Profiling water vapor mixing ratios in Finland by means of a Raman lidar, a satellite and a model

dc.bibliographicCitation.firstPage4303
dc.bibliographicCitation.issue11
dc.bibliographicCitation.lastPage4316
dc.bibliographicCitation.volume10
dc.contributor.authorFilioglou, Maria
dc.contributor.authorNikandrova, Anna
dc.contributor.authorNiemelä, Sami
dc.contributor.authorBaars, Holger
dc.contributor.authorMielonen, Tero
dc.contributor.authorLeskinen, Ari
dc.contributor.authorBrus, David
dc.contributor.authorRomakkaniemi, Sami
dc.contributor.authorGiannakaki, Elina
dc.contributor.authorKomppula, Mika
dc.date.accessioned2023-02-27T08:51:28Z
dc.date.available2023-02-27T08:51:28Z
dc.date.issued2017
dc.description.abstractWe present tropospheric water vapor profiles measured with a Raman lidar during three field campaigns held in Finland. Co-located radio soundings are available throughout the period for the calibration of the lidar signals. We investigate the possibility of calibrating the lidar water vapor profiles in the absence of co-existing on-site soundings using water vapor profiles from the combined Advanced InfraRed Sounder (AIRS) and the Advanced Microwave Sounding Unit (AMSU) satellite product; the Aire Limitée Adaptation dynamique Développement INternational and High Resolution Limited Area Model (ALADIN/HIRLAM) numerical weather prediction (NWP) system, and the nearest radio sounding station located 100 km away from the lidar site (only for the permanent location of the lidar). The uncertainties of the calibration factor derived from the soundings, the satellite and the model data are < 2.8, 7.4 and 3.9 %, respectively. We also include water vapor mixing ratio intercomparisons between the radio soundings and the various instruments/model for the period of the campaigns. A good agreement is observed for all comparisons with relative errors that do not exceed 50 % up to 8 km altitude in most cases. A 4-year seasonal analysis of vertical water vapor is also presented for the Kuopio site in Finland. During winter months, the air in Kuopio is dry (1.15±0.40 †kg-1); during summer it is wet (5.54±1.02 †kg-1); and at other times, the air is in an intermediate state. These are averaged values over the lowest 2 km in the atmosphere. Above that height a quick decrease in water vapor mixing ratios is observed, except during summer months where favorable atmospheric conditions enable higher mixing ratio values at higher altitudes. Lastly, the seasonal change in disagreement between the lidar and the model has been studied. The analysis showed that, on average, the model underestimates water vapor mixing ratios at high altitudes during spring and summer.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11526
dc.identifier.urihttp://dx.doi.org/10.34657/10560
dc.language.isoeng
dc.publisherKatlenburg-Lindau : Copernicus
dc.relation.doihttps://doi.org/10.5194/amt-10-4303-2017
dc.relation.essn1867-8548
dc.relation.ispartofseriesAtmospheric measurement techniques : AMT 10 (2017), Nr. 11
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subjectAIRSeng
dc.subjectAMSUeng
dc.subjectatmospheric modelingeng
dc.subjectcalibrationeng
dc.subjectlidareng
dc.subjectmixing ratioeng
dc.subjectradioeng
dc.subjectsatellite dataeng
dc.subjectseasonal variationeng
dc.subjecttroposphereeng
dc.subjectFinlandeng
dc.subjectKuopioeng
dc.subjectPohjois-Savoeng
dc.subject.ddc550
dc.titleProfiling water vapor mixing ratios in Finland by means of a Raman lidar, a satellite and a modeleng
dc.typearticle
dc.typeText
dcterms.bibliographicCitation.journalTitleAtmospheric measurement techniques : AMT
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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