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000020012 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000020012 1001_ $$0P:(DE-Juel1)6775$$aLi, X.$$b0$$uFZJ
000020012 245__ $$aExploring the atmospheric chemistry of nitrous acid (HONO) at a rural site in Southern China
000020012 260__ $$aKatlenburg-Lindau$$bEGU$$c2012
000020012 300__ $$a1497 - 1513
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000020012 440_0 $$09601$$aAtmospheric Chemistry and Physics$$v12$$x1680-7316$$y10
000020012 500__ $$3POF3_Assignment on 2016-02-29
000020012 500__ $$aThis work was supported by the China National Basic Research and Development Program 2002CB410801, and the National High Technology Research and Development Program of China (863 Program) 2006AA06A301.
000020012 520__ $$aWe performed measurements of nitrous acid (HONO) during the PRIDE-PRD2006 campaign in the Pearl River Delta region 60 km north of Guangzhou, China, for 4 weeks in June 2006. HONO was measured by a LOPAP in-situ instrument which was setup in one of the campaign supersites along with a variety of instruments measuring hydroxyl radicals, trace gases, aerosols, and meteorological parameters. Maximum diurnal HONO mixing ratios of 1-5 ppb were observed during the nights. We found that the nighttime build-up of HONO can be attributed to the heterogeneous NO2 to HONO conversion on ground surfaces and the OH + NO reaction. In addition to elevated nighttime mixing ratios, measured noontime values of approximate to 200 ppt indicate the existence of a daytime source higher than the OH + NO -> HONO reaction. Using the simultaneously recorded OH, NO, and HONO photolysis frequency, a daytime additional source strength of HONO (P-M) was calculated to be 0.77 ppb h(-1) on average. This value compares well to previous measurements in other environments. Our analysis of P-M provides evidence that the photolysis of HNO3 adsorbed on ground surfaces contributes to the HONO formation.
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000020012 7001_ $$0P:(DE-Juel1)16306$$aBrauers, T.$$b1$$uFZJ
000020012 7001_ $$0P:(DE-Juel1)5628$$aHäseler, R.$$b2$$uFZJ
000020012 7001_ $$0P:(DE-Juel1)2693$$aBohn, B.$$b3$$uFZJ
000020012 7001_ $$0P:(DE-Juel1)7363$$aFuchs, H.$$b4$$uFZJ
000020012 7001_ $$0P:(DE-Juel1)16326$$aHofzumahaus, A.$$b5$$uFZJ
000020012 7001_ $$0P:(DE-Juel1)16342$$aHolland, F.$$b6$$uFZJ
000020012 7001_ $$0P:(DE-Juel1)VDB46831$$aLou, S.$$b7$$uFZJ
000020012 7001_ $$0P:(DE-Juel1)6776$$aLu, K.D.$$b8$$uFZJ
000020012 7001_ $$0P:(DE-Juel1)16347$$aRohrer, F.$$b9$$uFZJ
000020012 7001_ $$0P:(DE-HGF)0$$aHu, M.$$b10
000020012 7001_ $$0P:(DE-HGF)0$$aZeng, L.M.$$b11
000020012 7001_ $$0P:(DE-HGF)0$$aZhang, Y.H.$$b12
000020012 7001_ $$0P:(DE-HGF)0$$aGarland, R.M.$$b13
000020012 7001_ $$0P:(DE-HGF)0$$aSu, H.$$b14
000020012 7001_ $$0P:(DE-HGF)0$$aNowak, A.$$b15
000020012 7001_ $$0P:(DE-HGF)0$$aWiedensohler, A.$$b16
000020012 7001_ $$0P:(DE-HGF)0$$aTakegawa, N.$$b17
000020012 7001_ $$0P:(DE-HGF)0$$aShao, M.$$b18
000020012 7001_ $$0P:(DE-Juel1)16324$$aWahner, A.$$b19$$uFZJ
000020012 773__ $$0PERI:(DE-600)2069847-1$$a10.5194/acp-12-1497-2012$$gVol. 12, p. 1497 - 1513$$p1497 - 1513$$q12<1497 - 1513$$tAtmospheric chemistry and physics$$v12$$x1680-7316$$y2012
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