2020
DOI: 10.1002/joc.6593
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Dry season circulation‐type classification applied to precipitation and temperature in the Peruvian Andes

Abstract: We present the first systematic classification of circulation regimes that characterize the Tropical Andes during the dry season (May-August). We apply the hierarchical k-means clustering method to ERA-Interim reanalysis data of daily mean geopotential height at 500-and 200-hPa levels for the period 1981-2015. Specifically, by combining the variability in intensity and location of geopotential anomalies we identify 12 circulation types (CTs). We then

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Cited by 2 publications
(4 citation statements)
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“…Therefore, the four central months of the dry (MJJA) and wet (DJFM) seasons were considered as proposed in previous works (eg. Bonshoms et al 2020;Francou et al 2003;Kane 2000;Rosales et al 2022;Segura et al 2019). These four-month periods allowed us to reduce distortions that could arise due to regional differences in the length of both seasons.…”
Section: Hourly Assessment and Mean Daily Cyclesmentioning
confidence: 98%
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“…Therefore, the four central months of the dry (MJJA) and wet (DJFM) seasons were considered as proposed in previous works (eg. Bonshoms et al 2020;Francou et al 2003;Kane 2000;Rosales et al 2022;Segura et al 2019). These four-month periods allowed us to reduce distortions that could arise due to regional differences in the length of both seasons.…”
Section: Hourly Assessment and Mean Daily Cyclesmentioning
confidence: 98%
“…In general terms, fluctuations in upperlevel zonal winds are related to the moisture transport variability at the diurnal (Garreaud et al 2009;Reuder and Egger 2006), intraseasonal (Falvey and Garreaud 2005;Garreaud 2000) and interannual time scales (Garreaud and Aceituno 2001;Garreaud et al 2003;Vuille and Keimig 2004;Segura et al 2016). However, in the southern Peruvian Andes negative (positive) anomalies in daily maximum and minimum temperatures (precipitation) during the DS were related to the presence of extratropical upper tropospheric troughs located off the southern coast of Peru (Bonshoms et al 2020). In addition, the influence of dynamic and orographic convergence of moist air from the Amazon may have an impact on precipitation over the eastern Andes glaciers (Cordillera Vilcanota and, to a lesser intensity, in Cordillera Blanca).…”
Section: Study Areamentioning
confidence: 99%
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