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EMISI METAN DARI LAHAN GAMBUT SEJUTA HEKTAR KALIMANTAN TENGAH
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PENGURANGAN EMISI GAS RUMAH KACA SEKTOR ENERGI DI INDONESIA:ULASAN HASIL-HASIL STUDI ASEAN LEAST-COST GREENHOUSE GAS ABATEMENT STRATEG PROJECT
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PENGARUH PENYIMPANAN TERHADAP KECEPATAN RESPIRASI, KEBOCORAN DAN DAYA PERKECAMBAHAN BENIH KUBIS
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KOEFISIEN PEMADAMAN TANAMAN KEDELE PADA BEBERAPA TINGKAT RADIASI
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SELEKSI FAKTOR-FAKTOR YANG MEMPENGARUHI DEBIT AIR PADA BEBERAPA DAS DI JAWA BARAT DENGAN MENGGUNAKAN ANALISIS REGRESI LINIER BERGANDA
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THE EFFECT OF LATITUDE, SEASON, TIME OF DAY AND ASPECT ON DIRECT SOLAR RADIATION
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KETERPADUAN ANTARA UNSUR ILKLIM DAN SIFAT TANAH UNTUK MENILAI KESESUAIAN LAHAN BAGI TANAMAN KAPAS DI DAERAH GONDANG-SELENGEN, LOMBOK BARAT, NTB
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ANALISIS PERUBAHAN IKLIM LOKAL DAN DEBIT SUNGAI DI DAS CIDANAUANALYSIS OF LOCAL CLIMATE CHANGE AND DISCHARGE IN CIDANAU WATERSHED
Climate change causes uncertainty in water availability. The change may include annual rainfall, evapotranspiration and the shift of rainy and dry seasons, thus, it affects hydrological response in the region. Water demand will increase over time with population, industrial and business growth but the water availability has not been ascertained to sustainably satisfy those needs.ย Cidanau Watershed has wetland ecosystem so-called the Rawa Danau (Caldera), with an area of around 2,500 ha. This watershed receives average annual rainfall around 2,500 mm. Climate change especially the local climate in the region of Cidanau was analyzed to illustrate how the relationship with Cidanau river discharge. It is expected that climate change does not affect the water availability in the watershed. In this study, the analysis of local climate change and its impact on the availability of water resources on Cidanau Watershed was based on climate trends, water balance analysis, and estimation ofย discharge of Cidanau Watershed. This research was carried out using climate data and discharge from 1996 until 2010. The results showed that climate variables have changed from 1996 to 2010. This change mainly occurred in temperature, annual rainfall, and evapotranspiration. Based on the analysis, the discharge of Cidanau Watershed will decrease due to changes in rainfall and evapotranspiration. The estimated minimum river discharge of Cidanau Watershed ranges from 0.5 to 1 m3/s until 2050
PENGARUH SUHU DAN LAMA PEMYIMPANAN TERHADAP VIABILITAS BIJI PINANG JAWA (Pinanga javana BL.)EFFECT OF TEMPERATURE AND STORAGE DURATION ON SEED VIABILITY ON PINANG JAWA (Pinanga javana BL.)
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PENGARUH PENGAIRAN DAN WAKTU TANAM TERHADAP PRODUKSI DAN MUTU MINYAK MENTA (Mentha arvensis)THE EFFECTS OF WATERING AND PLATING TIME ON YIELD AND QULITY OF MINT OIL (Mentha arvensis)
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