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"ABSTRAKPeat forest are unique and sensitive ecosystems, have complex hydrological systems and bear important economic service function. In Southeast Asian countries, peatland degradation has been increasingly severe in the last decade due to the exploitation of natural resources, which concerns the structure and function of the system. Ecological rehabilitation, includign hydrological restoration, is believed to be useful for restoring the function of forest/peat swamp systems. Protection of critical areas in the form of National Park is also applied to reduce disturbance and further degradation of the area. A literature review is conducted to analyze the extent to which ecological restoration can achieve system resilience, especially socio-ecological resilience as a 'complex-adaptive system' using resilience concepts. The linkage between the ecological function of peat forest restoration by restoring hydrological systems, the diversity of flora and fauna, and enhancing social resilience with social networking and community livelihood is and important key in achieving resilience. Area Protection (in the form of National Park) needs to pay attention to interconnection systems in the "panarchy" model, not for system isolation, but directed to strengthening effective adaptation governance. The study of the selected Sebangau peatland forest in Central Kalimantan, which implemented hydrological restoration and post-Mega Rice Project (MRP) National Park to restore 85% of the damaged land. Sebangau peatland ' socio-ecological resilience' is assessed to increase after the restoration and determination of the national park, although peatland clearance still continues. Strengthening governance of national park and controlling on the main variables on the main variables of peat and 'sustainable livelihood' is essential to improve resilience."

"Hidrologi hutan rawa gambut merupakan faktor penting yang menjadi kunci keberadaan dan kelestarian gambut itu sendiri. Perubahan hidrologi pada gambut terutama yang diakibatkan oleh kanalisasi mengakibatkan adanya fluktuasi tinggi muka air tanah yang dapat berdampak pada peningkatan pelepasan CO2, kekeringan yang berakibat kebakaran dan banjir yang lebih cepat terjadi sehingga perlu adanya upaya mitigasi untuk mengurangi risiko tersebut. Pengolahan citra Landsat TM dan ETM serta SPOT 4 menggunakan teknik klasifikasi segmentasi berbasis objek yang dipadukan dengan hasil pengukuran tinggi muka air dan elevasi permukaan tanah dilakukan untuk menghasilkan pola perubahan genangan air hutan rawa gambut di SubDAS Bakung, Kalimantan Tengah. Berdasarkan hasil analisis, pola perubahan genangan air sebagian besar terjadi di bagian hilir subDAS dengan faktor pengontrol berupa ketinggian dan lereng. Analisis multitemporal dari tahun 1998 – 2012 menjelaskan bahwa parameter curah hujan yang paling tinggi pengaruhnya terhadap perubahan genangan air adalah curah hujan dua bulanan sebelumnya dengan R sebesar 0,669. Adapun kerapatan aliran lebih berpengaruh terhadap genangan air di bagian hulu SubDAS Bakung.

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Hydrology of peat swamp forest is an important factor that is a key to the existence and preservation of the peat. Therefore, with the change in the hydrology of peat mainly caused by canalization it may result in fluctuations in ground water level that can impact on increasing the release of CO2, resulting in drought and peat fires, and early flood so it is need mitigation effort to reduce the risk. Processing of Landsat TM and ETM and SPOT 4 imagery using object-based classification technique are performed to produce pattern of water body change of peat swamp forest in Bakung Sub-watershed, Central Kalimantan. According to analysis, water body change pattern mostly occur in downstream area with controlled factor is topography. analysis conducted by multi-temporal in 1998 - 2012 found that rainfall parameters that influence the changes in water body is 2-monthly rainfall before observation time with R of 0.669. In addition, drainage density is more influence for occurring water body changes in the upstream area of Bakung Sub-watershed."