Matches in SemOpenAlex for { <https://semopenalex.org/work/W2073803854> ?p ?o ?g. }
- W2073803854 endingPage "1199" @default.
- W2073803854 startingPage "1189" @default.
- W2073803854 abstract "In our previous research (Power et al., 2006), we analysed the variability in spectral aerosol optical depth (τa), as well as Ångström's wavelength exponent (α), which represents the relative size distribution of aerosols, at 27 sites across North America. The variability was assessed by incorporating the Spatial Synoptic Classification (SSC) surface weather type across each of these sites. In this research, we further our analysis by examining the effect of different 850-hPa flow patterns within the lower troposphere on variability in τa and α. To accomplish this, an 850-hPa flow classification was first developed from principal components analysis (PCA) and cluster analysis on National Centers for Environmental Prediction (NCEP)/The National Center for Atmospheric Research (NCAR) reanalysis geopotential-height data, normalized by month of year. Nine flow types were identified. Cluster analyses yielded five clusters for both τa and α. For τa, spatially cohesive regions were identified, with a western cluster with low aerosol optical depth and minimal synoptic variability, and eastern clusters that showed higher turbidity as well as synoptic variability. In these clusters, higher turbidity was associated with southerly advection. For α, results were less cohesive, with clusters largely representing the different seasonal patterns of the variable, with synoptic variability difficult to interpret. Jackknifing was also utilized to evaluate whether τa and α could be predicted based on SSC weather type and 850-hPa flow type. Results varied at the three stations evaluated, with the method yielding potentially useful results for τa across the two eastern sites, where synoptic variability at the surface and 850-hPa is greater. At the western site, τa could not be successfully predicted. Synoptic variability is too weak for α to be predicted effectively at any of the sites examined. Copyright © 2007 Royal Meteorological Society" @default.
- W2073803854 created "2016-06-24" @default.
- W2073803854 creator A5034635720 @default.
- W2073803854 creator A5040283053 @default.
- W2073803854 creator A5088180348 @default.
- W2073803854 date "2008-07-01" @default.
- W2073803854 modified "2023-09-24" @default.
- W2073803854 title "A further analysis of the spatio‐temporal variability in aerosols across North America: Incorporation of lower tropospheric (850‐hPa) flow" @default.
- W2073803854 cites W1965805473 @default.
- W2073803854 cites W1978739931 @default.
- W2073803854 cites W1993474599 @default.
- W2073803854 cites W1996107442 @default.
- W2073803854 cites W1996593539 @default.
- W2073803854 cites W1996772807 @default.
- W2073803854 cites W2003948052 @default.
- W2073803854 cites W2011327925 @default.
- W2073803854 cites W2012247153 @default.
- W2073803854 cites W2016381774 @default.
- W2073803854 cites W2018616425 @default.
- W2073803854 cites W2023033225 @default.
- W2073803854 cites W2024489189 @default.
- W2073803854 cites W2037065132 @default.
- W2073803854 cites W2048892302 @default.
- W2073803854 cites W2049937218 @default.
- W2073803854 cites W2054598953 @default.
- W2073803854 cites W2057635062 @default.
- W2073803854 cites W2063915806 @default.
- W2073803854 cites W2064098025 @default.
- W2073803854 cites W2064817129 @default.
- W2073803854 cites W2070158576 @default.
- W2073803854 cites W2077535427 @default.
- W2073803854 cites W2089433206 @default.
- W2073803854 cites W2093270164 @default.
- W2073803854 cites W2094139680 @default.
- W2073803854 cites W2151659785 @default.
- W2073803854 cites W2155674062 @default.
- W2073803854 cites W2173251738 @default.
- W2073803854 cites W2176774719 @default.
- W2073803854 doi "https://doi.org/10.1002/joc.1628" @default.
- W2073803854 hasPublicationYear "2008" @default.
- W2073803854 type Work @default.
- W2073803854 sameAs 2073803854 @default.
- W2073803854 citedByCount "8" @default.
- W2073803854 countsByYear W20738038542017 @default.
- W2073803854 countsByYear W20738038542020 @default.
- W2073803854 countsByYear W20738038542021 @default.
- W2073803854 countsByYear W20738038542022 @default.
- W2073803854 crossrefType "journal-article" @default.
- W2073803854 hasAuthorship W2073803854A5034635720 @default.
- W2073803854 hasAuthorship W2073803854A5040283053 @default.
- W2073803854 hasAuthorship W2073803854A5088180348 @default.
- W2073803854 hasConcept C105795698 @default.
- W2073803854 hasConcept C107054158 @default.
- W2073803854 hasConcept C121332964 @default.
- W2073803854 hasConcept C127313418 @default.
- W2073803854 hasConcept C153294291 @default.
- W2073803854 hasConcept C154945302 @default.
- W2073803854 hasConcept C160121416 @default.
- W2073803854 hasConcept C164866538 @default.
- W2073803854 hasConcept C171420983 @default.
- W2073803854 hasConcept C192901106 @default.
- W2073803854 hasConcept C199360897 @default.
- W2073803854 hasConcept C205649164 @default.
- W2073803854 hasConcept C27438332 @default.
- W2073803854 hasConcept C2779345167 @default.
- W2073803854 hasConcept C33923547 @default.
- W2073803854 hasConcept C39432304 @default.
- W2073803854 hasConcept C41008148 @default.
- W2073803854 hasConcept C41524352 @default.
- W2073803854 hasConcept C49204034 @default.
- W2073803854 hasConcept C5072599 @default.
- W2073803854 hasConcept C9075549 @default.
- W2073803854 hasConcept C91586092 @default.
- W2073803854 hasConcept C94747663 @default.
- W2073803854 hasConcept C97355855 @default.
- W2073803854 hasConceptScore W2073803854C105795698 @default.
- W2073803854 hasConceptScore W2073803854C107054158 @default.
- W2073803854 hasConceptScore W2073803854C121332964 @default.
- W2073803854 hasConceptScore W2073803854C127313418 @default.
- W2073803854 hasConceptScore W2073803854C153294291 @default.
- W2073803854 hasConceptScore W2073803854C154945302 @default.
- W2073803854 hasConceptScore W2073803854C160121416 @default.
- W2073803854 hasConceptScore W2073803854C164866538 @default.
- W2073803854 hasConceptScore W2073803854C171420983 @default.
- W2073803854 hasConceptScore W2073803854C192901106 @default.
- W2073803854 hasConceptScore W2073803854C199360897 @default.
- W2073803854 hasConceptScore W2073803854C205649164 @default.
- W2073803854 hasConceptScore W2073803854C27438332 @default.
- W2073803854 hasConceptScore W2073803854C2779345167 @default.
- W2073803854 hasConceptScore W2073803854C33923547 @default.
- W2073803854 hasConceptScore W2073803854C39432304 @default.
- W2073803854 hasConceptScore W2073803854C41008148 @default.
- W2073803854 hasConceptScore W2073803854C41524352 @default.
- W2073803854 hasConceptScore W2073803854C49204034 @default.
- W2073803854 hasConceptScore W2073803854C5072599 @default.
- W2073803854 hasConceptScore W2073803854C9075549 @default.
- W2073803854 hasConceptScore W2073803854C91586092 @default.
- W2073803854 hasConceptScore W2073803854C94747663 @default.