2001
DOI: 10.1029/2000wr900395
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Seasonally in ENSO‐related precipitation, river discharges, soil moisture, and vegetation index in Colombia

Abstract: Abstract. An analysis of hydrologic variability in Colombia shows different seasonal effects associated with E1 Nifio/Southern Oscillation (ENSO) phenomenon. Spectral and cross-correlation analyses are developed between climatic indices of the tropical Pacific Ocean and the annual cycle of Colombia's hydrology: precipitation, river flows, soil moisture, and the Normalized Difference Vegetation Index (NDVI). Our findings indicate stronger anomalies during December-February and weaker during March-May. The effec… Show more

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Cited by 231 publications
(219 citation statements)
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“…On the other hand, the process variables (PRC and EVP) are the most complex in the region HPREC= 0.76 and HEVP= 0.71. This result confirms the diversity of factors that make part of the hydro-climatic variance at interannual timescale, thus reflecting the implicit complexity of the linkages between these two processes over TropSA [44,46,59,[70][71][72]. The high entropy of EVP can be also explained in terms of the multivariate influence of water and energy fluxes in TropSA [22,47,73].…”
Section: Svd Noise Reduction and Entropysupporting
confidence: 65%
“…On the other hand, the process variables (PRC and EVP) are the most complex in the region HPREC= 0.76 and HEVP= 0.71. This result confirms the diversity of factors that make part of the hydro-climatic variance at interannual timescale, thus reflecting the implicit complexity of the linkages between these two processes over TropSA [44,46,59,[70][71][72]. The high entropy of EVP can be also explained in terms of the multivariate influence of water and energy fluxes in TropSA [22,47,73].…”
Section: Svd Noise Reduction and Entropysupporting
confidence: 65%
“…However, during intense El Niño-Southern Oscillation (ENSO) events, the ITCZ can extend anomalously far south bringing drought conditions in the MRB. In contrast, during La Niña events the MRB experiences heavier than normal rains and colder conditions that often extend-sometimes even bridging ITCZ events, leading to rainy periods that can last a year 10 or longer (Poveda, Jaramillo, Gil, Quiceno, & Mantilla, 2001;Poveda & Mesa, 1997). The strong relation between anomalously high or low stream flow conditions at four stations in the MRB and the Oceanic Niño Index, a measure of ENSO, is illustrated in Figure 2.…”
Section: System Descriptionmentioning
confidence: 99%
“…Seasonal forecasts of soil moisture could give a useful indication of flood risk in dry regions of Africa (Fig. 4), and these forecasts are also likely to have seasonal predictability in areas where they can be well initialized, notably due to the persistence of soil moisture (Kanamitsu et al, 2002;Koster et al, 2010;Poveda et al, 2001). This also takes evaporation into account.…”
Section: Discussionmentioning
confidence: 99%