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000866944 1001_ $$0P:(DE-HGF)0$$aThompson, A. M.$$b0$$eCorresponding author
000866944 245__ $$aOzonesonde quality assurance: The JOSIE-SHADOZ (2017) experience
000866944 260__ $$aBoston, Mass.$$bASM$$c2019
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000866944 520__ $$aThe ozonesonde is a small balloon-borne instrument that is attached to a standard radiosonde to measure profiles of ozone from the surface to 35 km with ∼100-m vertical resolution. Ozonesonde data constitute a mainstay of satellite calibration and are used for climatologies and analysis of trends, especially in the lower stratosphere where satellites are most uncertain. The electrochemical concentration cell (ECC) ozonesonde has been deployed at ∼100 stations worldwide since the 1960s, with changes over time in manufacture and procedures, including details of the cell chemical solution and data processing. As a consequence, there are biases among different stations and discontinuities in profile time series from individual site records. For 22 years the Jülich (Germany) Ozonesonde Intercomparison Experiment (JOSIE) has periodically tested ozonesondes in a simulation chamber designated the World Calibration Centre for Ozonesondes (WCCOS) by WMO. During October–November 2017 a JOSIE campaign evaluated the sondes and procedures used in Southern Hemisphere Additional Ozonesondes (SHADOZ), a 14-station sonde network operating in the tropics and subtropics. A distinctive feature of the 2017 JOSIE was that the tests were conducted by operators from eight SHADOZ stations. Experimental protocols for the SHADOZ sonde configurations, which represent most of those in use today, are described, along with preliminary results. SHADOZ stations that follow WMO-recommended protocols record total ozone within 3% of the JOSIE reference instrument. These results and prior JOSIEs demonstrate that regular testing is essential to maintain best practices in ozonesonde operations and to ensure high-quality data for the satellite and ozone assessment communities.
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000866944 7001_ $$0P:(DE-Juel1)16203$$aSmit, Herman G.J.$$b1$$ufzj
000866944 7001_ $$0P:(DE-HGF)0$$aWitte, J. C.$$b2
000866944 7001_ $$0P:(DE-HGF)0$$aStauffer, R. M.$$b3
000866944 7001_ $$0P:(DE-HGF)0$$aJohnson, B. J.$$b4
000866944 7001_ $$0P:(DE-HGF)0$$aMorris, G.$$b5
000866944 7001_ $$0P:(DE-HGF)0$$avon der Gathen, P.$$b6
000866944 7001_ $$0P:(DE-HGF)0$$avan Malderen, R.$$b7
000866944 7001_ $$0P:(DE-HGF)0$$aDavies, J.$$b8
000866944 7001_ $$0P:(DE-HGF)0$$aPiters, A.$$b9
000866944 7001_ $$0P:(DE-HGF)0$$aAllaart, M.$$b10
000866944 7001_ $$0P:(DE-HGF)0$$aPosny, F.$$b11
000866944 7001_ $$0P:(DE-HGF)0$$aKivi, R.$$b12
000866944 7001_ $$0P:(DE-HGF)0$$aCullis, P.$$b13
000866944 7001_ $$0P:(DE-HGF)0$$aHoang Anh, N. T.$$b14
000866944 7001_ $$0P:(DE-HGF)0$$aCorrales, E.$$b15
000866944 7001_ $$0P:(DE-HGF)0$$aMachinini, T.$$b16
000866944 7001_ $$0P:(DE-HGF)0$$ada Silva, F. R.$$b17
000866944 7001_ $$0P:(DE-HGF)0$$aPaiman, G.$$b18
000866944 7001_ $$0P:(DE-HGF)0$$aThiong'o, K.$$b19
000866944 7001_ $$0P:(DE-HGF)0$$aZainal, Z.$$b20
000866944 7001_ $$0P:(DE-HGF)0$$aBrothers, G. B.$$b21
000866944 7001_ $$0P:(DE-HGF)0$$aWolff, K. R.$$b22
000866944 7001_ $$0P:(DE-HGF)0$$aNakano, T.$$b23
000866944 7001_ $$0P:(DE-HGF)0$$aStübi, R.$$b24
000866944 7001_ $$0P:(DE-HGF)0$$aRomanes, G.$$b25
000866944 7001_ $$0P:(DE-HGF)0$$aCoetzee, G. J. R.$$b26
000866944 7001_ $$0P:(DE-HGF)0$$aDiaz, J. A.$$b27
000866944 7001_ $$0P:(DE-HGF)0$$aMitro, S.$$b28
000866944 7001_ $$0P:(DE-HGF)0$$aMohamad, M.$$b29
000866944 7001_ $$0P:(DE-HGF)0$$aOgino, S. X.$$b30
000866944 773__ $$0PERI:(DE-600)2029396-3$$a10.1175/BAMS-D-17-0311.1$$gVol. 100, no. 1, p. 155 - 171$$n1$$p155 - 171$$tBulletin of the American Meteorological Society$$v100$$x0003-0007$$y2019
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