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contributor authorPodestá, Guillermo P.
contributor authorMessina, Carlos D.
contributor authorGrondona, Martín O.
contributor authorMagrin, Graciela O.
date accessioned2017-06-09T14:07:10Z
date available2017-06-09T14:07:10Z
date copyright1999/10/01
date issued1999
identifier issn0894-8763
identifier otherams-12777.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148153
description abstractAssociations are investigated between yields of major crops in the Argentine Pampas (central-eastern Argentina) and El Niño?Southern Oscillation (ENSO) phase. For maize and sorghum, higher (lower) yield anomalies occur more frequently than expected by chance alone during warm (cold) ENSO events. For both crops, the depression of yields during cold events is, on average, larger and less variable than yield increases are during warm events. A yield decrease during cold events also is observed in soybean yields, although the effect of warm events is not statistically significant. There is a marginally significant tendency for low sunflower yields to occur less frequently than expected during cold events. Wheat, the only winter crop considered, did not show an association with ENSO. Precipitation anomalies during October?February (the period with strongest ENSO signal in the Pampas) are summarized through principal component analysis. Precipitation anomalies during November?January are significantly correlated with maize, sorghum, and soybean yield anomalies. In turn, those precipitation anomalies show a distinct ENSO signal. Late spring?early summer precipitation, then, appears to mediate associations between ENSO phase and yields of maize, sorghum, and soybean in the Pampas.
publisherAmerican Meteorological Society
titleAssociations between Grain Crop Yields in Central-Eastern Argentina and El Niño–Southern Oscillation
typeJournal Paper
journal volume38
journal issue10
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1999)038<1488:ABGCYI>2.0.CO;2
journal fristpage1488
journal lastpage1498
treeJournal of Applied Meteorology:;1999:;volume( 038 ):;issue: 010
contenttypeFulltext


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