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000028466 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000028466 1001_ $$0P:(DE-HGF)0$$aKanzawa, H.$$b0
000028466 245__ $$aValidation and data characteristics of water vapor profiles observed by the Improved Limb Atmospheric Spectrometer (ILAS) and processed with Version 5.20 algorithm
000028466 260__ $$aWashington, DC$$aWashington, DC$$bUnion$$bUnion$$c2002
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000028466 440_0 $$03369$$aJournal of Geophysical Research$$v107$$x0022-1406
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000028466 520__ $$a[1] Vertical profiles of water vapor concentration at high latitudes (57-72 degreesN; 64-89 degreesS) were observed by the Improved Limb Atmospheric Spectrometer (ILAS) solar occultation sensor aboard the Advanced Earth Observing Satellite (ADEOS). These measurements were made continuously from November 1996 through June 1997 with some additional periods in September to October 1996. A validation study of the water vapor data processed with the version 5.20 ILAS retrieval algorithm is presented in this paper. Uncertainty and general characteristics of the ILAS water vapor measurements are briefly reviewed. Comparisons are made with data obtained by (1) the ILAS validation balloon campaigns at Kiruna, Sweden and at Fairbanks, Alaska; (2) the aircraft measurements under the Photochemistry of Ozone Loss in the Arctic Region in Summer (POLARIS) campaign; and (3) available satellite measurements of the version 19 Halogen Occultation Experiment (HALOE) and the version 6 Stratospheric Aerosol and Gas Experiment II (SAGE II). The agreement between ILAS water vapor and all independent reliable correlative measurements in the altitude region of 15-60 km is better than 10% for the majority of cases and better than 20% for all comparisons, with the exception of some isolated cases detailed in this paper. Climatological comparisons of ILAS data with Upper Atmosphere Research Satellite (UARS) climatology and HALOE data show the overall consistency of ILAS water vapor data considering the known features of atmospheric circulation. The characteristics of ILAS measurements, i.e., high sampling frequency in polar latitudes with high vertical resolution along with the good data quality, make the ILAS water vapor data set valuable for various polar stratospheric research applications.
000028466 536__ $$0G:(DE-Juel1)FUEK257$$2G:(DE-HGF)$$aChemie und Dynamik der Geo-Biosphäre$$cU01$$x0
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000028466 65320 $$2Author$$awater vapor
000028466 65320 $$2Author$$apolar stratosphere
000028466 65320 $$2Author$$avalidation
000028466 65320 $$2Author$$asatellite sensor
000028466 65320 $$2Author$$aImproved Limb Atmospheric Spectrometer (ILAS)
000028466 7001_ $$0P:(DE-Juel1)VDB1410$$aSchiller, C.$$b1$$uFZJ
000028466 7001_ $$0P:(DE-HGF)0$$aOvarlez, J.$$b2
000028466 7001_ $$0P:(DE-HGF)0$$aCamy-Peyret, C.$$b3
000028466 7001_ $$0P:(DE-HGF)0$$aJesek, P.$$b4
000028466 7001_ $$0P:(DE-HGF)0$$aOelhaf, H.$$b5
000028466 7001_ $$0P:(DE-HGF)0$$aStowasser, M.$$b6
000028466 7001_ $$0P:(DE-HGF)0$$aTraub, W. A.$$b7
000028466 7001_ $$0P:(DE-HGF)0$$aJucks, K. W.$$b8
000028466 7001_ $$0P:(DE-HGF)0$$aJohnson, D. G.$$b9
000028466 7001_ $$0P:(DE-HGF)0$$aToon, G. C.$$b10
000028466 7001_ $$0P:(DE-HGF)0$$aSen, B.$$b11
000028466 7001_ $$0P:(DE-HGF)0$$aBlavier, J.-F.$$b12
000028466 7001_ $$0P:(DE-HGF)0$$aPark, J.$$b13
000028466 7001_ $$0P:(DE-HGF)0$$aBodeker, G. E.$$b14
000028466 7001_ $$0P:(DE-HGF)0$$aPan, L. L.$$b15
000028466 7001_ $$0P:(DE-HGF)0$$aSugita, T.$$b16
000028466 7001_ $$0P:(DE-HGF)0$$aNakamjima, H.$$b17
000028466 7001_ $$0P:(DE-HGF)0$$aYokota, T.$$b18
000028466 7001_ $$0P:(DE-HGF)0$$aSuzuki, M.$$b19
000028466 7001_ $$0P:(DE-HGF)0$$aShiotani, M.$$b20
000028466 7001_ $$0P:(DE-HGF)0$$aSasano, Y.$$b21
000028466 773__ $$0PERI:(DE-600)2016800-7$$a10.1029/2001JD000881$$gVol. 107, p. D24$$pD24$$q107<D24$$tJournal of geophysical research / Atmospheres$$v107$$x0022-1406$$y2002
000028466 8567_ $$uhttp://dx.doi.org/10.1029/2001JD000881
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