This proceeding is a compilation of findings and progress activities of research collaboration between the Forest Department Sarawak (FDS) and the Japan Research Consortium for Tropical Forests in Sarawak (JRCTS). To highlight the research findings, An International Symposium entitled "Frontier in Tropical Forest Research: Progress in Joint Projects between the Forest Department Sarawak and the Japan Research Consortium for Tropical Forests in Sarawak" was ii held in Kuching, Sarawak on 21-22 September 2015.The hydrological cycle in tropical rainforests is very active. Hydrological data such as rainfall, runoff, and evapotranspiration (ET) are important for not only forecasting of global-scale environmental changes and predicting disaster b...
Sumber Jaya (54,194 hectares) is a district in West Lampung, Indonesia, located at the upper part of...
The objectives of this paper were to determine evapotranspiration (ET) from an oak-beech dominated f...
A procedure for estimating the impact of CO2-induced climate and vegetation changes on actual evapo...
ABSTRACT: Forested areas play a dominant role in the global hydrological cycle. Evapotranspiration i...
Forested areas play a dominant role in the global hydrological cycle. Evapotranspiration is a domin...
We examined the water balance and hydrological characteristics of tropical montane forests in Kinaba...
While timber harvesting has plateaued, repeat-logging and conversion into plantations (especially oi...
Short Time Period Water Budget (SPWB) and Catchment Water Balance (CWB) methods were used for estima...
ABSTRACT The study was conducted in Musi Rawas and Musi Banyuasin area. This area is choosen because...
Within tropical rainforest environments, rainfall pattern and canopy structure regulates the partiti...
flow in a catchment area for a certain period of the circulating water. In the hydrological system o...
Understanding the intensity and duration of tropical rain events is critical to modelling the rate a...
Reference evapotranspiration (ET?) was determined using the Penman-Monteith (P-M) combination equati...
Although erosional impacts of rainforest logging are well established, changes in hydrological dynam...
Generally, the tropical montane cloud forest (TMCF) has known to be the headwater for rivers which a...
Sumber Jaya (54,194 hectares) is a district in West Lampung, Indonesia, located at the upper part of...
The objectives of this paper were to determine evapotranspiration (ET) from an oak-beech dominated f...
A procedure for estimating the impact of CO2-induced climate and vegetation changes on actual evapo...
ABSTRACT: Forested areas play a dominant role in the global hydrological cycle. Evapotranspiration i...
Forested areas play a dominant role in the global hydrological cycle. Evapotranspiration is a domin...
We examined the water balance and hydrological characteristics of tropical montane forests in Kinaba...
While timber harvesting has plateaued, repeat-logging and conversion into plantations (especially oi...
Short Time Period Water Budget (SPWB) and Catchment Water Balance (CWB) methods were used for estima...
ABSTRACT The study was conducted in Musi Rawas and Musi Banyuasin area. This area is choosen because...
Within tropical rainforest environments, rainfall pattern and canopy structure regulates the partiti...
flow in a catchment area for a certain period of the circulating water. In the hydrological system o...
Understanding the intensity and duration of tropical rain events is critical to modelling the rate a...
Reference evapotranspiration (ET?) was determined using the Penman-Monteith (P-M) combination equati...
Although erosional impacts of rainforest logging are well established, changes in hydrological dynam...
Generally, the tropical montane cloud forest (TMCF) has known to be the headwater for rivers which a...
Sumber Jaya (54,194 hectares) is a district in West Lampung, Indonesia, located at the upper part of...
The objectives of this paper were to determine evapotranspiration (ET) from an oak-beech dominated f...
A procedure for estimating the impact of CO2-induced climate and vegetation changes on actual evapo...