Assimilation of lidar planetary boundary layer height observations

dc.contributor.authorTangborn, Andrew
dc.contributor.authorDemoz, Belay
dc.contributor.authorCarroll, Brian J.
dc.contributor.authorSantanello, Joseph
dc.contributor.authorAnderson, Jeffrey L.
dc.date.accessioned2020-08-17T19:33:06Z
dc.date.available2020-08-17T19:33:06Z
dc.date.issued2020-07-07
dc.description.abstractLidar backscatter and wind retrievals of the planetary boundary layer height (PBLH) are assimilated into 22 hourly forecasts from the NASA Unified – Weather and Research Forecast (NU-WRF) model during the Plains Elevated Convection Convection at Night (PECAN) campaign on 11 July 2015 in Greensburg, Kansas, using error statistics collected from the model profiles to compute the necessary covariance matrices. Two separate forecast runs using different PBL physics schemes were employed, and comparisons with 5 independent sonde profiles were made for each run. Both of the forecast runs accurately predicted the PBLH and the state variable profiles within the planetary boundary layer during the early morning, and the assimilation had little impact during this time. In the late afternoon, the forecast runs showed decreased accuracy as the convective boundary layer developed. However, assimilation of the doppler lidar PBLH observations were found to improve the temperature, water vapor and velocity profiles relative to independent sonde profiles. The computed forecast error covariances between the PBLH and state variables were found to rise in the late afternoon, leading to the larger improvements in the afternoon. This work represents the first effort to assimilate PBLH into forecast states using ensemble methods.en_US
dc.description.sponsorshipB. Demoz was funded by National Science Foundation award (AGS-1503563) to the University of Maryland, Baltimore County and through NOAA Cooperative Science Center in Atmospheric Sciences and Meteorology, funded by the Educational Partner ship Program at NOAA in collaboration with Howard University.en_US
dc.description.urihttps://amt.copernicus.org/preprints/amt-2020-238/en_US
dc.format.extent19 pagesen_US
dc.genrejournal articlesen_US
dc.identifierdoi:10.13016/m2pqba-ckyo
dc.identifier.citationTangborn, Andrew; Demoz, Belay; Carroll, Brian J.; Santanello, Joseph; Anderson, Jeffrey L.; Assimilation of lidar planetary boundary layer height observations; Atmospheric Measurement Techniques (2020); https://amt.copernicus.org/preprints/amt-2020-238/en_US
dc.identifier.urihttps://doi.org/10.5194/amt-2020-238
dc.identifier.urihttp://hdl.handle.net/11603/19449
dc.language.isoen_USen_US
dc.publisherEGU Publicationsen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Physics Department Collection
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology (JCET)
dc.relation.ispartofUMBC Faculty Collection
dc.rightsThis item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author.
dc.rightsAttribution 4.0 International (CC BY 4.0)*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.titleAssimilation of lidar planetary boundary layer height observationsen_US
dc.typeTexten_US

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