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Forest is an ideal ecosystem for a hydrological cycle, however converting forests to agroforestry or rainfed\udagriculture is inevitable. This study elaborates a hydrological response of infiltration, runoff, and soil moisture in\udthree land uses at Renggung watershed. Field measurements were conducted in 2014−2015 in those system with soil\udtypes of entisols at upstream, inceptisols at the middle, and vertisols at downstream. Results showed that constant\udinfiltration rate at upstream in forest was 55.6 cm hr-1, in 15−30 years agroforestry was 32.4 cm hr-1 on average and in\udrainfed was 26.4 cm hr-1. Infiltration in agroforestry at the middle and downstream was 16.8 cm hr-1 and 11.2 cm hr-1,\ud-1 -1 -1\udrespectively, while in rainfed was 2.4 cm hr and 4.8 cm hr . Runoff at upstream with 29.3 mm hr rainfall in forest\ud-1 -1\udwas zero, in agroforestry was 0.026 mm hr and in rainfed was 0.071 mm hr . Runoff in agroforestry at the middle\udand downstream with 37.1 mm hr-1 and 23.8 mm hr-1 rainfall were 0.045 mm hr-1, and 0.026 mm hr-1. There was a half\udand one third of that in rainfed. Soil water content in successive order from high to low was in forest, agroforestry,\udand rainfed. So, capacity of agroforestry in sustaining the hydrology cycle was in between forests and rainfed\udagricultur

Changes in Hydrological Response of Forest Conversion to Agroforestry and Rainfed Agriculture in Renggung Watershed, Lombok, Eastern Indonesia