Evapotranspiration of tropical peat swamp forests

© 2014 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 21(2015), 5 vom: 15. Mai, Seite 1914-27
1. Verfasser: Hirano, Takashi (VerfasserIn)
Weitere Verfasser: Kusin, Kitso, Limin, Suwido, Osaki, Mitsuru
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2015
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Research Support, Non-U.S. Gov't ENSO Southeast Asia disturbances drainage eddy covariance energy balance fire groundwater level smoke
LEADER 01000naa a22002652 4500
001 NLM239019156
003 DE-627
005 20231224115033.0
007 cr uuu---uuuuu
008 231224s2015 xx |||||o 00| ||eng c
024 7 |a 10.1111/gcb.12653  |2 doi 
028 5 2 |a pubmed24n0796.xml 
035 |a (DE-627)NLM239019156 
035 |a (NLM)24912043 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Hirano, Takashi  |e verfasserin  |4 aut 
245 1 0 |a Evapotranspiration of tropical peat swamp forests 
264 1 |c 2015 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Completed 14.01.2016 
500 |a Date Revised 20.04.2015 
500 |a published: Print-Electronic 
500 |a Citation Status MEDLINE 
520 |a © 2014 John Wiley & Sons Ltd. 
520 |a In Southeast Asia, peatland is widely distributed and has accumulated a massive amount of soil carbon, coexisting with peat swamp forest (PSF). The peatland, however, has been rapidly degraded by deforestation, fires, and drainage for the last two decades. Such disturbances change hydrological conditions, typically groundwater level (GWL), and accelerate oxidative peat decomposition. Evapotranspiration (ET) is a major determinant of GWL, whereas information on the ET of PSF is limited. Therefore, we measured ET using the eddy covariance technique for 4-6 years between 2002 and 2009, including El Niño and La Niña events, at three sites in Central Kalimantan, Indonesia. The sites were different in disturbance degree: a PSF with little drainage (UF), a heavily drained PSF (DF), and a drained burnt ex-PSF (DB); GWL was significantly lowered at DF, especially in the dry season. The ET showed a clear seasonal variation with a peak in the mid-dry season and a large decrease in the late dry season, mainly following seasonal variation in net radiation (Rn ). The Rn drastically decreased with dense smoke from peat fires in the late dry season. Annual ET forced to close energy balance for 4 years was 1636 ± 53, 1553 ± 117, and 1374 ± 75 mm yr(-1) (mean ± 1 standard deviation), respectively, at UF, DF, and DB. The undrained PSF (UF) had high and rather stable annual ET, independently of El Niño and La Niña events, in comparison with other tropical rainforests. The minimum monthly-mean GWL explained 80% of interannual variation in ET for the forest sites (UF and DF); the positive relationship between ET and GWL indicates that drainage by a canal decreased ET at DF through lowering GWL. In addition, ET was decreased by 16% at DB in comparison with UF chiefly because of vegetation loss through fires 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a ENSO 
650 4 |a Southeast Asia 
650 4 |a disturbances 
650 4 |a drainage 
650 4 |a eddy covariance 
650 4 |a energy balance 
650 4 |a fire 
650 4 |a groundwater level 
650 4 |a smoke 
700 1 |a Kusin, Kitso  |e verfasserin  |4 aut 
700 1 |a Limin, Suwido  |e verfasserin  |4 aut 
700 1 |a Osaki, Mitsuru  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Global change biology  |d 1999  |g 21(2015), 5 vom: 15. Mai, Seite 1914-27  |w (DE-627)NLM098239996  |x 1365-2486  |7 nnns 
773 1 8 |g volume:21  |g year:2015  |g number:5  |g day:15  |g month:05  |g pages:1914-27 
856 4 0 |u http://dx.doi.org/10.1111/gcb.12653  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_350 
951 |a AR 
952 |d 21  |j 2015  |e 5  |b 15  |c 05  |h 1914-27