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Koichiro Kuraji

Researcher at University of Tokyo

Publications -  71
Citations -  1602

Koichiro Kuraji is an academic researcher from University of Tokyo. The author has contributed to research in topics: Surface runoff & Watershed. The author has an hindex of 18, co-authored 63 publications receiving 1379 citations. Previous affiliations of Koichiro Kuraji include National Taiwan University & Tokyo Institute of Technology.

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Annual water balance and seasonality of evapotranspiration in a Bornean tropical rainforest

TL;DR: In this paper, the results of 2 years combined field measurements of water vapor exchange with the atmosphere and simplified model calculations at Lambir Hills National Park, Sarawak, Malaysia (4812 0 N, 114802 0 E).
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Irregular droughts trigger mass flowering in aseasonal tropical forests in asia

TL;DR: It is shown that this phenomenon is most likely triggered by irregular droughts based on 10 years of observations, and changes in the ENSO cycle resulting from global warming, may have serious ramifications for forest regeneration in this region.
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Transpiration, canopy conductance and the decoupling coefficient of a lowland mixed dipterocarp forest in Sarawak, Borneo: dry spell effects

TL;DR: In this paper, the authors investigated key factors controlling materials-exchange, such as canopy (gc) and aerodynamic conductance (ga) and the decoupling coefficient (Ω), in an intact lowland mixed dipterocarp forest in Sarawak, Borneo.
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Ten-year evapotranspiration estimates in a Bornean tropical rainforest

TL;DR: In this article, the authors 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.
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Water cycling in a Bornean tropical rain forest under current and projected precipitation scenarios

TL;DR: In this paper, a simplified hydrologic model is developed with its primary forcing term being rainfall statistics, and the effects of increased (or decreased) precipitation on increased or decreased) cloud cover and hence evapotranspiration is explicitly considered.