2005
DOI: 10.1007/s00704-005-0182-8
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Characteristics of large-scale atmospheric circulation related to extreme monthly rainfall anomalies in the Pampa Region, Argentina, under non-ENSO conditions

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Cited by 32 publications
(24 citation statements)
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“…The ENSO negative (El Niño) and positive phases (La Niña) were related to rainfall and Sea Surface Temperature (SST) anomalies in the main oceanic currents (Brazil and Malvinas). Several studies have related, for the Buenos Aires province, the occurrence of extreme wet (dry) events with negative (positive) ENSO phases [9][10][11][12][13]. Phytoplankton blooms are the main sign of enhancement of the pelagic activity [14], and their occurrence is tightly related to biogeochemical fluctuations in sea water, and the variability in the annual recruitment of fishes (e.g., [15,16]).…”
Section: Introductionmentioning
confidence: 99%
“…The ENSO negative (El Niño) and positive phases (La Niña) were related to rainfall and Sea Surface Temperature (SST) anomalies in the main oceanic currents (Brazil and Malvinas). Several studies have related, for the Buenos Aires province, the occurrence of extreme wet (dry) events with negative (positive) ENSO phases [9][10][11][12][13]. Phytoplankton blooms are the main sign of enhancement of the pelagic activity [14], and their occurrence is tightly related to biogeochemical fluctuations in sea water, and the variability in the annual recruitment of fishes (e.g., [15,16]).…”
Section: Introductionmentioning
confidence: 99%
“…Annual rainfall decreases from 1000 mm in the NE to 800 mm in the SW (see Fig. 1C), although inter-annual variability of rainfall is quite frequent in the Pampas with extensive rainfall or drought (Labraga et al, 2002;Scian et al, 2006). According to data provided by the Servicio Meteorológico Nacional of Argentina (SMN, Exp_144540), the first year of our study was considered as a normal period (%800-900 mm, see Fig.…”
Section: Study Areamentioning
confidence: 99%
“…They concluded that El Niño–Southern Oscillation (ENSO) could be responsible for most of the interannual variability during the summer season. Nevertheless, in 2006 an interesting paper 18 showed that central‐eastern Argentina experienced severe drought and wet conditions during the last decades under non‐ENSO years. A dipolar structure of SST anomalies has also been shown to accompany interannual intensification of the SACZ over the southwestern Atlantic 19 .…”
Section: Climatic Descriptionmentioning
confidence: 99%