this source takes place in clouds. The magnitude of the&lt;br /&gt;
global SOA source from dicarbonyls is comparable to that computed in GEOS-Chem&lt;br /&gt;
from the standard mechanism involving reversible partitioning of semivolatile&lt;br /&gt;
products from the oxidation of monoterpenes, sesquiterpenes, isoprene, and aromatics.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
'''Publication |''' '''Fu, T.-M.*''', D. J. Jacob, F. Wittrock, J. P. Burrows, M. Vrekoussis, and D. K. Henze (2008), Global budgets of atmospheric glyoxal and methylglyoxal, and implications for formation of secondary organic aerosols, ''J. Geophys. Res.'', 113, D15303, doi:10.1026/2007JD009505. [http://162.105.245.3/~tmfu/web/papers/Fu_et_al_2008.pdf PDF]&lt;/div&gt;</summary>
		<author><name>Atmoschem</name></author>	</entry>

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