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hydrology in degraded tropical peatlands in the former Mega Rice Project in Central Kalimantan, Indonesia. In: Abang F, Jusoh I, Ui Hang ED, Han Hoy AW, Roslan HA (Eds.) Conference:
International Symposium and Workshop on Tropical Peatlands ‘Peatland development: wise
use and impact management’At: Kuching, Sarawak Volume, Proceedings, pp. 260–269
Swails E, Jaye D, Verchot L, Hergoualc’h K, Schirrmann M, Borchard N, Wahyuni N, Lawrence D
(2017) Will CO 2 emissions from drained tropical peatlands decline over time? Links between
soil organic matter quality, nutrients, and C mineralization rates. Ecosystems 21:868–885
van Bellen S, Larivière S (2020) The ecosystem of peatland research: a bibliometric analysis. Mires
Peat 26(15):30
van der Ent RJ, Savenije HHG, Schaefli B (2010) Origin and fate of atmospheric moisture over
continents. Water Resour Res 46:W09525
Wang-Erlandsson L, van der Ent RJ, Gordon LJ, Savenije HHG (2014) Contrasting roles of
interception and transpiration in the hydrological cycle – part 1: temporal characteristics over
land. Earth Syst Dynam 5:441–469
Worden J, Noone D, Bowman K (2007) Importance of rain evaporation and continental convection
in the tropical water cycle. Nature 445:528–532
Wösten H, Ritzema H (2001) Land and water management options for peatland development in
Sarawak, Malaysia. Int Peat J 11:59–66
Yamanaka MD (2016) Physical climatology of Indonesian maritime continent: an outline to
comprehend observational studies. Atmos Res 178–179:231–259
86
T. Kato et al.