Studying Anomalous Discrepancies between MODIS and CALIOP Cloud Observations CyberTraining: Big Data + High-Performance Computing + Atmospheric Sciences

dc.contributor.authorAbraham, Christine
dc.contributor.authorNorman, Olivia
dc.contributor.authorShepherd, Erick
dc.contributor.authorZheng, Jianyu
dc.contributor.authorZhang, Zhibo
dc.date.accessioned2021-03-31T18:34:53Z
dc.date.available2021-03-31T18:34:53Z
dc.date.issued2020
dc.description.abstractWhen examining collocated data from the A-Train satellite constellation, there are a notable number of clouds that CALIOP identifies as transparent but MODIS paradoxically reports as having a high cloud optical thickness (COT), therefore implying that the cloud is opaque. We refer to these as ”anomalous transparent clouds”. Our team is investigating two hypotheses in an effort to explain the occurrence of these anomalies. The first hypothesis is that the anomalies could be MODIS COT retrieval errors due to the misclassification of high albedo surfaces, such as snow and sea ice, as clouds. The other hypothesis is that the anomalies could be clouds which are misidentified as having a high COT due to 3D radiative effects. The former hypothesis was tested by collocating the single-layer cloud anomalies that were over water with NSIDC AMSRE sea ice observations using a k-nearest neighbors (k-NN) algorithm. We determined that around 50% of such anomalies occur over areas with high sea ice concentrations (95-100%). Further research is required to account for the other half of the anomalies that showed no correlation with high albedo surfaces. We have taken preliminary steps toward exploring whether the cloud 3D radiative effects hypothesis might explain the remaining anomalies.en_US
dc.description.sponsorshipThis work is supported by the grant “CyberTraining: DSE: Cross-Training of Researchers in Computing, Applied Mathematics and Atmospheric Sciences using Advanced Cyberinfrastructure Resources” from the National Science Foundation (grant no. OAC–1730250). The hardware used in the computational studies is part of the UMBC High Performance Computing Facility (HPCF). The facility is supported by the U.S. National Science Foundation through the MRI program (grant nos. CNS–0821258, CNS–1228778, and OAC–1726023) and the SCREMS program (grant no. DMS–0821311), with additional substantial support from the University of Maryland, Baltimore County (UMBC). See hpcf.umbc.edu for more information on HPCF and the projects using its resources.en_US
dc.description.urihttp://hpcf-files.umbc.edu/research/papers/CT2020Team2.pdfen_US
dc.format.extent11 pagesen_US
dc.genretechnical reportsen_US
dc.identifierdoi:10.13016/m2wegr-famv
dc.identifier.citationAbraham, Christine; Norman, Olivia; Shepherd, Erick; Zheng, Jianyu; Zhang, Zhibo; Studying Anomalous Discrepancies between MODIS and CALIOP Cloud Observations CyberTraining: Big Data + High-Performance Computing + Atmospheric Sciences; http://hpcf-files.umbc.edu/research/papers/CT2020Team2.pdfen_US
dc.identifier.urihttp://hdl.handle.net/11603/21269
dc.language.isoen_USen_US
dc.publisherUMBC HPCFen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Information Systems Department Collection
dc.relation.ispartofUMBC Physics Department
dc.relation.ispartofUMBC Faculty Collection
dc.relation.ispartofUMBC Student Collection
dc.relation.ispartofseriesHPCF;2020–12
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.subjectUMBC High Performance Computing Facility (HPCF)
dc.titleStudying Anomalous Discrepancies between MODIS and CALIOP Cloud Observations CyberTraining: Big Data + High-Performance Computing + Atmospheric Sciencesen_US
dc.typeTexten_US

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