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000052928 084__ $$2WoS$$aGeosciences, Multidisciplinary
000052928 1001_ $$0P:(DE-HGF)0$$aWarneke, T.$$b0
000052928 245__ $$aSeasonal an latitudinal variation of atmospheric methane: A ground-based an ship-borne solar IR spectroscopic study
000052928 260__ $$aWashington, DC$$bAmerican Geophysical Union$$c2006
000052928 300__ $$aL14812
000052928 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
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000052928 440_0 $$02249$$aGeophysical Research Letters$$v33$$x0094-8276
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000052928 520__ $$aColumn-averaged volume mixing ratios of CH4 were retrieved with a precision of better than 0.5% from infrared solar absorption spectra obtained at Ny-Alesund ( Spitsbergen, 79 degrees N) between 1997 and 2004 and during two ship cruises (54 degrees N - 34 degrees S) on the Atlantic in 2003. The retrieval has been performed in a spectral region available to all operational FTIR ( Fourier Transform InfraRed) spectrometers performing solar absorption measurements. The seasonality and the long-term increase of the tropospheric volume-mixing ratio, derived from the infrared measurements agree well with data from surface sampling at this site. The latitudinal variation of ship-borne measurements between 54 degrees N and 34 degrees S is in agreement with inverse model simulations which are optimized vs. the global NOAA/ESRL measurements.
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000052928 7001_ $$0P:(DE-HGF)0$$aMeirink, J. F.$$b1
000052928 7001_ $$0P:(DE-HGF)0$$aBegamaschi, P.$$b2
000052928 7001_ $$0P:(DE-Juel1)129122$$aGrooß, J.-U.$$b3$$uFZJ
000052928 7001_ $$0P:(DE-HGF)0$$aNotholt, J.$$b4
000052928 7001_ $$0P:(DE-HGF)0$$aToon, G. C.$$b5
000052928 7001_ $$0P:(DE-HGF)0$$aVelazco, V.$$b6
000052928 7001_ $$0P:(DE-HGF)0$$aGoede, A.P.H.$$b7
000052928 7001_ $$0P:(DE-HGF)0$$aSchrems, O.$$b8
000052928 773__ $$0PERI:(DE-600)2021599-X$$a10.1029/2006GL025874$$gVol. 33, p. L14812$$pL14812$$q33<L14812$$tGeophysical research letters$$v33$$x0094-8276$$y2006
000052928 8567_ $$uhttp://dx.doi.org/10.1029/2006GL025874
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