日本地球惑星科学連合2018年大会

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[JJ] 口頭発表

セッション記号 A (大気水圏科学) » A-CG 大気水圏科学複合領域・一般

[A-CG40] 陸域生態系の物質循環

2018年5月24日(木) 10:45 〜 12:15 106 (幕張メッセ国際会議場 1F)

コンビーナ:加藤 知道(北海道大学農学研究院)、平野 高司(北海道大学大学院農学研究院)、佐藤 永(海洋研究開発機構 地球表層物質循環研究分野、共同)、平田 竜一(国立環境研究所)、座長:佐藤 永(海洋研究開発機構)

11:15 〜 11:30

[ACG40-03] 飛騨高山冷温帯落葉広葉樹森林観測サイトにおける炭素収支及び大気中CO2濃度の年々変動及び長期トレンド

*村山 昌平1石戸谷 重之1前田 高尚1近藤 裕昭1山本 晋1三枝 信子2村岡 裕由3 (1.国立研究開発法人産業技術総合研究所、2.国立研究開発法人国立環境研究所、3.岐阜大学)

キーワード:森林生態系、年々変動、長期トレンド、炭素収支、大気中二酸化炭素濃度

Impacts of climate change on terrestrial biospheric activities have been predicted in recent studies. In East Asia strongly influenced by Asian Monsoon, changes not only in temperature but also in amounts of precipitation and length of the rainy season associated with the climate change could have much influence on the carbon budget in the terrestrial biosphere. However, responses of the terrestrial biosphere to climate change are not yet fully understood. For the better understanding of the responses, further analyses using long-term measurement data related to the carbon budget in terrestrial ecosystem are necessary.

We have made long-term systematic measurements of the CO2 flux between the atmosphere and forest ecosystem, the atmospheric CO2 concentration, and meteorological parameters in a 60-year-old cool-temperate deciduous forest at Takayama (TKY; 36o08’N, 137o25’E, 1420 m a.s.l.), Japan since 1993. Using these data, we have examined their inter-annual variations, long-term trends and environmental factors governing these variations. The results obtained from the analyses are as follows:

(1) Annual net ecosystem production (NEP) and the gross primary production (GPP) vary significantly from year by year, while inter-annual variation in the annual ecosystem respiration (ER) is relatively small. The inter-annual variation in the annual NEP depends strongly on the annual GPP.

(2) Annual NEP shows a statistically significant positive correlation with the monthly NEP in June and July. Higher insolation during the summertime tends to produce higher amount of the annual NEP.

(3) In the warm-spring years, budding, beginning of the daily positive NEP and the spring downward zero crossing of atmospheric CO2 concentration tend to occur early.

(4) These inter-annual variations may be influenced by those of meteorological conditions associated with the ENSO event.

(5) Significant long-term trends in the increased annual NEP, GPP and ER, the enhanced seasonal amplitude of atmospheric CO2 above the canopy during the daytime and the delayed occurrences in the leaf-fall are found.