首页> 外文期刊>Global Biogeochemical Cycles >Estimating wetland methane emissions from the northern high latitudes from 1990 to 2009 using artificial neural networks
【24h】

Estimating wetland methane emissions from the northern high latitudes from 1990 to 2009 using artificial neural networks

机译:使用人工神经网络估算1990年至2009年北部高纬度地区的湿地甲烷排放量

获取原文
获取原文并翻译 | 示例
           

摘要

Methane (CH_4) emissions from wetland ecosystems in nothern high latitudes provide a potentially positive feedback to global climate warming. Large uncertainties still remain in estimating wetland CH_4 emisions at regional scales. Here we develop a statistical model of CH_4 emissions using an artificial neural network (ANN) approach and field observations of CH_4 fluxes. Six explanatory variables (air temperature, precipitation, water table depth, soil organic carbon, soil total porosity, and soil pH) are included in the development of ANN models, which are then extrapolated to the northern high latitudes to estimate monthly CH 4 emissions from 1990 to 2009. We estimate that the annual wetland CH_4 source from the northern high latitudes (north of 45°N) is 48.7 Tg CH_4 yr~(-1) (1 Tg = 10~(12) g) with an uncertainty range of 44.0~53.7 Tg CH_4 yr~(-1). The estimated wetland CH_4 emissions show a large spatial variability over the northern high latitudes, due to variations in hydrology, climate, and soil conditions. Significant interannual and seasonal variations of wetland CH 4 emissions exist in the past 2 decades, and the emissions in this period are most sensitive to variations in water table position. To improve future assessment of wetland CH_4 dynamics in this region, research priorities should be directed to better characterizing hydrological processes of wetlands, including temporal dynamics of water table position and spatial dynamics of wetland areas. Key Points Develop wetland CH_4 emissions model using artificial neural networks Estimate wetland CH_4 emissions from the northern high latitudes The wetland CH_4 emissions are most sensitive to variations in water table depth
机译:来自北部高纬度地区湿地生态系统的甲烷(CH_4)排放量为全球气候变暖提供了潜在的积极反馈。在区域范围内估算湿地CH_4排放量仍存在很大的不确定性。在这里,我们使用人工神经网络(ANN)方法和CH_4通量的现场观测值,开发了CH_4排放的统计模型。 ANN模型的开发包括六个解释变量(气温,降水,地下水位深度,土壤有机碳,土壤总孔隙度和土壤pH),然后将其外推至北部高纬度,以估算来自该地区的每月CH 4排放量。 1990年至2009年。我们估计北部高纬度(北纬45°N)的年度湿地CH_4源为48.7 Tg CH_4 yr〜(-1)(1 Tg = 10〜(12)g),不确定范围为44.0〜53.7 Tg CH_4 yr〜(-1)。由于水文,气候和土壤条件的变化,估计的湿地CH_4排放在北部高纬度地区显示出很大的空间变异性。在过去的20年中,湿地CH 4的排放存在明显的年际和季节变化,这一时期的排放对地下水位的变化最为敏感。为了改善对该地区湿地CH_4动态的未来评估,应将研究重点放在更好地表征湿地的水文过程,包括地下水位的时间动态和湿地区域的空间动态。要点使用人工神经网络建立湿地CH_4排放模型估算北部高纬度地区的湿地CH_4排放湿地CH_4排放对地下水位变化最敏感

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号