Articles | Volume 10, issue 3
Hydrol. Earth Syst. Sci., 10, 383–393, 2006
https://doi.org/10.5194/hess-10-383-2006
Hydrol. Earth Syst. Sci., 10, 383–393, 2006
https://doi.org/10.5194/hess-10-383-2006

  02 Jun 2006

02 Jun 2006

Throughfall and temporal trends of rainfall redistribution in an open tropical rainforest, south-western Amazonia (Rondônia, Brazil)

S. Germer1, H. Elsenbeer1, and J. M. Moraes2 S. Germer et al.
  • 1Institute of Geoecology, University of Potsdam, Potsdam, Germany
  • 2CENA, University of São Paulo, Piracicaba, S.P., Brazil

Abstract. Throughfall volumes and incident rainfall were measured between 23 August and 2 December 2004 as well as from 6 January to 15 April 2005 for individual rain events of differing intensities and magnitudes in an open tropical rainforest in Rondônia, Brazil. Temporal patterns of throughfall spatial variability were examined. Estimated interception was compared to modeled interception obtained by applying the revised Gash model in order to identify sources of throughfall variability in open tropical rainforests.

Gross precipitation of 97 events amounted to 1309 mm, 89±5.6% (S.E.) of which reached the forest floor as throughfall. The redistribution of water within the canopy was highly variable in time, which we attribute to the high density of babassu palms (Orbignya phalerata), their seasonal leaf growth, and their conducive morphology. We identified a 10-min rainfall intensity threshold of 30 mmh-1 above which interception was highly variable. This variability is amplified by funneling and shading effects of palms. This interaction between a rainfall variable and vegetation characteristics is relevant for understanding the hydrology of all tropical rainforests with a high palm density.

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