Evapotranspiration

Humberto R. Da Rocha, Antonio O. Manzi, W. James Shuttleworth

Research output: Chapter in Book/Report/Conference proceedingChapter

19 Citations (Scopus)

Abstract

We review the measurements of latent and sensible heat flux made at seven flux tower sites during the Large-Scale Biosphere-Atmosphere Experiment for tropical humid, transitional and semideciduous forests, floodplain (with cerrado), and cerrado ecosystems. Measurements over farmlands in Amazonia vary from 1.2 (for bare soil) to 3 mm d-1, with a reduction in the dry season. Estimates of evapotranspiration for Amazonia based on atmospheric reanalysis are generally higher than the measurements. Remarkably, for all the seven sites, the mean annual sensible heat flux ranged from 20 to 38 W m -2, lower during the wet season and higher in the late dry season, consistent with the variation of net radiation and soil moisture. Based on the seasonal evapotranspiration, the sites are divided into two functional groups: tropical forest and savanna. At the northern sites (Manaus, Santarém), precipitation is above 1900 mm a-1, monthly evapotranspiration is fairly constant during the wet season, ranges from 2.8 to 3.6 mm d-1, progressively increases along the dry season up to 4 mm d-1, and is dominated by net radiation and vapor density deficit. The western semideciduous forest in Rondônia presents similarities with the forest group, with monthly evapotranspiration that varies little but concurrent with net radiation year round, and peaks more exactly in the dryto-wet season transition. At the southern and eastern sites, precipitation is below 1700 mm a-1, seasonal evapotranspiration is limited by soil moisture, ranges from 3 to 4 mm d-1 in the wet season, and decreases in the dry season to 2.5 mm d-1 in the transitional forest (Mato Grosso) and floodplain (Tocantins), and to 1 mm d-1 in the São Paulo cerrado.

Original languageEnglish (US)
Title of host publicationGeophysical Monograph Series
PublisherAmerican Geophysical Union
Pages261-272
Number of pages12
Volume186
StatePublished - 2009

Publication series

NameGeophysical Monograph Series
Volume186

Fingerprint

evapotranspiration
wet season
dry season
cerrado
net radiation
sensible heat flux
soil moisture
floodplain forest
heat flux
latent heat flux
bare soil
radiation
savanna
biosphere
tropical forest
functional group
farmlands
floodplain
agricultural land
latent heat

ASJC Scopus subject areas

  • Geophysics

Cite this

Da Rocha, H. R., Manzi, A. O., & Shuttleworth, W. J. (2009). Evapotranspiration. In Geophysical Monograph Series (Vol. 186, pp. 261-272). (Geophysical Monograph Series; Vol. 186). American Geophysical Union.

Evapotranspiration. / Da Rocha, Humberto R.; Manzi, Antonio O.; Shuttleworth, W. James.

Geophysical Monograph Series. Vol. 186 American Geophysical Union, 2009. p. 261-272 (Geophysical Monograph Series; Vol. 186).

Research output: Chapter in Book/Report/Conference proceedingChapter

Da Rocha, HR, Manzi, AO & Shuttleworth, WJ 2009, Evapotranspiration. in Geophysical Monograph Series. vol. 186, Geophysical Monograph Series, vol. 186, American Geophysical Union, pp. 261-272.
Da Rocha HR, Manzi AO, Shuttleworth WJ. Evapotranspiration. In Geophysical Monograph Series. Vol. 186. American Geophysical Union. 2009. p. 261-272. (Geophysical Monograph Series).
Da Rocha, Humberto R. ; Manzi, Antonio O. ; Shuttleworth, W. James. / Evapotranspiration. Geophysical Monograph Series. Vol. 186 American Geophysical Union, 2009. pp. 261-272 (Geophysical Monograph Series).
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