日本地球惑星科学連合2021年大会

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

[A-CG37] 陸域生態系の物質循環

2021年6月5日(土) 15:30 〜 17:00 Ch.08 (Zoom会場08)

コンビーナ:加藤 知道(北海道大学農学研究院)、市井 和仁(千葉大学)、伊勢 武史(京都大学フィールド科学教育研究センター)、寺本 宗正(鳥取大学乾燥地研究センター)

15:45 〜 16:00

[ACG37-08] Ground-Based Measurement of Solar-Induced Chlorophyll Fluorescence in Wetland by High-Spectral Resolution

*Kitpanuwat TANATARAKEREE1、Tomomichi Kato2,3、Tomoki Morozumi3、KANOKRAT BUAREAL2、Masahito Ueyama4、Naohisa Nakashima3、Hideki Ninomiya2、Lan Wu5 (1.Graduate School of Agriculture, Hokkaido University、2.Graduate School of Global Food Resources, Hokkaido University、3.Research Faculty of Agriculture, Hokkaido University 、4.Graduate School of Life and Environmental Science, Osaka Prefecture University、5.Hainan University)

キーワード:Solar-Induced Chlorophyll Fluorescence , Gross Primary Production, Ground-Based Measurement, Wetland, High-Spectral Resolution

Solar-induced chlorophyll fluorescence (SIF) has been observed and discovered to relate linearly to gross primary production (GPP) in terrestrial ecosystem [Krause and Weis, 1991; Meroni et al., 2009; Frankenberg et al., 2011; Paul-Limoges et al., 2018]. However, SIF variations under different plant growth stages and sky conditions, and water table depth effects appear to limit the understandings about SIF-GPP relationship at the field-based measurement. It remains ambiguous linked to how this relationship is affected by varying changes of palnt growth stage, sky, and water table, especially for wetland where is a critical part of carbon sinks. We conducted the ground-base measurement of canopy-top SIF in wetland, Bibai Mire, northern Japan, Hokkaido (43º19'N, 141º48'E, 16 m above sea level) during the growing season (from March to November) in 2020, and examined its relationship to the eddy-covariance GPP [Ueyama et al., 2020]. QEPro spectroradiometer (range of wavelength 648-808 nm, the full width half maximum (FWHM) of 0.31 nm, Ocean Optics, Dunedin, FL, USA) and the spectral fitting method (SFM; Meroni and Colombo., 2006; Meroni et al., 2010; Mazzoni et al., 2012) were used for SIF retrievals at the oxygen absorption band (O2-A, centered around 760 nm). SIF was captured by the spectra of downwelling and upwelling at the height of 2 meters above the ground by hemisphere spectroradiometer. The downward solar irradiance was estimated from cosine corrector fiber (CC fiber) from field of view (FOV) at 180º and the upward canopy-reflected radiance was received by bare fiber FOV 25º and CC fiber FOV 180º. The slope and correlation in positive linear regression between SIF and GPP were found to vary among the growth stages (slope = -2.99, 107.60, 62.57 and 47.97 (µmolmW-1s-1nm) and r2 = 0.01, 0.41, 0.73 and 0.65 in Pre-Growing (DOY74-135), Growing (DOY144-179), Mature (DOY180-256) and Senescence (DOY260-295), respectively), suggesting that vegetation growth has a strong impact on the seasonal variations of canopy SIF and its realtion to GPP. In contrast, we found that sky conditions such as sunny (clearness index > 0.5) and cloudy (clearness index ≦ 0.5) have no clear influence on relationship of SIF and GPP (slope = 59.59 and 91.06 (µmolmW-1s-1nm) and r2 =) and r2 = 0.68 and 0.75 in sunny day and cloudy day, respectively).