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Closing the carbon budget of estuarine wetlands with tower-based measurements and MODIS time series

机译:使用基于塔的测量值和MODIS时间序列来结束河口湿地的碳收支

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摘要

Compared to other ecosystems, estuarine ecosystems have distinct carbon flux dynamics – the lateral carbon flux incurred by tidal activities, and methane generation under the anaerobic conditions of wetland soils. The conventional estimation of gross primary production (GPP) based on the light use efficiency (LUE) model used for non-wetland terrestrial ecosystems, therefore, cannot be applied directly to estuarine wetland ecosystems. In this paper, we estimated the 2005's annual carbon budget of an estuarine wetland on Chongming Island, Shanghai, and partitioned the losses of carbon due to lateral tidal dynamics and anaerobic methane production using an innovative technique. The average GPP calculated from eddy covariance between March and November was 261.79 μmol m?2 day?1, whereas that from the LUE model was 58.84 μmol m?2 day?1. The correlation coefficient between GPP simulated from the LUE model and that calculated from flux tower data was low in the growing season (R2=0.55). We hypothesized that tidal activities and uncounted methane release were responsible for the difference, which can be predicted from measurements of remote sensing products such as land surface water index (LSWI), evapotranspiration (ET), and tide height (TH). We developed an integrated GPP model by combining the LUE model and an autoregression model to estimate carbon budget. The average GPP from the modified model increased to 263.38 μmol m?2 day?1, and R2 for the correlation between the simulated and calculated data increased to 0.88, demonstrating the potential of our technique for GPP estimation and quantification of seasonal variation in estuarine ecosystems. The approach developed in this study has great potential for correcting unavoidable errors when estimating carbon budget of coastal wetlands. Furthermore, global warming is expected to accelerate sea level rise, which may enhance the effect of tidal activities and increase the difficulty in estimating coastal carbon budgets using conventional methods.
机译:与其他生态系统相比,河口生态系统具有独特的碳通量动态-潮汐活动引起的横向碳通量,以及在湿地土壤厌氧条件下产生的甲烷。因此,基于用于非湿地陆地生态系统的光利用效率(LUE)模型的传统的初级生产总值(GPP)估算无法直接应用于河口湿地生态系统。在本文中,我们估算了上海崇明岛河口湿地2005年的年度碳预算,并使用一种创新技术对由于横向潮汐动力学和厌氧甲烷生产而造成的碳损失进行了划分。根据三月和十一月之间的涡度协方差计算的平均GPP为261.79μmolm?2 day?1,而根据LUE模型得出的平均GPP为58.84μmolm?2 day?1。 LUE模型模拟的GPP与通量塔数据计算的GPP之间的相关系数在生长期较低(R2 = 0.55)。我们假设潮汐活动和未计数的甲烷释放是造成差异的原因,这可以通过遥感产品的测量来预测,例如陆地表面水指数(LSWI),蒸散量(ET)和潮汐高度(TH)。我们通过组合LUE模型和自回归模型来估算碳预算,从而开发了集成的GPP模型。改进模型的平均GPP增加到263.38μmolm?2·day?1,模拟和计算数据之间的相关性的R2增加到0.88,证明了我们的技术对GPP估计和定量化河口生态系统季节性变化的潜力。本研究中开发的方法在估计沿海湿地的碳收支时具有纠正不可避免的错误的巨大潜力。此外,预计全球变暖将加速海平面上升,这可能会增强潮汐活动的影响,并增加使用传统方法估算沿海碳预算的难度。

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