HR: 0800h
AN: B51C-0209 [Abstracts]
TI: Estimating NEP by micrometeorological and biometric methods in a larch forest in Hokkaido,
Japan
AU: * Hirata, R
EM: hirata.ryuichi@nies.go.jp
AF: National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki, 305-8506
Japan
AU: Hirano, T
EM: hirano@env.agr.hokudai.ac.jp
AF: Graduate School of Agriculture, Hokkaido University, Kita 9, Nishi 9, Kita-ku, Sapporo, Hokkaido,
060-8589
Japan
AU: Saigusa, N
EM: n.saigusa@aist.go.jp
AF: National Institute of Advanced Industrial Science and Technology, 16-1 Onogawa, Tsukuba, Ibaraki,
305-8569
Japan
AU: Takagi, K
EM: kentt@exfor.agr.hokudai.ac.jp
AF: Field Science Center for Northern Biosphere, Hokkaido University, Toikanbetsu, Horonobe, Hokkaido,
098-2943
Japan
AU: Yone, Y
EM: yone.yasumichi@nies.go.jp
AF: PASCO Corporation, 1-2, Higashiyama 1-chome, Meguro-ku, Tokyo, 153-0043
Japan
AU: Liang, N
EM: liang@nies.go.jp
AF: National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki, 305-8506
Japan
AU: Inukai, K
EM: inukai.ko@nies.go.jp
AF: National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki, 305-8506
Japan
AU: Fujinuma, Y
EM: fujinuma@nies.go.jp
AF: National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki, 305-8506
Japan
AB:
We report comparison of NEP of a temperate larch forest between micrometeorological and biometric methods. The study site is
a Japanese larch plantation in Hokkaido, Japan (42°44'N, 141°31'E). The canopy height was approximately
15 m and tree age was about 45 years old. Canopy LAI reached the maximum at 5.5m2 m-2 in July. We measured NEE
(-NEP) using eddy covariance method with open- and closed-path systems. We estimated biometric NEP from biomass increment,
litter fall of overstory and understory, and heterotrophic respiration measured by chamber method. However, Biometric NEP
should have a large uncertainty, because we neglect a fine root production. Daytime NEE tended to be slightly negative for
open-path than for closed-path. In contrast, nighttime NEE tended to be slightly less positive for open-path than for
closed-path. Consequently, the small difference of half-hourly NEE between from open- and closed-pass provided the large
annual bias. High frequency loss corrections using Bandpass covariance method or experimental transfer function improved the
daytime bias. However, they made the nighttime bias large. The annual NEPs obtained from open- and closed-path systems were
compared with that estimated by the biometric method. NEP estimated by biometric method was close to that estimated by
closed-path system.
DE: 0400 BIOGEOSCIENCES
DE: 0426 Biosphere/atmosphere interactions (0315)
DE: 0428 Carbon cycling (4806)
DE: 0459 Macro- and micropaleontology (3030, 4944)
SC: Biogeosciences [B]
MN: Fall Meeting 2005