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Measurements of an anomalous global methane increase during 1998

机译:1998年全球甲烷异常增加的测量

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Measurements of atmospheric methane from a globally distributed network of air sampling sites indicate that the globally averaged CH4 growth rate increased from an average of 3.9 ppb yr(-1) during 1995-1997 to 12.7 +/- 0.6 ppb in 1998. The global growth rate then decreased to 2.6 +/- 0.6 ppb during 1999, indicating that the large increase in 1998 was not a return to the larger growth rates observed during the late-1970s and early-1980s. The increased growth rate during 1998 corresponds to an increase in the imbalance between CH4 sources and sinks equal to similar to 24 Tg CH4, the largest perturbation observed in 16 years of measurements. We suggest that wetland and boreal biomass burning sources may have contributed to the anomaly. An adaptation of a global process-based model, which included soil-temperature and precipitation anomalies, was used to calculate emission anomalies of 11.6 Tg CH4 from wetlands north of 30 degreesN and 13 Tg CH4 for tropical wetlands during 1998 compared to average emissions calculated for 1982-1993. For 1999, calculated wetland emission anomalies were negative for high northern latitudes and the tropics, contributing to the low growth rate observed in 1999. Also 1998 was a severe fire year in boreal regions where similar to1.3 x 10(5) km(2) of forest and peat land burned releasing an estimated 5.7 Tg CH4. [References: 24]
机译:对全球分布的空气采样点网络中的大气甲烷进行的测量表明,全球平均CH4增长率从1995-1997年的平均3.9 ppb yr(-1)增加到1998年的12.7 +/- 0.6 ppb。 1999年,该速率下降到2.6 +/- 0.6 ppb,这表明1998年的大幅增长并没有恢复到1970年代末和1980年代初的较大增长率。 1998年增长率的增加对应于CH4源和汇之间的不平衡增加,相当于增加了24 Tg CH4,这是16年测量中观察到的最大扰动。我们建议湿地和北方生物质燃烧源可能是造成异常的原因。根据全球基于过程的模型(包括土壤温度和降水异常)进行了改编,用于计算1998年北纬30度以北湿地的CH1甲烷CH4排放异常和热带湿地13°Tg CH4的排放异常,而计算得出的平均值为1982年至1993年。对于1999年,计算得出的湿地排放异常对于北部高纬度地区和热带地区为负,导致1999年观测到的低增长率。另外,1998年是北方地区的严重火灾年份,其类似于1.3 x 10(5)km(2) )被烧毁的森林和泥炭地释放出约5.7 Tg CH4。 [参考:24]

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