scholarly journals Environmental controls on growing-season sap flow density of Quercus serrata Thunb in a temperate deciduous forest of Korea

2012 ◽  
Vol 35 (3) ◽  
pp. 213-225 ◽  
Author(s):  
Nahida Laiju ◽  
Dennis Otieno ◽  
Eun-Young Jung ◽  
Bo-Ra Lee ◽  
John Tenhunen ◽  
...  
Keyword(s):  
Sap Flow ◽  
Deciduous Forest ◽  
Growing Season ◽  
Quercus Serrata ◽  
Flow Density ◽  
Temperate Deciduous Forest ◽  
Environmental Controls ◽  
Temperate Deciduous ◽  
Sap Flow Density

scholarly journals Can vegetation index track the interannual variation in gross primary production of temperate deciduous forests?

2021 ◽  
Vol 10 (1) ◽  
Author(s):  
Fan Liu ◽  
Chuankuan Wang ◽  
Xingchang Wang
Keyword(s):  
Primary Production ◽  
Vegetation Index ◽  
Near Infrared ◽  
Deciduous Forest ◽  
Gross Primary Production ◽  
Growing Season ◽  
Temperate Deciduous Forest ◽  
Near Infrared Reflectance ◽  
Modis Ndvi ◽  
Temperate Deciduous

Abstract Background Vegetation indices (VIs) by remote sensing are widely used as simple proxies of the gross primary production (GPP) of vegetation, but their performances in capturing the inter-annual variation (IAV) in GPP remain uncertain. Methods We evaluated the performances of various VIs in tracking the IAV in GPP estimated by eddy covariance in a temperate deciduous forest of Northeast China. The VIs assessed included the normalized difference vegetation index (NDVI), the enhanced vegetation index (EVI), and the near-infrared reflectance of vegetation (NIRv) obtained from tower-radiometers (broadband) and the Moderate Resolution Imaging Spectroradiometer (MODIS), respectively. Results We found that 25%–35% amplitude of the broadband EVI tracked the start of growing season derived by GPP (R2: 0.56–0.60, bias < 4 d), while 45% (or 50%) amplitudes of broadband (or MODIS) NDVI represented the end of growing season estimated by GPP (R2: 0.58–0.67, bias < 3 d). However, all the VIs failed to characterize the summer peaks of GPP. The growing-season integrals but not averaged values of the broadband NDVI, MODIS NIRv and EVI were robust surrogates of the IAV in GPP (R2: 0.40–0.67). Conclusion These findings illustrate that specific VIs are effective only to capture the GPP phenology but not the GPP peak, while the integral VIs have the potential to mirror the IAV in GPP.

scholarly journals Growing season moisture drives interannual variation in woody productivity of a temperate deciduous forest

2019 ◽  
Vol 223 (3) ◽  
pp. 1204-1216 ◽  
Author(s):  
Ryan Helcoski ◽  
Alan J. Tepley ◽  
Neil Pederson ◽  
Jennifer C. McGarvey ◽  
Victoria Meakem ◽  
...  
Keyword(s):  
Interannual Variation ◽  
Deciduous Forest ◽  
Growing Season ◽  
Temperate Deciduous Forest ◽  
Temperate Deciduous

scholarly journals Contrasting Rhizospheric and Heterotrophic Components of Soil Respiration during Growing and Non-Growing Seasons in a Temperate Deciduous Forest

Forests ◽  
2018 ◽  
Vol 10 (1) ◽  
pp. 8 ◽  
Author(s):  
Zhen Jiao ◽  
Xingchang Wang
Keyword(s):  
Soil Respiration ◽  
Deciduous Forest ◽  
Growing Season ◽  
Heterotrophic Respiration ◽  
Temperate Deciduous Forest ◽  
Northern Forest ◽  
Growing Seasons ◽  
Temperate Deciduous ◽  
Total Soil Respiration ◽  
Annual Period

The contributions of heterotrophic respiration (RH) to total soil respiration (RS) for the non-growing season, growing season, and annual period are 84.8%, 60.7%, and 63.3%, respectively.Few studies have partitioned RS into its rhizospheric (RR) and heterotrophic components throughout the year in northern forest ecosystems. Our objectives were to quantify the contributions of non-growing season and heterotrophic respiration. We conducted a trenching experiment to quantify RR and RH in a temperate deciduous forest in Northeast China over two years using chamber methods. Temperature sensitivities (Q10) for RS and for RH were both much higher in the non-growing season (November to April) than those in the growing season. The Q10 for RS was higher than Q10 for RH in both seasons, indicating a higher temperature sensitivity of roots versus microorganisms. Mean non-growing season RS, RH, and RR for the two years were 94, 79 and 14 g carbon (C) m−2, respectively, which contributed 10.8%, 14.5%, and 4.5% to the corresponding annual fluxes (869, 547 and 321 g C m−2 year−1, respectively). The contributions of RH to RS for the non-growing season, growing season, and annual period were 84.8%, 60.7%, and 63.3%, respectively. Using the same contribution of non-growing season RS to annual RS, to scale growing season measurements, to the annual scale would introduce significant biases on annual RH (−34 g C m−2 yr−1 or −6%) and RR (16 g C m−2 yr−1 or 5%).We concluded that it was important to take non-growing season measurements in terms of accurately partitioning RS components in northern forests.

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