@Article{TomasellaHoCuNoWaOl:2007:EfInVa,
author = "Tomasella, Javier and Hodnett, Martin G. and Cuartas, Luz Adriana
and Nobre, Antonio D. and Waterloo, Maarten J. and Oliveira,
Sylvia M.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and Department
of Hydrology and Geo-environmental Sciences, Faculty of Earth and
Life Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV
Amsterdam, The Netherlands and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas da
Amaz{\^o}nia} and Department of Hydrology and Geo-environmental
Sciences, Faculty of Earth and Life Sciences, Vrije Universiteit,
De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands and
{Instituto Nacional de Pesquisas da Amaz{\^o}nia}",
title = "The water balance of an Amazonian micro-catchment: the effect of
interannual variability of rainfall on hydrological behaviour",
journal = "Hydrological Processes",
year = "2007",
volume = "*",
number = "*",
pages = "*",
month = "Oct.",
keywords = "water balance • Amazonian micro-catchment • interannual
variability.",
abstract = "In humid tropical systems, the large intraseasonal and interannual
variability of rainfall can significantly affect all components of
the water balance. This variability and the lack of detailed
hydrological and meteorological data in both temporal and spatial
scales have created uncertainties regarding the closure of the
water balance for the Amazon basin. Previous studies in Amazonian
micro-catchments suggested that both the unsaturated and
groundwater system, which are not taken into consideration in
basin-wide water budgets published in the literature, play an
important role in controlling the timing of runoff generation. In
this paper, the components of the water balance and the variations
in different storages within the system were examined using 3
years' data from a 6·58 km2 micro-catchment in central Amazonia.
The role and relative importance of the various stores were
examined. The results show a strong memory effect in the
groundwater system that carries over seasonal climate anomalies
from one year to the next and affects the hydrological response
well beyond the time span of the anomaly. In addition, the deep
unsaturated zone was found to play a key role in reducing most of
the intraseasonal variability and also affected the groundwater
recharge. This memory effect is crucial for sustaining streamflow
and evaporation in years with rainfall deficiency. The memory
effect caused by storage in the groundwater and unsaturated
systems may also prevent the closure of annual large-scale water
balances, which assume that storage returns to a standard state
each year. Copyright © 2007 John Wiley \& Sons, Ltd..",
doi = "10.1002/hyp.6813",
url = "http://dx.doi.org/10.1002/hyp.6813",
issn = "0885-6087",
language = "en",
targetfile = "Tomasella et al, 2008. the water balanace of an amazonian
micr-catchment-1.pdf",
urlaccessdate = "26 abr. 2024"
}