1996
DOI: 10.1016/0169-8095(95)00025-9
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Evaluation and analysis of daily atmospheric circulation patterns of the 500 HPA pressure field over the southwestern USA

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Cited by 19 publications
(13 citation statements)
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“…Kidson (1994) clustered 9 years of daily analyses (at 00 : 00h UTC) of 1000 hPa geopotential height over the New Zealand region, identifying 13 synoptic groups, assuming a less than perfect representation of the low-pressure centres. Over the southwestern USA, Galambosi et al (1996) applied these multivariate methodologies to daily 500 hPa pressure fields at 12 : 00 UTC, coupling PCA and clustering in order to describe and generate local hydrological variables. Applied to wind erosion events in sandy soil agricultural areas of southern Sweden, Ekstrom et al (2002) classified daily SLP circulation data and identified (via the definition of an index of erosion severity) the patterns associated with large erosion damage.…”
Section: Methodsmentioning
confidence: 99%
“…Kidson (1994) clustered 9 years of daily analyses (at 00 : 00h UTC) of 1000 hPa geopotential height over the New Zealand region, identifying 13 synoptic groups, assuming a less than perfect representation of the low-pressure centres. Over the southwestern USA, Galambosi et al (1996) applied these multivariate methodologies to daily 500 hPa pressure fields at 12 : 00 UTC, coupling PCA and clustering in order to describe and generate local hydrological variables. Applied to wind erosion events in sandy soil agricultural areas of southern Sweden, Ekstrom et al (2002) classified daily SLP circulation data and identified (via the definition of an index of erosion severity) the patterns associated with large erosion damage.…”
Section: Methodsmentioning
confidence: 99%
“…Solman and Menén-dez (2003) found that daily winter 500 hPa geopotential heights over the southern part of the South American continent could be grouped into five frequently occurring circulation types and that two of the five circulation types had anomalously high frequencies during positive ENSO events. Galambosi et al (1996) classified 500 hPa pressure field heights over southwestern United States for each season into eight or nine classes and Burlando (2009) found that eight wind flow patterns adequately explained the wind climate over the Mediterranean.…”
Section: Introductionmentioning
confidence: 99%
“…Kidson, on the basis of S-mode and covariance dispersion matrix in PCA, used Ward's hierarchical CL to determine the number of groups and their centroids for the K-means algorithm. Over south-western USA, Galambosi et al (1996) applied these multivariate methodologies to daily 500 hPa pressure fields at 12:00 UTC (diamond structured grids), coupling PCA (S-mode of decomposition and correlation matrix) and CL (K-means) in order to describe and generate local hydrological variables. Galambosi et al (1996), as did Bogardi et al (1993), selected the number of groups for the K-means method in a subjective way, denoting this as a typical subjective step in the automated classification procedure.…”
Section: Introductionmentioning
confidence: 99%
“…Over south-western USA, Galambosi et al (1996) applied these multivariate methodologies to daily 500 hPa pressure fields at 12:00 UTC (diamond structured grids), coupling PCA (S-mode of decomposition and correlation matrix) and CL (K-means) in order to describe and generate local hydrological variables. Galambosi et al (1996), as did Bogardi et al (1993), selected the number of groups for the K-means method in a subjective way, denoting this as a typical subjective step in the automated classification procedure. In this way, and to analyse precipitation variability in Portugal in relation to large-scale circulation, Corte-Real et al (1998) applied an information measure based on the precipitation series for determining the optimal number of groups for K-means, eliminating subjectivity in this step of the classification.…”
Section: Introductionmentioning
confidence: 99%