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Ten-year evapotranspiration estimates in a Bornean tropical rainforest
Authors:Tomonori Kume  Nobuaki TanakaKoichiro Kuraji  Hikaru KomatsuNatsuko Yoshifuji  Taku M SaitohMasakazu Suzuki  Tomo’omi Kumagai
Institution:a School of Forestry and Resource Conservation, National Taiwan University, Taipei 106, Taiwan
b University Forest in Aichi, The University of Tokyo, Seto, Aichi 489-0031, Japan
c Kasuya Research Forest, Kyushu University, Sasaguri, Fukuoka 811-2415, Japan
d Graduate School of Agriculture, Kyoto University, Sakyo-ku, Kyoto 606-8502, Japan
e River Basin Research Center, Gifu University, Yanagido, Gifu 501-1193, Japan
f Graduate School of Agricultural and Life Sciences, The University of Tokyo, Bunkyo-ku, Tokyo 113-8657, Japan
g Hydrospheric Atmospheric Research Center, Nagoya University, Chikusa-ku, Nagoya 464-8601, Japan
Abstract:This study was undertaken to quantify interannual variations of total evaporation (ET) in a tropical rainforest in Sarawak, Malaysia. To this end, we conducted 10-year meteorological measurements and formulated a simplified big-leaf model that reproduces transpiration (Et), rainfall interception (Ei), and ET as the sum of these. The model was validated independently using eddy covariance fluxes, rainfall interception based on throughfall and stemflow measurements, and sap flow measurements conducted for more than 2 years. Using the model, Et, Ei, and ET were estimated for the period 2000-2009. Annual Et, Ei, and ET averaged over 10 years were estimated as 1114, 209, and 1323 mm, respectively, with small seasonal fluctuations. The derived estimates showed conservative year-to-year variations in annual Et, Ei, and ET (CV = 5-7%) in contrast to considerable year-to-year variations in annual rainfall (CV = 11%). Specific rainfall characteristics (e.g. intense short duration storms) at this site can explain the conservative year-to-year Ei variations. Small interannual variations in meteorological conditions and absence of severe drought during the study period can explain the small year-to-year Et variations. To characterize ET at our site, we also compared Ei and ET at our site with those of other tropical forests. Based on the derived ET characteristics, we discuss possible ET changes in response to changes in rainfall regime at this site.
Keywords:Tropical rainforest  Eddy covariance method  Rainfall interception  Sap flow  Evapotranspiration
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