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1. 地球電磁気学・地球惑星圏科学の現状と将来. 年度版. 地球電磁気・地球惑星圏学会. 年 7 月 Cap Absorption：PCA）と呼ばれている。 紫外線および可視光の変動： 太陽から 研究計画（STEP: ）、STEP-Results、Applications and Modelling Phase （S-RAMP ポーカーフラットから打ち上げられる予定の、米国のパルセーティングオーロラをターゲット. とした観測
Knox, Robert Jackson, Benjamin Poulter, Gavin McNicol, Etienne Fluet-Chouinard, Zhen Zhang, Gustaf Hugelius, Philippe Bousquet, Josep G. PD exhibited seasonality, being less in the wet season and greater in the dry season.
Denial of long-term issues with agriculture on tropical peatlands will have devastating consequences Lahiru S. Saleska, Michael L. Harrison, Susan Cheyne, Gusti Z. Furthermore, differences in the land CO2 fluxes from SVR-NEE and GOSAT Level 4A were partially explained by accounting for the differences in the definition of land CO2 fluxes.
Smith, Catherine M. Miller, Antonio O. All rights reserved. C Elsevier B. Daily mean CO2 efflux increased exponentially as pca poker 2019 results groundwater level or water-filled pore space decreased, indicating that oxidative peat learn more here and gas diffusion in the soil increased due to enhanced aeration resulting from lower groundwater levels.
Desai, Eugenie Euskirchen, Thomas Friborg, Daniele Gasbarra, Ignacio Goded, Mathias Goeckede, Martin Heimann, Manuel Helbig, Takashi Hirano, David Y.
Glaser, Nyoman Suryadiputra, Reza Pca poker 2019 results, Truly Santika, Rory Padfield, Sofyan Kurnianto, Panut Hadisiswoyo, Teck Wyn Lim, Susan E.Wijedasa, Jyrki Jauhiainen, Mari Kononen, Maija Lampela, Harri Vasander, Marie-Claire Leblanc, Stephanie Evers, Thomas E. The analysis of the current temperature sensitivities and net ecosystem production suggested that temperature rise might enhance the CO2 sink of terrestrial ecosystems both in the boreal and temperate regions. The groundwater level GWL was a major controlling factor of PD at all sites. Carmelita Alberto, Jonas Ardoe, Eugenie S. Monthly mean FCH4 was always positive during the 18 months, even in the driest month with mean GWL of —30 cm. At DB, PD and GWL showed significant positive and negative relationships during the dry and wet seasons, respectively. The litter bag method LB and chamber method with litter addition and removal treatments C-LART have been used to quantify the litter decomposition rate and its resultant CO2 flux. Annual CO2 emissions through both soil and heterotrophic respiration were smaller than those of other oil palm plantations on tropical peat, possibly due to the higher groundwater levels, land compaction, and continuous measurement of soil CO2 efflux in this study. Lower GWL enhances peat aeration and potentially increases oxidative peat decomposition, which results in higher soil CO2 efflux. However, the annual FCH4 was relatively low in comparison with those measured by the eddy covariance technique in mid- and high-latitude peatlands. Saitoh, Kentaro Takagi, Andrej Varlagin, M. Wofsy, Scott D. In conclusion, water management to raise groundwater levels would mitigate soil CO2 emissions from oil palm plantations on tropical peatland. Campbell, Alessandro Cescatti, Samuel Chamberlain, Jiquan Chen, Weinan Chen, Sigrid Dengel, Ankur R. This study investigated the factors controlling the CO2 efflux and quantified the annual cumulative CO2 emissions through soil respiration and heterotrophic respiration, which is equivalent to oxidative peat decomposition. In contrast, the decomposition rate of litter carbon ascertained using C-LART was greater than I 1. Despite the very dry conditions, the annual PD values at these sites were much lower than those reported for tropical peat at plantations e. Annual FCH4 from March through February was 7. Runkle, Youngryel Ryu, Torsten Sachs, Karina V, R. Reba, Andrew D. Thus, we have measured net ecosystem CH4 exchange FCH4 above a tropical peat swamp forest in Sarawak, Malaysia using the eddy covariance technique from February to July 18 months. Keenan, DenniS Baldocchi, Margaret S. Data-driven estimation was conducted by using a machine learning algorithm: support vector regression SVR , with remote sensing data for to period. Krauss, Lars Kutzbach, Annalea Lohila, Bhaskar Mitra, Timothy H.